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#202 From: "cogombra" <cogombra@...>
Date: Fri Nov 10, 2006 11:12 am
Subject: Book List on Paleontology from China
cogombra
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From: <lcx@...>
To: <cogombra@...>
Subject: Book List on Paleontology from China
Date: Fri, 10 Nov 2006 15:57:57 +0800

Dear Sir/Madam:

Following please find publications list on Paleontology from China.
May
be
these books are useful to your library collection and your research
work.
More books and details please visit:  http://www.hceis.com

1. New!
*********************************************************************
********************
The Fossil Selection of Extinct Organism of Guizhou
http://www.hceis.com/book.asp?id=4707
¹óÖݹÅÉúÎﻯʯ¾«Ñ¡ In Chinese with English summary,Latin names
*********************************************************************
********************
2006/240x305mm/179 pages/Special/$128

Guizhou, called the Kingdom of the Paleobiologic Fissils, is rich in
paleobiologic fossils of which there is an evidence of theexistence
of
the
early life 600, 000, 000 years ago before the wide spreading of the
early
animals, especially the Keichousaurus and the Metacrinus.
This album of the sorted specimens of the paleobioligic fossils is
enjoyable
from a popular scientist¡¯s standpoint.
Guizhou, called the Kingdom of the Paleobiologic Fissils, is rich in
paleobiologic fossils of which there is an evidence of theexistence
of
the
early life 600, 000, 000 years ago before the wide spreading of the
early
animals, especially the Keichousaurus and the Metacrinus.
This album of the sorted specimens of the paleobioligic fossils is
enjoyable
from a popular scientist¡¯s standpoint.Guizhou Plateau is a land of
miracles. Possesing abundant, diverse, ancient organisms fossil of
both
scientific value and ornamental value, Guizhou is known as a kingdom
of
ancient organism. In the past 20 years, geologists and
palaeontologist
found
large quantities of rare fossils formed and preserved in the
distinctive
circumstances in their exploration on Weng¡¯an Biota, Kaili Biota,
and
Guanling Biota. This new discovery has not only enlarged the fossil
family
of this land, but also attracted attention of the counterparts home
and
abroad due to its uniques. Many of them come to Guizhou for
investigation.
By providing rich pictures and captions, from a unique visual angle,
The
Selection of Fossils of Guizhou-the of Ancient Organisms presents to
you
some snapshouts of the evolution process of the lives on this planet
in
the
past several hundred million years.


Contents
1.Weng¡¯an Biota
Weng¡¯an Biota was named by Yuan Shunlai in 1993. it came into being
in
the
phosphorites of Early Sinian Doushantuo Formation. The fossils were
phosphatized and preserved in solid forms. Containing filamentous
and
globular cyanophyte and metazoan embryo fossils, it was a multi-
phyla
fossil
biota dominated by bottom dwelling multicellular algae and large
size
spiniferous acritarch.
2.Miaohe Biota
Miaohe Biota was first discovered by Zhu Gougan and Chen Meng in the
blackly
carbonaceous shale at the top of the Doushantou Formation of
Neoproterozic
in Miaohe, Zigui, Hubei in 1978. it is mainly composed of benthonic
megascopic algae, including a few putative metazoans. They were
persevered
by arbonaceous compressions on surfaces of the black shale at upper
of
Doushantou Formation in Miaohe, Zigui, Hubei.
3.Niutitang Biota
The Niutitang Biota discovered by M.Steiner, E.Wallis from
Technological
University of Berlin and Prof. Zhao Yuanlong, post-graduated student
Guo
Qingjun, Assistant Zhou Zhen, Ph..D.student Yang Ruidong from
Guizhou
University. It occurs in black mudrock of the Niutitang Formation at
the
Heehapao, Songlin Town, Zunyi County, Guizhou, includes a great
number
sponge fossils of Leptomitus, Saetaspongia, Choia, Solatinella,
Crumillospongia, Triticispongia, Haylosinca of porifea and Naraoia,
Isoxys,
Perspicaris, Tsunyidiscus, Songlinella of arthropda etc. up to now
the
Niutitant Biota is composed of fossils over 26 genera among 6 phyla.
They
are: 1. algae; 2. porifera; 3. colenterata; 4. worms; 5. mollusca;
6.
arthropods, including trilobitomorphs, large bivalve arthropods,
bradoriids.
The Niutitang Biota imparts new information about Cambrian of early
Metazoa.
Discovery of the Biota, makes evolutionary series of Cambrian
Burgess
Shale-type Biota extend down closer to the Pre-Cambrian and Cambrian
boundary; provides other important information for the definition of
the
Cambrian Explosion Appearance of great number of sponges, shows time
of
diversification of sponges earlier than Chengjiang Biota, and
provides
information concerning the origin the fauna and its paleogeography.
Occurrence of the Niutitang Biota and Chengjiang Biota, also shows
Burgess
Shale-type Biota are origin the South-west China. Therefore, this is
and
important Biota who has scientific significance.
4.Kaili Biota
The Kaili Biota contains for representatives of 11 phyla, namely:
1.algae,
including red algae, brown algae, and coralline algae etc. 2.
acritarchs; 3.
porifera, including sponges and chancelloriids; 4. coelenterate,
including
cnidaria, 5. ¡°worm¡±; 6. lobopodia, 7. medusiform fossils; 8.
brachiopoda;
9. mollusca; including hyolithids, monoplacophorids andbivalves; 10.
arthropods, including trilobite, trilobitioids, bradorriias, large
bivalve
arthropods, and other arthropods, 11. the fossils of uncertain in
classification, including Wiwaxia, Triplexia.
5.Guizhou Dinosaur Fauna
The Guizhou Dinosaur Fauna in this album refers to the multi-phyla
fossil
biota, discovered in the Upper Triassic Zhuganpo member of Falang
Formation
(about 230 million years age) in Xingyi of Guizhou Province and the
surrounding areas, represented by the Hu;s Guizhou Dinosaurs and
other
marine reptiles, and associated with losts of thishes, ammonites,
bivalves,
brachiopods, shrimps, crinoids and conodonts. This fauna widely
distributed
in the Zhuganpo member of Falang Formation in southwestern Guizhou
(Longguang of Anlong, Dingxiao and Wusha of Xingyi) and southwestern
Yunnan
(Luopong and Fuyuang and etc). it was a fauna living in a
comparatively
deeper water of the shallow sea.
6.Guanling Fossil Biota
Guanling Fossil Biota-the major Discovery of Triassic Marine Animals
in
China. Guanling Fossil Biota was found in the Upper Triassic Wayao
Member of
Falang Formation (about 220 million years ago) at Xinpu of Guanling
Buyi and
Miao Autonomous Coutny and its adjacent areas. The fossils biota is
characterized by the rich marine reptiles and crinoids, accompanied
with
abundant fishes, cephalopods (ammonite, nautilus), bivalves,
conodonts,
brachiopods, and diverse terrestrial plants. It is therefore praised
as
the
only treasury of late Triassic marine reptiles in the world.

2. New!
*********************************************************************
***
Jurassic Dinosaur Faunas in Zigong
http://www.hceis.com/book.asp?id=4708
×Ô¹±µØÇøÙªÂ޼ͿÖÁú¶¯ÎïȺ In Chinese with English summary
*********************************************************************
***
Peng Guangzhao/2005/185x260mm/236 pages/Hardcover/$55

Zigong, a famous historical and cultural city of China, is situated
in
southern Sichuan province and covers an area of about 433.13 km2, it
is
a
hilled region that exposes a continuous and widespread Mesozoic red
beds in
which contain rich fossil vertebrates, especially the Jurassic
fossil
dinosaurs. Since 1915 of the first dinosaur fossil discovered by an
American
geologist Dr. George D. Louderback from Rongxian (Jung Hsien), more
than 180
localities of fossil vertebrated have been found from Zigong region,
among
which about 130 localities of fossil dinosaurs. As a result, Zigong
has
become the most famous region of fossil dinosaurs and other
vertebrates, and
is named as the Hometown of Dinosaurs.
After the works of ninety years by numerous geologists and
paleontologists
from home and abroad, countless of fossil dinosaurs and other
vertebrates
have been excavated and a great of academic achievemens have been
made.
Especially in recent 30 years or more, a lot of important
discoveries
and
historical breakthroughs have been achieved, Zigong has become a
focus
region to which paleontologists pay more attention. This book is a
step
systematic conclusion about the discoveries of fossil dinosaurs and
other
vertebrates from Zigong region and achievements of scientific
researches as
well as a few new finds from the aspect of the vertebrate
assemblages.
It is
dedicated to Dr. George D. Louderback and all the people that have
made
contributions to the discoveries, excavations and studies of fossil
dinosaurs and other vertebrates from Zigong region.
The Jurassic continental sediments in Zigong region are well
developed.
The
thickness of the deposits is about 1034-2220m, composed mainly of
grey
limestones, purplish red mudstones and light grey sandstones, and
covers
about 75% of the earth surface of this region. These sediments
present
characteristic of the fluvial or lacustrine facies, and were
classified
from
lower to upper as the early Jurassic Zhenzhuchong and Ziliujing for
mations,
the Middle Jurassic Xintiangou and Xiashaximiao (Lower Shaximiao)
formations, the late Jurassic Shangshaximiao (Upper Shaximiao),
Suining
and
Penglaizhen formations. Rich and various remains of dinosaurs and
other
vertebrates have been found in these strata and can be divided into
three
related faunas: the early Jurassic Prosauropoda-Lufengosaurus Fauna,
the
Middle Jurassic Sauropoda-Shunosaurus Fauna, and the Late Jurassic
Sauropoda-Mamenchisaurus Fauna.

3.
*********************************************************************
*****
Paleontological Atlas of Jilin China
http://www.hceis.com/book.asp?id=4700
¼ªÁÖÊ¡¹ÅÉúÎïͼ²á In Chinese and Latin names index
*********************************************************************
*****
Edited by Bureau of Geology and Mineral Resources of Jilin
Province/1992/190x270mm/726 pages + 272 plates/Hardcover/$95
The Paleontological Atlas describes stragraphy and fossils Parts.

4.
*********************************************************************
**************************************************************
Ancient Life and Modern Approaches-Abstracts of the Second
International
Palaeontological Congress June 17-21, 2006, Beijing, China
Ô¶¹ÅÉúÃüÓëÏÖ´úÑо¿Í¾¾¶£ºµÚ¶þ½ì¹ú¼Ê¹ÅÉúÎïѧ´ó»áÂÛÎÄժҪר¼­ In English
*********************************************************************
**************************************************************
Edited by Qun Yang, Yongdong Wang & Elizabeth A.
Weldon/2006/210x285mm/553
pages/Paperback/$98

A total of 680 abstracts, submitted by participants from over 50
countries,
are presented in this volume, a number far surpassing our
expectations.
The
are grouped in the proposed congress session programme (i.e.,
Plenary,
Special, General and Topical sessions). Although some of sessions
may
not
run for oral presentation in the final congress programme, the
session
titles and their designated abstracts are retained in this book

5.
**************************************************************
The Dawn of Animal World http://www.hceis.com/book.asp?id=3858
¶¯ÎïÊÀ½çµÄÀèÃ÷ In Chinese and English names index
**************************************************************
By Chen Junyuan/2004/222*292mm/366 pages/Hardcover/$110

The Cambrian is a geologic period that began around 542 million
years
ago
(see below) and ended about 490 million years ago. The Cambrian
Period
is
the earliest period in whose rocks are found numerous large,
distinctly-fossiliz- able multicellular organisms more complex than
sponges
or medusoids. During this time, roughly fifty separate major groups
of
organisms or"phyla"(including almost all the basic body plans of
modern
animals) emerged suddenly, in most cases without evident precursors.
This
radiation of animal phyla is referred to as the Cambrian explosion.
The
dawn
of animal world had came through wenan radicalization, yidikala
radiation,
meishucun radiation, and maotianshan radiation one by one. This
process
is
Punctuated Equilib- rium that different from after 500 million years.
In this book, 547 color photos were embodied.

6.
**************************************************
Rudists and Facies of the Periadriatic Domain
In English
**************************************************
By Riccardo Cestari & Dario
Sartorio/1995/250x305mm/207pages/Hardcover/$55

Rudists are fossil bivalves that lived on the margins of the Tethyan
Ocean
and adjacent areas from the end of the Jurassic until the end of the
Cretaceous. These sessile benthic organisms flourished in carbonate
platform
environments and characterize several Cretaceous successions as
significant
organic builders and sediment producers. This makes it possible to
correlate
different paleogeographic domains from the Gulf of Mexico to the
Middle
East. The aim of this atlas is to examine in detail the particular
role
that
Rudist facies played in the development and history of Cretaceous
carbonate
platforms of the Periadriatic Domain. In this area, which in a
paleogeographical sense belongs to the Apulian Plate, many Mesozoic
carbonate platform successions crop out. These successions belong to
broad
platform complexes which display a pattern aligned with the present-
day
1sea. In these limestones, various Rudist facies are present, often
making
it possible to date and to correlate successions encountered by
wells
with
those observable in outcrops. For this reason, we though it would be
useful
to assemble and to illustrate the ample documentations that has been
acquired over the years so as to update the situation as regards
Rudists and
the related facies in the this area. This present volume has been
conceived
as and aid to all those who are working on these topics by taking
different
approaches including sequence stratigraphy, which is considered to
be
an
important methodology for analyzing the evolution of carbonate
platforms.
Another objective of our work is to better define the Rudist-bearing
Periadriatic successions and to compare them with those of other
Tethyan
Domains that developed in different tectono-sedimentary settings.
The
first
chapter of the atlas illustrates the evolution of the main Rudist
families
as well as those features useful for theiri dentification and
taxonomic
determination, both in outcrop and core analysis. To simplify the
presentation of their characteristics, in view of the difficulty of
isolating complete specimens of Rudists from the mainly massive
limestones
of the Periadriatic Domain, some specimens collected from other
regions
have
also been illustrated. Genera with particular stratigraphic
significance for
this Domain are also briefly discussed. This chapter closes with an
illustration of the stratigraphic distribution of the most
significant
Rudists of the Periadriatic area. The next chapter, regarding Rudist
sediments and their depositional environments, also introduces a
classification of Rudist facies that can be applied both to outcrop
and
sub-surface and which can be easily utilized in oil exploration. The
third
chapter illustrates the most important Rudist assemblages of the
Periadriatic Domain in time. SeventeenRudist events (from Event A to
Event
Q) have been identified in stratigraphic succession, taking into
account
macro-and micropaleontological assemblages and correlations with
other
areas
(France, Spain, North Africa, Middle East and others) where the
same,
or
similar, facies comprise important paleontological markers such as
the
ammonites and planktonic forams. In this chapter several Rudist
facies,
mainly of outcrops, are shown in considerable detail in thin and
polished
sections and often with their micropaleontological assemblages.
The final chapter concerns the role played by these mollusks in oil
and
gas
exploration. In fact, their shells and the bioclasts that derive
there
from
often improve the petrophysical features of the rocks that
characterize
many
oil and gas reservoirs, including those of the Periadriatic Domain.

7.
*********************************************************************
**
Studies On Ecological Environment of Guanling Biota
¹ØÁëÉúÎïȺÉú̬»·¾³Ñо¿ In Chinese http://www.hceis.com/book.asp?
id=3977
*********************************************************************
**
By Wang Shangyan/2005/185x260mm/78pages+14plates/Paperback/$25

Contents Preface Introduction Chapter 1 Overview Chapter 2 Regional
Geology
Background Chapter 3 Fossil Assemblage Chapter 4 Environment of
Guanling
Biota Chapter 5 Environment Significance of Geochemical Elements
Chapter 6
Environment Significance of Carbon and Oxygen Isotope Chapter 7
Environment
Evolution of Guanling Biota Concluding Appendix 1 Data of
Geochemical
Elements Rock, Ration of Part Elements and Standard Data of REE and
Chondrite Elements Apendix 2 Section Describe of First Section of
Xiaowa
Formation of Upper Triassic in Bamaoling village, Guanling,
Guizhou;References;Plates and its explanatory

8.
*********************************************************************
*************************
Guanling Biota-A Window Probing the Secrets of Oceanic Biological
World, 200
Million Years Ago
¹ØÁëÉúÎïȺ-̽Ë÷Á½ÒÚÄêǰº£ÑóÉúÎïÊÀ½ç°ÂÃØµÄ´°¿Ú In Chinese
*********************************************************************
*************************
Wang Xiaofeng/2004/290x220mm/120 pages/Hardcover/$65

9.
*********************************************************************
*******************
The Jehol Biota-The Emergence of Feathered Dinosaurs, Beaked Birds
and
Flowering Plants
In English
*********************************************************************
*******************
Mee-mann Chang/2003/280x290mm/208 pages/Hardcover/$130

In the recent years, the late Mesozoic Jehol Biota of northern China
has
shown the world some of the most astonishing fossil finds ever since
the
discovery of the first complete skeleton of Archaeopteryx in 1861,
and
thus
has become the focus of many important paleontological researches in
the
global arena. On the Biota"s fabu-lous roster are the four-winged
dinosaur
and many feathered ones, first beaked bird and many of its allies,
first
plants with flowers and fruits, fishes with the potential to un-lock
the
mystery of their origins, mammals of the special interests to their
early
evolution, pterosaurs that rules the Mesozoic skies, and thousands
species
of inver-tebrates (e.g.,mollusks,conchostracans,
ostracods,shrimps,insects,and spiders)that constitute a community of
truly
"wonderful life".
These exquisitely preserved fossils not only give us a vivid picture
of
once
a thriving biodiversity but also shed new light on a number of
interesting
theoretical issues in evolutionary biology today, such as the origin
and
angin and early evolution of some major taxonomic groups(e.g.,
amphibians,birds and angiosperms),the origin of feather and avian
fligt, and
the co-evoution of pollinating insects and flowering plants.The
Jehol
Biota
also bears significantly on paleobiogeography, paleoecology,
paleoclimate
and paleobiography, paleoecology, paleoclimate and paleoenvironments
during
the Mesozoic.
This book has pieced together the most up-to-date information on the
Jehol
Biota that is otherwise
Scattered in the vast technical literature and unavailable to the
general
readers. The first two chapters give an inviting introduction to the
Jehol
Biota in terms of its history of studies, its main components, its
scientific importance, its geographical, geological and
biostratigraphic
framework,and its renowned fossil discoveries. Each of the remaining
chapters deals with a particular organismal group of the Biota by
its
leading expert(s). In addition, the book is lavished with nearly 280
illustrations,which include 200 photographs that show diversity of
the
taxa
and beauty of their preservations. The colored life restorations,
elegantly
done by some of China"s most celebrated primarily at an educated
public, the
book is also an invalu-able source of information for the students
and
professionals in paleontology,geology, evolutionary biology, and
science
education in general

10.
************************************************
Mesozoic Jehol Biota of Western Liaoning, China
ÖйúÁÉÎ÷ÖÐÉú´úÈȺÓÉúÎïȺ In Chinese
************************************************
Ji Qiang/2004/290x220mm/375 pages/Hardcover/$88

11.
*****************************************************************
Jehol Biota-Splendid Lives From More Than 100 Million Years Ago
ÈȺÓÉúÎïȺ In Chinese
*****************************************************************
Zhang Miman/2001/290x215mm/150 pages+183 figs/Hardcover/$58

1.Invertebrates: Gastropoda,Bivalvia,Ostracoda,shrimps,insects and
spiders
2.Veterbrates: Fishes, Amphibian, Turtles, Dinosaurs,Birds,Mammals;
Plants:
Charophytes,higher plants, Spore and pollen

12.
*******************************************
Jehol Biota
ÈȺÓÉúÎïȺ In Chinese with English summary
*******************************************
Chen Pei-ji/1999/185x260mm/342 pages+ Plates/Paperback/$55

This book contains following papers:
1.Palaeobotany (1) A Preliminary Study of the Jehol Flora from
Western
Liaoning (2)Charophytes of the Yixian Formation from Northern Hebei
and
Western Liaoning (3)Sporomorphy Assemblage from the Basal Yixian
Formation
in Western Liaoning and Its Geological age
2.Invertebrate Palaeontology (1)Fossils Gastropods of the Lower Part
of
the
Yixian formation from Sihetun Area, Western Liaoning, China (2) A
Study
of
Nonmarine Bivalve Assemblage Succession from the Jehol Group (3)
Fossil
Conchostracans from the Yixian Formation of Western Liaoning, China
(4)
Nonmarine Ostracods of the Lower Part of the Yixian Formation in
Sihetun
Area, Western Liaoning, China (5) Restudies in Aeschnidiids (6)
Liaoningogriphus quadripartitus from the Jehol Biota and Notes on
Its
Paleoecology
3.Vertebrate Palaeontology (1) Middle and Late Mesozoic
Acipenseriforms
from
Northern Hebei and Western Liaoning, China (2) The Skuyll of
Manchurochelys
liaaxiensis from the Yixian Formation of Beipiao, Liaoning and
Phylogenetic
(3) Some Microstructure Difference among Confuciusornis, Alligator
and
a
Small Theropod Dinosaur, and Its Implications
4.Stratigraphy (1) The Sihetun fossil Vertebrate Assemblage and its
Geological Setting Western Liaoning, China
5.Index of New Genera and Species

13.
************************************************
Sinian Miaohe Biota
Õ𵩼ÍÃíºÓÉúÎïȺ In Chinese with English summary
************************************************
Dingg Lianfang/1996/180x260mm/221pages+20 plates/Hardcover/$28

1.The Stratigraphy; 2.The Miaohe Biota and its classification of
organisms;
3.Micropalaeophyta; 4.Macroscopic Alge fossil; 5.Eumetazoa and
Profera;
6.Trace Fossil 7.Sedimentary facies and Environments and
Palaeoecology;
8.Conclusions 9.Reference 10.Summary in English 11.Explanation of
plates and
Plates

14.
*********************************************************************
Biota and Palaeoenvironment In Northern Jiangsu, China Since 10000a
Bp
In English
*********************************************************************
Gou Yunxian and Tang Lingyu/2000/185x260mm/126 pages + 24
plates/Hardcover/$44

The purpose of this book is to present the results of our studies on
the
alteration of the Holocene biota in time and space and the
sedimentary
and
geochemical indicators in Jianhu and the adjacent areas, northern
Jiangsu,
and to discuss the palaeoenvironmental changes, essentially to study
future
environmental changes in these regions. The authors carried out
field
investigations in the study area and collected fossil specimens and
sediment
samples at the Qingfeng section of Jianhu, Jianhu brick-field and
Sanchakou
brick-field of Jianhu, the Liujun section of Huai' an and the Xiyuan
section
of Funing. Systematic sampling was madde in the Qingfeng section,
where
eight kinds of fossils including sporo-pollen, charophytes,
foraminifers,
ostracods, gastropods, bivalves, microinsects and acarids were
forund
and
identified. The 8 palynological zones were estabilished and 3
foraminiferal
assemblages, 4 ostracod assemblages and 3 bivalve communities were
recobgnized in the section. Gastropods, micro-insects and acarids
are
restricted to several layers in the section and charophytes are only
distribted in its top part. The palaeoecology of these faunas is
discussed.
The biotic alternation is clearly showed in the Qingfeng section. On
the
basis of the biotic variance, it is suggested that the Holocene
transgression started at about 6900a BP and the highest sea level
appeared
in the time from 6400a BP to 5400a BP in the study area. After 5400a
BP
the
sea level was gradually declined and the sea water rapidly retreated
from
this area at about 4500a BP. From 2200a BP to 1000a BP happened
another
transgression, which was much smaller in intensity than the
preceding
one.
The Holocene palaeoenvironment can be reconstructed in Qingfeng
region
as
follows: coastal muddy marsh - coastal salted mud flat - inner bay -
neritic
bay - salted nearshore lowland-freshened lagoon. According to the
palynological data, the Hypsithermal interval is deted at 8500-3700a
BP
in
Jianhu and the climatic corresponded well to the Holocene global
climatic
changes.

15.
*********************************************************************
Doushantuo Fossils: Life on the Eve of Animal Radiation
¶¸É½ãûÆÚÉúÎïȺ-ÔçÆÚ¶¯Îï·øÉäǰϦµÄÉúÃü In Chinese with English summary
*********************************************************************
Yuan Xunlai/2002/285x210mm/171 pages/Paperback/$55

Terminal Proterozoic rocks outcrop on the Yangtze Platform in South
China,
from Yunnan Province in the west to Jiangsu and Zhejiang provinces
in
the
east, and from the Yangtze Gorges area to Guizhou province and
Guangxi
Zhuang Automomous Region. These proterozoic successions are little
metamorphosed and contain abundant and diverse beautifully preserved
fossils. Building upon the research of dozens of palaeontologists in
the
last few decades, we begin to understand the Terminal Proterozoic
biodiversity through the taphonomic windows preserved in Doushantuo
rocks at
Weng'an, Miaohe, and Lantian. The Weng'an Biota in Guizhou Province
is
best
known for its phosphatized algae and animals, exquisitely preserved
at
cellular level and in three dimensions. The Miaohe Biota, rivaling
the
Burgess Shale in preservational style and quality, contains
beautifully
preserved carbonaceous compressions on the banks of the equally
beautiful
yangtze Gorges. The Lantian Flora, entombed in terminal Proterozoic
rocks
near Lantian,-a southern Anhui town rich in culture and history,
also
features diverse carbonaceous compressions. These three biotas are
of
similar geological age, follwing the proterozoic glaciation recorded
in
the
Nantuo Tillite about 600 million years ago but preceding the
Cambrian
Explosion 544 million years ago. In combination, these three fossil
assemblages allow a clearer and more complete understanding of the
proterozoic biosphere just before the Ediacaran and Cambrian
diversification
animas.

16.
**************************************************************
Early Cambrian Chengjiang Fauna in Eastern Yunnan China
ÔÆÄ϶«²¿Ô纮ÎäÊÀ³Î½­¶¯ÎïȺ In In Chinese with English abstract
**************************************************************
Chen Liangzhong/2002/206/Hardcover/$35

Early evolution of metazoans and the Cambrian Explosion are not only
the hot
topics in paleontology, but also are the mysteries in geosciences
and
life
sciences.The Chengjiang Fauna, wihich is firstly discovered in
Maotianshan,
Chengjiang county, Yunnan Province, provides one of the best
evidences
for
interpreting the Cambrian Explosion. Soft-bodied fossils are
commonly
found
in the yellowish green mudstone of the medium0upper part of the
Yuanshan
Member of the Heilinpu Formation during the Qiongzhusian Stage of
the
Early
Cambrian in Eastern Yunnan. It represents a significant window to
the
ancient sea world 530 million years ago and contains valuable
materials
to
understand the Cambrian Explosion comprehensively¡­¡­

17.
*********************************************************************
***************
The Chengjiang Fauna--Exceptionally Well Preserved Animals From 530
Million
Year Ago
³Î½­¶¯ÎïȺ In Chinese
*********************************************************************
***************
Hou Xianguang/1999/180x260mm/170/Paperback/$75

This book record one of the most amazing finds in the 20th century
the
find
of the Chengjiang fauna in true and detail. It has more than 200
kinds
firs
hand precious pictures of fossil, and provides their Chinese names,
Latin
names, Locality. It reappears the wonderful spectacles about the
life
of
marine animals and the original characteristics of the existing
living
beings on the earth from 530 million years ago. It provides precious
materials for enriching the theory of evolution. The Cambrian
represents the
beginning of a long sequence of geological time known collectively
as
the
Phanerozoic. This term is composed of the Greek words planners,
meaning
visible, obvious, and Zion, animal. This was to stress the
difference
from
the older, once seemingly unfossiliferous Precambrian rocks, the
Cryptozoic.
Although both microfossils and macrofossils are now known from
Precambrian
rocks, particularly from late Precambrian, there is the striking
difference
in numbers and types of fossils with those in the Phanerozoic.
However,
the
situation varies in detail. In some areas Cambrian rocks may contain
many
fossils, whereas in others there are sandstone's or other rocks that
are
commonly poorly fossiliferous. In addition, different fossils occur
in
the
Cambian in different parts of the world, which makes it difficult
when
making comparisons to know if we are talking about strata of exactly
the
same age.
1.Division of geological time 2.Evolution of Early Life on Earth
3.Cambrian
and the Cambrian Explosion 4.Discovery and study of the Chengjiang
Fauna
5.Distribution and Geological Setting of the Chengjiang fauna
6.Stratugraphy
across the Precambrian-Cambruan Boundary 7.Significance of the
Chengjiang
fauna 8.Characterustucs of the Chengjiang fauna 9.Systematic
Palaeontology
of the Chengjiang Fauna 10.Phylum Echinodermata Klein,1734
11.Uncertain
taxa

18.
*********************************************************
Early Cambrian Chengjiang Fauna from Kunming Region China
À¥Ã÷µØÇøÔ纮ÎäÊÀ³Î½­¶¯ÎïȺ In Chinese with English summary
*********************************************************
Luo Huilin/1999/185x260mm/129 pages +32 plates ,46 figs/Hardcover/$45

In the Kunming region, the Chengjiang fauna-bearing strata of Lower
Cambrian
Heilinpu Formation, especially the Yuanshan Member are well
developed
and
widely spreaded, having great potential in searching for new
localities
of
the Chengjiang fauna. From 1992 to 1998, sponsored by the Yunnan
Provinceial
science & Technology Conmission and the Ministry of Geology and
Mineral
Resources, we carried out searching and exploring of the Chengjiang
fosssils
round the Kunming region, and about 5000 speciemens were collected
at
Haikou, Kunming, including abundant soft-bodied arthropods and
diversed
worms, lophophorates, sponges, brachiopods, hyolithes, macroalgal
fossils,
uncertain taxa and ichnofossils.
This book gives a detailed introduction about the research history,
stratigraphic horizon and geographic distribution of Chengjiang
fauna
in the
kunming region. The classification and composition of the fauna are
discussed with comparison to that in the Chengjiang region. The
paleoecology
and taphonomy of some early taxa are briefly reviewed. It is
important
to
note that a new softbodied fauna, named as Gaunshan fauna is here
reported
for the first time from the Lower Cambrian Wulongqing Formation in
the
Kunming region, and a comparison of its composition to the
Chengjiang
and
the malong faunas is made.
Altogether 111 species assigned to 101 genera of 18 fossil groups
are
described from the Kunming region, among them 48 species and 36
genera
are
new. They belong respectively to the Chengjiang and Guanshan faunas.
The new
significant discovery greatly enriches the contents of early faunas
and
is
of great importance for understanding the geological and
geographical
distribution of the Early Cambrian biotas in eastern Yunnan and
their
paleoecological and taphonomic environments.
1. The Cambrian explosion of life 2. Features and kinds of biota
assemblages
of the Chengjiang fauna 3. Discovery and distribution of the
Chengjiang
fauna from Kunming region 4. The Chengjiang fauna in Haikou area,
Kunming 5.
Correlation of the fossil assemblages of the Chengjiang fauna
between
Chengjiang and Kunming regions 6. Paleoecology and taphonomy of the
Chengjiang fauna in Kunming region 7. The Guanshan fauna from
Canglangpu Age
of Early Cambrian in Kunming region 8. Systimatic paleontology 9.
Reference
10.Plates and explanation

19.
******************************************************************
The Fauna From the Neolithic Site at Hemudu, Zhejiang
Õã½­ÓàÒ¦ºÓÄ·¶ÉÐÂʯÆ÷ʱ´úÒÅÖ·¶¯ÎïȺ In Chinese with English summary
******************************************************************
Wei Feng/1989/185x260mm/125 pages + 17 plates/Hardcover/$35

1. Invrtebrata
(1) Eulamellibranchia (2) Mesogastropoda (3) Dccapoda
2. Vertebrata
(1) Pisces (2) Reptilia (3) Aves (4) Mammalia

20.
*********************************************************************
********
Intertidal Trace-Making Faunas and their Traces in the Northern Gulf
of
China
±±²¿Íå³±¼ä´øÔì¼£¶¯ÎïȺ¼°ÆäÒż£ In Chinese with English summary
*********************************************************************
********
Wang Zhenru/1994/185x260mm/97 pages +8 plates/Hardcover/$18

Abundant animals in the intertidal zone form the characteristic
trace-making
faunas and their living traces. Totally, 156 species (including 16
indetermined species) are identified, and they belong to 69
families,
16
classes and 10 phyla respectively. Detailed study on the
characteristics and
regularities of various faunas, including their structural levels,
living
habitats and traces, etc., have been done in this article.

21.
*********************************************************************
****************************
Reports of Paleonotogical Expedition to Sinkiang(II)¡ªPeterosaurian
Fauna
from Wuerho, Sinkiang
н®¹ÅÉúβ챨¸æ£¨¶þ£©-ÎÚ¶ûºÌÒíÁú¶¯ÎïȺ In Chinese with English
summary
*********************************************************************
****************************
Edited by Dong Zhiming/1973/185x260mm/51pages+17plates/Paperback/$15

An early Cretaceous(Tugulo series) reptilian fauna is described in a
series
of papers in the present memoir. The materials were collected in
1964
by
members of the paleontological expedition to Sinkiang of IVPP from
Wuerho
district, in the northwestern part of Dzungar Basin.
This fauna includes the following reptile species: Chelonian,
Pterosauria,
Crocodilian, Plesiosauria, Saurischia And Ornithischia. The
reptilian
fossils are all found in a series (Tugulo) of lacustrine sediments.
The
fauna in general can be slosely correlated with that of Morrison
fauna
of
the Rocky Mountain region of the western north America, but some of
the
forms are nearer to those of Cloverly formation.
A leading form in this fauna is Dsungaripterus, which is considered
by
Young
to represent a new family and suborder of the pterosaurs. It is a
large
form
with well-developed medial crest on the skull and the anterior teeth
entirely disappeared. Based on these advanced characteristics Young
has
suggested an early Cretaceous age for it. The occurrence of a small
theropoda, Phaedrolosaurus ilikensis,, which is comparable with
Deinonychus
from the Lower Cretaceous of Montana, supports this view. Therefore,
We
have
tentatively set the age of the Tugulo fauna of Wuerho at the early
Early
Cretaceous.

22.
*********************************************************************
*********************************************
Cambrian Stratigraphy, Lithofacies, Paleogeography and Trilobite
Faunas
of
East Qinling-Dabashan Mountains, China
In English
*********************************************************************
*********************************************
Yang Jialu/1991/185x260mm/246 pages + 24 plates/Hardcover/$56

East Qinling-Dabashan area is one of the important places for the
study
of
the Early Paleozoic crustal evolution in East China. This book will
detail
the 16 Cambrian sections in the area and systematically describe
trilobites
found there; the 81 genera or subgenera and 161 species or
subspecies
(or
undetermined and indelinite species) blonging respectively to 4
orders,
4
suborders, 14 superfamilies, 36 families, in which there are 2 new
families,
12 new genera (or subgenera) and 71 new species. Based on this , the
sequence of the Cambrian system in each stratigraphic areas is
reconstructed
in which there are 2 new groups, 12 new formations and 20 trilobite
assemblage zones (or zones) established; many genera and species of
agnositids, present in upper Middle Cambrian, provide facility for
intercontinental correlation of the trillobite zones; in addition, 7
maps of
lithofacies and paleogeography have been made. The study of the
Cambrian
strata, lithofacies, paleogeography and trilobites in this area is
of
great
significance for a better understading of the trilobite geographic
proincialization, the Cambrian crustal volution and the distribution
law of
the useful mineral resoures in the black rock series. There are 24
plates,
58 tex-figures and 19 tables included in the book.

23.
*********************************************************
The Upper Cave Fauna of Choukoutien -New Series C, NO.10
In English
*********************************************************
By Pei Wen-chuang/1940/220x295mm/84 pages, with VIII plates and 38
text
figures/Paperback/$190

Introduction
The present volume contains the study of the fauna, except the
avifauna
found in the Upper Cave of Choukoutien. This Cave, as previously
reported on
several occasions, has yielded an industry of Palaeolithic nature,
human
fossils of Homo sapiens type and a rich fauna. This is the first
time
that
such a cave is known in China or Easter Asia. And the study of it
marks
the
beginning of a new stage in palaeolithic research in this part of
the
world,
along the most classical lines of European prehistory. A description
of
the
Upper Cave Industry has already been published (Pei, 1939f)
containing,
as
an introductory note, the history of the excavation, the description
of
the
Cave, and also the geological evidence leading us to fix the correct
age fo
the site. However, the dating of the Upper Cave as Late Pleistocene
is
largely determined by the fauna. In the present volume we will
analyse
this
fauna in detail and then discuss the position of this animal
¡°assemblage¡±
in the evolution of Chinese mammals in the Quaternary times. The
fossils
collected in the Upper Cave are mostly in an excellent state of
preservation. Complete skeletons and skulls were often met with
throughout
the Cave during the excavation. In the Lower Recess (vide Pei,
1939f,
P. 9),
skeletons of deer, bear, Hyaena, etc. were piled in a limited space.
Such
conditions favour the assumption that this deep cave had acted as a
natural
trap for animals, or else, that part of them were brought in as prey
by
some
carnivorous beasts. The durations of human occupation seem to have
been
very
short, since the cultural layers are always thin and limited to a
restricted
a area in the deposits. On the other hand, the numerous remains of
tigers,
young and old, suggest that this animal was periodically the master
of
the
place. This whole series is NO.125

24.
*********************************************************************
****************************
Fossils from the Middle-upper Jurassic and Lower Cretaceous in
Eastern
Heilongjiang Province, China (2 Volumes set) (Used)
ºÚÁú½­Ê¡¶«²¿ÖС¢ÉÏÙªÂÞͳÓëϰ×ÛÑÓëϰ×ÛÑͳ»¯Ê¯ In Chinese with
English
summary
*********************************************************************
****************************
By Chen Daokuo/1984/185x260mm/343pages+64plates/Paperback/$55

Part I
Research team on the Mesozoic coal-bearing formations in eastern
Heilongjiang
CONTENTS (112pages+16plates)
1. Preface
2. A brief note on stratigraphy
3. Fossil plants from the Longzhaogou group in eastern Heilongjiang
province
4. Fossil plants from the Longzhaogou group in eastern Heilongjiang
province
5. A discussion of palynological characters and geological ages of
several
new localities in eastern Heilongjiang province
6. New rhynchonellid brachiopods from upper Jurassic of Hulin
county,
eastern Heilongjiang province
7. Some late Mesozoic gastropods from eastern Heilongjiang
8. Some bathonian ammonoids from E. Heilongjiang
9. Ostracoda from the Longzhougou group and the Xiachengzi formation
in
E.
Heilongjiang
10. Some insect fossils from the east of Heilongjiang province
11. Late Mesozoic fossil fishes from eastern Heilongjiang, China
Part II
Research team on the Mesozoic coal-bearing formations in eastern
Heilongjiang
1. Fossil plants form the Longzhaogou group in eastern Heilongjiang
province
2. Fossil plants from early cretaceous Tongshan formation in Mishan
county
of Heilongjiang province
3. Preliminary study on Jurassic and cretaceous bivalves of eastern
Heilongjiang Province in China

25.
*************************************************************
The Handbook of Nanling Fossil (Used) (Nanling Huashi Shouce)
ÄÏÁ뻯ʯÊÖ²á In Chinese
*************************************************************
By the editorial group/1963/145x210mm/192pages+76plates/Hardcover/$35

26.
***************************************************
Fossil Treasures from Liaoning
ÁÉÄþ¹ÅÉúÎﻯʯÕ䯷 In Chinese and English bilingual
***************************************************
Wu Qicheng/2002/185x260mm/138/Hardcover/$58

Liaoning Province is famous for producing abundant fossils,
especially
those
from the Jehal Biota, which includes many internationally known,
rare,
and
excellently preserved taxa of extraordinary diversity. Liaoning has
recently
won the reputation of treasure house of fossils in this book, 100
representative species of fossils are carefully selected from
Liaoning,
comprising 78 animals and 22 plants. The pictures are followed by
both
Chinese and English brief explanations. All pictures are collected
from
those already published by paleontologists. These pictures basically
reflect
the original features of the specimens; therefore, it is highly
recommended
for collection. In the frief explanations of the fossils, we have
provided
information about the scientific name, locality, horizon, age,
morphology,
diagnosis and even reconstruction of the habits of the fossil. This
book
should be interesting for such readers as geologists,
paleontologists,
college teachers, and all who are interested in fossils. We hope
this
book
will stimulate the interest of more people in studying the
geological
history of Liaoning, appreciating the value of the deposits in
Liaoning, and
further exploring the mysterious evoluion of earth life.

27.
**************************************
Fossil Atlas of Yunnan (2 Volume set)
ÔÆÄÏ»¯Ê¯Í¼²á (2 ¾í) In Chinese
*************************************
1974/200x140mm/Vol.1: 864 pages Vol.2: 296 plates/Hardcover/$250

28.
*************************************************************
Acritarch Study in China
ÖйúÒÉÔ´À໯ʯ In Chinese, English summary and Latin names index
**************************************************************
By Yin Leiming/2006/185x260mm/222pages+52plates/Hardcover/$48

Organic-welled microfossil have been studied in china as long as
nearly
half
century. More than hundreds publications concerning with acritarchs
from
Archena to Cenozoic strata recorded the evolutive history of
microphytoplankton, as the fundamental chain of oceanic nutrition.
To
study
acritarchs in more detail ad in-depth is not only necessary of
biostratigraphy, especially for Precambrian and Paleozoic, but also
provides
significant information for searching origin and evolution of life
in
early
geological time of Earth and for reconstruction of old-age marine
ecological
system.
Sedimentary rocks of nearly whole geological time from Archean to
Cenozoic
outcrop wide-spread in China. Abundant and well-preserved
microplanktonic
fossils have been found from rocks of different geological ages. Of
which
the terminal Precambrian Doushantuo microbiota of South China is
much
famous
in the world ad many Proterozoic and early Paleozoic acritarch
assemblages
have became the attentive focuses or common cited data in
international.
In the early days, acritarch study in China was mainly on
Precambrian
biosratigraphy and they are taken as the important fossil evidences
from
shale where are normally absence of stromatolites. The
representative
acritarchs and acritarch assemblages of different geological ages in
China
¡­¡­

29.
*********************************************************************
****************************
Mesozoic and Cenozoic Fossil Atlas from the Qaidam Basin, Qinghai
Province(two volumes set)(used)
²ñ´ïľÅèµØÖС¢ÐÂÉú´ú»¯Ê¯Í¼²á In Chinese and Latin names index
*********************************************************************
****************************
By the institute geology of oil administration in Qinghai
Province/1978/185x260mm/178pages+42plates/Hardcover/$70

The first volume describes the common fossil 69 genera, 146 species.
The
last volume describes 47 genera, 95 species in which 41 species
wasn¡¯t
named.

30.
*********************************************************************
******************
The Tertiary 'Miscellaneous Fossils' from Jiyang Depression,
Shandong
Province (used)
ɽ¶«¼ÃÑôÛêÏݵÚÈý¼ÍÔÓÀ໯ʯ In Chinese with English summary
*********************************************************************
******************
Edited by Li Linli, Yao Yimin & Xiang
Weida/1992/190x260mm/101pages+28plates/Hardcover/$25

The number of described genera and species of the ¡® miscellaneous
fossils¡¯
from the Jiyang depression here are as follows:
Four genera and 4 species of fish; 2 families, 3 subfamilies and 10
incertae
species of pharyngeal tooth; 21 new species of otolithes; 7 genera
and
14
species, including 1 new species of bivalves; 4 genera and 1 new
species of
foraminiferas; 5genera and species of insects; 3 species, including
1
new
species, of cladoceres; 3 species, including 1 new species, of
cladosiphonales; 2 genera and 2 species, including 1 new species of
polychaetes; 2 trace fossil facies and 1 type of fecal pellets; 10
new
species of incertae sedis for Lagenalis; one type of Trapites; 4
families
and 4 genera, including 2 species, 3 incertae species and 5
indeterminated
genera and species of plant seeds; one incertae genera and species
of
reptiles and 1 genus and species of mammal. With the evolution of
the
¡®Miscellaneous Fossils¡¯ themselves and the change of the
paleoenvironment,
the ¡®Miscellaneous Fossils¡¯ developed in a number of different
groups.
Based on the stratigraphical distribution and the component
difference
of
the groups, 11 assemblages of the ¡®Miscellaneous Fossils¡¯ have
been
established here.

31.
**********************************************************
Aspects of Cambrian-Ordovician Boundary in Dayangcha China
Öйú´óÑô²íº®Îä-°ÂÌÕϵ½çÏß²ãÐÍ In English
**********************************************************
Chen Jun-Yuan/1986/185x260mm/410 pages+100 plates/Hardcover/$55

1. Introduction 2. Geological Setting 3. Description Of Sections 4.
Lithofacies Sequence 5. Remark On Sedimentary Environment 6. Clay
mineral
composition aspects and relevant implication Of diagenetic- process
7.
Rare
Earth And Other Trace Elements In Biogenic Apatite 8. Across The
Cambrian-Ordovician Boundary 9. Rb-Sr Dating On The Cambrian-
Ordovician
Boundary Interval 10.Towards A Common Language--Assessment Of
Xiaoyangqiao
Boundary- Stratotype
12.Conodonts 13.A New Planktonic Graptolite Fauna 14.Trilobites
15.Acritarchs 16.Review Of Lithofacies And Graptolite-Based
Biofacies
Of
Three Critical- Cambrian-Ordovician Boundary Stratotype Sections
17.Idexes

32.
************************************************
Guizhou-Palaeontological Kingdom
¹óÖÝ-¹ÅÉúÎïÍõ¹ú In Chinese with English summary
************************************************
Zhao Yuanlong/2002/185x260mm/213 pages/Hardcover/$38

The sedimentary rock in Guizhou is well developed and widely
distributed.
Stratigraphical units of sedimentary rock are perfect from the
middle
Proterozic to Quaternary system in this area. Because Guizhou area
in
geological history still was covered by seawater before late
Triassic
period, the abundantly fossiliferous marine strata is well
developed.
Continental strata consists of a little rock of Jurassic,
Cretaceous,
Tertiary and soil of quaternary. The Jurassic strata exposed over
western
Guizhou as a whole, while the others only scatter.
The fossils discovered in strata of Guizhou are very abundant and
have
various types in preserved. They are distributed among 20 phyla and
include
a more than 4000 species, 2000 genera, 200 families, based on the
above
features, Guizhou is aptly named as "Palaeontological Kingdom"

33.
*********************************************************************
***************
Papers on the Devonian-Carboniferous Transition Beds of Central
Hunan,
South
China
In English
*********************************************************************
***************
M.Coen & L.Hance/1999/298x210mm/232 pages,7 color photos,468
white/Hardcover/$50

34.
*********************************************************************
****************************
Mass Extinction and Recovery-Evidence from Paleozoic and Triassic of
South
China (two volume set)
ÉúÎï´óÃð¾øÓ븴ËÕ¡ªÀ´×Ô»ªÄϹÅÉú´úºÍÈýµþ¼ÍµÄÖ¤¾Ý(ÉÏϾí) In Chinese
with
English summary
*********************************************************************
****************************
Rong Jiayu etc./2004/1132pp./Paperback/$100

This is a mongrphy to discuss mass extinctionand recoveryin
prehistory.
It
is edited by 39 specialists in this field.

35.
****************************************
Phanerozonic Geology of Northwest China
In English
****************************************
Zhou Zhiyi/1997/185x260mm/316/Hardcover/$110

On the basis of precise regional stratigraphic classification and
correlation with analysis of biofacies and lithofacies, Phanerozoic
palaeogeography of Northwest China is reconstructd period by period.
Outline
of plate tectonic patterns in different epoch and geolgoical
development is
revealed largely according to the spatial and temporal distribution
of
characteristic biotas and similar facies belts. As a whole,
palaeozoic
history is essentially one of rifting, dispersal and collision
involving the
Siberia, Kazakhstan, Tarim and North China plates, resulting in
their
gradual incorporation. From the Middle Triasic onwords the
geological
evolution is mainly the process of amalgamation of the Qinghai-
Xizang
Plateau into Eurasia follwong northward subductions of the India
Plate.
In
addition, the geological characters and displacements of the
Altun-Beishan
Geowedge and west junggar Nappe are also discussed in detail.

36.
****************************************
Atlas of the Palaeogeography of China
In English
****************************************
Institute of Geology and Wuhan College of
Geology/1985/380x280mm/301/Hardcover/$77

The atlas is in octavo volume. It includes 123 plates consisting of
palaeogeographic maps, palaeobiogeo graphic maps, columnar sections
and
sedimentation profiles, etc. They are arranged in groups in the
order
of
diminishing age, in accordance with tectonic stages. The map groups
of
each
stage usually begin with a palaeotectonic map and each geologic
period
starts with an outcrop map. An outline map showing a geotectonic
units
of
China and a series of regional tectonic profiles showing their
historic
development came last in the atlas with the function of a summary. A
topographic map of China was put in advance of other maps as a
reference for
location of specific geographic names. In the general legend are
included
those commonly used in palaeogeographic maps, columnar sections and
sedimentation profiles, which are given in the beginning of the
volume.
Legends used only in specified maps, such as the palaeotectonic and
palaeobiogeographic, are given in the respective plates. A separate
legend
is compiled for the quaternary. The explanatory texts amounts to
about
200,000 words and appear after all the maps, arranged in order of
age.
For
the convenience of foreign readers an abridged English explanation
has
been
prepared, which contains a complete translation of the first
chapter(general
account) and abstracts of the remaining chapters. Legends and
professional
annotation on the maps are also given in English an Chinese. The
main
aim of
this atlas is thus to reveal the fundamental course in
palaeogeographic
development and crustal evolution of China, and to appraise its
position and
implication in global tectonics. We hope this Atlas will fullfill
the
following requirements: 1.Through the combined research in
palaeogeography
and palaeotectonics and the coordination of the plate tectonics
theory
and
classical geotectonic concepts, it will lead t a better
understanding
of the
interesting and varied tectonic and palaeogeographic development of
China,
so as to enrich and supplement the new globle tectonics theory. 2.
It
will
provide a general information on sedimentary environment and
geotectonic
background for a strategic perspective of sedimentary and strata-
bound
mineral deposits and furnish basic geological data material for
study
of
their distribution and metallogenetic conditions. 3. With its clear
and
systematic viewpoint and mode of presentation, with the coordination
of
the
various maps and explanations, it will help geologists working in
various
fields, teachers and students in geology and geography in
universities,
colleges to understand the general history of crustal evolution of
China,
and to furnish scientific workers in other fields with relevent
information
they may need.

37.
*********************************************************************
********************************
Some New Discoveries About the Groups of Palaeoecological Geography
in
xinjiang and the study of them
н®¹ÅÉú̬µØÀíȺµÄз¢ÏÖ¼°ÆäÑо¿ In Chinese with English abstract
*********************************************************************
********************************
Hai Tao/1993/185x260mm/63 pages + 96 plates/Hardcover/$45

This book consists of seven parts: Part I, Palaeo-fish; Part II.
Palaeo-amphibian; Part III. Palaeo-bird; Part IV. Palaeo-insect and
some
other arthropod; Part V. Palaeoplant: Part VI. Palaeoecological
geography;
Part VII. Palaeoecological atlas of the Permian inland lake basin in
Xinjiang.
The subjects discussed in this book are as follws; the evolution of
the
palaeo-environment of the inland lake basin during the Permain
period
in
Xinjiang; the interrelation of the groups of palaeoecological
geography
during the evolution; the evolution of palaeo-ecosystem; the feature
of
palaeo-
Part I. Palaeo-Fish Part II. Palaeo-Amphibian Part III. Palaeo-Bird
Part IV.
Palaeo-Insect and some other Arthropod Part V. Palaeo-Plant Part VI.
Palaeoecological Geography

38.
***************************************
Palaeocology of China Vol.1
ÖйúµÄ¹ÅÉú̬ѧ£¨1£© In English
***************************************
Edited by by Jin Yu-gan, Wang Jun-geng & Xu
Shan-hong/1991/185x260mm/372pages+17plates/Hardcover/$45

CONTENTS  Editors¡¯ preface 1. Ecological History of Doushantuo
Period
in
Yangtzed Gorge District, S. China 2. A Preliminary Study on Growth
Rate
and
Environment of Pseudogymnosolenid-Stromatolitic Bioherms from
Proterozoic in
N.China 3. Palaeoecological Aspects of Brachiopods from Chiungchussu
Formation of Early Cambrian Age, Eastern Yunnan, China 4. Emsian and
Eifelian Marine Communities of South China 5. Paleoecology of Late
Devonian
and Early Carboniferous Ostracodes from Guilin and Its Vicinity,
Guangxi 6.
On Relationship between Ammonoid Distribution and Development of
Syndepositional Taphrogenesis During Late Palaeozoic and Triassic in
China
7. Preliminary Discussion on Effects of Environments on Late
Palaeozoic
Miospore Assemblages 8. Successional Change of Late Carboniferous
Autochthonous Clastic Swamp Taphonomic Phytocommunities from
Xiaheyan,
zhongwei, Ningxia 9. Transitional Palynofloras from Basal Lower
Triassic of
China and Their Ecological Implications, with Special Reference to
Paleophyte/Mesophyte Problems 10. Permian Sedimentary Facies and
Biofacies
in Lower Yangtze Region, China 11. Paleobiogeographic Analysis of
Jurassic
Radiolaria 12. Larval shell of Aucellina and Its Ecological,
Biogeographical
and Classificatory Significance 13. Lower Turonian Gastropod Ecology
and
Biotic Interaction in Helicaulax Community from Western Tarim Basin,
Southern Xinjiang, China 14. Some Major External Effects on
Successional
Processes of Cenozoic Vegetation in China 15. Sedimentology and
Microfacies
Analysis of Reef Mound from Late Permian Changhsing Formation at
Laolongdong, Beipei of Chongqing, China 16. Fluctuation of Carbon
and
Oxygen
Isotopes in Sokolowia buhsii(Grewingk) of Early Tertiary and Its
Ecological
Implications 17. Palaeoecology of Quaternary Lamprotula from Lower
Reaches
of Fenhe River, Shanxi 18. A Preliminary Study of Climatic Sequence
(7500-5000 YR. B. P.) in Middle and Lower Reaches of Yangtze River
19.
Amino
Acid Levels in Core Sediments from Changbai Mountains Area and Their
Bearing
on Climatic Changes since 13, 500 YR.BP

39.
*********************************************************************
*****
Sixth Symposium on Mesozoic Terrestrial Ecosystems and Biota Short
Papers
In English
*********************************************************************
*****
By Ailing Sun/1995/285x210mm/250 pages/Hardcover/$67

CONTENTS
Prologue 1. Divisions of non-marine Mesozoic of China and the
paleoclimatic
implications based on paleobotanical data 2. Paleoecological
implications of
the fishes and plants from the Lower Cretaceous Dalazi Formation of
Luozigou
Basin, easter Jilin, China 3. Late Mesozoic Acipenseriforms
(Osteichthyes:
Actinopterygii) in Central Asia and their biogeographical
implications
4.
Correlation of the Early Cretaceous lacustrine beds between Kyushu
of
Japan
and southeastern China on the basis of a comparison of the fish
fossils
5.
Palaeozoic relic in Triassic tetrapod ocmmunites: the last
anthracosauian
amphibians 6. A new Late Permian vertebrate fauna from Dashankou,
Gansu
with
comments on Permain and Triassic vertebrate assemblage zones of
China
7.
Vertebrate biozonation of the Upper Beaufort Series of South Africa-
a
new
look on correlation of the Triassic biotic events in Euramerica and
southern
Gondwana 8. on the relationship between the history of Triassic
tetrapods
form eastern Europe and climate evolution 9. Late Cretaceous fossil
record
and paleobiogeography of iguanian squamates 10. Lizards: evolution,
early
radiation and biogeography ......

40.
*********************************************************************
**********
Permo-Carboniferous Biostratigraphy and Sedimentary Environment of
West
Qinling
Î÷ÇØÁëʯ̿¼Í¡¢¶þµþ¼ÍÉúÎïµØ²ã¼°³Á»ý»·¾³ In Chinese with English
summary
*********************************************************************
**********
Zeng Xuelu/1996/185x260mm/334 pages + 55 plates/Paperback/$38

Chapter 1 Introduction of regional geology Chapter 2 Description of
selected
sections Chapter 3 Lithostratigraphy Chapter 4 Biota and
biostratigraphy
Chapter 5 Discussion on boundaries between Carboniferous and Permian
Chapter
6 Sedimentary facies of selected sections and regional
palaeogeography
Chapter 7 Systematic description References; English summary and
description
of new genera and new species; Index of genera and species; Plates
and
its
explanation

41.
*****************************
The Fossil Animals Of China
In Chinese-English-Japanese
*****************************
Guan Jian/1998/280x210mm/197 ,about 550 color pictures/Hardcover/$85

In recent years, many revolutionary discoveries from China have been
adding
to and rewriting the history of evolution. Examples include evidence
of
the
bio-explosion of early Cambrian-Chengjiang fauna; new discovery of
earliest(580 million years ago bio-fauna from Guizhou) abundant
dinosaur
fossils in different areas of China; ancient birds from Liaoning;
discovery
of and research on the Miocene mammals of northwestern China; and
the
new
human fossil discoveries such as Hexian Man and Tangshan Man. These
discoveries bring illumination and hope for paleontologists during a
difficult time. This book outlines the kinds of fossil animals
discovered in
China. The latest fossil discoveries are highlighted including early
Cambrian invertebrate fossils from Chenjiang, Yunnan, Shunosaurus
fauna
from
Sichuan, late Jurassic primitive bird, and Rehe fauna from Liaoning,
late
Jurassic sauropod fauna from Yunnan, and fossil mammals from
northwestern
China. In coordination with philadelphias's Dinofest's 98 and the
exhibition
at the Lake Biwa Museum, this book supplements the materials on
display
including Lufeng prosauropod fauna from Yunnan. Miocene Mammalian
fauna
from
Ningxia and the most recent bird discoveries.

42.
*********************************************************************
*********************************************************************
**********
(Memoirs of the Institute of Vertebrate Paleontology and
Paleoanthropology
Academia Sinica No.16)Osteology and Phylogenetic Relationoship of
Rhinotitan
Mongoliensis
ÄÚÃɹÅÃɹÅÀ×Ê޵ĹÇ÷ÀÐÎ̬ºÍϵͳ·ÖÀà In Chinese with English summary
*********************************************************************
*********************************************************************
**********
By Wang Banyue/1982/185x260mm/75pages+36plates/Paperback/$20

Rhinotitan mongoliensis is member of titanothere perissodactyla, it
lived in
Asia in the late Eocene time. Their fossils have been extensively
found
in
China in the provinces of Shanxi, Henan and Nei Monggol, and are
particularly abundant in the latter region.
A team of the 1959 Sino-Soviet Paleontological Expedition excavated
an
amazingly rich collection of titanothere fossils at Ula Usu, Nei
Monggol.
The skeleton of Rhinotitan mongoliensis described in this monograph
was
one
of the most interesting and best preserved specimens in the
collection.
In the present paper the osteology and mycology of R. monogoliensisi
are
studied in detail with respect to the functional morphology. The
phylogenetic and systematic position of the genus and species and
their
relationship with American titanotheres are discussed.

43.
*********************************************************************
***********************
Memoirs of Institute of Vertebrate Palaeontology and
Paleoanthropology
Academia Sinica No.18
Öйú¿ÆÑ§Ôº¹Å¼¹×µ¶¯ÎïÓë¹ÅÈËÀàÑо¿Ëù¼¯¿¯ µÚ18ºÅ In Chinese with
English
summary
*********************************************************************
***********************
By Zhang Pei Wenzhong & Han
Defen/1987/185x260mm/193pages+27plates/Paperback/$30

This book has two papers
CONTENTS
Foreward
I. Carnivora, Proboscidea and Rodentia from Liucheng Gigantopithecus
Cave
and Other Caves in Guangxi
In the present Memoir, the author has described 28 forms of
Quaternary
fossils of the order Carnivora collected in the years 1956-1961 from
about
80 caves in Guangxi Zhuang Autonomous Region, including one cave of
Early
Pleistocene (No.5704, the Liucheng Gigantopithecus Cave), one of
Neolithic
age (No. 5619) and all others of Middle and Late Pleistocene. These
28
forms
comprise 7 families and 14 genera. Twenty of them have their
specific
names
determined, while eight are not identified. And there are also 2
forms
whose
generic names are doubtful or indeterminable.
This paper described Carnivora 7 families, 12 species, Proboscidea 3
families, 6 species and Rodentia 2 familes, 4 species.
II. Artiodactyla Fossils from Liucheng Gigantopithecus Cave in
Guangxi
The present paper deals with the Artiodactyla fossils from
Gigantopithecus
Cave in Liucheng County, Guangxi. They consist of the following taxa.
Suidae Graym, 1821
Dicoryphochoerus ultimus (sp.nov); Potamochoerus nodosarius
(sp.nov);
Susxiaozhu Han, Xu et Yi; Sus liuchengensis (sp.nov) ; Sus australis
(sp.nov) ; Sus peii (sp.nov); Suidae gen.et sp. Indet.1 ; Suidae
gen.et
sp.
Indet.2.
Tragulidae Milne-Edwards, 1864
Dorcabune liuchengense Han
Cervidae Gray, 1821
Muntiacus lacustris Teihard et Trassaert ; Cervavitus fenqii
(sp.nov) ;
Cervus (Rusa) yunnanensis Lin, Pan et Lu Bovidae Gray, 1821
Megalovis Guangxiensis (sp.nov) ; Bibos sp. Caprinae gen. et sp.
Indet.1;
Caprinae gen. et sp. Indet. 2.

44.
*********************************************************************
***********************
Memoirs of Institute of Vertebrate Palaeontology and
Paleoanthropology
Academia Sinica No.19
Öйú¿ÆÑ§Ôº¹Å¼¹×µ¶¯ÎïÓë¹ÅÈËÀàÑо¿Ëù¼¯¿¯ µÚ19ºÅ In Chinese with
English
summary
*********************************************************************
***********************
By Zhang Senshui & Hou
Lianhai/1993/185x260mm/295pages+26plates/Paperback/$40

CONTENTS
I. Comoprehensive Study on the Jinniushan Paleolithic Site----by
Zhang
Senshui et al.
Jinniushan is a small isolated hill with an elevation of 69.3m and
only
covers an area of about 0.3 square kilometers. It is situated in the
lower
course of the Liaohe River and about 20km to the east of Yinkou City
and 5km
south of Dashiqiao Town. The hill is lithologically composed of
proterozoic
dolomite-marble, sericite-marble, pinolite, binary-schist,
quartz-schist and
tremolite-schist. The rock strata were forced by strong geotectonic
movements into there presents 60o-70o dip angles. In order to get a
systematic overview of the Jinniushan site, the leader of the Yinkou
Museum,
invited the authors of this report to make a synthetic study of
these
materials and the following results have been obtained.
II. Avian Fossils of Pleistocene from Zhoukoudian------By Hou Lianhai
This paper presents the results of our investigation of a large
collection
of fossil bird materials excavated from the caves of Pleistocene of
Zhoukoudian during the field seasons of 1927-1980. Altogether 122
species
are described, including one new genus and six new species. They are
refewed
to 78 genera, 31 families, and 13 orders. On the basis of ecological
studies
and the comparisons with the other known groups of the Pleistocene
birds, we
are of the opinion that the Chinese groups of Pleistocene birds from
Zhoukoudian have close phylogenetic relationships with those of
Europe
and
have similarities with Pleistocene birds of Africa and America.

45.
*********************************************************************
***********************
Proceedings of the Seventh Annual Meeting of the Chinese Society of
Vertebrate Paleontology
µÚÆß½ìÖйú¹Å¼¹×µ¶¯ÎïѧѧÊõÄê»áÂÛÎļ¯ In Chinese with English summary
*********************************************************************
***********************
Wang Yuanqing/1999/180x260mm/274/Paperback/$32

This proceeding contains 31 papers listed as following:
1.Vertebrate Assemblages of the Jehol Biota in Western Liaoning,
China
2.Stratigraphic Sequence of the Late Mesozoic in Fuxin Basin,
Western
Liaoning, China
3.Vertebrate Assemblage of the Lower Shaximiao Formation of Sichuan
Basin,
China
4.Jurassic Stratigraphical and Paleontological Outline in Yuxi,
Yunnan,
China
5.The Early Cretaceous Vertebrate Fossils of Toba City, Mie
Prefecture,
Southwest Japan.
6.Tertiary Strata in Yuxi District, Yunnan, China
7.Biostratigraphic Study on the Bahe Formation
8.Report of Remigolepis from Upper Devonian, S. China
9.The Preliminary Study of Nasal Cavity of Ikechosaurus Sunailinae
(Reptilia, Choristodera)
10.Psittacosaur Fossils and their Stratigraphical Implications.......

46.
*********************************************************************
***********************
Proceedings of the Eighth Annual Meeting of the Chinese Society of
Vertebrate Paleontology
µÚ°Ë½ìÖйú¹Å¼¹×µ¶¯ÎïѧѧÊõÄê»áÂÛÎļ¯ In Chinese with English summary
*********************************************************************
***********************
Deng Tao/2001/260x185mm/301/Paperback/$45

This book contains following papers:
1.Postcranial skeleton of Xinpusaurus
2.Advance in the study of Mesozoic lissamphibians from China
3.The diet of prosauropods and sauropods from Lufeng, Yunnan
Province,
China
4.A forefoot of sauropod from the Tuchengzi Formation of Chaoyang
area
in
Liaoning, China
5.A preliminary report on a sauropod from the Hasandong formation (
Lower
Cretaceous), Korea
6.The first multituberculate from Japan
7.Dinosaur fossils from the Heyuan Basin in Guangdong Province, China
8.On the Upper Cretaceous Jiayin Group of Heilongjiang Province,
China
9.The Late Cretaceous dinosaur fauna and strata from Tianzhen,
Shanxi
and
Yangyuan, Hebei, China
10.The lover part of Tunggur formation and the age of its underlying
stratum
.......
30.The geological and ecological environmental characteristics in
the
source
area of the Yellow River

47.
*********************************************************************
***********************
Proceedings of the Ninth Annual Meeting of the Chinese Society of
Vertebrate
Paleontology
µÚ¾Å½ìÖйú¹Å¼¹×µ¶¯ÎïѧѧÊõÄê»áÂÛÎļ¯ In Chinese with English Abstract
*********************************************************************
***********************
Dong Wei/2004/185x260mm/307 pages/Hardcover/$35

1.Databases in paleobiology and the database building on the
Permian-Triassic fossil Vertebrates in China
2.The dinosaur mass graves found in the Wulaga Region, heilongjiang
Province
3.Biostratigraphy of the National Geopark of dinosaurs in jiayin,
heilongjiang
4.The dinosaur footprints from heyuan and the dinosaur eggs from
Huizhou in
Guangdong Province, China
5.Research status quo about the E/K boundary in Nanxiong Basin
6.Ancient diet of two species of Late Miocene Chilotherium from
Fugu,
Shaanxi, China: Evidence from stable carbon isotopes and hypsodonty
index
7.Discovery of Propotamochoerus hysudricus from Tanguanyao area in
yongren,
Yunnan Province, China
8.Review on the systematic and functional studies of saber0toothed
felids
.......
30.Paleontological resource exploration and some suggestive tips
31.Postscript

48.
*********************************************
Trace Fossils of China
ÖйúÒż£»¯Ê¯ In Chinese with English summary
*********************************************
Zhang Jianping/2004/266x192mm/353 pages+64 plates/Hardcover/$48

The first chapter, Identification, Nomenclature and Classification
of
Trace
Fossils, introduces definitions of ichnology. It covers information
on
how
to identify and distinguish trace fossils from other sedimentary
markers.
Classification of trace fossils is briefly discussed with the
emphasis
on
the Seilacher¡¯s ethological classification. It may generate
readers¡¯
interest to focus on the characters that are used as classification
criteria
for ichnogenus and ichnospecies. The second chapter, Methods and
Techniques
of Ichnology, offers current research methodology for studies of
trace
fossils, including both field methods and laboratory techniques for
fossil
and modern traces. Trace fossils from drill cores are emphasized due
to
its
practical application values in the oil industry. Dill core sections
containing trace fossils are exemplified, and their identification
criteria
are also discussed. Paleoecological application of ichnofossils is
illustrated in the chapter three. It mainly concerns with the
reconstruction
of paleoenvironments using trace fossils. Identification of ancient
environmental factors, such as water depth, salinity, oxygen, water
energy
and substrate are discussed. The usage of trace fossils in
recognizing
geological events and in distinguishing marine, non-marine and
transitional
facies is the main coverage for this chapter. Ichnofabric and
bioturbation
in drill cores and applications of ichnofossils to sequence
stratigraphy is
also covered. The fourth chapter discusses ichnocoenoses and their
paleoenvironmental significance in China, focusing on ichnocoenoses
that
have been reported from China.
Chapter1 Identification, Nomenclature, and Classification of Trace
Fossils
Chapter2 Methods and Techniques of Ichnology
Chapter3 Application of Ichnofossils to Paleoenvironments and
Paleoecology
Chapter4 Ichnocoenoses and Their Sedimentary Environments in China
Chapter5 Systematic Description of Chinese Trace Fossils

49.
*****************************************************************
The Chinese Fossil Proboscidea (Used) (Zhongguo de Xiang Huashi)
ÖйúµÄÏó»¯Ê¯ In Chinese
*****************************************************************
By Zhou Mingzhen & Zhang
Yuping/1974/185x260mm/74pages+32plates/Hardcover/$29

This book systematical describes the Chinese Fossil Proboscidea 16
genera,
59 species, with index tables and plates

50.
****************************************************************
Researches of Ailuropoda¡ªStegodon Fauna from Gulin China
Öйú¹ÅÝþ´óÐÜèһ½£³ÝÏó¶¯ÎïȺÑо¿ In Chinese with English summary
****************************************************************
By Yang Xinglong & Yang Daihuai/1995/140x200mm/73pages/Paperback/$8

The findings collected from Yiemao Cave contain 1 kind of spiral
shell(an
invertebrate), 38 kinds of mammals, 9 teeth of humanity and 3
spieces
of
potsherd, of which Ailuropoda melanolenca baconi, Stegodon
orientalis,
Megatapirus augustus, Rhinoceros sinensis, Sus cf xiaozhu and so on
become
extinct and most of them are living species. The fauna is
characterized
by
clear late Pleistocene through a study on it. As some humanity¡¯s
teeth
of
the Neolithic period and potsherd with a rope pattern are unearthed
from the
fossiliferous horizon it is considered that the Gulin fauna is not
the
late
Pleistocene, but the Holocene in age. Through an anlysis of
sporopollenin
and based on 14C dating, its absolute period is eventually dated the
Holocene of 13 800 ¡À560aB.P.. The present paper is testified that
the
Gulin
fauna has the charater of transition from the Ailuropoda¡ªStegodon
Fauna of
late Pleistocene to modern fauna and the extinct time of
Ailuropoda¡ªStegodon dates back to the Holocene. The discovery of
Gulin
fauna has an important Significance in studying on the animals¡¯s
evolution,
in differentiating the geological age of the Quaternary period, in
making a
comparison between strata and in variations of the paleoclimate and
the
paleongeography.

51.
*********************************************************************
**************************
Taphonomy of Longjiagou Hipparionine Fauna (Turolian,Miocene) Wudu
County,Gansu Province,China
¸ÊËàÎä¶¼Áú¼Ò¹µÈýÖºÂí¶¯ÎïȺÂñ²ØÑ§ In Chinese with English summary
*********************************************************************
**************************
Zhang Yunxiang/1994/185x260mm/96 pages+8 plates/Paperback/$18

The materials studied in this paper were collected fifty years ago
by
Prof.
Wang Yongyan near Longjiagou, Wudu County, Gansu Province. According
to
the
dressing of fossils at present. there are 4537 specimen in total, in
which
2292 specimen can be classified, 640 specimen can' t be classified
but
identified into the parts of the animals and1605 specimen are
fragment
bone
unidentified.

52.
**********************************************************
Chinese Fossil Horses of Equus and Their Environment
ÖйúµÄÕæÂí»¯Ê¯¼°ÆäÉú»î»·¾³ In Chinese with English summary
**********************************************************
Deng Tao & Xue Xiangxu/1999/180x260mm/158 pages+ 20
plates/Hardcover/$38

The materials studied in this book come mainly from the Early
Pleistocene
Bajiazui fauna in Qingyang County and the Late Pleistocene Loufangzi
fauna
in Huanxian County, Gansu Province, and partially from other
localities. By
way of the research to the Chinese fossils of the genus Equus, some
new
conclusions on the taxonomy, evolution, biostratigraphy,
paleoclimatology,
chronology and so on about the genus Equus are achieved, which gets
better
knowledge of the Chinese fossils of the genus Equus and develops
applications of mammal fossils on climatic changes. The review and
revision
to the Chinese fossils of the genus Equus have important theoretic
significance. The exploration and discussion of climatic changes on
the
basis of the genus Equus have effective practical value.

53.
*********************************************************************
*************************************************
Reports of Paleonotogical Expedition to Sinkiang(IV)- Mesozoic
Vertebrate
Fossil Stratigraphy in the Northern Xinjiang
н®±±²¿ÖÐÉú´ú¼¹×µ¶¯ÎﻯʯµØ²ã In Chinese
*********************************************************************
**************************************************
By Zhao Xijin/1980/187x259mm/120 pp. +5plates/Paperback/$22

54.
*********************************************************************
*******************************************
Reports of Paleontological Expedition to Sinkiang (III) Permian And
Triassic
Vertebrate Fossils Of Dzungaria Basin And Tertiary Stratigraphy And
Mammalian Fossils Of Turfan Basin
×¼¸Á¶ûÅèµØÄÏÔµ¶þµþ¡¢Èýµþ¼Í¼¹×µ¶¯Îﻯʯ¼°
ͳ·¬ÅèµØµÚÈý¼ÍµØ²ãºÍ²¸ÈéÀ໯ʯ
In
Chinese
*********************************************************************
*******************************************
1978/187x259mm/132 pages+32 plates/Paperback/$28

1. Permian And Triassic Vertebrate Fossils Of Dzungaria Basin
(1) The Upper Permian fish-fauna of Dzungaria Basin, Sinkiang (2)
Two
New
Genera of Dicynodontidae (3) A complete skeleton of Chasmatosaurus
yuani
from Sinkiang (4) On occurrence of Parakannemeyeria in Sinkiang (5)
A
new
Triassic palaeoniscoid fish from Fukang, Sinkiang (6) A Late
Triassic
vertebrate fauna from Fukang, Sinkiang
2. Tertiary Stratigraphy And Mammalian Fossils Of Turfan Basin
(1) Stratigraphy of the Mammal-bearing Tertiary of the Turfan Basin,
Sinkiang (2) Late Paleocene Mammals of the Turfan Basin, Sinkiang
(3)
Two
new Early Eocene Mammals from Sinkiang with Remarks on the age of
Gashato
Formation (4) More Fossil evidences favouring on Early Eocene
connection
between Asia and Neoarctic (5) Description of some Late Eocene
Mammals
from
Lian-kan Formation of Turfan Basin, Sinkiang (6) Late Oligocene
Mammals
from
the Taoshuyuanzi Formation of Eastern Turfan Basin (7) New Materials
of
Giant Rhinoceros

55.
**************************************************
Ordovician Conodonts of Henan Province, China
ºÓÄÏÊ¡°ÂÌÕ¼ÍÑÀÐÎʯ In Chinese with English summary
**************************************************
Pei Fang/1987/185x260mm/128 pages + 14 plates/Hardcover/$18

The conodonts described and illustrated herein are belonged to 96
species
and subspecies within 37 genera, among them 1 genus and 20 species
and
subspecies are new.

56.
********************************************************
Paleozoic Stratigraphy and Conodonts In Xinjiang
н®¹ÅÉú´úµØ²ã¼°ÑÀÐÎʯ In Chinese with English summary
********************************************************
Zhao Zhixin/2000/213x285mm/340 pages+81plates/Paperback/$55

Palaeozoic strata in Xinjiang are an important field at oil and gas
exploration. Paleozoic strata and conodonts in this area have been
throughly
studied. A great number of fossils, such as conodonts, graptolites,
corals,
foraminifers, chitinozoans, spore and pollens, trilobites and
brachiopods
were collected from this area. About 40700 (approximately)
identifiable
conodont elements were recovered from 23 outcrop sequences and 73
subsurface
sequences in Xinjiang. 43 conodont Zones have been discussed and 238
species
have been described, including 4 new species, 1 gen, et sp. Nov.
This
monograph describes conodonts were extracted principally from
subsurface
section in Tarim Basin.

57.
*********************************************************************
**
The Conodonts of the Marginal Areas around the Ordos Basin, North
China
¶õ¶û¶à˹ÅèµØÖÜÔµµÄÑÀÐÎʯ In Chinese with English summary
*********************************************************************
**
An taiyang/1990/185x260mm/201 pages + 17 plates/Paperback/$45

The research work of this book was carried out from 1984 to 1988.
Totally 41
sectins in 18 different areas around the Ordos Basin were measured
as
shown
in Text-fig. 1 (in Chinese), including 3 Cabrian sections, 28
Ordovician
sections, 2 Silurian sections and 8 Carboniferous sections.
Altogether
2500
conodont samples were processed, and th recovery of them is about
one
third.
In terms of quantity, the Ordovician conodonts are most numerous, th
Carbonifrous conodonts are secondary in abundance, there are only a
few
Cambrian and Silurian conodonts.

58.
**********************************
Fossil and Recent Turtles of China
In English
*********************************
Ye Xianrui/1999/140x203mm/112/Hardcover/$38

China possesses abundant turtles both fossil and extant. It has a
fossil
record ranging continuously from early Jurassic to Quaternary, and
the
living ones are also flourishing. The present monograph describes
systematically all the species of this animal group known in China
before
1991. It offered not only the diagnosis, locality and horizon of
every
species, but also the related biogeography, evolution , comment,
even
revision etc. in some cases. We believe that the data presented will
serve
as valuable references in study of turtles domestically and abroad.

59.
*****************************************************************
New Galeaspids (Agnatha) From the Silurian and Devonian of China
In English
*****************************************************************
Pan Jiang/1992/185x260mm/77 pages+7 plates, 35 figs/Hardcover/$45

Chapter 1. Introduction Chapter 2. Historical remarks on the
agnathans
of
china Chapter 3. Localities and Stratigraphical Range Chapter 4.
Morphology
of the Galeaspida Chapter 5. Internal Anatomy of Galeaspids Chapter
6.
Systematic Revision Chapter 7. Description of the New Taxa;
References;
Appendix 1 Abbreviations of Galeaspids used in this volume
(morphology)
Appendix 2 Index of main place names of Silurian and Devonian
vertebrates in
China Appendix 3 Index of Chinese author's names used in this volume
Appendix 4 Index of Silurian and Devonian formations of China used
in
this
volume

60.
*********************************************************************
*******
Late Mesozoic Fossil Fishes from the Jiuquan Basin of Gansu
Province,China
¸ÊËà¾ÆÈªÅèµØÓ㻯ʯ¼°³Á»ý»·¾³ In Chinese with English summary
*********************************************************************
*******
Ma Fengzhen/1993/103 pages+18 plates/Hardcover/$17

61.
********************************************
The Pseudosuchians in China
In Chinese and English bilingual
********************************************
Chung-Chien Young/1964/225x300mm/205 pages, 64 figures, 10
plates/Paperback/$65

The present paper deals with the systematic study of the
pseudosuchians
from
Wuhsiang, Yueshe, Ningwu, Chinglo and Shinghsien, collected by the
members
of the Institute of Veterbrete Palaeoanthropology during the years
1955,
1956, 1959 and 1960. Three genera and four species of pseudosuchians
are
described, attributing to three super-families of this sub-order.
Shansisuchus shansisuchus is richly represented, forming the main
bulk
of
the whole material. On account of the presence of two preorbital
openings,
so different from all other known pseudosuchians, it is suggested to
erect a
new family for it.
A small species probably of the same genus is described as
Shansisuchus
heiyuekouensis. The third form is a large pseudosuchian with the
lateral
side of the dorsal vertebrate crested and covered scutes. It is
described as
Fenhosuchus cristatus. It belongs to the super-family
chirotherioidea.
The
fourth form is a small pseudosuchian, also with scutes, belonging to
the
super-family Ornithosuchoidea Wangisuchus tzeyii.

62.
*****************************************************
Quaternary Rodents of Sichuan-Guizhou Area, China
´¨Ç­µØÇøµÚËļÍÄö³ÝÀà In Chinese with English summary
*****************************************************
Zheng Shaohua/1993/185x260mm/270/Hardcover/$38

1.Sciuridae Gray, 1821; 2.Cricetidae Rochebrune, 1883, 3.Cricetinae
Murray,
1866, 4.Arvicolidae Gray, 1821, 5.Platacanthomyidae Miller et
Gidley,
1918;
6.Rhizomyidae Miller et Gidley,1918; 7.Hystricidae Burnett, 1830;
8.Muridae
Gray, 1821;

63.
********************************************************************
Cenozoic Mammals and Environment of Hengduan Moutains Region
ºá¶ÏɽµØÇøÐÂÉú´ú²¸È鶯Îï¼°ÆäÉú»î»·¾³ In Chinese with English summary
********************************************************************
Zong Guanfu/1996/185x260mm/242 pages +35 plates/Hardcover/$35

In this book, the Cenozoic mammalian fossils of the area under study
include
106 species belonging to 63 genera of the 10 orders. There are
thirteen
new
species among these. Some Human remains of later age were also found
in
certain sites. Narration of the species included the scientific
name(with
the author and date), the type(be collected from the region), the
locality
and horizon(age), the description and discussion. We have endeavored
to
group the species by their morphogenesis, affinities as well as
chronologically and according to evolutionary lineage, where such
are
recognized.
Ten orders described: Lagomorpha Brandt, 1885; Rodentia Bowdich,
1821;
Creodonta Cope, 1875; Condylarthra Cope 1881; Carnivora Bowdich,
1821;
Hyracoidea Huxley, 1869; Proboscidea Illiger, 1811; Perissodactyla
Owen,
1848; Artiodactyla Owen, 1848; Primates Linnaeus, 1758.

64.
*************************************************************
Middle Miocene Micromammalian Fauna From Tunggur, Nei Mongol
In Chinese with English summary
*************************************************************
Qiu Zhuding/1996/185x260mm/216pages+6plates , 74 figures/Hardcover/
$40

Tunggur is a Miocene mammalian fossil locality, located about 70 Km
east of
Erlian. It was discovered in 1928 by the Third Central Asiatic
Expedition
organized by the American Museum of Natural History. And an
intensive
excavation was carried out later in 1930. An expedition organized by
Institute of Vertebrate Paleontology and Paleoanthropology, Academia
Sinica
in 1986. Detailed descriptions of the collected small mammals with
discussion of the Tunggur fauna are given in this paper. Families
described:
Erinaceidae, Talpidae, Talpinae, Incertae Subfamiliae,Soricidae,
Soricinae,
Incertae Familiae, Aplodontidae, Sciurinae, Castoridae, Eomyidae,
Gliridae,
Zapodidae, Dipodidae, Cricetidae, Gobicricetodontinae subfam.,
Cricetodontinae, Cricetinae, Ochotonidae

65.
*********************************************************************
**************************************************
Middle Eocene Small Mammals from Liguanqiao Basin of Henan Province
and
Yuanqu Basin of Shanxi Province, Central China
In Chinese with English summary
*********************************************************************
**************************************************
Tong Yongsheng/1997/185x260mm/256 pages, 12 plates, 70 figures+ 38
tables/Hardcover/$42

The Liguanqiao basin is about 600 km2. The small mammals are found
in
thin
gray carbonaceous mudstones. The Yuanqu basin is a small
intermountane
sink
in the Zhongtiao range, conrtaining Eocene sediments more than 1,000
m
thick. Since 1986, more than thousand samples have been collected in
the
Middle Eocene of the Liguanqiao and Yuanqu basins, central China,
representing 67 taxa of Insectivora, Chiroptera, primates,
Lagomorpha,
rodentia and proteutheria. An outline of micromammalian faunas in
the
later
Eocene of China is included in this report.

66.
********************************************************************
Before Dinosaurs - Land Vertebrates of China 2000 Million Years Ago
In English
********************************************************************
Ailing Sun/1988/250x250mm/113, 113photos, 17 diags color
illustrated/Hardcover/$58

CONTENTS
Preface History of Studies; Geographical distribution; Late Permian;
Early
Triassic; Early to Middle Triassic; Middle Triassic; Upper Triassic;
Early
Jurassic; Stratigraphic Correlation of Bone-Beds in China; Index;
Acknowledgements

67.
******************************************************
The Dinosaur eggs fossils in Nanyang, China
ÖйúÄÏÑô¿ÖÁúµ° In In Chinese and English illustration
******************************************************
By Zhou Shiquan/2005/215x305mm/100pages+40plates/Hardcover/$65

Contents
1 Survey 2 Retrospection and evolvement of research on dinosaur eggs
fossils
3 The distributing and stratum of dinosaur eggs fossils 4 Structural
of
basin with dinosaur eggs and its evolving characteristic 5
Classification of
dinosaur eggs fossils and their composition 6 Ancient ecological
characteristic of dinosaur eggs fossils 7 Meaning of combination
types
of
dinosaur eggs fossils and other strata periods 8 Division of Chalk¡¯
s
boundary 9 Ancient climate in late Cretaceous 10 Extinction of
dinosaur
pack
and boundaries and events 11 Protection of dinosaur eggs fossils;
Picture
Information and Plate; Illuminate; Postscript; Main References

68.
******************************************************
Annals of the Dinosaur Fossils from Zigong
×Ô¹±¿ÖÁú»¯Ê¯Ö¾ In Chinese and English introduction
******************************************************
By Guo Yunlin/1993/130x185mm/219 pages + 64 plates/Hardcover/$18

The dinosaur fossils from Zigong are well known in the world by the
numerous
quantity, various categories, beautiful preservation and dense
accumulation.
To exploit and utilize fully the dinosaur fossil resources of Zigong
is
of
significance for the development of the paleontology of our country
and
the
economic development of Zigong. The publication of ¡°annals of the
Dinosaur
Fossils from Zigong¡± is doubtless conducive to pushing the
exploitation and
utilization of the dinosaur fossils forward.
¡°Annals of the Dinosaur Fossils from Zigong¡± is characterized by
clear
ideas and proper style, real details and objective description. This
book,
supplements with pictures, tables and appendices, described all-
sidedly
the
geographical distribution of the dinosaur fossils and the history
and
current situation of the collections, preparations and studies. It
is a
special annals with much more details, science and knowledge. It is
of
certain referential value to the paleontologists and museologists.
It
is
also of certain benefit for paleontological amateurs and people with
lofty
ideals on the exploitation and utilization of the dinosaur fossils.

69.
*********************
Dinosaur of Sichuan
ËÄ´¨¿ÖÁú In Chinese
*********************
By Zhou Shiwu/1996/130x185mm/89 pages +6 color photo/Hardcover/$18

70.
*********************************************************************
******************
Geologic Tripping Guidebook to Zigong Dinosaur and the Karst
landscape
in
South Sichuan
×Ô¹±¿ÖÁúºÍ´¨ÄÏÑÒÈܵØÖÊ¿¼²ìÖ¸ÄÏ In Chinese and English bilingual
*********************************************************************
******************
By Chen Maoxun/1991/140x210mm/8 pages + 8 plates/Paperback/$15

This book has introduced the geologic investigation route for the
30th
International Geology Conference which will be hele in China.South
Sichuan,an important geologic scenic area in Sichuan
Province,includes
a
group of caves of dinosaur fossils in Zigong which has extremely
high
investigation value, and the grand karst landscape and a number of
worthwhile natural or artificial scenery as well.
The planned route starts from Chengdu ,through Zigong,Yibin ,Junlian
,Gongxian,Xingwen,Changning and other cities or counties ,and
returns
to
Chengdu.The main investigative contents are the dinosaur fossils of
Dashanpu
(Zigong),the history of ancient salt industry development and the
karst
landform at Junlian and Xingwen .In addition ,the planned scenic
spots
include Zigong City ,Yibin City ,the Hanging Coffins of the Bo
Nationality
in Gongxian,the ¡°Immense Bamboo Forest¡±in southern Sichuan ,etc.
This book has introduced the development and study history ,the
formation
,the geologic and physiographic survey and characteristics of the
above-mentioned landscapes ,and has given in detail the
investigative
route
,time ,board and lodging places .This Chinese -English bilingual
guidebook
is easy to understand with excellent pictures and
compositions.Therefore,it
is suitable not only for geologists from home and aboard ,but also
for
geoscience amateurs ,and universities or high school students

71.
***************************************************
Dinosaur Footprints from Mesozoic of Sichuan Basin
ËÄ´¨ÅèµØ¿ÖÁú×ãÓ¡»¯Ê¯ In Chinese
***************************************************
Yang Xinglong and Yang Daihuan/1987/Hardcover/$22

This paper describs about 200 dinosaur footprint fossils discovered
from
upper triassic strata at the 7 sites in sichuan basin ,sets up 9 new
genus
and 11 new species on the other hand we makes a investigation about
the
lift
habit the way of motions and the body structures of the dinosaur
etc.moreover we also brifly introduce the history of the study of
dinosaur
footprints in China ,the process of the discovery of the footprint
in
sichuan basin from 1981-1986 and stratigraphical distribution of
dinosaur
footprint fossils of the mesozic era

72.
*********************************************************************
********************
A New Complete OS-Teology of Prosaurpoda In Lufeng basin Yunnon
China
---Jingshanosanrus
Öйú»·áÅèµØÒ»ÐµÄÍêÕûÔ­òá½ÅÀà¿ÖÁú»¯Ê¯½ðɽÁú In Chinese with English
summary
*********************************************************************
********************
Zhuang Yihong and Yang Zhaolong/1995/185x260mm/100pages/Hardcover/$28

Since the past half a century ,the paleontologists and geologists
around the
world have been paying their great attention to the well¡ªknown
Lufeng
Basin
..The Lufeng Sauris china fauna was discovered by late professor
Bian
Meiliang ,a famous Chinese geologist,in 1938.Praofessor Bian and
professor
Yang Zhongjian ,a late leading paleontotogidt of China ,did a lot of
excavations during the period of 1938 and 1939 and made a further
research
to Lufeng Red Strata and the fossils collected from the Lufeng
Basin.Both of
them published so many papers and monographs in home and
abroad .Since
1949
,the institute of Vertebrate Paleontology and Paleoanthropology of
Academia
Sinica,the Gelological Museum of China,Beijing Natural History
Museum
etc.and many ferign exports used to do a lot of fieldworks and
collected a
large numbers of fossils from the basin.After that,they achived
mumorous new
scientifical researches ,and so far ,33 speices and 23 genura were
established in the Lufeng Saurischian fauna,which was listed more
than
9
species and 6 genura of dinosaurs.From the data mentioned above ,the
Lufeng
Saurichian fauna is one of the most types and complete paleovertebra
faunae
in the world

73.
*******************
Lufeng Dinosaur
»·á¿ÖÁú In Chinese
*******************
Dong Zhiming/2003/63/Hardcover/$12

74.
*********************************************************************
***
Dinosaurs from China
Öйú¿ÖÁú(Zhongguo Konglong) In text in Chinese with a summary in
English
*********************************************************************
***
Zhen, Shuonan/1997/5.7 x 8.2/297 pp.10 color
illustrations/Hardcover/$18

China is one of a few countries with the largest deposits of
dinosaur
remains. This volume introduces the reader to many of the rare
species
found
in China.

75.
************************
Dinosaurs from China
Öйú¿ÖÁú In English
************************
Dong Zhiming/1988/260x260mm/114/Hardcover/$45

Dinosaurs from China introduces the history of dinosaur tudies in
the
country, then chronicles, in geological sequence and by geographical
area,
all the discoveries made by Chinese dinosaur workers including the
animals
that were cntemporaries of these reptiles in the Mesozoic Era. The
geological localities and formations containing dinosaur fossils are
illustrated in detail.
This is the most comprehensive and best illustrated book about
Chinese
dinosaurs that has ever been published. Many of the 180 photographs
and
lifelike reconstructions are published here for the first time, and
the
book
will appeal to geologists, palaeontologists, biologists and indeed
anyone
interested in the history and evolution of these fascinating animals.

76.
*****************************************************
Oviraptorid Dinosaurs from Southern China
ÖйúÄÏ·½ÇÔµ°ÁúÀ໯ʯ In Chinese and English bilingual
*****************************************************
Lu Junchang/2005/185x260mm/200 pages + 8 plates/Paperback/$28

Heyuannia huangi Lu, 2003 from the Late Cretaceous of Southern China
is
described in detail. The revised diagnosis of Heyuannia huangi
includes
the
following characters: quadratojugal articular surface of the
quadrate
groove-lke, the quadrate diverticulum entering the quadrate
anterolaterally,
metacarpal I wrapped around metacarpal II proximally, pneumatic
foramina
present on the neural arches and ribs of cervical vertebrae, the
angle
between the scapula and coracoid approximately 145o, the ratio of
coracoid
length to scapular length approximately 0.35, the pubis as long as
ischium,
and the ratio of femur length to tibia length 0.8. Two new
oviraptorids
from
the nanxiong Basin are also described. A phylogenetic analysis was
carried
out in two parts. The first phylogenetic analysis is to test the
systematic
position of Oviraptorosauria among ceolurosaurid dinosaurs. This
analysis
shows that Oviraptorosauria form a monophyletic group.
Incisivosaurus
gauthieri is the most basal oviraptorosaur and Caudipteryx is the
second
most primitive form. Alvarezsauridae is a sister group to TO
(Therizinosauroidea and oviraptorosauria). Within this more
inclusive
analysis (among Ceolurosauria), all the derived forms of
Oviraptorosauria
(excluding the Primitive forms such as Incisivosaurus gauthieri and
Caudipteryx zoui) form an unresolved polytomy. The second analysis
is
to
determine the interrelation-ships among oviraptorosaurs. This less
inclusive
analysis (only a few groups of Ceolurosauria were employed for
analysis)
allows better resolution within Oviraptorosauria. The analysis shows
that
all oviraptorosaurs form a monophyletic group, Incisivosaurus
gauthieri
is
the most basal oviraptotosaur, Caudipteryx zoui is the second most
primitive
form and Avimimus portentosus is basal to the derived
oviraptorosaurs.
The
two new taxa from Nanxiong Basin are not nested within same
clade.Specimen
BPV-112 may be the first caenagnathid oviraptorosaur found from
southern
China.

77.
******************************
The Dinosaur fossils of Gansu
¸ÊËà¿ÖÁú In Chinese
******************************
Zhang Xing/2002/140x210mm/184/Paperback/$35

78.
*********************************************************************
***************************************************
The Characteristics of the Composition of the Trace Elements in
Jurassic
Dinosaur Bones and Red Beds in Sichuan Basin
ËÄ´¨ÅèµØÙªÂ޼ͿÖÁú¹Ç÷À¼°ºì²ãµÄ΢Á¿ÔªËØ×éºÏÌØÕ÷ In Chinese with
English
summary
*********************************************************************
***************************************************
Li Kui/1999/180x260mm/155/Hardcover/$25

In general, this rearch made a great deal of work for systematically
providing the composition features of trace elements of fossils of
Jurassic
dinosaur bones and Jurassic Red Beds: nearly 100 spots of dinosaur
fossils
were surveyed; 3 Jurassic sections were tested and drawn; 80 fossil
samples
of dinosaur bones, other plants and modern animals were collected;
as
well
as 80rocks samples in the Jurassic Red Beds, in which 150 samples
were
studied with INAA, and 20 polished section were observed through
micro
photos and pictures of SEM. To probe the evolution of Jarassic
dinosaurs and
several dinosaur faunas in the Basin with their biogeochemic
environment, we
try to reveal the mystery that why dinosaurs died in groups and how
they
became extinct with our new materia ls and method. dinosaurs died in
groups
and how they became extinct with our new materials and method.

79.
**************************************************************
On the Cretaceous Fossil Eggs of Xixia County, Henan Province
ºÓÄÏÎ÷Ï¿°×ÛѼ͵°»¯Ê¯ In Chinese with English summary
**************************************************************
Fang Xiasi et al/1998/185x260mm/125 pages+21plates/Paperback/$28

1. Introduction
2. Brief review on the study of the Cretaceous in Xixia
3. Regional geology and stratigraphy of Xixia (1) Sangping-Xiaguan
Basin (2)
Xiping-Chimei basin
4. Description of some major sections (1) Huangsha section, Sangping
basin,
Xixia County (2) Sections in Xiping-Chimei basin
5. Discussion on the Late Cretaceous stratigraphy and
palaeoenvironment
of
Xiping-Chimei and Sangping basins (1) upper Cretaceous lithofacies
and
palaeogeographical characteristics of Xixia (2) Discussion on
stratigraphy
6. Fossils (1) Introduction to fossil eggs (2) Fossil Description
7. Biochemical, genetical and mineralogical researches on the
flocculent
content of the fossils egg (XL-01) (1) The DNA isolation and
sequencing
in
fossil egg (XL-01) (2) The research on the morphology, composition
and
structure of the minerals from the egg (3) The distribution of trace
elements in eggshell
8. Explanation of the plate and Plates

80.
*********************************************************************
**********
The Middle Jurassic Dinosaur Fauna from Dashanpu, Zigong, Sichua(5
volume
set)
In Chinese with English summary
*********************************************************************
**********
1984/180x260mm/Paperback/$100

Volume I: "The Ornithopod Dinosaurs.Äñ½ÅÀà¿ÖÁú
Contents
Part 1 Yandusaurus multidens He et Cai, 1983
1. Classification 2. Description of specimen 3. On the size,
individual
variation and immature specimens of Yandusaurus multidens 4. The
skeletion
reconstruction of Yandusaurus multidens
Part 2 On the desctiption and comparison of Yandusaurus hongheensis
1.
Description of specimen 2. The comparison between Yandusaurus
multidens
and
Y. hongheensis
Part 3 Discussion on Yandusaurus 1. The relationships between
Yandusaurus
and other ornithopodous dinosaurs of Sichuan district 2. The
systematic
position of Yandusaurus and the relationships between which and
other
allied
genera and species

Volume II: Stegosaurs ½£Áú
Volume III: "Sauropod dinosaur (I). Shunosaurus." òá½ÅÀࣨһ£©ÊñÁú
Contents 1. Osteology of Shunosaurus 2. Protognathus oxyodon, gen.
Et.
Sp.nov 3. Discussion 4. References 5. Abstract 6. Explanation of
plates
7.
Acknowlegements 8. Plates I-XV

Volume IV: Sauropod Dinosaurs (2): Omeisaurus tianfuensis
òá½ÅÀࣨ¶þ£©Ì츮¶ëüÁú English abstract
Contents 1. Introduction 2. Descriptions 3. Restoration of the
skeleton
4.
Taphonomic features and Palaeoecology 5. Appendix: Descriptions on a
new
Omeisaurus species (O. luoguanensis Li) 6. Explanation of
abbreviations
used
in text figures and plates 7. References 8. Abstract (in English) 9.
Explanation of plates 10. Plates I-XX

Volume V: The burial environment of dinosaurs and characteristics of
lithofacies and paleogeography ¿ÖÁúÂñ²Ø»·¾³¼°ÑÒÏà¹ÅµØÀíÌØÕ÷
Contents 1. Stratigraphic division and fossil features 2. The
petrological
features of regional sedimentary rocks 3. The features of regional
sedimentary facies and paleogeography 4. The burial environment of
dinosaur
fauna in Xiashaximiao formation from Dashanpu, Zigong 5. The burial
environment of dinosaur fauna in Xiashaximiao formation from
Dashanpu,
Zigong 6. Conclusion 7. Appendix I The composition and fabric of
dinosaur
bones 8. Appendix II Initial study of taphonomy of Jurassic dinosaur
fossils, Sichuan Basin 9. References 10.Abstract 11.Plates and
explanation

81.
*************************
Mamenchisaurus Hechuan
ºÏ´¨ÂíÃÅϪÁú In Chinese
*************************
Yang Zhongjian/1972/185x260mm/30 pages +15 plates/Hardcover/$25

82.
*********************************************************************
*******
The First Mamenchisaurian Skeleton with Complete Skull
Mamenchisaurus
Youngi
µÚÒ»¾ß±£´æÍêÕûÍ·¹ÇµÄÂíÃÅϪÁú-ÑîÊÏÂíÃÅϪÁú In Chinese with English
summary
*********************************************************************
*******
Ouyang Hui and Ye Yong/2002/110pp+20 plates/Hardcover/$25

Since British paleontologist Richard Owen first described
Cetiosaurus
in
1841, a loarge a mount of sauropod materials have been excavated on
all
continents except the Antarctic. At least 100 genera and 170 species
of
the
sauropods have been identified to date, of which, about one-sixth
are
distributed in China.

83.
*********************************************************************
************
A complete Carnosau Skeleton From Zigong, Sichuan- Yangchuanosaurus
Hepingensis
ËÄ´¨×Ô¹±Ò»ÍêÕûÈâʳÁú»¯Ê¯-ºÍƽÓÀ´¨Áú In Chinese with English summary
*********************************************************************
************
Gao Yuhui/1999/185x260mm/80pp+33figures, 16 tables and
20plates/Paperback/$25

1. Introduction 2. Description 3. Discussion on megalosauridae 4.
The
Positions of Yangchuanosaurus in carnosaur relationships 5. Function
of
Yangchuanosaurus hepingensis anatomy 6. References 7. Abstract (in
English)
8. Explanation of plates 9. Plate I-XX

84.
******************
Keichousaurus
¹óÖÝÁú In Chinese
******************
Zhao Xijin and Xu Xing/1999/210x290mm/61/Hardcover/$28

The first Triassic marine reptile specimen was collected by Chengzhi
Hu
In
1956 at a site in Xingyi, Guizhou. In the following decades,
thousands
of
marine reptile specimens were collected at this site and a few other
sites
in the neighbouring areas as well. To date, altogether there have
been
3
orders, 5 families, 11 genera, and 13 species identified and
established,
including Chinchenia sungi Young, Sanchiaosaurus dengi Young,
Keichousaurus
hui Young, Keichousaurus yuananensis Young, Shingyisaurus unexpectus
Young,
Kwangsisaurus orientalis Young, Nanchangosaurus suni Wang,
Himalayasaurus
tibetensis Dong, Tibetosaurus tingjiensis Young et al, Mixosaurus
maoteiensis Young, Chaohusaurus geishanensis, Hupehsuchus
nanchangensis
young, and Hanosaurus hupehensis Young.

85.
********************************************
Shantungosaurus Giganteus
¾ÞÐÍɽ¶«Áú In Chinese and English bilingual
********************************************
Hu Chengzhi/1999/185x260mm/139 pages +18 plates/Hardcover/$35

In August 1964, a comprehensive research party of the Bureau of
Petroleum
Geology, Ministry of Geology discovered a new fossiliferous site and
collected some fossil remains from the Cretaceous beds in Zhucheng
County,
Shandong Province. These fossils include tibia bone of a fairly
large-sized
hadrosaur. Later excavations were made at the same site in 1964,
1965,
1966
and 1968 by the Institute of Geolgoy and the Museum of Geology, as a
result
of which a large quantity about thirty tons of dinosaurian bones
were
collected. The fossils were found in a layer of greyish green
conglomeratic
sandstone, belonging to the Wangshi.Group of late Cretaceous age.
The
site
lies at the end of a gully named Longgujian which is about on
kilometer
north of Kugou village in the district of Lubiao, Zhucheng County.
All
fossils were excavated from the single quarry, which the bones had
been
disarticulated during deposition. Among the collections there are
about
ten
more or less preserved maxillae, five right and five left ones,
which
represent at least five individuals of hadrosaurians in the quarry.
After
the preparation of dinosaurian bones a omposite skeleton was mounted
up, and
displayed in the Palaeontological Hall of the Beijing Museum of
Natural
History from April 1972 to October 1982. The mounted skeleteon is
about
1470cm in length. As some of the fossil remains were somewhat
obscured
after
the mounting of the skeleton and the time for their study was
limited,
only
a preliminary research was made. A new generic and specific name
Shantungosaurus giganteus was proposed in the paper published 1973.
The
composite skeleton is preserved in trhe National Geological Museum
of
China
and designated by Catalogue number V 1780. The type of the skull is
rather
long, low, and narrow in front but high and broad posteriorly. The
absent
parts of the skull have been restored and the skeleton mounted up
once
again. The restored skull is 1630mm in length. The most important
osteological features of the species are briefly given below. The
skull
is
tolerably preserved from the plane of the exoccipital to the
anterior
end of
frontals. The postorbital is well preserved of the right side, but
it
is
damaged on the left side. The skull is 620mm in length, 465mm in
breadth of
posterior part and 325mm in height. On its superior surface, there
is a
low
depression extending toward the anterior end of frontals. The
frontal
bone
has the shape of a shallow dish. The supratemporal fossa is
anterior-posteriorly elongated. The exoccipital is roughened on the
surface.
The sutures around the squamosal and parietals are clearly visible.
There is
a perfect process of parietal on the right side, but the left one
has
been
broken away from the beam. A tubercle-like element of interparietal
is
prominent and lies at the posterior end of the frontals which is
nearly
rectangular and constricted at the lateral margins. Its outline
though
obscured in the rear is clearly visible.

86.
*********************
Rise of the Dragon
ÌÚ·ÉÖ®Áú In Chinese
*********************
Edited by Readings from Nature on the Chinese Fossil
Record/2001/185x260mm/130pages+30 halftones/Paperback/$20

Over the past decade, fossil finds from China have stunned the
world,
grabbing headlines and changing perceptions with a wealth of new
discoveries. Many of these finds were first announced to English
speakers in
the journal Nature. Rise of the Dragon gathers together sixteen of
these
original reports, some augmented with commentaries originally
published
in
Nature's "News and Views" section. Perhaps the best known of these
new
Chinese fossils are the famous feathered dinosaurs from Liaoning
Province,
which may help end one of the most intense debates in
paleontology¡ªwhether
birds evolved from dinosaurs. But other finds have been just as
spectacular,
such as the minutely preserved (to the cellular level) animal
embryos
of the
670 million-year-old Duoshantuo phosphorites, or the world's oldest
known
fish, from the Chengjiang formation in southwestern Yunnan Province.
Rise of
the Dragon makes descriptions and detailed discussions of these
important
finds available in one convenient volume for paleontologists and
serious
fossil fans.

87.
*********************************************************************
************************
Photo Album of Beipiao Bird FossilL Community Nature Preservation
Zone
of
Liaoning in China
ÁÉÄþ±±Æ±Äñ»¯Ê¯Èº¹ú¼Ò¼¶×ÔÈ»±£»¤ÇøÍ¼Æ¬¼¯ In Chinese
*********************************************************************
************************
Fan Guoqing/2000/210x285mm/77/Paperback/$38

The origin of birds is still an unsolved mystery. Archaeoteryx,
which
was
discovered in marine stratum of 145Ma in German in 1861, has been
considered
to be the sole representative of Jurrassic and the ancestor of birds
before.
Since the discovery over a century ago, studies on the origin of
birds
have
nearly not any new progress, and have also became one of the four
difficulties of life development history. But from 1987, at
Chaoyang,
Beipiao, Lingyuan in West Liaoning of China, 16 genus and 20 species
of
fossil birds have been discovered, part of which are a little older
than
Archaeoptery. It is an important discovered and has great scientific
values
to the studies on the origin and evolution of birds. It produces
wide
repercussions in academic circles all over the world. All of Chinese
people
feel proud of it. The bird fossil community is co-existing with
abundant
other animal and plant fossils (Jehol Biota), animal fossils
including
Reptilia, Fish, Estheria, Ostracoda, Insecta, Bivalva, Gastropoda
and
so on;
plant fossils including Rteridophuta, Cycadophyta, Ginkophyta,
Coniferophyta, Angiospermae and other classification unclear
fossils,
such
as silicified wood, Seed, Spore-pollen. At Beipiao, there are six
bird-bearing beds with a large buried density, for example in a 16
square
meters area in a tuffaceous shale bed, 11 pieces of well-preserved
bird
fossils have been discovered. Such a buried density is unprecedented
in
the
researching history of paleo-birds all over the globe. We have
videotaped at
sampling places. It is greatly significant to the studies on the
origin,
evolution, and death and then buried conditions of birds, and their
paleoecological and paleogeographical characteristics.

88.
*********************************************
Fossil Birds of China
Öйú¹ÅÄñÀà In Chinese and English bilingual
*********************************************
Hou Lianhai/2003/280x210mm/234 pages/Paperback/$78

The content of this book includes not only the 16 reconstructions in
the
first picture book, but also adds 30 kinds of Miocene bird fossil
reconstructions, which have been published and studied in China.
Roughly
includes birds' fossils found in China in all geological periods. To
allow
readers to have a more systematic understanding of Chinese bird
fossils,
this bood is classified according to bird systems, from old to new
period:
Archaeornithes, Enantiornithas, Ornithurae. I need to explain that
the
Miocene bird fossils found mostly are only partial, incomplete
skeletons.
They are the early representatives of present birds, excluding some
exceptions. Although the skeleton is incomplete, we can reconstruct
its
skeleton according to similar present species because Cenozoic
bird's
skeleton fossil is especially closer to present-day birds than those
of
late
period birds.

89.
*************************************************
Picture Book of Chinese Fossil Birds
Öйú¹ÅÄñÀàͼ¼ø In Chinese and English bilingual
*************************************************
Hou Lianhai/2000/220x268mm/89/Hardcover/$48

This is the most comprehensive book in China about the study of
Chinese
Mesozoic birds and the discussion of the origin of birds and their
fight. It
includes sauriurine birds with a total of 16 species (including
Archaeopteryx). Each bird is represented by three parts, One is the
color
picture of the specimen, the second is the skeletal reconstruction
and
the
third is the color life reconstruction. Each is accompanied by both
Chinese
and English explanations about locality, age and the other
information.
1.Preface 2.Introduction 3.A soul passage through the Jurassic 4.I
am
happy
to bring Mesozoic birds to life in my paintings 5.A poem 6.Picture
book

90.
**********************************************
Mesozoic Birds from Western Liaoning in China
ÖйúÁÉÎ÷ÖÐÉú´úÄñÀà In Chinese
**********************************************
Hou Lianhai/2002/185x260mm/120/Hardcover/$56

1. The geological age of the Jehol Biota in western Liaoning, China
2.
The
Confuciusornis Avifauna 3. The Cathayornis Avifauna 4. The origin of
birds
and the disvovery of feathered dinosaurs 5. The origin of avian
flight
6.
The histological and physiological study of Confuciusornis and some
reptiles
7. The development of feathers and their early evolution

91.
*********************************************************************
************************************
Proceedings of the 5th Symposium of the Society of Avian
Paleontology
and
Evolution(Beijing,1-4June 2000)
In English
*********************************************************************
************************************
Zhou Zhonghe and Zhang Fucheng/2002/190x270mm/311/Hardcover/$96

1. Forword 2. Preface 3. Pleistocene Birds (1) A New Teratorn (Aves:
Teratornithidae) from the Upper Pleistocene of Oregon, USA (2) An
Overview
of the Genus Athene in the Pleistocene of the Mediterrancean
Islands,
with
the Description of Athene trinacriae n.sp. (Aves: Strigidae) 4.
Neogene
Birds
(1) Neogene Avifauna of Bulgaria (2) Phylogeny of Tertiary Giant
Anhingas
(Pelecaniformes: Anhingidae) from South Amrica (3) Additional
Material
of
Macranhiga paranensis (Aves: Pelecaniformes; Anhingidae) from the
Upper
Miocene Ituzatingo Formation of Entre Rios Province, Argentina 5.
Paleogene
Birds
(1) A Preliminary Report on the Diversity and Stratigraphic
Distribution of
the Plotopteridae (Pelecaniformes) in Paleogene Rocks of Washington
State,
USA (2) Avian Remains from the Middle Eocene of the Geiscltal
(Sachsen-Anhalt, Germany) (3) Revision of the Cathartidae (Aves:
Ciconiiformes) from the Middle Eocene to the Upper Oligocene
Phosphorites du
Quercy, France 6. Birds Crossing the K-T Boundary (1) New
Interpretations of
the Birds from the Navesink and Hornerstown Formations, New Jersey,
USA
7.
Mesozoic Birds (1) The Morphology and Systematics of Polarornis, a
Cretaceous Loon (Aves: Gaviidae) from Antarctica (2) The
Significance
of
Early Cretaceous Bird Tracks (3) New Information on the
Hesperornithiform
Radiation 8. Controversial Birds (1) Oviraptorosaurs Compared to
Birds
9.
Form and Function (1) The Evolution of Avian Cranial Kinesis (2) The
Pelvis
in Early Birds and Dinosaurs 10. Feather and Flight (1) Biology of
Basal
Birds and the Origin of Avian Flight (2) The Aerodynamically
Streamlined
Body Shape of Birds: Implications for the Evolution of Birds,
Feathers,
and
Avian Flight (3) Wing Loading in Primitive Birds 11. Species and
Evolution
(1) The Evidence for th eTiming of Speciation of Modern Contincental
Birds
and the Taxonomic Ambiguity of the Quaternary Fossil Record (2)
Avian
Species Turnover and Species Longevity in the leistocene of the
palearctic
12. Paleogeography and Stratigraphy (1) Palaeogeographical
Implications
Concerning Early History of Chosen Groups of Birds
(2) Are Confuciusornis and Archaefructus Jurassic Fossils? (3) Early
Cretaceous Maars, Depositional Environments and Their Relationship
to
the
Fossil Preservation in Sihetun, Liaoning, Northeast China

92.
*********************************************************************
**
All kinds of fossils in China ¨C Stromatoporoids of China (Second
Hand)
Öйú¸÷ÃÅÀ໯ʯ- ÖйúµÄ²ã¿×³æ In Chinese
*********************************************************************
**
Yang Jingzhi & Dong
Deyuan/1962/185x260mm/40pages+14pictures/Paperback/$12

93.
*********************************************************************
*******
All kinds of fossils in China¨CLamellibranchia fossils of China
(Second
Hand)
Öйú¸÷ÃÅÀ໯ʯ- ÖйúµÄ°êÈúÀ໯ʯ In Chinese
*********************************************************************
*******
1976/185x260mm/522pages+150pictures/Hardcover/$55

94.
*********************************************************************
****
All kinds of fossils in China ¨C Polyzoa( Bryozoa) of China (Second
Hand)
Öйú¸÷ÃÅÀ໯ʯ-ÖйúµÄ̦޺³æ In Chinese
*********************************************************************
****
Yang Jingzhi/1962/185x290mm/89pages+28pictures/Paperback/$19

95.
********************************************************
Fossils Cephalopods of China
Öйú¸÷ÃÅÀ໯ʯ¨DÖйúµÄÍ·×ãÀ໯ʯ (SecondHand) In Chinese
********************************************************
Zhao Jinke/1965/185x260mm/389 pages + 85 plates/Hardcover/$70

96.
********************************************
Fossils Gastropod of China
Öйú¸÷ÃÅÀ໯ʯ¨DÖйúµÄ¸¹×ãÀ໯ʯ In Chinese
********************************************
Yu Wen/1963/185x260mm/362 pages +66 plates/Hardcover/$45

97.
****************************************
Chinese Fusulinids
Öйú¸÷ÃÅÀ໯ʯ-ÖйúµÄòÑÀà In Chinese
****************************************
Sheng Jinzhang/1962/185x260mm/177 pages+ 27 plates/Hardcover/$48

98.
*****************************************************************
All kinds of fossils in China ¨C Corallite of China (Second Hand)
Öйú¸÷ÃÅÀ໯ʯ- ÖйúµÄɺº÷»¯Ê¯ In Chinese
*****************************************************************
Yu Changmin/1963/185x260mm/390pages+94pictures/Hardcover/$40

99.
************************************************
The Trilobites of China ( Vol.1)
Öйú¸÷ÃÅÀ໯ʯ-ÖйúµÄÈýÒ¶³æ (ÉÏ ²á) In Chinese
************************************************
Lu yanhao/1965/185x260mm/Vol.1 362+66 pls. Vol.2 403 pp.+68
pls./Paperback/$96

Vol.1 Contents 1. AGNOSIDA Kobayashi,1935 2. REDLICHIDA Richer, 1933
3.
CORYNEXOCHIDA Kobayashi, 1935 4. PTYCHOPARIIDA Swinnerton, 1915 5.
Plate(1-66)

100.
*****************************************************************
Panderian Organ and Enrollment of Ordovician Trilobites
°ÂÌÕ¼ÍÈýÒ¶³æµÄÅ˽ܶûÆ÷¹Ù¼°¾íÇú In Chinese with English summary
*****************************************************************
Han Nairen/2002/185x260mm/81 pages + 12 plates/Hardcover/$20

Panderian Organs of trilobites, some pits, grooves, furrows,
projection
and
pygidium, are coaptative structure about enrollment on the doublure
of
trilobites. The author expounded the structure of shield of stopping
enrollment from the following three aspects:
1. Cephalic doublure and the marginal region of dorsal cephalic; 2.
Coaptative structure on the pleural; 3. Coaptative structure of the
pygidium
doublure and dorsal pygidium.
The compositive of coaptative structure in enrollment of trilolbites
could
subdivided roughly into seven categories:
1. Sphaeroidal enrollment; 2. Hemspiral enrollment; 3. Unrolled
spiral
enrollment; 4. Spiral enrollment; 5. Unroll-inverted spiral
enrollment;
6.
Inverted spiral enrollment; 7. Discoidal enrollment.
Hemisoiral enrollment equal to¡°unrolled spiral enrollment" from
Borgstrom(1973). These categories of trilobites enrollment depend on
defferent coaptative structure and Panderian organs. In the
Ordovician,
second is Hemispiral enrollment, most of trilobites are sphaeroidal
enrollment
In this paper. The author studied and counted 102 species of
enrollment
specimens of the Ordovician trilobites from China and some parts of
the
world in the following ways.
1. From enrollment types: Spaeroidal enrollment (58%)£»Hemispiral
enrollment(14%)£»Discoidal enrollment (8%£©£»Spiral enrollment have
not
been
found.
2. From stage£¨six stages) in the Ordovician: Llanvernian (the first
peak)
enrollment specimens (25%)£»Ashgilian(the
second peak£©enrollment specimens£¨22%£©£»Other four stages(53%)£®
3. From relation of habits and enrollment: nekton enrollment
(40%)£»Pelgic
enrollment (31%)£»Nekton-benthic enrollment (21%)£»drill-mud
enrollment
(8%).
Studying trilobites enrollment is helpful to research ecology.

101.
*********************************************************************
*********************************************************
Trilobite fauna of the Kaili Formation (uppermost Lower Cambrian-
lower
Middle Cambrian) from southeastern Guizhou, South China
Ç­¶«ÄÏÔç¡¢Öк®ÎäÊÀ¿­Àï×éÈýÒ¶³æ¶¯ÎïȺ In Chinese with English summary
*********************************************************************
**********************************************************
Yuan Jin-Liang/2002/185x260mm/285 pages+ 68 plates/Hardcover/$39

The terminal Early Cambrian extinction of the Redilichiida and other
trilobites from the Kaili Formation is documented for the first
time.
Kaili's trilobite fauna includes 4 orders, 17 families and 3
subfamilies, 62
genera and subgenera, 145 species, subspecies and species indet, of
which, 1
subfamily, 6 genera, 2 subgenera and 53 species and subspecies are
new.

102.
*********************************************************************
********************************
Cambrian Trilobites of North China-Chinese Cambrian Trilobites
Housed
in the
Smithsonian Institution
In English
*********************************************************************
*********************************
Zhang Wentang/1987/185x260mm/332 pages + 125 plates/Hardcover/$89

This book is a modern review of the major collection of Cambrian
trilbites
from the North China Platform. This collection, houssd in the
U.S.National
Museum of Natural History, Smithsonian Institution, was acquired
through the
Camegie Institution Expedition of 1903-4 and ruiji Endo during his
working
at the northeastern China. Two major monographs, by C. D.Walcott in
1913 and
by Ruifi Endo an dC. E. Resser in 1937. provided the initial
descriptions,
and the present book seeks to improve th eillustration as a hasis
for
fitting the taxa involved into ht emodern taxonomy. The 1100
illustrated
typespecimens bolonging to 300 species of 107 genera, 30 families
represent
more than half of the known Cambrian trilobtte fauna of th eregion
and
inciude a high proportion of genotypes, critical to such studies
throughout
the world.

103.
*********************************************************************
**************
Polymerid Trilobites from the Cambrian of Northwestern Hunan, China
(2
volumes set)
In  English
*********************************************************************
**************
Peng Shanchi/2004/190x270mm/I.205 pages+ 63 plates;2.198 pages + 78
plates/Hardcover/$120

The Wulingshan Mountains region of northwestern Hunan and eastern
Guizhou
provinces, China, contains some of the most complete and
fossiliferous
strata known in the upper part of the Cambrian. Easy access to good
exposures has helped make this area the subject of numerous
systematic,
biostratigraphic, lithostratigraphic, chemostratigraphic, and
sequence-stratigraphic studies.
The purpose of this two-volume set is to document the polymerid (or
non-agnostoid) trilobites from the Huaqiao Formation of northwestern
Hunan.
A total of 196 species, some in open nomenclature, are reported,
including a
large number of new genera and new species. Some additional
individual
sclerites remain undetermined however, so the true diversity of
polymerid
taxa in the Huaqiao Formation is slightly greater than that reported
here
based on good, identifiable material. The polymerids have
paleogeographic
distributions ranging from regional to intercontinental. Most of the
genera
and some of the species are useful as biostratigraphic zonal
indicators
within Gondwana, and a few have utility intercontinentally.
Volume 1 of this set contains general geologic information
concerning
the
Huaqiao Formation of northwestern Hunan, lithostratigraphic data,
biostratigraphic zonation, detailed descriptions of three
stratigraphic
sections, and the systematics of corynexochid, lichid, and as aphid
trilobites. Volume 2 contains systematic treatments of
ptychopariids,
eodiscids, trilobites of uncertain affinity, and some undetermined
sclerites. In both volumes, considerable effort was made to
reillustrate
type material of many previously described taxa. In some older
literature,
illustrations were not always reproduced well, so the new
illustrations
should help to clarify taxonomic concepts.

104.
*********************************************************************
*********************************************************************
*****
Stratigraphy and Paleontology Series B Volume 3 No.1-Cambrian
Trilobite
Fauna of Guizhou and Hunan West (Guizhou JiHunan Xibu Hanwuji
Sanyechong
Dongwuqun) (One Copy)
¹óÖݼ°ºþÄÏÎ÷²¿º®Îä¼ÍÈýÒ¶³æ¶¯ÎïȺ In Chinese and Latin names
*********************************************************************
*********************************************************************
*****
Edited by Xiang Liwen et al./1963/185x260mm/88 pages+14
plates/Paperback/$25

This book describes 32 genera, 31 species, of which 5 genera and 11
species
of new species and genera were the first established.
CONTENTS 1. Yunnanocephalidae Hupe 2. Redlichiidae Poulsen 3.
Alokistocaridae Resser 4. Asaphisciae Raymond 5. Dolichometopidae
Walcott 6.
Dorypygidae Kobayashi 7. Pagodiidae Kobayashi 8. Olenidae Burmeister
9.
Solenopleuridae Angelin 10. Obolidae King 11. Damesellidae 12.
Kobayashi 13.
Liostracinidae Raymond 14. Asaphidae Burmeister 15. Ceratopygidae
Raymond
16. Anomocaridae Poulsen 17. Dolichometopidae Walcott 18.
Leiostoegiidae
Bradley 19. Eoacidaspidae Poletaeva 20. Anomocarellidae Hupe 21.
Pagodiidae
Kobayashi 22. Ptychopariidae Matthew 23. Agnostoidea McCoy

105.
*********************************************************************
********
Classification, Evolution and Biogeography of the Palaeozoic Corals
of
China
Öйú¹ÅÉú´úɺº÷·ÖÀàÑÝ»¯¼°ÉúÎï¹ÅµØÀí In Chinese with English summary
*********************************************************************
********
Wang Hongzhen/1989/190x265mm/391 pages + 81 plates/Hardcover/$55

This book is an outcome of a collective research on the subject by
the
authors. The contents include two parts. Part I contains nine
chapters
and
deals mainly with the skeletal structures and classification of the
Palaeozoic corals. The first chapter is introductory. The main theme
of
this
work is to investigate the minute skeletal structures and to attempt
a
revised classification on that basis, especially of tugose corals.
This
forms the content of chapter 2. Two different kinds of primary
skeleton, the
lamellat skeleton characterized by calcite flakes and the fibrous
skeleton
dominated by calecite needles or fibres, may be distinguished in
Rugosa,
Tabulata and also in Heterocorallia. The skeletal structures of the
Rugosa
is the most interesting and complicated. Altogether 75 genera of
Rugosa. 24
of Tabulata and one of Heterocorallia are studied by SEM method, and
the
photographs are illustrated in 73 plates out of the 81 in total.

106.
*********************************************************************
*
Monograph of Palaeozoic Corals-Tabulatomorphic Corals (2 volumes set)
´²°åɺº÷ÐÎɺº÷ (¶þ¾í£© In Chinese with English summary
*********************************************************************
*
Lin Baoyu/1988/185x260mm/Hardcover/$80

Vol.1 content: 1. History of the Subclass Tabulatomorpha 2.
Morphology
of
Subclass Tabulatomorpha 3. Methods of study of the Subclass
Tabulatomorpha
4. Classification of the Subclass Tabulatomorpha (I) Superorder
Tabulata (1)
Order Lichenariida Sokolov, 1950 (2) Order Sarcinulida Sokolov, 1950
(3)
Order Tetradiida Okulitch, 1936 (4) Order Favositida Wedekind, 1937
(II)
Superorder Heliolitoidea Frech (1) Order Protaraeida Leith (2) Order
Pragnellida Lin in Lin et Show, 1977 (3) Order halysitida Sokolov,
1950
(III) Superorder Chaetetoidea (1)Order Chaetetida Okulitch, 1936 5.
Evolutionary trends 6. Palaeobiogeographical provinces of
Tabulatomorphic
Corals 7. Palaeoecology of Tabulatomorphic Corals Vol.2 contnets: 1.
Preface
2. Introduction 3. Usage of the tables 4. Tables of specific
characters
of
Tabulatomorphic Corals in China 5. References

107.
*********************************************************************
*******************************
The Late Palaeozoic Rugose Corals Of Xizang(Tibet) and Adjacent
Regions
And
Their Palaeobiogeography
ÖйúÎ÷²ØÓëÁÚÇøÍí¹ÅÉú´úÖåÎÆÉºº÷¼°ÆäÉúÎï¹ÅµØÀí In English
*********************************************************************
*******************************
Fan Yingnian/2003/260x185mm/606 pages+73 plates/Paperback/$88

A systemation study of internal structure, ontogenesis, evolution,
assemblage and distribution of a great deal of the Late Palaeozoic
Rugose
corals are made. Affinities, assemblages and sequences of some
genera
are
put forward on the basis of carbon and oxygen isotope compsition of
coral
skeleton. Sedimentary facies in Xizang and its adjacent region is
divided
into Palaeotethysan neritic facies, Slope facies and Gondwanan
facies.
Palaeotethysan neritic facies: The Rugose corals are very rich, and
they are
dominated by the elements with dissepiments. The Coexistent fossils:
With
representatives of almost all the classas. Their carbon and
oxygen-isotope
values are generally shown by a small positive figure and a middle
negative
figure (see Table 3-8). Slope facies: The Rugose corals are sparse,
most of
them are small solitary without dissepiments. The coexistent
fossils:
With
conodonts except the adaptable and cryophilic elemens. Their
carbon-isotope
values are very small positive figure, the oxygen-isotope values are
middle
negative figure (See Table 9). Gondwanan facies: At the beginning of
the
glacial action, almost all Rugose corals are small solitary without
dissepiments, The coexistent fossils are only the strongly adaptable
and
cryophilic elemens such as Zaphrentites, Eurydesma, Trigonotreta and
Stepanoviella; the conodonts almost no appear in the existence of
the
giacial action. The carbon isotope values are middle negative
figure,
the
oxygen-isotope values are large negative figure (see Table 11). In
late
Carboniferous, the glacial action was very intense, the Rugose
corals
are
sparse and no dissepiments, their carbon and oxygen-isotope values
are
all
larger negative (see Table 12). On the hand, when the glacial action
was not
appeared and should be conclued, the Rugose corals except no
dissepiments
ones, may are appeared solitary and compound with dissepiments,
their
carbon
and oxygen-isotope values are similar to those of Palaeotethysan
neritic
facies (see Table 10, 13, 14). Biogeographical region for the Late
Palaeozoic Rugose corals is divided into Boreal Realm,
Palaeotethysan
Realm
and Gondwanan Realm which are subdivided into Province. This
monograph
believes that the boundary between the Palaeotethysan and the
Gondwanan
Realm (Landmasses) from the Early Carboniferous to the early of
Middle
Permian was Huorparco to Dongqiao and Nujiang fault. In the late or
Middle
Permain (maokou Age), northwards moving the Indian plate went into
the
Palaeotethysan Realm which resulted in Palaeotethysan deposit
containing a
great amount of compound corals with dissepiments, and hermatypic
corals.
These furnish convincing palaeobiologicla proof to the research on
the
Late
Palaeozoic geological framework, stratigraphy (stratigraphical
divisin
and
correlation), taxonomy of Rugose corals and geological history, and
to
the
recognition of sedimentary environment at that time in Xizang and
its
adjacent regions.

108.
*********************************************************
Monograph of Palaeozoic Corals-Rugosa and Heterocorallia
ÖåÎÆÉºº÷ÓëÒìÐÎɺº÷ In Chinese with English summary
*********************************************************
Lin Baoyu/1999/180x260mm/778 pages with 924 figures + 8
plates/Hardcover/$68

In Chinese with English abstracts (p.718-756)
The present monograph deals with all Palaeozoic Rugosa and
Heteerocoralla.
It includes the morphology, evolution and origins, palaeoecology,
Palaeozoogeograplic provinces, sequences of faunas, techmiques of
study,
classificationa nd systematic descriptions (about 4 orders, 20
suborders,
102 families, 53 subfamilies and 939 genera, among which 3 suborders
are new
).

109.
**************************************
Reefs Through Geological Ages in China
In English
*************************************
Zeng Dingqian/1992/213X300 mm/Hardcover/$35

Chapter 1 Introduction  Chapter 2 Essentials of Typical Reefs
through
Geological Ages in China Chapter 3 Features of Reefs through
Geological
Ages
in China Chapter 4 Reservoir Characteristics of Biolithites Chapter
5
Reef
Identification and Exploration Methods. Chapter 6 Raising
Exploration
Efficiency for Seeking Hidden Hydrocarbon Reef Reservoirs

110.
**************************************************************
Ordovician Reefs in South-Western Margin Ordos Basin
¶õ¶û¶à˹ÅèµØÎ÷ÄÏÔµ°ÂÌÕ¼ÍÉúÎク In Chinese with English summary
**************************************************************
Ye Jian/1995/185x260mm/67 pages + 6 plates/Hardcover/$10

111.
*****************************************************************
Devonian Reefs and Reef Complexes in Guilin, Guangxi, China
¹ãÎ÷¹ðÁÖÄàÅè¼ÍÉúÎクºÍÉúÎク×éºÏ In Chinese with English summary
*****************************************************************
1998/185x260mm/168 pages + 27 plates/Hardcover/$48

A professional volume contains rich data on Devonian refs and reef
complexes
in guilin, South China. Based on the result of a long term study
under
multidisciplinary principles of geology and palaeobiology,
especially
based
on th result of paleobiologic study on many fossil groups and
bioevents, on
the lithostratigraphic, biostratigraphic, sequence stratigraphy,
chronostratigraphy, on th sedimentology, microfacies analysis of
carbonate
rocks, etc. It reveals that the region of present Guilin and its
adjacent
region was covered by warm and shallow marine and was prosperous
with
the
reef development in the Middle and Late Devonian. B the beginning of
th
egeologic time interval approximately equivalent to the varcus
conodont
zone
there strarted a record of carbonate deposition in Guilin. It was
until
the
late Famennian and earliest Carbniferous that the reefs were
intermittently
developed along the margin of carbonate platform, an in places in
the
interior of platform. As a whole the marine Devonian form a
megacycle
mainly
composed of the clastics at the base, and of the carbonates at the
above,
where some hiates of various scale can be found. Some patch reefs,
fringing
reefs and algal mounds of smaller size occurred mainly in the
earlier
stage
of the carbonate platform development in Givetian, whereas the
barrier
reefs
along the margin of platform and rare patch reefs behind them were
growing
int eh late developmental stage mainly in Frasnian, locally in
Famennian. A
discussion is made on the global or subglobal eustasy and tectonic
controlling result in the sea level changes and bioevents, and how
to
effect
on the reef development. A synthesis on the mode of development of
the
Devonian reef complexes in Guilin is displayed at the final section.
This
volume covers with 27 plates, 57 text-figures and 3 tables.

112.
*************************************************************
Permian Reefs and Paleoecology in South China
ÖйúÄÏ·½¶þµþ¼ÍÉúÎクÓë¹ÅÉú̬ In Chinese with English summary
*************************************************************
By Zhang Wei & Zhang
Xiaolin/1992/185x260mm/147pages+10plates/Hardcover/$15

Permian is an important period in the development of reef and
reef-building
organisms on the world. Numerous Middle and Upper Permian reefs with
abundant fossils are widely distributed and well developed in South
China.
This book shows the results of the authors¡¯ comprehensive research
in
the
reefs, with emphasis on reef paleontology and paleoecology, which
have
been
obtained through a series of field investigations and laboratory
analysis
during the last few years. The remarkable work have given a
foundation
for
comparison study between Chinese and global Permian reefs in Chapter
1;
Morphologic and structural features of organisms found in different
reef
facies are discussed in Chapter 2; Chapter 3 is dedicated to the
description
of the main groups of calcareous sponges. Twenty species of 12
genera
of
sphinctozoans, nine species of 6 genera of inozoans and two
ecological
types
of Tabulozoa (scelerosponges) are described in the Chapter; Chapter
4
deals
with some important terms of paleoecolgy; Chapter 5 presents a
systematic
description and exhaustive study of reef-building organism
communities
from
various regions of South China; some important differences in
structural
features and compositions of these carbonate buildups are given in
Chapter
6; Chapter 7 is a comprehensive Summing-up. Some important
conclusions
are
presented.

113.
*********************************************************************
**************************************
Some Important Graptolite Faunas of the Middle and Upper Ordovician
from
Chongyi and Yongxin Areas, Jiangxi
½­Î÷³çÒåÓÀеØÇøÖÐÉϰÂÌÕÍ³ÖØÒª±Êʯ¶¯ÎïȺ In Chinese with English
summary
*********************************************************************
**************************************
Huang Zhigao/1998/185x260mm/296 pages + 26 plates/Paperback/$38

1. Preface 2. Description of Strata (1) Upper Ordovician Section
extending
from Hanjiang to Shikou village Yongxin county (2) Middle and Upper
Ordovician Section exposed at Duiershi village, Sishum area, Chongyi
county
(3) Middle Ordovician Section exposed at Chnggouwan, Sishun area,
Chongyi
county 3. Stablishment of graptolite zones, and the features and
correlation
of its associations 4. Discussion of some questions (1) The question
with
regard to the Genus Jiangxigraplus should be erected or not (2) The
question
with regard to the Genus Rectograptus Should be indpendence or not
(3)
Discussing the boundary of Lower and Middle Ordovician from the
stage
of
evolution and development of graptolite faunas 5. Systematic
description of
species 6. References 7. English Summary; Explanations to plates and
Plates

114.
****************************
Fossil Graptolites of China
Öйú±Êʯ In Chinese
****************************
Mu Enzhi/2002/190x270mm/1205 pages + 256 plates/Hardcover/$85

1. Introduction 2. Research history of graptolites in China 3.
Division
and
correlation of graptolite zones 4. Division of Ordovician
stratigraphy
and
character of lithofacies and biofacies in China 5. Types of
Ordovician
graptolite fauna and biogeographical division in China 6. Evolution
and
classification of graptolites 7. Systematic description 8.
Correlation
of
the graptolite-bearing strata in China 9. Stratigraphical
distribution
of
graptolites in China 10. References 11. Index of genera and species
12.
Plates (1-256) and their explanation

115.
**************************
Graptolite Research Today
In English
**************************
Edited by Chen Xu, B.-D.Erdtmann and Ni
Yu-nan/1994/185x260mm/262pages+48plates/Paperback/$40

The present conference volume Graptolite Research Today includes
most
of the
contributions which were presented as indoor lectures during the
scientific
sessions at the Nanjing institute of Geology and Palaeontology, but
also a
few articles which were submitted as manuscripts by authors who were
unable
to attend the conference. Altogether 30 papers were accepted by the
editors
of this volume. Due to a slightly extended format of the submitted
manuscripts the editors decided to modify the thematic framework and
to
reorganize the contributions into seven chapters as indicated by the
table
of contents.
CONTENTS 1. Taxonomy and Evolution 2. Biostratigraphy 3.
Palaeocology
4.
Preservation 5. Biogeography 6. Geochemistry 7. Short Notes

116.
***************************************************
Palaeozoic Fossils of Northern Xinjiang, China
н®±±²¿¹ÅÉú´ú»¯Ê¯ In Chinese with English summary
***************************************************
1999/185x260mm/314pages+109plates/Paperback/$28

CONTENTS 1.On the Miospore Assemblages of the Heishantou Formation
at
Aherbruckomha 2. Hoboksar, Xinjiang, with Additional Reference to
the
Transition Stratum from Devonian to Carboniferous 3.
Famenian-Tournaisian
Bryozoans of the Aergati Mt., NW Xingjiang 4. Some Palaeozoic
Tabulate
Corals from Northern Xinjiang 5. Emsian Brachiopods with Reference
to
the
Palaeobiogeographic Provincialism and Plate 6. Tectonics in the
Junggar
Basin of Xinjiang
7. Discovery of Brachiopods from the Hujiersite Formation in West
Junggar
and its Significane

117.
*********************************************
The Lower Paleozoic Conodonts of South China
ÖйúÄϲ¿Ôç¹ÅÉú´úÑÀÐÎʯ In Chinese
*********************************************
An Taiyang/1987/185x260mm/238 pages + 35 plates/Hardcover/$35

94 conodont Zones have been discussed and 212 species and sub-
species
have
been described
1.Introduction 2.Stratigraphy sections, Conodont faunas and
Correlation
(1)Cambrian (2)Ordovician (3)Silurian 3.On the relation between the
Cambrian
and Ordovician in South China and South Korea 4.Conodont
Paleoecology
and
provinces of the south China 5.On the colour alteration of conodonts
and
maturity of organic matter 6.Systematic descriptions (1)Cambrian
conodonts
(2)Ordovician conodonts (3)Silurian conodonts 7.Bibliography 8.Index
9.Plates

118.
*********************************************************************
**********
Permian Brachiopods and Community Succession in the Huaying
Mountains,
Sichuan
»ªÝöɽ¶þµþ¼ÍÍó×㶯ÎïȺÓëȺÂäÑÝÌæ In Chinese with English summary
*********************************************************************
**********
Zeng Yong/1995/185x260mm/163 pages +22 plates/Paperback/$25

220 species, belonging to 67 genera and 35 families, have been
indentified,
in which there are 24 new species and 4 new subspecies.
1. An Outline of the physical Geography in the Huaying Mountains
2. An Outline of Geology in Huaying Mountains
3. Introduction of the Measured Geologic Sections
4. The Features of the Brachiopod fauna
5. Characteristics of Brachiopod Assemblage
6. Correlation of Brachiopod Assemblage Sequence
7. Succession and Replacement of Palaeocommunities
8. Description of new species
9. Summary in English
10. Bibliography
11. Plates Explanation and Fossil Plates

119.
*********************************************************************
****
Lengwu Formation of Permian and Its Brachiopod Fauna in Zhejiang
Province
Õã½­¶þµþϵÀäÎë×é¼°ÆäÍó×㶯ÎïȺ In Chinese with English summary
*********************************************************************
****
Liang Wen-Ping/1990/180x260mm/522 pages + 83 plates/Hardcover/$76

The main idea of this book is to describe a transitional Horizon and
a
transitional brachiopod fauna between the Early Permian and Late
Permian of
the Tonglu area in the west Zhejiang, I. e. the Lengwu Formation and
Lengwu
brachiopod fauna. By the detail studies, analysis's and contrasts
for
the
new horizon and fauna put forward a scheme to divide the Permian
System
of
south China into three groups and six chronostratigraphical units.
The
writer has furnished large numbers of fossil materials of
brachiopods
and
has described 106 genera and 235 species with 30new genera and 153
new
species included in this monograph. In this basis, especially the
discovery
of punctate produtoids, writer has made a try in the classification
of
brachiopods and has erected four new subclasses under the two
traditional
classes. In addition, he has divided the Lengwu brachiopod fauna
into
two
assemblages and four ecological communities, and has made detail
discussion
for this fauna's relations of universe and its character of
geographical
provincialism.

120.
***************************
Brachiopod Fauna from Zhesi
ÕÜ˹Íó×㶯ÎïȺ In Chinese
***************************
Wang Chengwen/2003/185x260mm/210 pages + 50 plates/Hardcover/$48

Brachiopoda Dumeril, 1806
1. Rhynchonelliformea Williams et others, 1996
(1) Strophomenata Williams et others, 1996
(2) Rhynchonellata Wiliams et others, 1996

121.
*********************************************************************
***********************
Research on Brachiopod fauna and Stratigraphy of the Late paleozoic
in
North
China Platform
»ª±±µØÌ¨Íí¹ÅÉú´úÍó×㶯ÎïȺ¼°ÆäµØ²ãÑо¿ In Chinese with English
summary
*********************************************************************
***********************
Fan Bingheng/1999/185x260mm/179 pages + 40 plates/Hardcover/$22

The late Paleozoic strata (Carboniferous to Lower Permian) in
studied
area,
mainly composed of detrital deposits, coal and carbonate deposits
containing
numerous marine fossils, was remarkably developed. It is very
important
for
the further biostratigraphic work to the exploration of coal and
other
new
energy resources. Abundant brachiopod fossils were collected from
seven
sections and locations respectively situated Shanxi, Hebei, Shandong
and
Liaoning. Altogether, 66 genera and 230 species are identified,
among
them 1
genus and 71 species are new (Some new data have been published in
1995).
The new forms as well as some previously reported ones are described
and
remarked in detail. Up to now, this is the most complete and
abundant
data
on brachiopods in north China Platform.

122.
*********************************************************************
******************************************************
Late Cretaceous and Early Tertiary Gastropod, Echinoids and
Brachiopods
from
the Western Tarim Basin, South Xinjiang,China
н®ËþÀïľÅèµØÎ÷²¿Íí°×ÛÑÊÀÖÁÔçµÚÈý¼Í¸¹×ãÀຣµ¨ºÍÍó×ãÀà In Chinese
with
English summary
*********************************************************************
*******************************************************
Sun Dongli/1999/180x260mm/149 pages+20 plates/Hardcover/$35

123.
*******************************************************
Early Tertiary Gastropods from The Dongpu Region
¶«å§µØÇøÔçµÚÈý¼Í¸¹×ãÀà In Chinese with English summary
*******************************************************
1999/185x260mm/51 pages + 8 plates/Hardcover/$30

Early Tertiary deposits,which are divided in asceding order into
three
formations: Kongdian, Shahejie, and Dongying formations with rich
invertebrate faunas, are widely distributed in the Dongpu Region.
The
fossil
gastropods described in the present paper were discovered only from
the
Shahejie Formation, They contain 61 species, 39 genera, among which
2
genera
(Dongmingella and Nodusapyrgula) and 17 species are new. The
geologic
distribution of all species are shown in table.1. Based on the
faunal
characteristics and stratigraphic distribution.

124.
**************************************************************
Early Tertiary Gastropod Fossils from Coastal Region of Bohai
²³º£Ñذ¶µØÇøÔçµÚÈý¼Í¸¹×ãÀà In Chinese with English summary
**************************************************************
the editorial group/1978/180x260mm/157 pages+33plates/Hardcover/$45

The gastropod fossils are found mostly in the Member 1 of the
Shahejie
Zu,
minor in the Dongying formation, rare in the Kongdian zu, the
general
aspect
of the gastropod fossils, most of them are characteristic of the
Orient,
more or less shows an affinity with those in the coastal region of
south
China. After preliminary examination, they amount to 237 species and
92
genera (subgenera) within 39 families (subfamilies), including 224
new
species, 15 new gnera, 2 new subgenera and 1 new family.

125.
*************************************************
Fossil Bivalves of Yunnan
ÔÆÄϵÄË«¿ÇÀ໯ʯ In Chinese with English summary
*************************************************
Guo Fuxiang/1985/185x260mm/319 pages + 46 plates/Hardcover/$37

1. Preface 2. Introduction 3. Known bivalves of each geological time
of
Yunnan (1) Paleozoic bivalves of Yunnan (2) Triassic bivalves of
Yunnan
(3)
On bivalve stratigraphic problems of Yunnan Triassic (4) Jurassic
bivalves
of Yunnan (5) Cretaceous bivalves of Yunnan 4. Descriptions of new
genera
and species of Yunnan bivalves (for further details, please see the
contents
in Chinese) 5. References 6. Summary 7. Index of genera and species
8. Explanation of plates 1-46 9. Plates 1-46

126.
*********************************************************************
***********
Late Cretaceous-Early Tertiary Marine Bivalve Fauna From the Western
Tarim
Basin
н®ËþÀïľÅèµØÎ÷²¿Íí°×ÛÑÊÀÖÁÔçµÚÈý¼ÍË«¿ÇÀදÎï In Chinese with
English
summary
*********************************************************************
***********
Lan Xiu/1995/185x260mm/212pages+66plates/Hardcover/$34

The fossil bivalves described in the present paper were collectd
from
the
Late Cretaceous-Early Tertiary strata at Wuqia, Keping, Baicheng,
Wensu
in
the piedmont of south Tianshan Mountains; Qimugan, Wuyitake,
Yigeziya,
Aertashi, Duwa, Kiliyang, Lop in West Kunlun Mountains; and Mazartag
in
the
cntral area of the Taklimakan. They contain 94 genera, including 1
new
genus
and 26 new species described and illustrated. The distribution and
horizons
of all species are shown in Tables.

127.
*********************************************************************
****
Lower Cretaceous Bivalves from the Eastern Heilongjiang Province of
China
In English
*********************************************************************
****
Gu Zhiwei/1997/185x260mm/301/Paperback/$52

In this book 190 marine to brackish bivalvian species mainly from
the
Longzhaogou Group and the lowermost Chengzihe Formation of Jixi
Group
together with 23 freshwater species from the Chengzihe and Muleng
Formations
of Jixi Group in the eastern Heilongjiang Province were described
.These
bivalves comprise 32 species and 1 new genus and species in the
Palaeotaxodonta ,1 species in the Cryptodonta,95species (7 species
new
)and
1new genus in the Pteriomorphia ,12 species in the Palaeoheterodonta
,59
species in the Heterodonta, and 13 species in the Anomalodesmata.
Based
on
Jupiteria (Ezonuculana) aff. mactraeformis (Na-geo), Portlandia aff.
sanchuensis(Yabe et Nagao)and Thracia (Sow.)in the upper marine
member
of
the Peide Formation and Aucellia aptiensis(D' Orb.), A. caucasica
(v.Bicj) ,
Expgura ? erecta Gu sp. nov . , Amphidonte subhaliotoidea (Nagao0,
Aetostreon aff . xouloni (Defrance), Owtrea spp. , Arctica cf .
saussuri(Brongn .)and Thracia rotundata (J. de C. Sow.)in the
Yunshan
Formation to Aptian and principally Aptian . The Longzhaogou and
Jixi
Groups
could be correlated with each other. Aucellina and Arctica together
with
Pinna ,Isog-nomon and Filosina indecate a temperate climate in the
region of
the Groups .The ingressed Late Early Cretaceous sea from the east in
the
ancient Wanda and Jixi areas as well as theLate Jurassic sea in the
Suibin
area appeared not of great depths ,yet most probably of embaymental
palaeoenvironment. The freshwater species of the Jixi Group belong
to
Jehol
or Witim faunas, entirely of Asian or Holarctic nonmarine
faunas ;they
are
of late Early Cretaceous instead of Late Jurassic age as held for a
long
time.

128.
*************************************************************
Taxonomy and Biostratigraphy of Small Shelly Fossils in China
ÖйúС¿Ç»¯Ê¯·ÖÀàѧÓëÉúÎïµØ²ãѧ In Chinese with English summary
*************************************************************
1999/184x260 mm/247/Paperback/$38

Chapter I Classification and early evolution of different groups of
SSF
Chapter II Preservation, shell wall composition and microstructure
of
SSF
Chapter III Geologyical and geographical distribution of SSF, with
discussion on Early Cambrian geographical provinces
Chapter IV Review on global Precambrian-Cambrian boundary stratotype
and its
intercontinental correlation
Chapter V Cambrian explosion and geological events

129.
************************************************************
Tertiary Ostracode Fauna from Qaidam Basin, NW China
²ñ´ïľÅèµØµÚÈý¼Í½éÐÎÀදÎïȺ In Chinese with English summary
************************************************************
1988/185x260mm/190 pages + 95 plates/Hardcover/$35

Here have been described totally 30 genera and 205 species, of which
5
genera: Youshashania, Qaibeigouia, Gauricypris, Qaidamocythere and
Eulimnocythere, and 149 species are new, all of which belong
respectively to
Cypridacea, Cytheracea and Darwinulacea.
The Tertiary ostracode fauna may be divided into 6 assemblages and 3
subassemblages, from bottom to top
1. A General account of stratigraphy 2. Characteristics of ostracode
assemblages and their geological ages 3. Ecology and paleoecology of
some
ostracode genera and species, their significance to environmental
indication
4. A preliminary study of the evolutionary relationships with part
of
ostracode genera and species 5. Systematic paleontology (1)
Superfamily
Cypridacea (2) Superfamily Cytheracea (3) Superfamily Darwinulacea
6.
References 7. Abstract (in English) 8. Index 9. Plates with
explanation

130.
********************************************************
Cretaceous Conchostracans from Songliao Basin
ËÉÁÉÅèµØ°×ÛѼÍÒ¶Ö«½é»¯Ê¯ In Chinese with English summary
********************************************************
Cui tongcui/1987/185x260mm/120 pages + 44 plates/Hardcover/$36

In Songliao basin, Crtaceous deposits were extensively distributed,
ostracods, pelecypods, fish, gastropods, plant and algae fossils,
especially
abundant conchostracans were found to occur in the Denglonku-
Mingshui
group.
They were mainly collected from Qingshankou and Nenjiang formation.
The
fossil Conchostracans dealt with in this monograph contain 169
species
in 32
genera, 10 families, of which 81 species, 7 genera are new to
science.
1. Estheriteoidea 2. Afrograptioidea 3. Vertexioidea 4.
Lioestherioidea

131.
******************************************************
Early Tertiary Ostracoda from the Dongpu Region
¶«å§µØÇøÔçµÚÈý¼Í½éÐÎÀà In Chinese with English summary
******************************************************
Research Institute of Exploration and Development, hongyuan
Petroleum
Exploration Bureau/1989/185x260mm/72 pages + 25 plates/Hardcover/$19

In Dongpu region, including northern Henan province and western
Shangdong
province, the Early Tertiary sediments with rich fossils are
well-developed
as those in the coastal region of Bohai and can be divided in
ascending
order into three units, the names of which are the same of the
coastal
region of Bohai as follows: the Kongdian Formation, the Shaheji
Formation
and the Dongying Formation. In this region the Early Tertiary
nonmarine
ostracode fauna contains 23 genera and 94 species, including 16 new
species.
This ostracode fauna is similar to that from the coastal region of
Bohai. In
the former fauna there are, together with usual freshwater genera, a
large
number of endemic forms previously appearing in the Early Tertiary
deposits
of the coastal region of Bohai, but the former one is less abundant
than the
latter. In this ostracode fauna seven ostracode assemblages, closely
corresponding to those from the coastal region of Bohai, have been
recognized in ascending order as in Table 1: After analysing the
characters
of these two ostracode faunas mentioned above, it is suggested that
they
belong to the same biogeographic realm and possess the similar
ecological
conditions.

132.
*********************************************************************
***************************************
Cretaceous Volcanic Sequences and Their Ostracoda Fauna in Zhejiang,
Fujian
and Jiangxi Province of China
Õã¡¢Ãö¡¢¸ÓµØÇø°×ÛѼͻðɽ³Á»ýµØ²ã¼°½éÐÎÀදÎïȺ In Chinese
*********************************************************************
***************************************
Shou Zhixi/1995/185x260mm/156 pages +14 plates/Hardcover/$20

This specieal publication is the results of the author's work from
1981-1985. During the field seasons, members of the division of
Paleontology
of Nanjing Institute of Geology and Mineral Resources, participants
from the
provincial regional geological survey teams of Zhejiang, Fujian and
Jiangxi,
petroleum exploration team of Zhejiang and Jiangxi also took part in
for
same days. Prof. Hao Yishun and Assoc. Prof. Pang Qiqing carefully
review
the manuscript and gave comments. The author would like to thank for
their
proposals and also expresses her sincere thanks to those who have
ever
supported to her.

133.
*********************************************************************
*******************
Late Cretaceous-Early Tertiary Ostracod Fauna From Western Tarim
Basin
S.Xinjiang China
н®ËþÀïľÅèµØÎ÷²¿Íí°×ÛÑÊÀÖÁÔçµÚÈý¼Í½éÐÎÀදÎïȺ In Chinese with
English
summary
*********************************************************************
********************
Yang Hengren & Jiang Xiangting/1995/185x260mm/173 pages + 28
plates/Hardcover/$42

Based on the morphological, characteristics ornamentation and
vertical
distribution of species, the ostracod fauna may be divided in
ascending
order into 9 assemblages, indicating environments of lagoons,
offshore,
inner shelf shallow water, etc. Here described and illustrated are
45
gnera,
1 subgenus and 163 species including 36 new species belonging to 15
families.
1. Podocopina Sars, 1866 (1) Bairdiidae Sars, 1888 (2)
Paracyprididae
Sars,
1923 (3) Pontocyprididae G.W.Muller, 1894 (4) Brachycytheridae Puri,
1954
(5) Bythocytheridae Sars, 1926 (6) Cytherettidae Triebel, 1952 (7)
Cytherideidae Sars, 1925 (8) Cytheruridae G.W.Muller, 1899 (9)
Leguminocythereididae Howe, 1961 (10) Loxoconchidae Sars, 1925 (11)
Progonocytheridae Sylvester-Bradley, 1948 (12) Schizocytheridae
Howe,
1961
(13) Trachyleberididae Sylvester-Bradley, 1948 (14) Xestoleberididae
Sars,
1928 2. Platicopina Sars, 1866 (1) Cytherellidae Sars, 1866

134.
*********************************************************************
**********
Fossil Ostracoda of China (Vol.1)-Superfamilies Cypridacea and
Darwinulidacea
Öйú½éÐÎÀ໯ʯ In Chinese with English summary
*********************************************************************
**********
Hou Youtang, Gou Yunxian/2002/190x265mm/1090 pages + 317
plates/Hardcover/$85

In this book , the taxis and phylogeny of Cypridacea and
Darwinulidacea
were
studied and a phylogenetic diagram was platted was plotted. It is
shown
,
that the content of the past classification was really supplemented.
The
muscle scars of the type-genus of each family included in these two
superfamilies are diagramed and explained. The living environment of
non-marine ostracod fauna and the living habit of some important
genera
and
species are generally explained. Based on the regularity of
distribution in
the strata the fossil ostracod assemblages were erected by the
Chinese
ostracodologists. After a general discussion and analysis, a new
revised
sequence of non-marine ostracod assemblages is established in this
book.
Thus the subdivision, correlation and classification of strata,
depend
upon
ostracods, are rather reasonable and more scientific.
In this book 127 genera and 1863 species including in the
superfamilies
Cypridacea and Darwinulidacea were revised and redescribed. Among
them,
there are 124 genera respectively belonging to 17 families (6 are
new )
and
13 subfamilies (2 are new ) of superfamily Cypridacea; 1 of the
other 3
genera belonging to family Darwinulidae and 2 belonging to
Panxianidae
of
superfamily Darwinulidacea.
1. Distribution, classification and evolution of Cypridacea and
Darwinulidacea
2. Microstructure in some genera of Cypridacea and Darwinulidacea
3. Distribution and their living environment of Cypridacea and
Darwinulidacea
4. Non-marine fossil ostracod assemblages, geological ages of
fossil-bearing
strata and relative problems
5. Fossil ostracod assemblages and evolution
6. Applying modern methods and techniques to study fossil ostracods
in
China
7. Conclusion
8. Systematic classification and description
9. References
10.Index and list of genera and species
11.Plates and explanations

135.
*****************************************************
Stratigraphy and Ostracods of Xinjiang in China
н®µØ²ã¼°½éÐÎÀ໯ʯ In Chinese with English summary
*****************************************************
Jiang Xianting/1995/185x260mm/577 pages + 122 plates/Hardcover/$80

The Paleozoic strata in the Xinjiang area occur mainly in the
Tianshan
Mts.,
Kunlun Mts. And Altai Mts. Fold systems, with sediments
predominantly
of
marine origin. The Mesozoic-Cenozoic strata are confined in the
Junggar,
Tarim and Turpan Basins as well as in some small intermontane
basins,
being
all of continental origin except for the marine sediments of Upper
Cretaceous and Lower Tertiary exposed in the west of the Tarim
Basin.
Ostracods are rich in both the Paleozoci and the Mesozoic-Cenozoic
strata,
but their distribution is far from homogeneous in time and space. By
their
occurrence in the strata, the ostracods persisting from
Carboniferous
to
Quaternary are classified into the following the ostracods
persisting
from
Carboniferous to Quaternary are classified into the follwing 18
assemblages.
Those ostracods faunae whose biostratigraphic boundaries remaining
for
further study or those which are not able to be distinguished into
independent assemblages, e. g. the ones of Ordovician through
Devonian,
are
not discussed in this paper.

136.
***********************************************************
Mesozoic Fossil Insects of Jiuquan Basin in Gansu Province
¾ÆÈªÅèµØÀ¥³æ»¯Ê¯ In Chinese
************************************************************
Hong Youchong/1982/185x260mm/187 pages + 39 plates/Hardcover/$45

1. Introduction 2. Study Story of fossil insects in China 3.
Stratigraphic
unites and its fossil insects 4. Assemblage of fossil insect in
different
formation 5. Characteristics of different fossil insect and its
entomologica
problems 6. The problem of th eboundary between in th eupper
Jurassic
and
the Lower Cretaceous of Jiuquan Basin 7. Morphology of fossil
insects
8.
Systematic description

137.
*********************************************
Fossil Insects From Shanwang, Shandong, China
ɽÍúÀ¥³æ»¯Ê¯ In Chinese with English summary
*********************************************
Zhang Junfeng/1989/184x260mm/459/Hardcover/$48

Shan wang, one of the most famous fossil localities in the world,
lies
22
kilometers east of the Linqu town in central Shandong province,
China
(see
text-fig.1). The fossils are embedded in the Shanwang formation, an
accumulation of thousands of diatomaceous layers. It is like a
natural
museum, with a wide variety of fairly well-preserved plant and
animal
fossils. Chinese paleontologists regarded the Shanwang tripolite
beds
as
mid-Miocene sediments, but some researchers , such as Li and others
(1984)
as well as Qiu and others (1986), believed that it is of the early
mid-Miocene age. The fossil insects collected from the Shanwang
formation
and described here include 272 species within 161 genera of 74
families
in
12 orders, of which 45 species of 37 genera have been published not
long
before (Hong, 1979,1983,1985;Hong and Wang, 1985; Lin 1982).
Reexamining
those holotypes, however, a revision of their diagnoses and
taxonomic
positions has been made in this writing by the present writer. All
the
type
specimens described in this work are conserved in Shandong
Provincial
Museum
and Linqu Paleontological Museum

138.
********************************************************
Miocene Insects and Spiders From Shanwang, Shandong
ɽ¶«É½ÍúÖÐÐÂÊÀÀ¥³æÓëÖ©Öë In Chinese with English summary
********************************************************
Zhang Junfeng/1994/185x260mm/42 plates+298 pages/Hardcover/$22

This monograph deals with the insects and spiders from the miocene
Shanwang
Formation at Shanwang Village in Linqu County of Shandong province,
China.
There are 135 insect species within 100 genera of 50 families, 11
orders,
among them 104 species, 31 genera and one family are new to science.
While
23 spider species belonging to 14 genera of seven families are
recovered, of
which 16 species and five genera are assigned into new taxa.
1. Insecta (1) Odonata Fabricius, 1793 (2) Blattaria Burmeister,
1829
(3)
Orthoptera Olivier, 1789 (4) Isoptera Comstock, 1895 (5) Dermaptera
Leach,
1815
(6) Homoptera Leach, 1815 (7) Heteroptera Latreille, 1810 (8)
Lepidoptra
Linnaeus, 1758 (9) Coleoptera Linnaeus, 1758 (10) Hymenoptera
Linnaeus,
1758
(11) Diptera Linnaeus, 1758 2. Arachnida (1) Araneida Clerck, 1757

139.
*************************
Amber Insect of China
ÖйúçúçêÀ¥³æÖ¾ In Chinese
*************************
Hong Youchong/2002/190x270mm/653 pages + 48 plates/Hardcover/$68

This monograph consists mainly of two parts. The first part givesa
geological background for the formation of Fushun Coal Mine and its
amber
insects, including such aspects as stratigraphical subdivision,
basin-structure, Paleogeography and paleoclimatology. The second
part
discusses the taxonomy of amber insects, including 8 orders:
Ephemeroptera,
Blattaria, Homoptera (Aphidoidea), Heteroptera, Psocoptera,
Coleoptera,
Diptera and Hymenoptera, covering 10 suborders, 30 subfamilies, 8
tribini,
185 genera, and 172 species are new. These new taxa from the Fushun
amber,
collected from the Xilutian Opencut Mine, are here reported for the
first,
time.
1. Ephemeroptera Hyatt et Arms, 1890 (Handlish, 1908; Plectoptera
Packard,
1886; Ephemerida Leach, 1817)
2. Blattaria Burmeister, 1829 ( Blattodea Brunner, 1882)
3. Homoptera Leach, 1815
4. Heteroptera Linne, 1758 ( Latreille, 1810)
5. Psocoptera Leach , 1815 (Shiplay, 1904; Corrodentia, Copeognatha)
6. Coleoptera Linne, 1758
7. Diptera Linne, 1758
8. Hymenoptera Linne, 1758 (Laicharting, 1781)

140.
*************************************************
Cambrian Bradoriida of China
Öйúº®Îä¼Í¸ß¼¡³æ In Chinese and English bilingual
*************************************************
Huo Shicheng & Shu Degan/1991/180x260mm/250 pages + 46
plates/Hardcover/$35

The book consists of 8 chapters:
1. History, present situation and prospect for the research of
cambrian
bradoriida of China
2. Carapace of the bradoriid
3. Soft body of the bradoriida
4. Reproduction, ontogeny, phylogeny of bradoriids and origin of the
Crustacea
5. Systematic classification of bradoriida
6. Paleo-biogeography and paleoecology of cambrian bradoriida of
China
7. Geological succession of cambrian bradoriida from China
8. Systematic description

141.
*********************************************************************
***************
Cambrian and Lower Ordovician Bradoriida From Zhejiang, Hunan and
Shaanxi
Provinces
ÕãÎ÷¡¢ÏæÎ÷¼°ÉÂÄϺ®Îä¼ÍÖÁÔç°ÂÌÕÊÀµÄ¸ß¼¡³æ In Chinese with English
summary
*********************************************************************
****************
Shu Degan/1990/185x260mm/95 pages+20 plates/Hardcover/$38

The investigation of bradoriids of South China began at the
beginning
of
this century. However, it was since 1950's that a lot of work has
been
done.
A six years of extensive investigation and collection of bradoriid
fossils
was made by as many as twenty students and teachers of Department of
Geology
at the northwest University in Shaanxi, Sichuan, Yunnan, Guizhou,
Hubei
and
Guandong Provinces. On the basis of those extremely abundant
materials
the
second monograph on Bradoriida in the world-"Cambrian Bradoriida of
South
China" was published . Although more than 240 bradoriid species of
China was
described and several of theoretical problems on Bradoriida were
discussed
in the book, there are still many problems remained for further
study:
1.
The geological range and geographical distribution of bradoriids in
South
China are not fully known, and field investigation ought to be made
on
more
horizons at more localities. 2. The important microstructural
features
of
bradoriid carapaces were nearly not dealt with at all. 3. The system
atical
position of Bradoriida in Crustacea and its taxonomy need to be
restudied.
Thus, to solve these problems is the aim of the present paper.

142.
****************************************************
Cambrian Bradoriida of South China
ÖйúÄϲ¿º®Îä¼Í¸ß¼¡³æ In Chinese with English summary
****************************************************
1985/185x260mm/251 pages+ 37 plates/Hardcover/$38

The Bradoriida include extinct marine small bivalved crustaceans,
which
seem
to be limited to the Cambrian, only a few forms have been found in
the
Lower
Ordovician.The fossils of Cambrian bradoriids are very abundant in
South
China, which may attain a half in the number of species of the
world.
The
taxonomic position of Bradorida in Crustacea has long been a
debatable
issue. The bradoriids were considered to be related to the Ostracoda
by
Jones, as the Conchostraca by Ulrich and Bassler, but they came to
be
so
widely accepted as the Ostracoda by Matthew, Ivanova, Sylvester-
Bradley
and
Muller. Raymond and Opik assigned them to be related to the
Phyllocarida,
Adamczak made a comparison of them with egg cases of the Cladocera.
On
the
basis of making a thorough investigation and study of taxonomic
history
of
the Bradoriida and whole contents of bivalved crustaceans, after a
full
discussion of the corresponding relation between the soft body and
carapace,
the writers propose eight criteria for the classification of higher
categories of the bivalved and bivalve-like crustaceans: 1. presence
or
absence of valves gaping at the ends or along the ventral margin, 2.
number
of valves, 3. form and character of the hingement, 4. position of
the
scars,
5. composition of the valve, 6. with or without growth lines, 7.
size
of the
valve, 8. number of body segments and structure of appendages. Based
on
these criteria bradoriids are a heterogeneous group of small
bivalved
crustaceans and the order bradoriida can be divided into two
suborders,
namely lipabdomina and Abdomina, the former is the ancestor of the
Ostracoda
and the latter is related to the Phyllocarida and consequently with
the
Malacostraca. Some bradoriids which have paragrowth lines on their
valves
show elose affinity between them and conchostracans.

143.
*********************************************************************
************
Fusulinids and The Foraminifers Except Fusulinids in The Important
Regions,
China
ÖйúÖØÒªµØÇøµÄ¹j¼°·Ç¹jÓп׳æ In Chinese and Latin names index
*********************************************************************
************
By Xu Bingchuan/2006/185x260mm/452pages+84plates/Paperback/$48

This book contains fusulinids and the foraminifers except fusulinids
111
genera, 724 species

144.
**********************************
Taxonomic Principles of Fusulinids
In Chinese and English bilingual
**********************************
Zhou Zuren/1993/185x260mm/70 pages+5 plates/Hardcover/$18

The Presence of foramen and Parachomata in Some Permian Staffelids
is
considered as a non-inheritable ecological variation related to
their
littoral habitat without taxonomic significance . The exclusive
occurrence
of staffellids in directly suggests their favour to restricted
shallow
water
environmentt. The staffellids originally possess a calareous shell
and
4-layered Fusulinella-type spirotheca systematically, they belong to
the
subfamily staffellinae, a side-branch of the family Fusulinidea.

145.
************************************************************
Late Paleozoic Foraminiferal Biostratigraphy of Hebei,China
ºÓ±±Íí¹ÅÉú´úÓп׳æÉúÎïµØ²ã In Chinese with English summary
************************************************************
Hebei Coal Geology and Exploration Corporation/1991/185x260mm/179
pages+27
plates/Hardcover/$25

The above-mentioned limestones are rich in foraminifers including
163
species and subspecies belonging to 32 genera ,and 186 species
belonging to
26 fusulinid genera.
1. Preface 2. Foreword 3. Division and Foraminiferal Fauna in
Carboniferous
and Permian from Hebei 4. Discussion on the Carboniferous-Permian
Boundary
in Hebei 5. Carboniferous and Permian Small Foraminifera from Hebei
6.
Carboniferous and Permian Fusulinids from Hebei 7. References 8.
Appendix of
Latin-Chinese foraminiferal list 9. English Summary 10. Plates and
Explanations

146.
*********************************************************************
***************
Fauna Sinica Phylum Granuloreticulosa Class Foraminiferea
Agglutinated
Foraminifera
In Chinese with English summary
*********************************************************************
***************
Zheng Shouyi and Fu Zhaoxian/2001/180x260mm/788pp with 129 figures +
123
plates/Hardcover/$78

Agglutinated foraminifera, in the loose sense here inclusive of the
allogromid,astrorhizid,and textularid foraminifera, are
geographically
the
most widespread group of benthic foraminifera. Their occurrence in
almost
all kinds of marine environment environment,ranging frommarginal
marine,hyposaline,hypersaline,to shelf and bathyal regions where
they
sometimes make up a large proportion of the benthonic foraminiferal
fauna is
attributed to their possession of a dissolution-resistant organic
membrane
or organic cement used in binding exogenous test-building
material.Their
specific and non-specific faunal trends are useful in ecological and
paleoecological interpretations.
Study material consisting of some 700 surface sediment samples were
collected from the Bohai Sea ,the Huanghai Sea,the East China Sea to
depths
of over 2000 m in the Okinawa Trough,the northern South China Sea to
a
depth
of 1010m (one station),as well as from the southern islands of
Guangdong
Province---the Zhongsha Islands,the Xisha Islands, and the Nansha
Islands
..These seas cover temperate,subtropical and tropical regions,and
range
from
shallow marginal,semi-enclosed to deep sea.Five hundred and thirty-
nine
species described and fully illustrated belong to 38 families and
140
genera,inclusive of the allogromiid genera Argillotuba and Nodellum
and
the
genus Carterina which was separated from the agglutinated
foraminifera
on
account of its peculiar wall structure on which basis it was at
first
transferred to the suborder Carterinina and later to the order
Carterinida(Loeblich and Tappan,1987,1992).

147.
*******************************************
Stromatoporoids of China
Öйú²ã¿×³æ In Chinese with English summary
*******************************************
Dong Deyuan/2001/190x265mm/423 pages +175 plates/Hardcover/$58

China is one of those countries that are extremely rich in
stromatoporoids
fossils in the world and has a history of over 60 years in the study
of
stromatoporoids fossils although there are only very few scholars
engaged in
the research on them. In this book a thorough, systematic, and
intensive
summary of the stromatoporoids found in China is made and serious
and
systematic amalgamation and revision of over 1100 species of
stromatoporoids
which have been described are also made. A total of 726 species and
97
genera are described herein, of which 78 genera and 675 species are
of
Paleozoic age and 19 genera and 51 species are Mesozoic in age. This
is
a
strenuous complicated but very important basic research work and is
also a
comprehensive summary of the stromatoporoids found in China. The
writer
gives a discusion on the fundamental structures, taxonomic value,
and
microstructures of stromatoporoids and their significances in the
classification and stratigraphic division, proposes the principle
and
plan
for the classification of Chinese stromatoporoids based on the
newest
classification plans of other countries and combined with the
Chinese
and
materials, and designs the evolutionary models of their origin,
development,
and extinction. Their existence, Paleoecological features and
stratigraphic
and geographic as well as the role they played in the reef-building
are
dealt with in this book also. This book is a comprehensive monograph
dealing
with the most abundant materials and most complete types of the
stromatoporoids in the present world. It will become an
indispensable
reference book for the study of stromatoporoides in and outside
China
and
will play an important role in teaching, scientific research and
production.

148.
***********************************************
Standard Fossils of China-Invertebrate (Fasc.1)
Öйú±ê×¼»¯Ê¯-ÎÞ¼¹×µ¶¯Îï (µÚÒ»·Ö²á) In Chinese
************************************************
Chen Xu/1955/185x260mm/95 pages + 51 plates/Hardcover/$25

1. Protozoa (1) Rhizopoda 2. Porifera 3. Coelenterata (1) Anthozoa
(2)
Stromatoporoidea (3) Graptolithina 4. Echinodermata (1) Cystoidea
(2)
Blastoidea
(3) Crinoidea

149.
***********************************************
Standard Fossils of China-Invertebrate (Fasc.2)
Öйú±ê×¼»¯Ê¯-ÎÞ¼¹×µ¶¯Îï µÚ¶þ·Ö²á In Chinese
***********************************************
1955/185x260mm/171 pages + 103 plates/Hardcover/$25

1. Bryozoa (1) Cyclostomata Busk (2) Trepostomata Ulrich (3)
Cryptostomata
Vine 2. Brachiopoda

150.
***********************************************
Standard Fossils of China-Invertebrate (Fasc.3)
Öйú±ê×¼»¯Ê¯-ÎÞ¼¹×µ¶¯ÎµÚÈý·Ö²á£© In Chinese
***********************************************
Yu Jian Zhang/1957/259x184mm/320 pages+30 plates/Hardcover/$25

1. Mollusca (1) Lamellibranchiata (2) Gastropoda (3) Cephalopoda 2.
Arthropoda (1) Trilobita (2) Crustacea , Branchiopoda (3) Ostracoda
(4)
Archaeostraca

151.
*********************************************************************
*********
Quaternary Biological Groups of the Nansha Islands and the
Neighbouring
Waters
ÄÏɳȺµº¼°ÆäÁÚ½üº£ÇøµÚËļÍÉúÎïÀàȺ In English
*********************************************************************
*********
the Multidisciplinary Oceanographic Expedition Team of Academ
Islandsia
Sinica to the Nansha/1999/185x260mm/552 pages + 102
plates/Hardcover/$68

1. Quaternary bioremain sediments of the Nansha Islands and the
neighbouring
sea areas 2. Holocene Bryozoans from the Nansha Sea Area 3.
Ostracoda
from
the Nansha Islands and the adjacent Sea Areas 4. Foraminifera in
surface
sediments of the Nansha Sea Area 5. Quaternary Calcareous
Nannoplankton
from
the Nansha Sea Area in the South china Sea 6. A study of Late
Quaternary
Palynological data from the Nansha Sea area in the South China Sea
7.
Dinoflagellate Cysts from Quaternary Sediments of Nansha, South
China
Sea 8.
Relationship between the distribution of Bivalves in the Nansha Sea
Area and
their Palaeogeography 9. Holocene Gastropods from the Nansha Sea
area,
South
China Sea 10. Distibution of Radiolarians in the southeastern area
of
the
Nansha Sea Area 11. Distriution of the Diatoms from the southeastern
area of
the Nansha Sea Area and their relationship to the environment

152.
*********************************************************************
********
Radiolaria From Surface Sediments of the Central and Northern South
China
Sea
In Chinese
*********************************************************************
********
1996/185x260mm/52 plates 271 pages/Hardcover/$46

153.
**********************************************************
Paleontology and Stratigraphy in Hong Kong (2- volume set)
Ïã¸Û¹ÅÉúÎïºÍµØ²ã (ÉÏ Ï²ᣩ In Chinese
**********************************************************
By Li Zuoming et
al./1998/195x265mm/242pages+83plates£¬206pages+57plates/Hardcover/$98

154.
*********************************************************************
****************************
Conodonts of Lower Yangtze Valley-An Indexes to Biostratigraphy and
Organic
Metamorphic Maturity
ÏÂÑï×ÓµØÇøÑÀÐδÌ-ÉúÎïµØ²ãÓëÓлú±äÖʳÉÊì¶ÈµÄÖ¸±ê In Chinese with
English
summary
*********************************************************************
****************************
By Wang Chengyuan/1993/185x260mm/326pages+60plates/Hardcover/$45

Lower Yangtze Valley is a crucial area for the study of
palobiogeography and
tectonic between Norh and South China Plateform, Paleozoic and
Triassic
conodonts in this area have been thoroughly studied by the common
efforts of
present authors, based on systematical collection throughout Lower
Yangtze
Valley. 53 conodont zones have established and more than 360 species
have
been described, including 24 new species. Many conodont species are
good
indexes to biostratigraphy.

155.
*********************************************************************
**************************
Stratigraphy and Palaeontology of Systemic Boundaries in China
Ordovician-Silurian Boundary (1)
Öйú¸÷ϵ½çÏߵز㼰¹ÅÉúÎï °ÂÌÕϵÓëÖ¾Áôϵ½çÏߣ¨Ò»£© In English
*********************************************************************
**************************
By Nanjing Institute of Geology and Palaeontology, Academia
Sinica/1984/185x260mm/475pages+41plates/Paperback/$55

Gathered together in this volume are eighteen reports, chiefly the
papers
read at the Symposium of the Cambrian-Ordovician and Odovician-
Silurian
boundaries held in Nanjing in October, 1983. most of them discuss
the
stratigraphy and palaeontology of the O-S boundary sections in
Yichang
of
Hubei, Jingxian of southern Anhui (actually cental Anhui) and Yuqian
of
Zhejiang. As pointed out in the first paper of this volume, apart
from
the
Yangzi Region, the O-S Boundary sections also are well-defined in
some
other
regions, such as the Tibet-W.Yunnan region, the S. China region and
the
N.W.China region. Detailed work on the O-S Boundary will be carried
out
continuously year by year, and the research results also will be
successively published in the near future. This volume is only a
starting
point for the publication of the O-S boundary.

156.
*********************************************************************
******************************************
The Palaeontology and Sedimentarv Environment of the Sinian System
in
Emei
Ganluo Area , Sichuan £¨second hand£©
ËÄ´¨¶ëü-¸ÊÂåµØÇø Õ𵩼͵زã¹ÅÉúÎï¼°³Á»ý»·¾³ In Chinese with English
summary
*********************************************************************
*******************************************
Yin Jicheng, Ding Lianfang & He Tinggui/1980/185x260 mm/268
pages/Paperback/$18

This work presents the results of a synthetical study on the
stratigraphic
division and the boundary between Sinian and Cambrian in Emei-Ganluo
region,
Sichuan province. The study has been done by the research party of
Sinian
System of Chengdu Geological College with the helps of the other
fraternal
units. The work consists of ten sections.

157.
************************************************************
Mixed Biostratigraphy of Devonian in Wenshan, Yunnan
ÔÆÄÏÎÄɽ»ìºÏÐÍÄàÅè¼ÍÉúÎïµØ²ã In Chinese with English summary
*************************************************************
Jin Shanyu, Shen Anjiang & Chen
Ziliao/2005/185x260mm/195pages+40pictures/Paperback/$28

Contents Preface Foreword 1. The Summary of Regional Geology 2. The
Brief
Introduction of Profiles 3. The Fossil Identification List and
Genera-species Description 4. Stratigraphic Division and Correlation
5.
The
Lithofacies and Paleogeography; Conclusion; References; Plates and
illustration

158.
*********************************************************************
*******************************
Devonian-Triassic Stratigraphy and Palaeontology from Yushu Region
of
Qinghai, China (2 volumes set)
ÇຣÓñÊ÷µØÇøÄàÅè¼Í---Èýµþ¼ÍµØ²ãºÍ¹ÅÉúÎï In Chinese with English
summary
*********************************************************************
*******************************
1990/185x260mm/485page+114plates/Paperback/$80

Vol.1
Contents Preface 1. Triassic Stratigraphy and Biota in Yushu Region,
Qinghai
2. Triassic Foraminifera from Yushu Region, Qinghai 3. Notes on Late
Triassic Scleractinian Corals from Yushu, Qinghai 4. New Material of
Triassic Brachiopod Fauna from Yushu Region, Qinghai 5. Several
Species
of
the Middle and Late Triassic Conodonts from Yushu, Qinghai 6.
Bivalves
from
the Middle and Late Triassic in Yushu Region, Qinghai 7. Triassic
Cephalopods from Yushu Region, Qinghai 8. Fossil Plants from the
Late
Triassic Jiezha Group in Yushu Region, Qinghai
Vol.2
Content 1. Devonian and Carboniferous Stratigraphy and Biota in
Yushu
Region, Qinghai 2. Carboniferous and Lower Permian Fusulinids from
Yushu
Area, Qinghai 3. On the Discovery of Late Devonian Rugose Coral ¡°
Peneckiella¡± halysodes Ouyang from Yushu Region, Qinghai 4. Some
Middle and
Upper Devonian Tabulate Corals from Qinghai 5. Late Upper
Carboniferous
Rugose Corals from Sangzhi¡¯akao, Yushu, Qinghai 6. Middle and Upper
Devonian Stromatoporoids from Southern Qinghai and Their
Paleoecological
Characters 7. Devonian Brachiopods from Yushu, Qinghai with
Additional
Reference to the Middle and Upper Devonian Boundary of South China
and
the
Devonian Tectonics of Qinghai and Xizang 8. Upper Paleozoic
Conodonts
from
Yushu Region, Qinghai 9. Late Paleozoic Bivalves from the Southern
Yushu
Region, Qingha

159.
*********************************************************************
***************
Sinian-Triassic Biostratigraphy of the Lower Yangtze Peneplatform in
Jiangsu
Region
½­ËÕµØÇøÏÂÑï×Ó×¼µØÌ¨Õ𵩼Í-Èýµþ¼ÍÉúÎïµØ²ã In Chinese
*********************************************************************
***************
1988/185x260mm/368pages+56plates/Paperback/$45

160.
*********************************************************************
*************************
Strata and Paleontology of Permian, Jurassic and Cretaceous from
Rutog
region, Xizang£¨Tibet£©
Î÷²ØÈÕÍÁµØÇø¶þµþ¼Í¡¢ÙªÂ޼͡¢°×ÛѼ͵ز㼰¹ÅÉúÎï In Chinese with
English
summary
*********************************************************************
*************************
By Sun Dongli and Xu
Juntao/1991/185x260mm/294pages+58plates/Paperback/$40

This book presents an intensively systematic description and
illustration of
9 fossil groups of Permian, Jurassic and Cretaceous, including
fusulinids,
corals, brachiopods, bryozoans, foraminifers, radiolaris,
scleractinis,
bivalves, gastropods and plants and amounting to 156 genera and 267
species,
among which are 4 new genera and 62 new species. The feature of each
biota,
the biotic successions and the evolution fo biogeographical
provinciality in
various period are respectively discussed in detail. A further
subdivision
and correlation of the Permian, Jurassic and strata has been summed
up.
On
the basis of the new achievements of studies and the
paleogeographical
evolution of Qinghai-Xizang(Tibet) Plateaus as the east part of
Tethy
is
briefly elaborated according to the changes of biofacies and
sedimentary
facies in different stratigraphical regions and the plate theory.

161.
*********************************************************************
****************************************
The Late Permian Coaly-Bearing Stratigraphy and Paleontology from
Western
Guizhou and Eastern Yunnan SW.China
Ç­Î÷µá¶«Íí¶þµþÊÀº¬ÃºµØ²ãºÍ¹ÅÉúÎïȺ In Chinese
*********************************************************************
****************************************
By the Nanjing institute of Geology and
Palaeontology/1980/185x260mm/220pages+57plates/Paperback/$35

162.
*********************************************************************
*******************************
Late Paleozoic Stratigraphy and Paleontology from Yanbian of Sichuan
Province and Its Adjacent Area
ËÄ´¨Ñα߼°ÆäÁÚÇøÍí¹ÅÉú´úµØ²ãºÍ¹ÅÉúÎï In Chinese with English summary
*********************************************************************
*******************************
Wei Min/1998/185x260mm/54 pages + 12 plates/Paperback/$28

1. History 2. Devonian (1) Lithos Tratigraphic Units (2)
Biostratigraphic
Unit (3) Chronostatigraphic Unit 3. Carboniferous-Permian (1)
Stratigraphic
Introduction (2) Stratigraphic Division (3) Stratigraphic
Correlation
4.
Description of Fossils 5. References 6. Abstract in English 7.
Explanation
and Plates

163.
*********************************************************************
********************************************
Late Triassic-Early Jurassic Stratigraphy and Paleontology of the
Circum-Pacific Region China and New Zealand (2)
ÖйúºÍÐÂÎ÷À¼»·Ì«Æ½ÑóÇøÍíÈýµþÊÀ£­ÔçÙªÂÞÊÀµØ²ã¹ÅÉúÎ2£© In Chinese
with
English summary
*********************************************************************
********************************************
Zhang Wangping/1997/185x260mm/131 pages + 5 plates/Paperback/$28

1. Late Triassic-Early Jurassic Sporo-Pollen Assemblages of New
Zealand
and
the Sychronous Sporo-Pollen Assemblages Correlation between New
Zealand
and
China (1) Brief Introduction of Stratigraphy (2) Taxonomy and
Assemblage
Sequence of Sporo and Pollen Grains (3) Geological Ages of Sporo-
Pollen
Assemblages (4) Discussion about the Microflora and Paleoclimate (5)
Correlation of Sporo-Pollen Assemblages between New Zealand and
China
(6)
Systematic Description (7) Selected References (8) Summary in
English
(9)
Explanation of Plates (10) Plates
2. Late Triassic-Early Jurassic Stratigraphy in Eastern Guangdong,
China (1)
Stratigraphic Classification and Correlation (2) Fossil Zones and
Their
Correlation in Jinji Formation (3) Sedimentary Facies and Facies
Sequence
(4) Analysis of the Sedimentary Basin (5) Postscript (6) Selected
References
(7) Summary in English (8) Explanation of Plates (9) Plates

164.
*********************************************************************
****************************
The Middle Silurian and Early Devonian Stratigraphy and
Palaeontology
in
Qujing District, Yunnan
ÔÆÄÏÇú¾¸µØÇøÖÐÖ¾ÁôÊÀ£­ÔçÄàÅèÊÀµØ²ã¼°¹ÅÉúÎï In Chinese with English
summary
*********************************************************************
******************************
Fang Runsen/1983/185x260mm/171 pages+ 37 plates/Paperback/$28

In the paper the Conodonts, Brachiopoda, Anthozoa, Trilobit,
Bryozoa,
Ostracoda, Bivalvia, pisces and plant are described comprising (a) 8
genera,
12 species, 2 confer species, 4 subspecies, 6 indeterminate species,
4
indeterminate genera of Conodonds, including 1 new species and 3 new
subspecies; (b) 13 genera, 39 species of Brachiopod including 15 new
species; (c) 14 genera, 24 species, 7 indeterminate species of
Anthozoa,
including 12 new species 5 new subspecies; (d) 5 genera, 7 species,
4
indeterminate species of Trilobitae, including 5 new species; (e) 9
genera,
18 species, 1 indeterminate of Bryozoa, including 17 new species;
(f) 9
genera, 2 subgenera, 15 species of Ostracoda including 1 genus, 1
new
species 13 genra, 32 species, of Bivalvia, including 2 new genera,
21
new
species, 1 new subspecies; (h) 17 genera, 30 species of pisces,
including 7
new species; (i) 17 gnera, 28 species of plant, including 2 new
genera,
14
new species.

165.
*********************************************************************
**
The Stratigraphy and Palaeontology of Laiyang Basin, Shandong
Province
ɽ¶«À³ÑôÅèµØµØ²ã¹ÅÉúÎï In Chinese with English summary
*********************************************************************
***
Regional Gological surveying Team, Shandong/1990/185x260mm/255 pages
+
37
plates/Hardcover/$37

1. Preface 2. Study history in Laiyang Basin 3. Stratigraphy 4. The
reise
and decline of the "Laiyang Lake" 5. Establishing of faunal and
floral
assemblages from Laiyang Formation, and discussion of their
geological
age
6. Systematic description (1) Bivalvia of Qingshan Formation (2)
Gastropoda
of Laiyang and Qingshan Formations (3) Ostracoda of Laiyang
Formation
(4)
Conchostraca of Laiyang formation (5) Insecta of Laiyang formation
(6)
Fishes of Laiyang Formation (7) Plants of Laiyang formation (8)
Sporo-pollen
of Laiyang Formation 7. Abstract in English 8. Plates and their
explanation

166.
*********************************************************************
****
Stratigraphy and Palaeontology in W.Sichuan and E. Xizang, China
(Part
2)
´¨Î÷²Ø¶«µØÇøµØ²ãÓë¹ÅÉúÎï(µÚ¶þ²á) In Chinese
*********************************************************************
****
1982/185x260mm/322 pages +113 plates/Hardcover/$45

1. Discovery of the Ordovician Calcareous Algae from Batang, Sichuan
2. Eocene Polynological Assemblage from the Gonjo Formation in
Eastern
xizng
3. Fossil Plants from the Late Triassic Lamaya Formation of Western
Sichuan
4. Early Cretaceous Plants from the tuoni Formation of Eastern Xizang
5. Upper Triassic Foraminifera of Eastern Xizang
6. Fusulinids of Eastern Qinghai-Xizang Plateau
7. Palaeozoic and Mesozoic Sponges from Southwest China
8. Hydrozoids from the Ningjiang Mountains of the Southwestern China
9. Carboniferous and Early Permian Bryozoas in the Qamdo Area,
Eastrn
Xizang
10. Palaeozoic Stromatoporoids from Markam of Xizang and Batang of
Sichuan
11. Early Palaeozoic Trilobites from Eastern Xizang and Westrn
Sichuan
12. Mesozoic Conchostracans of East Xizang and West Sichuan
13. Lower Ordovician Graptolites from the East Borders of Qinhai-
Xizang
Plateau

167.
********************************************************
The Mesozoic Stratigraphy and Biota of Beijing Area
±±¾©ÖÐÉú´úµØ²ã¼°ÉúÎïȺ In Chinese with English summary
*********************************************************
Xiao Zongzheng/1994/185x260mm/135 pages +10 plates/Hardcover/$25

This monograph comprises five chapters: The study history, Triassic
System,
Jurassic System and Cretaceous System ( the last chapter is omitted
in
this
abstract). References, 20 plates of fossils and rocks, 30 figures
and 9
tables are also included. There are some 260 thousand Chinese
characters all
together.
I. Research history
II. The Triassic System
III. The Jurassic System
IV. The Cretaceous System
V. The Mesozoic geological history of Beijing

168.
*********************************************************************
**********
The Late Devonian and Early Carboniferous Strata and
Palaeobiocoenosis
of
Hunan
ºþÄÏÍíÄàÅèÊÀºÍÔçʯ̿ÊÀµØ²ã¼°¹ÅÉúÎïȺ In Chinese with English summary
*********************************************************************
*********
Regional Geological Surveying Party/1987/185x260mm/200 pages + 31
plates/Hardcover/$25

1. Introduction 2. Stratigraphy (1) Lithostratigraphy (2) Some main
Sections
(3) Biostratigraphy (4) Devonian-Carboniferous boundary (5)
Mid-Carboniferous boundary (6) Stages (7) Conclusion 3. Description
of
Important fossils (1) Stromatoporoids (2) Conodonts (3) Foraminifers
(4)
Brachiopods (5) Corals
(6) Spores (7) Bryophyts (8) Crinoids 4. References 5. English
Summary
6.
Explanations and Plates

169.
*********************************************************************
**************************
Middle to Upper Carboniferous-Early Permian Gondwana Facies and
Palaeontology in Western Yunnan
ÔÆÄÏÎ÷²¿ÖÐÍíʯ̿ÊÀ-Ôç¶þµþÊÀ¸ÔÍßÄÉÏàµØ²ã¼°¹ÅÉúÎï In Chinese
*********************************************************************
**************************
Fang Runsen and Fan Jiancai/1995/185x260mm/121 pages + 48
plates/Hardcover/$18

The region of western Yunnan means the nrea west of the Ailaoshan
fault
in
Yunnan province. According to the analysis and study of Late-
Palaeozoic
river strata in western Yunnan with partieular reference to
sedimentary
formations, biostrata palaeomagnetism and geophysies the region of
Lancangjiang river structural zone western Yunnan was divided inte
Yangtze
area to the east of the Lancangjiang river boundary zone which
comprised
shallow-marine carbonate facies nearby the equator and the area west
of
the
boundary zone consisting of the Gondwana sequence which contained
the
cold-water facies situsted in the palaeozic high-middle south-
latitude
terrain.

170.
************************************************************
The Permian Coal-Bearing Strata Palaeobiocoenosis of Fujian
¸£½¨¶þµþ¼Íº¬ÃºµØ²ã¼°¹ÅÉúÎïȺ In Chinese
*************************************************************
Zhu Tong/1990/185x260mm/127 pages + 47 plates/Hardcover/$29

1. Preface 2. Division and correlation of th Permian coal-bearing
strata in
Fujian (1) Previous study (2) Distribution of strata (3) Division of
strata
(4) Correlation of the Upper Lower Permian of Fujian (5)
Characteristics and
gological significance of th principal fossil assemblages 3. Fossil
Description (1) Fusulinids (2) Cephalopods (3) Brachiopods (4)
Palaeobotany
4. References 5. Explanation of plates

171.
*********************************************************************
***************************************
The Mesozoic Stratigraphy and Paleontology of Guyang Coal-Bearing
Basin
Neimenggol Autonomous Region, China
ÄÚÃɹŹÌÑôº¬ÃºÅèµØÖÐÉú´úµØ²ã¹ÅÉúÎï In Chinese
*********************************************************************
***************************************
1982/185x260mm/224 pages + 55 plates/Hardcover/$39

1. Preface 2. A Brief history of research 3. Stratigraphy 4.
Description of
fossil Fauna and Flora (1) Lamellibranchia (2) Gastropoda (3)
Phyllopods (4)
Ostracoda (5) Insecta (6) Pisces (7) Reptilia (8) Palaeobotany (9)
Spores
and pollen

172.
*******************************************************************
The Coal-Bearing Strata and Fossils of Late Permian from Guangtung
¹ã¶«Íí¶þµþÊÀº¬ÃºµØ²ãºÍÉúÎïȺ In Chinese
*******************************************************************
Hou Hongfei/1979/185x260mm/166 pages + 47 plates/Hardcover/$35

1. Preface 2. Division and correlation of coal-bearing strata of
Late
Permian (1) Brief history of Study (2) Stratigraphic distribution
and
its
principle characteristics (3) Unified regional classification of
stratigraphy (4) Boundary between the Lower and Upper Permian (5)
Litho-stratigraphic descriptions
(6) Correlation of the Late Permian of Guangtung (7) Characteristics
of
the
Principle fossil assmblages 3. Descriptions of fossils (1) Fusulinid
(2)
Brachiopoda (3) Ammonoid (4) Palaeobotany 4. Reference 5. Plate and
Explanations

173.
*********************************************************************
**************************
Research on The late Paleonzoic Coal-Bearing Stratigraphy and Biota
in
Xuzhou, Jiangsu province
ÐìÖݵØÇøÍí¹ÅÉú´úº¬ÃºµØ²ã¼°ÉúÎïȺ In Chinese
*********************************************************************
***************************
1995/185x260mm/274 pages +26 plates/Hardcover/$25

Chapter 1 Introduction
Chapter 2 Description of the coal-bearing strata sections
Chapter 3 Rock types of the coal-bearing strata and the characters
of
the
key horizons
Chapter 4 Characters of biotas and zoning of assemblages
Chapter 5 Division and correlation of the coal-bearing strata
Chapter 6 The discovery of coal balls in Xuzhou and its significance
Chapter 7 Sedimentary environmental analysis for coal-bearing strata
of
the
Xuzhou area
Chapter 8 Description for biota fossils of various classes

174.
*********************************************************************
*********************
Research on the Late Paleonzoic Coal-Bearing Stratigraphy and Biota
in
Jungar, Nei Mongol
ÄÚÃɹÅ×¼¸ñ¶ûÆìÍí¹ÅÉú´úº¬ÃºµØ²ãÓëÉúÎïȺ In Chinese with English
summary
*********************************************************************
*********************
He Xilin/1990/260x190mm/407 pages+35 plates/Hardcover/$34

Chapter 1 Intoduction
Chapter 2 An Outline of the Physical Geography and Econonics in
Jungar
Coalfield
Chapter 3 An Outline of Geology and Its Studying History
Chapter 4 Introduction of the Measured Geologic Sections
Chapter 5 The Features of the Fuana and Flora and Comparision with
Those
from the Disserent Regions in the same Age
Chapter 6 Assemblage Zones of the Different Kinds of Biota
Chapter 7 Stratigraphic Classification and Correlation
Chapter 8 Discussion on Some Stratigraphic Boundaries
Chapter 9 Achievements and Conclusions
Chapter 10 Systematic Description to the Different Kinds of Fosslis

175.
*********************************************************************
********************************************
Late Triassic Stratigraphy, Paleontology and Paleogeography of the
northern
part of the Circum-Pacific Belt,China
Öйú»·Ì«Æ½Ñó±±¶ÎÍíÈýµþÊÀµØ²ã¹ÅÉúÎï¼°¹ÅµØÀí In Chinese
*********************************************************************
*******************************************
Mi Jiarong and Zhang Chuanbo/1993/185x260mm/219 pages + 66
plates/Paperback/$38

This book is an achievement of scientific research on the
stratigraphy,
paleontology and paleogeography in the eastern part of the northern
China.
The book deals with the continental Upper Triassic strata of nine
sectors in
this area, that have been discovered over the last decade and more
and
reported here with an analysis of their characteristics and the
proposal of
some new ideas. It describes many fossil groups, such as plants (
188
species of 54 genera ), spore and pollen ( 40 species of 29 genera),
bivalves ( 26 species of 5 genera ), conchostracans ( 7 species of 2
genera
), and insects ( 7 species of 6 genera ), and makes a number of new
taxonomic proposals.
Based on the systematic study of the fossils, the characteristics
and
their
geologic ages of fossil assemblages are given for different sectors.
The
authors further discuss the Late Triassic floristic paleogeography,
the
paleoclimatic zonation, the pattern of tectono-sedimentary
paleogeography,
the stratigraphic division and the time limit and character of the
Indosinian Movement in this area. Many new ideas are offered. There
are
66
fossil plates in this book.

176.
***********************************************
Cretaceous Ostracoda in Hailaer Basin
º£À­¶ûÅèµØ°×ÛѼͽéÐÎÀà In Chinese
***********************************************
Ye Dequan/2003/26 cm/208 + 42 pls/Hardcover/$38

This book describes Ostracoda fossil 127 species belonging to 21
genera

177.
*************************************************************
Cretaceous Ostracoda Biostratigraphy in Songliao Basin
ËÉÁÉÅèµØ°×ÛѼͽéÐÎÀàÉúÎïµØ²ã In Chinese with English summary
*************************************************************
2003/180x260mm/Hardcover/$38

178.
*********************************************************************
*****************
Cenozoic paleobiota of the Continental Shelf of the East China Sea
Micropaleobotanical
¶«º£Â½¼ÜÐÂÉú´ú¹ÅÉúÎïȺ-΢Ìå¹ÅÖ²Îï·Ö²á In Chinese with English summary
*********************************************************************
*****************
Research party of Marine Gology/1989/185x260mm/324 pages + 107
plates/Hardcover/$48

1. Preface 2. Stratigraphy (1) Brief account of the Stratigraphy (2)
Characteristic of the palaeontology and the geological age 3.
Description of
the Palaeontology (1) Sporo-pollen (2) Dinoflagellates (3)
Charophyte
(4)
Diatom (5) Calcareous Nannofossils 4. References 5. Abstract in
English
6.
Explanation of the Plates and Plates

179.
*********************************************************************
********************
Cenozoic paleobiota of the Continental Shelf of the East China
Sea-Paleozoological Volume
¶«º£Â½¼ÜÐÂÉú´ú¹ÅÉúÎïȺ-¹Å¶¯Îï·Ö²á In Chinese with English summary
*********************************************************************
********************
Research party of marine geology/1989/185x260mm/280 pages + 182
plates/Hardcover/$44

1. Preface 2. Stratigraphy (1) Brief account of the stratigraphy (2)
Characteristic of the palaeontology and the geological age 3.
Description of
the Palaeontology (1) Foraminifera (2) Ostracoda (3) Mollusca 4.
References
5. Abstract in English 6. Explanation of the Plates and Plates

180.
************************************************************
Cambrian System of China and Korea Guide to Field Excursions
ÖйúºÍº«¹úµÄº®Îäϵ In English
************************************************************
By Peng Shanchi & Zhu Maoyan/2005/185x260mm/300pages/Paperback/$48

This volume includes contributions from the Fourth International
Conference
on the Cambrian System, held in Nanjing, China, in august 2005. The
conference was combined with the Tenth Field Conference of the
Cambrian
Stage Subdivision Working Group. Eight Field excursions to Classical
Cambrian localities in China and South Korea were organized as a
part
of the
meeting, although only six trips were run. This book contains guides
to
the
field areas visited as part of the conference. As originally
planned.
Four
pre-conference trips involved excursions to eastern and northern
Guizhou,
western Hubei, western Zhejiang, and western Shandong, China; and
four
post-conference trips involved excursions to eastern Yunnan,
northwestern
Hunan, and southern Shaanxi, China, as well as the Teabaekshan
Basin,
South
Korea. Guides for the planned trips to western Zhejiang, China, and
the
Taebaeksan Basin are included here although the trips did not
actually
take
place¡­¡­

181.
*****************************************************
Late Precambrian Palaeontology of China
ÖйúÍíǰº®Îä¼Í¹ÅÉúÎï In Chinese with English summary
*****************************************************
Xin Yusheng/1985/185x260mm/243 pages + 42 plates/Hardcover/$65

1. Introduction 2. An outline of Upper Precambrian in China 3.
Micropalaeophyta 4. Macroscopic fossil algae 5. Stromatolites 6.
Microphytolites (oncolites and Catagraphia) 7. Metazoans and trace
Fossils
8. Origin and evolution of Precambrian life 9. Words from the
editors
10.
References 11. Summary (in English) 12. Plates and Explanations

182.
********************************************************
Stratotype Section for Lower Cambrian Stages in China
ÖйúϺ®Îäͳ½¨½×²ãÐÍÆÊÃæ In Chinese with English summary
********************************************************
Luo Huilin/1994/185x260mm/183 pages + 40 plates/Hardcover/$22

1. Stratigraphic division of the Early Cambrian in China 2. Early
Cambrian
biota in China 3. Lower Cambrian isotopic stratigraphy in Eastern
Yunnan 4.
Early Cambrian lithofacies and paleogeography in Eastern Yunnan 5.
Lower and
upper boundaries of the Lower Cambrian in China and its correlation
at
home
and abroad 6. Description of the main section 7. Description of the
fossils
8. Reference 9. Plates and their explanation

183.
*********************************************************************
*********
Sinian-Cambrian Boundary Stratotype Section at Meishucun Jinning
Yunnan,
China
ÖйúÔÆÄϽúÄþ÷Ê÷´åÕðµ©Ïµ-º®Îäϵ½çÏß²ãÐÍÆÊÃæ In Chinese with English
summary
*********************************************************************
***********
Luo Huilin/1984/185x260mm/154 pages + 22 plates/Hardcover/$26

1. Introduction 2. Description of the section 3. Sinian-Early
Cambrian
Lithostratygraphy and its Subdivisions 4. Sedimentary Facies and
Contact
Relationships Between Various Formations and Members 5. Biological
Characteristics of the Late Sinian Dengyingxia'an Stage and the
Early
Cambrian Meishucunian and Qiongzhusian Stages 6. Isotopic Age
Determinations
and Magnetostratigraphical Characteristics 7. The Definition of the
Sinian-Cambrian Boundary 8. Regional and Intercontinental
Correlation
of the
Meishucunian Stage and the Sinian-Cambrian Boundary Stratotype 9.
Explanation of Plates

184.
***********************************
The Palaeontological Atlas of Hunan
ºþÄϹÅÉúÎïͼ²á In Chinese
************************************
Geological bureau of Hunan/1982/190x265mm/996 pages+440
plates/Hardcover/$140

The 18 groups described, 1258 genera and 3665 species, of which 40
genera
and 758 species are new, making up 440 plates. "The Palaeontological
Atlas
of Hunan" gives a concise description and illustration of the
important
fossils collected from this province and is part of the summing up
activities connected with the geological mapping of the province on
the
scale of 1:200,000 organized by the Hunan Regional Geological
Research
Team,
under the Geological Bureau of Hunan. This atlas has been mainly
compiled by
the Regional Geological Research Team, assisted by the Geological
Brigade of
No. 5 Petroleum Prospecting Headquarters under the direct leadership
of
the
Geological Bureau of Hunan.

185.
*********************************************
Neogene Palaeontology From North of Shandong
ɽ¶«±±²¿ÍíµÚÈý¼Í¹ÅÉúÎïȺ In Chinese
********************************************
Shan Huaiguang/1997/185x260mm/191 pages+49 plates/Hardcover/$39

In the north of Shandong, Neogene is well developed, about 600-2000m
thick
and divided into two formation in ascending order as: Guantao
Formation
and
Minghuazhen Formation. Here have been described Ostracodes,
Gastropods,
Bivalves, Foraminifera, Charophytes, Sporopollen and Algae, totally
201
genera , 545 species, including 4 new genera, 76 new species.

186.
*************************************************
Shanwang Fossils
ɽÍú¹ÅÉúÎïͼ¼ø In Chinese and English bilingual
*************************************************
Sun Bo/1995/250x250mm/77pages£¬color photos/Paperback/$40

This book makes a systematic introduction to the animal and plant
fossils of
more than six handred species founded in the Shanwang Basin,
Shandong
Province since 1930s , and puts stress on the characters of the
ty1pical
genera and species of them. Besides, It revised several genera and
species
to some extent. There are 130 photographs in the book, and a
Latin-Chinese
index of the issued fossils is attached here.

187.
*******************************************************
Palaeontology of the HOH XIL Region, Qinghai
Çຣ¿É¿ÉÎ÷ÀïµØÇø¹ÅÉúÎï In Chinese with English summary
*******************************************************
Sha Jingeng/1995/270x190mm/177pages + 50 plates/Hardcover/$55

1 General Stratigraphical Situation 2 Palaeontology 2.1 Calcareous
Algae 2.2
Quaternary Sporo-pollen 2.3 Permian Foraminifers 2.4 Triassic
Foraminifers
2.5 Fusulinids 2.6 Radiolarians 2.7 Gastropods 2.8 Bivalves 2.9
Crinoids
2.10 Conodonts 2.11 Trace Fossils 2.12 Sponges and Problematical
Fossils 3
Biofacies, Sedimentary Characteristics and Palaeogeographical
Changes
4.
Explanation of Plates and Plates (1-50)

188.
************************************************************
Palaeotology of the Karakorum-Kunlun Mountains
¿¦À®À¥ÂØÉ½-À¥ÂØÉ½µØÇø¹ÅÉúÎï In Chinese with English summary
************************************************************
Wen Shixuan/1998/185x265mm/365 pages + 84 plates/Hardcover/$45

1.Stratigraphic outline in Karakorum and Kunlun Region
2.Palaeontological aspect in Karakorum and Kunlun Region
3.Devonian and Carboniferous foraminifers from northwest Qiangtang
4.Fusulinids from Karakorum and Kunlun Region
5.A radiolari assemblage of Middle Triassic from Karakorum Region
6.Palaeozoic corals from Karakorum Region
7.Lower Carboniferous and Middle Permian bryozoans from Karakorum
Region
8.Discovery of Early ordovician brachiopods of Yangtze type in
Karakorum
Region and its significance
9.Devonian brachiopods from Karakorum -Kunlun Region
10.Jurassic brachiopods from Karakorum Region and its
palaeobiogeographical
significance
11.Some fossil gsatropods from Karakorum - Kunlun Region
12.Some Trassic bivalves from Pamir and Karakorum Region
13.Some Jurassic bivalves in Pamir and Karakorum Region
14.Late Palaeozoic ostracods from Karakorum and Kunlun Region
15.Palaeozoic conodonts from northwest -Qingtang and Karakorum Region

189.
***********************************************
Paleontology of Ngari, Tibet (Xizang)
Î÷²Ø°¢Àï¹ÅÉúÎï In Chinese and English bilingual
************************************************
Yang Zunyi and Nie Zetong/1990/185x260mm/321 pages + 58
plates/Hardcover/$35

1. Preface 2. Introduction 3. Paleozoic Fossils of the Ngari Area 4.
Mesozoic Fossils of the Ngari Area 5. Tertiary Fossils of Ngari
Area,
Tibet
6. Conclusions 7. Referensis 8. English Text 9. Chinese-Latin Index
of
Genera and species 10. Explanation of plates 11. Plates

190.
*********************************************************************
*****************************
Palaeontology of Xizang(Book I)-The Series of the Scientific
Expedition
to
Qinghai-xizang Plateau
Î÷²Ø¹ÅÉúÎï µÚÒ»·Ö²á In Chinese with English summary
*********************************************************************
*******************************
Instituate Paleontology and Paleoanthropology, Chinese Academy of
Sciences/1980/180x260mm/106 pages + 30 plates/Hardcover/$25

This book contains 9 papers listed as following:
1.Preface 2. Forewords 3. Pliocene Stratum of Guizhong and Bulong
Basin,
Xizang 4. The Hipparion Fauna from Guizhong Basin, Xizang 5. The
Hipparion
Fauna of Bulong Basin, Biru, Xizang 6. The Quaternary Mammalian
Fossil
localities From Xizang 7. The Neolithic Human Skeletons and the
Cultural
Remains from Linzhi, Xizang 8. New discovery of the Microlithic
Materials
from North Xizang 9. Pollen-Spores Assemblages from localities of
Hipparion
Fauna in Xizang and Its Significance 10. The Environment of the
Pliocene of
Guizhong Basin, Xizang 11. An Analysis of the Pollen-Spores
Assemblages
and
the Age of the Stratum from Dati Palaeo-Lake Basin at
Nainnainxuonla,
South
Xizang

191.
*********************************************************************
**********************************
Palaeontology of Xizang(BOOK III) The Series of The Scientific
Expedition to
the Qinghai-Xizang Plateau
Î÷²Ø¹ÅÉúÎï µÚÈý·Ö²á In Chinese with English summary
*********************************************************************
**********************************
Nanjing Institute of Geology and Paleontology,Chinese Academy of
Sciences/1981/185x260mm/254 pages + 78 plates/Hardcover/$30

This book contains 13 papers listed as following:
1. Fusulinids from Xizang of China 2. Late Palaeozoic Bryozoans from
Xizang
3. Devonian Stromatoporoids from the Counties of Markam and Rutog in
Xizang
4. Upper Jurassic Stromatoporoids from Northern Xizang 5. Palaeozoid
Brachiopods from Xizang 6. The Mesozoic Brachiopods of Xizang 7.
Some
Nautiloids from Xizang 8. Some Triassic Ammonoids from Xizang 9.
Some
Early
Jurassic Ammonoids from Eastern Himalayas 10. Some Late Palaeozoic
Trilobites from Xizang 11. Upper Triassic Conchostracans form Qamdo
Region,
Xizang 12. Two New Species of Tertiary Insect Fossils from Northern
Xizang
13. Late Lower Cretaceous Fossil Decapoda from Lhasa Region, Xizang

192.
*********************************************************************
*********************************
Palaeontology of Xizang(Book IV)-The Series of the Scientific
Expedition to
the Qinghai-Xizang Plateau
Î÷²Ø¹ÅÉúÎï µÚËÄ·Ö²á In Chinese with English summary
*********************************************************************
*********************************
Nanjing Institute of Geology and Paleontology, Chinese Academy of
Sciences/1982/185x260mm/348 pages + 130 plates/Hardcover/$30

This book contains 17 papers listed as following:
1.Preface 2. Carboniferous and Permian Foraminifera of Xizang 3.
Some
Mesozoic Foraminifera from Xizang 4. Orbitolina (Foraminifera) from
Xizang
5. Fossil Radiolarians from Gyirong and Gyangze districts of
Southern
Xizang
6. Palaezoic Tabulate and Heliolitoid Corals from Xizang 7.
Palaeozoic
rugose corals from Xizang 8. Mesozoic Scleractinia Corals from
Xizang
9.
Mesoxoic Milleporina and Tabulatomorphic Corals from Xizang 10. Late
Palaeoxoic and Mesozoic fossil Sponges of Xizang 11. Mesozoic
Chaetetida
from Xizang 12. Some Mesozoic Spongiomorphoids from Xizang 13. Some
Fossil
Crinoids from Xizang 14. Some Late Palaeozoic and Triassic Bivalves
from
Xizang 15. Jurassic Bivalvia of Xizang 16. Some fossil Gastropods
from
Xizang 17. Mesozoic Coleoidea fauna from Xizang 18. Pliocene and
Quaternary
Ostracoda from Southern and Southwestern Xizang

193.
*********************************************************************
********************************
Palaeontology of Xizang(BOOK V)-the Series of the Scientific
expedition
to
the Qinghai-Xizang plateau
Î÷²Ø¹ÅÉúÎï µÚÎå·Ö²á In Chinese with English summary
*********************************************************************
********************************
Nanjing Institute of Geology and Paleontology,Chinese Academy of
Sciences/1982/185x260mm/240 pages + 91 plates/Paperback/$30

This book contains 10 papers listed as following:
1.Late Permian Plants from Northern Xizang 2.An Early Late Permian
Flora
from Toba, Qamdo District. Eastern Xizang 3.Fossil Plants from the
Upper
Triassic Tumaingela Formation in Amdo-Baqen Area, Northern Xizang
4.Late
Triassic Plants from Eastern Xizang 5.Tertiary Plants from Xizang
6.Sporo-Pollen Assemblage from the Tumaingela formation of Amdo,
Xizang
7.The Tertiary Sporo-Pollen Assemblages from Namling of Xizang
8.Early
Tertiary Palynoflora and Its Palaeogeography from Northern and
Eastern
Xizang 9.Cenozoic Charophyta from Xizang 10.Some Calcareous Algae
from
Xizang

194.
****************************************************************
The Palaeontological Atlas of South West China- Sichuan (Vol.1)
Î÷ÄϵØÇø¹ÅÉúÎïͼ²á-ËÄ´¨·Ö²á(Ò») Õ𵩼ÍÖÁÄàÅè¼Í In Chinese
****************************************************************
Southwest Geological Research Institute/1978/185x260mm/617 pages +
185
plates/Hardcover/$130

195.
***************************************************************
The Palaeontological Atlas of South West China Sichuan (Vol.2)
Î÷ÄϵØÇø¹ÅÉúÎïͼ²á-ËÄ´¨·Ö²á£¨¶þ£© In Chinese
****************************************************************
Southwest Geological Research Institute/1978/185x260mm/684 pages+191
plates/Hardcover/$85

196.
*******************************************************
Paleontological Atlas of Southwest China-Guizhou(Vol.1)
Î÷ÄϵØÇø¹ÅÉúÎïͼ²á(¹óÖÝ·Ö²á)(Ò») In Chinese
*******************************************************
1978/185x260mm/843 pages + 214 plates/Hardcover/$120

1. Archaeocyatha 2. Coelenterata 3. Brachiopoda Bumeril, 1806 4.
Mollusca 5.
Arthropoda 6. Hemichordata

197.
********************************************************
Paleontological Atlas of Southwest China-Guizhou(Vol.2)
Î÷ÄϵØÇø¹ÅÉúÎïͼ²á-¹óÖÝ·Ö²á (¶þ) In Chinese
*********************************************************
1978/185x260mm/638 pages + 165 plates/Hardcover/$120

198.
******************************************************************
Paleontological Atlas of Southwest China (Volume of Microfossils )
Î÷ÄϵØÇø¹ÅÉúÎïͼ²á-΢Ìå¹ÅÉúÎï·Ö²á In Chinese
******************************************************************
Chengdu Institute of Geology and Mineral
Resources/1983/185x260mm/802
pages
+ 164 plates/Hardcover/$120

1. Preface 2. Tables of Stratigraphical Correlation and their
Explanation 3.
Description of fossils (1) Kindom Animal a. Phylum Arthropoda b.
Conodont
(2) Kingdom Plant a. Sinian and Cambrian micropalaeoflora b.
Mesozoic
Spore-pollen c. Cenozoic Spore-pollen 4. Plates

199.
*********************************************************************
*****
Paleontological Atlas of Northwest China -Shaanxi-Gansu-Ningxia
Volume
(I)
Î÷±±µØÇø¹ÅÉúÎïͼ²á-ɸÊÄþ·Ö²á (Ò») In Chinese
*********************************************************************
******
Xian Institute of Geology and Mineral/1982/185x260mm/480 pages + 106
plates/Hardcover/$89

1. Preface 2. Editorial Explanation 3. Description of Fossils (1)
Phylum
Archaeocyatha (2) Phylum Coelenterata (3) Phylum Bryozoa (4) Phylum
Brachiopoda
(5) Phylum Mollusca (6) Phylum Anthropoda (7) Phylum Hemichordata
(8)
The
stromatolites 4. Index of Genera and Species 5. Plates with
explanation
of
plates 1-106

200.
*********************************************************************
**********
Paleontological Atlas of Northwest China-Shaanxi, Gansu and Ningxia
Volume
(II)
Î÷±±µØÇø¹ÅÉúÎïͼ²á-ɸÊÄþ·Ö²á(¶þ) In Chinese
*********************************************************************
**********
Xi'an Institute of Geology and Mineral Reslurces/1983/185x260mm/659
pages +
183 plates/Hardcover/$120

1. Preface 2. Editorial Explanation 3. Description Fossils (1)
Phylum
Protozxoa (2) Phylum Coelenterata (3) Phylum Bryozoa (4) Phylum
Brachiopoda
(5) Phylum Mollusca (6) Phylum Arthropoda (7) Phylum Chordata 4.
Index
of
Genera and Species 5. Plates (with explanation of plates 1-183) 6.
Correlation charts of the Devonian, Carboniferous and Permian in
Shaanxi,
Gansu and Ningxia

201.
*********************************************************************
***********************************
Paleontological Atlas of Northwest China -Shaanxi Gansu Ningxia
Volume)
Part
III-Mesozoic and Cenozoic
Î÷±±µØÇø¹ÅÉúÎïͼ²á-ɸÊÄþ·Ö²á(Èý) In Chinese
*********************************************************************
************************************
Xi'an Institute of Gology and Mineral Resources/1982/185x260mm/181
pages +
75 plates/Hardcover/$50

CONTENTS 1. Preface 2. Editorial Explanation 3. Description of
Fossils
(1)
Phylum Brachiopoda (2) Phylum Mollusca (3) Phylum Arthropoda (4)
Phylum
Echinodermata (5) Phylum Chordata (6). Phylum Spermatophyta 4. Index
of
Genera and Species 5. Plates (with explanation of plates 1-75) 6.
Correlation charts of the Devonian, Carboniferous and Permian in
Shaanxi,
Gansu and Ningxia (1-4)

202.
*********************************************************************
***
The Palaeontological Atlas of North West China-Xinjiang (Vol.1)
Î÷±±µØÇø¹ÅÉúÎïͼ²á-н®Î¬Îá¶û×ÔÖÎÇø·Ö²á(1):ÍíÔª¹Å´ú-Ôç¹ÅÉú´ú In
Chinese
*********************************************************************
****
Geological Burea of Xijiang/1981/185x260mm/331 pages +92
plates/Hardcover/$56

203.
****************************************************************
The Palaeontological Atlas of North West China-Xinjiang (Vol.2)
Î÷±±µØÇø¹ÅÉúÎïͼ²á-н®Î¬Îá¶û×ÔÖÎÇø·Ö²á(2):Íí¹ÅÉú´ú In Chinese
***************************************************************
Geological Burea of Xinjiang/1983/185x260mm/785 pages +226
plates/Hardcover/$89

204.
***************************************************************
The Palaeontological Atlas of North West China-Xinjiang (Vol.3)
Î÷±±µØÇø¹ÅÉúÎïͼ²á-н®·Ö²á-3 In Chinese
***************************************************************
Geological Burea of Xinjiang/1984/185x260mm/211 pages + 81
plates/Hardcover/$55

1. Non-Marine Bivalvia 2. Marine Bivalvia 3. Cephalopoda 4.
Gastropoda
5.
Echinodermata 6. Brachiopoda 7. Arthropoda 8. Cordata 9.
Pteridophyta
10.
Gymnospermae 11. Plantae Insertae sedis

205.
******************************************************
Paleontological Atlas of Northwest China -Qinghai (I)
Î÷±±µØÇø¹ÅÉúÎïͼ²á-Çຣ·Ö²á(Ò») In Chinese
*******************************************************
Geological Burea of Qinghai/1979/185x260mm/393 pages + 96
plates/Hardcover/$90

206.
******************************************************
Paleontological Atlas of Northwest China -Qinghai (II)
Î÷±±µØÇø¹ÅÉúÎïͼ²á-Çຣ·Ö²á(¶þ) In Chinese
******************************************************
Geological Burea of Qinghai/1979/185x260mm/219 pages + 82
plates/Hardcover/$80

207.
******************************************************************
Palaeontological Atlas of Central South China (1)-Early Paleozoic
ÖÐÄϵØÇø¹ÅÉúÎïͼ²á£¨Ò»£©Ôç¹ÅÉú´ú In Chinese
*******************************************************************
By Hubei Institute of Geology and
Science/1977/190x260mm/470pages+116plates/Hardcover/$85

CONTENTS 1. Preface 2. Editorial Explanation 3. Description of
Fossils
(1)
Phylum Archaeocyatha (2) Phylum Coelenterata (3) Phylum Bryozoa (4)
Phylum
Brachiopoda (5) Phylum Mollusca (6) Phylum Arthropoda (7) Phylum
Hemichordata 4. Correlation charts of the stratigraphy 5. Plates
(with
explanation of plates 1-116) 6. Index of Genera and Species

208.
*****************************************************************
Palaeontological Atlas of Central South China (2)-Late Paleozoic
ÖÐÄϵØÇø¹ÅÉúÎïͼ²á£¨¶þ£©Íí¹ÅÉú´ú In Chinese
*****************************************************************
By Hubei Institute of Geology and
Science/1977/190x260mm/856pages+253plates/Hardcover/$130

CONTENTS 1. Preface 2. Editorial Explanation 3. Description of
Fossils
(1)
Phylum Protozoa (2) Phylum Coelenterata (3) Phylum Bryozoa (4)
Phylum
Brachiopoda (5) Phylum Mollusca (6) Phylum Arthropoda (7) Phylum
Echinoderm
(8) Phylum Hemichordata (9) Phylum Pteridophyta (10) Phylum
Spermatophyta
4. Index of Genera and Species 5. Plates (with explanation of plates
1-253)
6. Correlation charts of the Central South China¡¯s Stratigraphy

209.
*********************************************************************
**
Palaeontological Atlas of Central South China (3)-Mesozoic and
Cenozoic
ÖÐÄϵØÇø¹ÅÉúÎïͼ²á£¨Èý£©ÖÐÐÂÉú´ú In Chinese
*********************************************************************
**
By Hubei Institute of Geology and
Science/1977/190x260mm/332pages+107plates/Hardcover/$70

CONTENTS 1. Preface 2. Editorial Explanation 3. Description of
Fossils
(1)
Phylum Brachiopoda (2) Phylum Mollusca (3) Phylum Echinoderm (4)
Phylum
Chordata (5) Phylum Pteridophyta (6) Phylum Arthropoda (7) Phylum
Spermatophyta 4. Index of Genera and Species 5. Plates (with
explanation of
plates 1-107) 6. Correlation charts of the Central South China¡¯s
Stratigraphy

210.
***************************************************************
Palaeontological Atlas of Central South China (4)-Microfossil
ÖÐÄϵØÇø¹ÅÉúÎïͼ²á£¨ËÄ£©Î¢Ì廯ʯ In Chinese
***************************************************************
By Hubei Institute of Geology and
Science/1978/190x260mm/765pages+167plates/Hardcover/$150

CONTENTS 1. Preface 2. Editorial Explanation 3. Description of
Fossils
(1)
Phylum Protozoa (2) Phylum Arthropoda (3) Phylum Gymnospermae (4)
Phylum
Bryophyta (5) Phylum Pteridophyta (6) Phylum Gymnospermae (7) Phylum
Anglospermae 4. Index of Genera and Species 5. Plates (with
explanation
of
plates 1-167) 6. Correlation charts of the Central South China¡¯s
Stratigraphy

211.
******************************************************************
Paleontological Atlas of North China (1) Paleozoic Volume
»ª±±µØÇø¹ÅÉúÎïͼ²á£¨Ò»£©¹ÅÉú´ú·Ö²á In Chinese with English summary
*******************************************************************
Tianjin Institute of Geology and Mineral
Resources/1985/185x260mm/731
pages
+ 205 plates/Hardcover/$150

In this book there is immense amount of fossil collection and
intensive
researching for Cambrian-Permian fossils in Shanxi, Hebei and Inner
Mongolia
Autonomous Region, thus a composite Palaeozoic succession is
established.
Part I. Animal 1. Protozoa 2. Coelenterata 3. Bryozoa 4. Brachiopoda
5.
Mollusca 6. Arthropoda 7. Echinodermata 8. Hemichordata 9. Chordata
Part II. Late palaeozoic era 1. Pteridophyta 2. Gymnospermae 3.
Incertae
Sedis

212.
***************************************************************
Palaeontological Atlas of North China (Vol.2) Mesozoic
»ª±±µØÇø¹ÅÉúÎïͼ²á(¶þ)ÖÐÉú´ú·Ö²á In Chinese with English summary
***************************************************************
Tianjin Institute of Gology and Mineral Resources/1984/185x260mm/384
pages
+178 plates/Hardcover/$78

1. Prefer 2. Stratigraphy 3. Systematic Dscription (1) Kingdom
Animal
(2)
Kingdom Plant 4. Index of Genera and Species 5. English Abstract
6. Plate and its Expanation 1-178

213.
*********************************************************************
Paleontological Atlas of North China (Vol.3) Micropaleontological
»ª±±µØÇø¹ÅÉúÎïͼ²á(Èý) ΢Ìå¹ÅÉúÎï·Ö²á In Chinese with English summary
*********************************************************************
1984/185x260mm/857 pages + 218 plates/Hardcover/$135

This volume includes Foraminifera, Ostracoda, Conodonts, Charophyte,
Spores
and pollen. They contain 450 gnera and 1774 species, among them 19
genera
(subgenera) and 501 species (subspecies), 47 combination species are
identified as new.
1. Preface 2. Stratigraphy 3. Systemmatic desceription (1)
Foraminifera
(2)
Ostracoda (3) Conodonts (4) Charophyte (5) Spores and Pollen 4.
Index
of
Genera and species 5. English Abstract 6. Plates (1-218) with
explanations
of plates

214.
********************************************************
Paleontological Atlas of North China-Inner Mongolia (1)
»ª±±µØÇø¹ÅÉúÎïͼ²á-ÄÚÃɹŷֲá (Ò») In Chinese
********************************************************
Inner Mongolia Institute of Geology/1976/185x260mm/502 pages + 232
plates/Hardcover/$120

215.
********************************************************
Paleontological Atlas of North China-Inner Mongolia(2)
»ª±±µØÇø¹ÅÉúÎïͼ²á-ÄÚÃɹŷֲá(¶þ) In Chinese
********************************************************
Inner Mongolia Institute of Geology/1976/185x260mm/261 pages + 120
plates/Hardcover/$65

216.
*************************************************************
Paleontological Atlas of Northeast China (Paleozoic Volume)
¶«±±µØÇø¹ÅÉúÎïͼ²á£¨Ò»£© In Chinese
*************************************************************
Shenyang Institute of Geology and Mineral
Resources/1980/185x260mm/686
pages
+ 261 plates/Hardcover/$150

1. Preface 2. Summary of Stratigraphy 3. Description of Fossils (1)
Phylum
Protozoa (2) Phylum Porifera (3) Phylum Coelenterata (4) Phylum
Bryozoa
(5) Phylum Brachiopoda (6) Phylum Mollusca (7) Phylum Anthropoda (8)
Phylum
Echinodermata (9) Phylum Hemichorodata (10) The Vegetable Kingdom 4.
Index
of Genera and Species 5. Plates (with explanation of plates 1-261)

217.
******************************************************************
Paleontological Atlas of Northeast China (II) Mesozoic and Cenozic
¶«±±µØÇø¹ÅÉúÎïͼ²á(¶þ)ÖÐÐÂÉú´ú·Ö²á In Chinese
******************************************************************
Shenyang Institute of Geology and Mineral/1980/185x260mm/403 pages +
210
plates/Hardcover/$110

1. Preface 2. Summary of Stratigraphy 3. Description of Fossils (1)
Phylum
Mollusca (2) Phylum Arthropoda (3) Phylum Chordata (4) Kingdom Plant
(5)
Phylum Bryophyta (6) Phylum Pteridophyta (7) Phylum Spermatophyta 4.
Index
of Genera and Species 5. Plates with Explanation of Plates

218.
***********************************************************
Paleontological Atlas of East China (Vol.1)-Early Paleozoic
»ª¶«µØÇø¹ÅÉúÎïͼ²á(Ò») Ôç¹ÅÉú´ú·Ö²á In Chinese
***********************************************************
Nanjing Institute of Geology and Mineral
Resources/1983/185x260mm/657
pages
+176 plates/Hardcover/$95

1. Coelenterata 2. Arthropoda 3. Brachiopoda 4. Mollusca 5.
Echinodermata 6.
Hmichordata 7. Chordata

219.
******************************************************
Paleontological Atlas of East China(2)-Late Paleozoic
»ª¶«µØÇø¹ÅÉúÎïͼ²á£¨¶þ£©Íí¹ÅÉú´ú·Ö²á In Chinese
*******************************************************
Nanjing Institute of Geology and Mineral
Resources/1982/190x265mm/495
pages+157 plates/Hardcover/$78

I.Animals 1.Protozoa 2.Coelenterata 3.Bryozoa 4.Brachiopoda
5.Mollusca
6.Arthropoda 7.Chordata II.Botany 1.Pteridophyta 2.Spermatophyta

220.
*****************************************************************
Paleontological Atlas of East China (Vol.3)-Mesozoic and Cenozoic
»ª¶«µØÇø¹ÅÉúÎïͼ²á(Èý) ÖС¢ÐÂÉú´ú·Ö²á In Chinese
*****************************************************************
Nanjiang Institute of Geology and Minral
Resources/1982/185x260mm/405
pages+
144 plates/Hardcover/$87

1. Mollusca (1) Lamellibranchiata (2) Gastropoda (3) Cephalopoda 2.
Arthropoda (1) Crustacea (2) Insecta 3. Chordata (1) Osteichthyes
(2)
Amphibia (3) Reptilia (4) Aves (5) Mammalia 4. Bryophyta 5.
Pteridophyta (1)
Lycopsida (2) Sphenopsida (3) Filices 6. Spermatophyta (1)
Pteridospermae
(2) Cycadopsida (3) Ginkgopsida (4) Coniferopsida (5) Dicotyledoneae

221.
*********************************************************************
Biostratigraphy of the Yangtze Gorge Area (1) Sinian
³¤½­ÈýÏ¿µØÇøÉúÎïµØ²ãѧ£¨1£©Õ𵩼ͷֲá In Chinese with English summary
*********************************************************************
Zhao Ziqiang/1985/185x260mm/143 pages + 21 plates/Paperback/$25

1. Preface 2. Introduction 3. Stratigraphic Sections 4. Basic
Features
of
Biota 5. Sedimentology and sedimentary environment 6. Glacier strata
7.
Time
of Sinian 8. Magnetic geology 9. Subdivision of Sinian and the
top.bottom
boundary 10. The stratigraphical correlation of home and abroad 11.
Abstract
English translation 12. Plates and explanation

222.
*********************************************************************
*
Biostratigraphy of The Yangtze Gorge Area (2) Early Palaeozoic
³¤½­ÈýÏ¿µØÇøÉúÎïµØ²ãѧ(2) Ôç¹ÅÉú´ú·Ö²á In Chinese with English summary
*********************************************************************
**
Wang Xiaofeng/1987/185x260mm/641 pages + 72 plates/Hardcover/$43

1. Archaeocyatha 2. Anthozoa 3. Brachiopoda 4. Cephalopoda 5.
Trilobita
6.
Ostracoda 7. Graptolithina 8. Conodonts 9. Small Shell Fossils 10.
Microflora

223.
*********************************************************************
**
Biostratigraphy of the Yangtze Gorge Area (3) Late Palaeozoic Era
³¤½­ÈýÏ¿µØÇøÉúÎïµØ²ãѧ£¨3£©Íí¹ÅÉú´ú·Ö²á In Chinese with English
summary
*********************************************************************
***
Feng Shaonan/1984/185x260mm/411 pages + 52 plates/Paperback/$42

1. Protozoa 2. Coelenterata 3. Brachiopoda 4. Mollusca 5. Arthropoda
6.
Bryophyta 7. Pteridophyta et Pteridospermopsida 8. Gymnospermae

224.
*********************************************************************
****************************************
Scientific Expedition Report on Mount Qomolangma Region-Part
Paleontology (
3 volumes) in Chinese (Used book)
ÖéÄÂÀÊÂê·åµØÇø¿ÆÑ§¿¼²ì±¨¸æ£¨1966-1968£©¹ÅÉúÎï(3 ¾í£© In Chinese
*********************************************************************
****************************************
1975/185x260mm/457/Hardcover/$35

225.
**************************
Biostratigraphy of China
In English
**************************
Zhang Wentang/2003/285x210mm/599 pages/Hardcover/$120

This book consists of 13 chapters, which cover the 13 major
geological
systems. Each chapter addresses: 1. Tectonic sedimentary domains; 2.
Current
biostratigraphic scheme; 3. Series boundaries; 4. Faunal and/or
floral
succession, evolutionary trends and bioevents; 5. Correlation of the
standard columns in China with other part of the World; 6. Facies
patterns;
7. Palaeo- biogeography and palaeogeography 8. Discusion of other
significant topics; 9. References. Because the text is in English,,
it
will
generate tremendous interest from and influence upon the earth
sciences
community around the world.

226.
***************************************************
Stratigraphy and paleontology of China (2 Vol. set)
In English
***************************************************
Yang Zunyi/1994/260x184mm/Hardcover/$98

This book is a new one of the national Publications sponsored by the
Commission on Stratigraphy & Paleontology under the Geological
Society
of
China . It aims at recording new advances in the study of
Stratigraphy
and
paleontology and their related subjects. Meanwhile, with emphases on
those
topics relating to global geology it will also embody some
comprehensive
themes in order to help the foreign readers who are not familiar
with
China
to know the geology of China . Volume 1 covers nine papers
concerning
the
records to foraminifers , brachiopods, bivalves and conodonts a
synthesis of
Famennian stratigraphy of South China; discussion on the boundaries
of
Cambrian and Ordovician and others . Volume 2 published in August
1994
Trilobita, Brachiopods, Coral, Stromatoporoids, Calcareous
nannofossils,
Conodonts and Graptolite, thermal maturity and others.

227.
***************************************************
Micropalaeontology of the Qiangtang Basin
ǼÌÁÅèµØÎ¢Ìå¹ÅÉúÎï In Chinese with English summary
**************************************************
Sha Jingeng/2005/190x270mm/292 pages +53 plates/Hardcover/$45

Chapter 1 Algae
Section 1 Jurassic Charophytes from Haixi, Hoh Xil
Section 2 Some Cenozoic Charophytes from Amdo
Section 3Middle to Early Late Eocene Charophytes Flora from Baingion
Section 4 Middle to Late Jurassic Marine Dinoflagellates from Haixi
Chapter 2 Pollen and Spores
Section 1 Late Triassic Palynological Assemblage from Shuanghu
Section 2 Middle Jurassic Palynological Assemblage from Amdo
Section 3 Late Jurassic Palynological Assemblage from Baingoin
Section 4 Early Cretaceous Palynoligical Assemblage from Baingoin
Section 5 Tertiary Palynological from Amdo
Chapter 3 protozoans
Section 1 Jurassic Foraminifers from Amdo
Section 2 Late Cretaceous Radiolarians from Xigaze
Chapter 4 Ostracods
Section 1 Jurassic Ostracods from Haixi and Other Regions
Section 2 Ostracods of the ¡°Shuanghu Formation ¡°from Amdo
Chapter 5 Conodonts
Section 1 Early Triassic Conodonts from Nyima
Section 2Triassic Conodonts Across the base and Top of the Middle
Triassic
Series from Nyalam

228.
*********************************************************************
*****************
Tertiary Stratigraphy and Micropaleontology of the Central Hebei
Pertroliferous Area
¼½ÖÐÓÍÆøÇøµÚÈý¼ÍµØ²ã¼°Î¢Ìå¹ÅÉúÎï In Chinese
*********************************************************************
******************
Cai Zhiguo/1998/210x290mm/550 pages+143 plates/Hardcover/57

Central Hebei petroliferous area is a large oil-and gas-bearing
depression
located in the western part of the Bohai Gulf Basin. Tertiary strata
are
well developed in this area consisting of the Kongdian, hahejie,
Dongying,Guantao, and Minhuazhen formation in ascending order. In
the
present paper,244 genera and 888 species of Ostracods, gastropods,
foraminifers, dinoflogellales, acritarchs, and pollen and spores
have
been
described.Three distinct shifts of depositional center have occurred
during
this period, leading to three sets of excellent oil-generating
formations
which contain abundant oil and gas resources

229.
***********************************
Marine Micropaleontology of China
In English
**********************************
Wang Pinxian/1985/285x185mm/70/Hardcover/65

230.
*********************************************************************
**************************
esearch on Micropalaeontology and Paleoceanography in Pearl River
Mouth
Basin, South China Sea
ÄϺ£Öé½­¿ÚÅèµØµÚÈý¼Í΢Ìå¹ÅÉúÎï¼°¹Åº£ÑóÑо¿ In Chinese with English
summary
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ao Yichun/1996/185x260mm/36 pages +20plates/Paperback/38

231.
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Acta Palaeontologica Sinica vol.40(Sup.) ¨C The Cambrian of South
China
¹ÅÉúÎïѧ±¨ µÚ40¾í2001 Ôö¿¯ ¨C »ªÄϺ®Îäϵ In English
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LiXing-xue/2001/210x290mm/240pages/Paperback/$39

CONTENTS
1. Preface
2. The international subcommission on Cambrian stratigraphy:
progress
report
2001
3. Early Cambrian stratigraphy of east Yunnan, southwestern China: A
Synthesis
4. Litho- and biostratigraphy of the lower Cambrian meishucunian
stage
in
the Xiaotan section ,eastern Yunnan
5. The Meishucunian stage and its small shelly fossil sequence in
China
6. The lower Cambrian of eastern Yunnan: Trilobite-based
biostratigraphy and
related faunas
7. Sedimentary environments of the early Cambrian Chengjiang biota:
sedimentology of the Yu¡¯anshan formation in Chengjiang county,
eastern
Yunnan
8. Litho-and biostratigraphy of the lower Cambrian Yu¡¯anshan
formation
near
the village of ercaicun, Haikou county, Eastern Yunnan province,
China
9. Biostratigraphy of archaeocyathan horizons in the lower Cambrian
Fucheng
section, south Shaanxi province: Implications for regional
correlations
and
archaeocyathan evolution
10. A potential GSSP for the lower and middle Cambrian boundary near
Balang
village, Taijiang county, Guizhou province China
11. Biostratigraphy of oryctocephalid trilobites
12. Potential global stratotype section and point for the base of an
upper
Cambrian series defined by the first appearance of the trilobite
glyptagnostus reticulateus, Hunan province, China
13. Middle and upper Cambrian slope deposits in the Wa¡¯ergang
section,
Taoyuan county, Northwestern Hunan province, South China
14. New extraordinarily preserved enigmatic fossils, possibly with
ediacaran
affinities, from the lower Cambrian of Yunnan, China
15. Notes on the classification and phylogeny of oryctocephalids(
Trilobita:
Arthropoda)
16. Discrete sclerites of Microdictyon(Lower Cambrian ) from the
Fucheng
section, Nanzheng, South Shaanxi
17. Primitive ptychoparioids from southern Anhui province, south
China.


The Series of Paleontologia Sinica are as follows:

232.
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Paleontologia Sinica (Series B, Volume 1, Fascicle 1) Ordovician
Fossils
from North China
Öйú±±²¿°ÂÌռͶ¯Îﻯʯ In English
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Amadeus W. Grabau S. D/1922/220x290mm/100 pages + 9
plates/Paperback/$120

1. Introduction 2. Stratigraphic summary (1) Fauna of the Machiakou
or
Actinoceras limestone (2) Lower Ordovician 3. Description of Species
(1)
Anthozoa
(2) Brachiopoda (3) Pelecypoda (4) Gastropoda (5) Cephalopoda (6)
Trilobita
4. Bibliography 5. List of Chinese localities referred to in the
text,
arranged alphabetically under the several provinces 6. Explanation
of
Plates

233.
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Paleontologia Sinica (Series B, Volume I, Fascicle 2) The Ordovician
Cephalopoda of Central China
ÖйúÖв¿°ÂÌÕ¼ÍÍ·×ãÀ໯ʯ In English
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C. C. Yu/1930/220x290mm/71 pages + 9 plates/Paperback/$89

1. Introduction 2. Terminology 3. Stratigraphy (1) Comparison of the
Ordovician beds in the different localities of Hupeh (2) The
geological
horizon of the so-called Neichiashan and Ichang formations (3) The
relationship between the Ordovician cephalopoda from Hupeh, central
China,
and those from the corresponding horizon in the northern as well as
southern
China 4. Description of Species (1) Genus Cameroceras Conrad (emend.
Hyatt)(2) Genus Endocerus Hall (3) Genus Vaginoceras Hyatt (4) Genus
Orthoceras Breyn (5) Genus Protocycloceras Hyatt (6) Genus
Cycloceras
M'coy
(7) Genus Discoceras Barrande
(8) Genus Lituites Brogniart (9) Genus Oncoceras Hall 5.
Bibliography
6.
Explanation of plates

234.
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Paleontologia Sinica (Series B, Volume I, Fascicle 4) Contributions
to
the
Cambrian Faunas of North China
Öйú±±²¿º®Îä¼Í¶¯Îﻯʯ In English
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Y. C. Sun/1924/220x290mm/90 pages + 5 plates/Paperback/$110

1. Introductin 2. Stratigraphic Summary (1) Chihli (2) Shantung (3)
Fengtien
3. Descripton of Species (1) Graptozoa (2) Annelida (3) Brachiopoda
(4)
Trilobita 4. Bibliography 5. List of Chinese localities referred to
in
the
text, arranged alphabetically under the several provinces 6.
Explanation of
Plates

235.
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Paleontologia Sinica (Series B, Vol 2, Fas 1)Palaeozoic Corals of
China
(Part I)Tetraseptata I
Öйú¹ÅÉú´úɺº÷»¯Ê¯ (Ò») In English
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Amadeus W. Grabau S. D/1922/220x290mm/69 pages + 1 plates/Paperback/
$95

1. Introduction
2. Descriptions of Families, Genera, and Species
(1) Suborder: Proteroseptata Graban
3. Explanation of Plate I

236.
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Paleontologia Sinica (Series B, Vol2, Fas 2)Palaeozoic Corals of
China
(Part
I)-Tetraseptata II Second Contribution to our Knowledge of the
Streptelasmoid Corals of China and Adjacent Territories
Öйú¹ÅÉú´úɺº÷»¯Ê¯¾í¶þ In English
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Amadeus W. Grabau/1928/220x290mm/151 pages + 6 plates and 22
Text/Hardcover/$280

1. Introduction 2. Discussion of Families and Genera with
description
of new
species (1) Family Petraiidae de Koninck (emend. Grabau) (2)
Aberrant
derivatives of the Petraiidae (3) Family Polycoelidae Roemer (4)
Family
Streptelasmaidae (emend. Gr) (5) The Genera Tachylasma Grabau,
Plerophyllum
Hinde, Pentaphyllum de Koninck, Plerophyllum Gerth, Cryptophyllum
Carruthers, Oligophyllum Pocta, and Ufimia Stuckenberg (6) Summary
3.
Table
of the Distribution of the Families, Subfamilies, Genera, Species
and
varieties described Including those described in Fascicle I 4.
Literature 5.
Explanation of Plates

237.
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Paleontologia Sinica (Series B, Volume II, Fascicle III) On the
Seasonal
Growth in Palaeozoic Tetracorals and the Climate During the Devonian
Period
¹ÅÉú´úËÄÉäɺº÷³É³¤Éϵĵļ¾ºò±ä»¯ÓëÄàÅè¼ÍµÄÆøºò In English
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***********
Ting Ying H. MA/1937/220x290mm/50 pages + 22 plates/Paperback/$90

1. Introduction
2. The Character of Seasonal Change in Growth
3. Measurement of Annual Length in Growth
4. Summary
5. Devonian Equator
6. Bibliography
7. Explanation of Map
8. Explanation of Plates

238.
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Palaeontologia Sinica (Series B, volume III, Fascicle 1) Lower
Ordovician
Trilobite fauna of Chekiang
Öйú¹ÅÉúÎïÖ¾-Õ㽭ϰÂÌÕ¼ÍÖ®ÈýÒ¶³æ»¯Ê¯ In English
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S.F.Sheng/1934/220x290mm/19 pages+4 plates/Paperback/$55

1. Introduction
2. Description of species
(1) Family Asaphidae Burmeister
(2) Family Illaenidae Corda
(3) Family Taihungshanida Sun
3. Bibliography
4. Explanation of Plates

239.
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Paleontologia Sinica : Series B, Vol.3 Fascicle 2 Silurian Faunas of
Eastern
Yunnan
ÔÆÄ϶«²¿Ö¾Áô¼Í¶¯Îﻯʯ In Chinese
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1926/210x280mm/91 pages + 4 plates/Hardcover/$100

The first Silurian fossils from Yunnan were described by Mansuy in
1912
in
his Paleontology of Eastern yunnan (Mansuy 1912) , but through a
misinterpretation of the stratigraphic relationships they were
originally
referred to the " Lower Silurian" i.e. Ordovician. Subsequently, in
1919,
this mistake was rectified by Mansuy in his Catalogue General
(Mausuy
1919)
where he referred these faunas to the Gothandian or Silurian in the
modern
sense. Mansuy described Silurian fossils from two localities in
Eastern
Yunnan. The first of these are from deposits in the vicinity of
Si-yang-tang, north-east of Yunnan-fu, where they occur at several
levels in
strata which are probably all referable to the Upper Silurian or
Monroan.
The beds apparently rest by overlap on the Cambrian, on which
account
they
were originally mistaken for Ordovician. The stratigraphy of the
region
is
still little known.
1. The Mientien Group
2. The Miaokao Group
3. Description of Species
4. Bibliography
5. Errata
6. Explanation of Plate I
7. Explanation of Plate II
8. Explanation of Plate III
9. Explanation of Plate IV

240.
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Paleontologia Sinica (Series B, Volume III, Fascicle 3) Devonian
Brachiopoda
of China I. Devonian Brachiopoda from Yunnan and Other Districts in
South
China
ÖйúÄàÅè¼Íòê×ãÀ໯ʯ(¾íÒ») In English
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Amadeus W. Grabau S. M. S. D/1931/220x290mm/545 pages with 54 plates
and 67
Text figure/Hardcover/$380

1. Introduction
2. Description of Species
(1) Order Atremata Beecher
(2) Order Neotremata Beecher
(3) Order Protremata Beecher
(4) Order Telotremata Beecher
3. Index to genera and species of Brachiopoda

241.
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Paleontologia Sinica (Series B, Volume V, Fascicle 1) Crinoids from
the
Taiyuan Series of North China
Öйú±±²¿Ì«Ô­Ïµº£°ÙºÏ»¯Ê¯ In English
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C. C. Tien/1926/220x290mm/51 pages + 3 plates/Paperback/$66

1. Introduction
(1) Previously Described Shpecies-I China
(2) Foreign Countries
2. Description of Genera and Species
3. Appendix
4. Bibliography
5. Explanation of Plate I
6. Explanation of Plate II
7. Explanation of Plate III

242.
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Paleontologia Sinica (Series B, Vol.5. Fascicle 3) Productidae of
China
(Part II) Chonetinae, Productinae and Richthofeninae
Öйú³¤Éí±´¿Æ»¯Ê¯(¾íÏÂ) In English
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Y.T. Chao/1928/220x290mm/81 pages + 6 plates/Paperback/$88

1. Subfamily Chonetine Waagen 2. Subfamily Productine Waagen 3.
Subfamily
Richthofenine Stoyanow 4. Table showing Distribution and Range of
Productids
in China 5. Explanation of Plate I 6. Explanation of Plate II 7.
Explanation
of Plate III 8. Explanation of Plate IV 9. Explanation of Plate V
10.
Explanation of Plate VI

243.
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Paleontologia Sinica (Series B. Vol IX, Fascicle I)Late Permian
Brachiopoda
of Southwestern China
ÖйúÎ÷Äϲ¿ºóÆÚ¶þµþ¼ÍÖ®Íó×ãÀà In English
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T.K.Huang/1932/230x290mm/107 pages + 9 plates/Hardcover/$150

1. Introduction 2. Description of Genera and Species (1) Family
Productidae
Gray (2) Family Lyttoniidae Zittel 3. Bibliography 4. Explanation of
Plates

244.
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Paleontologia Sinica (Series B. Vol. XI, Fascicle S) Cephalopoda of
the
Penchi and Taiyuan Series of North China
Öйú±±²¿±¾ÏªÏµ¼°Ì«Ô­ÏµÖ®Í·×ãÀ໯ʯ In English
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T.H.Yin/1933/230x290mm/32 pages + 5 plates/Hardcover/$80

1. Introducetion 2. Stratigraphical Summary 3. Description of
Species
(3)
Order Nautiloidea (4) Order Ammonoidea 4. Bibliography 5. Appendix

245.
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Paleontologia Sinica (Series B, Volume XII, Fascicle 5) Weiningian
(Middle
Carboniferous) Corals of China
ÖйúÖÐʯ̿¼ÍÍþÄþϵɺº÷»¯Ê¯ In English
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Yungshen S. Chi/1931/220x290mm/54 pages + 5 plates/Paperback/$78

1. Introduction 2. Discussion of Families and genera with
Description
of New
Species (1) Family Polycoellde Roemer (2) Family Lophophyllide Grabau
(3) Family Zaphrentide E. & H. (emend. Grabau) (4) Family
Cyathophyllide E.
& H (emend. Grabau) (5) Family Lithostrotiontide Grabau (6) Aberrant
Lithostrotiontide of Uncertain Affinities (7) Family Lonsdaleiide
Grabau (8)
Family Syringoporide E. & H (9) Family Moniloporide Grabau (10)
Family
Chaetetide E. & H 3. Table Showing the Distribution of the
Weiningian
(Middle Carboniferous) Corals of China 4. Literature 5. Explanation
of
Plates

246.
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Paleontologia Sinica (Series B, Volume XII, Fascicle 6) Additional
Fossil
Corals from the Weiningian Limestones of Hunan, Yunnan and Kwangsi
Provinces
in SW. China
Ôö²¹ºþÄÏÔÆÄϹãÎ÷Èýʡ֮ÍþÄþϵɺº÷»¯Ê¯ In English
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Yungshen S. Chi/1935/220x290mm/28 pages + 3 plates/Paperback/$55

1. Introduction 2. Stratigraphical Summary 3. Description of Genera
and
Species (1) Order Tetraseptata Grabau (2) Order Aseptata Crabau 4.
Table
Showing the Distribution of the Weiningian (Middle Don-Bassian)
Corals
of
China 5. Explanation of Plates

247.
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Paleontologia Sinica (Series B, Volume XIV, Fascicle 1) Ordovician
and
Silurian Graptolites from China
Öйú°ÂÌռͼ°Ö¾Áô¼ÍÖ®±Êʯ In English
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Y. C. Sun/1933/220x290mm/52 pages + 7 plates/Paperback/$65

1. Introduction 2. Descriptionof Species (1) Order Dendroidea
Nicholson
(2)
Order Graptoloidea Lapworth (3) General List of Fossils 3. Conclusion
4. Bibliography 5. Explanation of Plates

248.
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Paleontologia Sinica (Series B. Vol. Xiv, Foscicle 2)Lower
Ordovician
Graptolite-Faunas of North China
Öйú±±²¿Ï°ÂÌÕ¼ÍÖ®±Êʯ In English
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Y.C. Sun/1935/225x300mm/13 pages + 3 plates/Hardcover/$35

1. Introduction 2. Description of Species (1) Order Graptoloidea
Lapworth
(2) Order Dendroloidea Nicholson 3. Explanation of Plate I 4.
Explanation of
Plate II 5. Explanation of Plate III

249.
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Paleontologia Sinica (Series B, Volume XV, Fascicle 1) Lower
Triassic
Cephalopoda of South China
ÖйúÄϲ¿ÏÂÈýµþ¼Í֮ͷ×ãÀ໯ʯ In English
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C. C. Tien/1933/220x290mm/43 pages + 4 plates/Paperback/$78

1. Introduction 2. Description of Species (1) Order Ammonoidea (2)
Order
Nautiloidea 3. Correlation of Lower Triassic Cephalopod Zones 4.
Bibliography
5. Explanation of Plates

250.
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Paleontologia Sinica (Series B, Volume XV, Fascicle 2) Fossiles
Paleozoiques
et Mesozoiques Du Sud-Ouest De La Chine
ÖйúÎ÷Äϲ¿¹ÅÉú´ú¼°ÖÐÉú´ú¶¯Îﻯʯ (one copy) In German
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Etienne Patte/1935/220x290mm/40 pages + 4 plates/Paperback/$66

1. Introduction 2. Indications Stratigraphiques 3. Liste Des
Gisements
Fossiliferes 4. Description Des Especes (1) Famille des Lingulidae
King
(2)
Famille des Discinidae (3) Famille des Productidae Gray (4) Famille
des
Terebratulidae King (5) Famille des Beyrichidae Jones (6) Famille
des
Encrinuridae Linnarson (7) Famille des Pleurotomariidae d'Orbigny
(8)
Famille des Neritopsidae Fischer (9) Famille des Pyramidellidae Gray
(10)
Famille des Aviculidae Lamarck (11) Famille des Pernidae Zittel (12)
Familes
Limidae d'Orbigny (13) Famille des Pectinidae Lamarck (14) Famille
des
Spondylidae Gray (15) Famille des Myalinidae Frech (16) Famille des
Mytilidae (17) Famille des Anthracosiidae Amalitzky (18) Famille des
Nayadidae Lamarck (19) Famille des Trigoniidae Lamarck (20) Famille
des
Lucinidae Deshayes (21) Famille des Cyrenidae Adams (22) Famille des
Grammysiidae Fisher (23) Famille des Gephyroceratidae Haug
(24) Famille des Ceratitidae V.Buch (25) Famille des Palaeoniscidae
Vogt
emend. Traquair 5. Bibliographie 6. Legendes Des Planches

251.
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Paleontologia Sinica (Series B, Volume XVI, Fascicle 1) On the
Growth
Rate
of Reef Corals and its Relation to Sea Water Temperature
Ô콸ɺº÷µÄ³É³¤Âʼ°ÆäÓ뺣ˮζȵĹØÏµ In English
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Ting Ying H. Ma/1937/220x290mm/226 pages+another vol of 100
pls/Paperback/$330

1. Introduction an dAcknowledgements 2. Scope 3. Localities 4. Water
Temperature 5. Measurements (1) Suborder Madreporaria Imperforata
(2)
Suborder Madreporaria Fungida (3) Suborder Madreporaria Perforata 6.
Averaged Measurement of Annual Growth 7. Explanation of the Marks in
the
Growth-Temperature Graphs 8. Growth-Temperature Graphs 9.
Explanation
of
Plates

252.
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Palaeontologia Sinica (Whole Number 138 New Series B. No.5)The New
Materials
of The Dendroid Graptolites of China
Öйú¹ÅÉúÎïÖ¾£­ÖйúÊ÷ÐαÊʯ In Chinese with English summary
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A.T. Mu/1955/210x290mm/62 pages + 6 plates/Hardcover/$68

The dendroid graptolites of China have been studied for more than
two
decades. Many important species of the genera Dictyonema,
Desmograptus,
Callograptus, Dendrograptus and Acanthograptus have been previously
described by Professors Y.C.Sun, T.H.Yin and Singwu C. Hsli. All
these
dendroids are the Lower Ordovician (Tremadocian and Arenigian) forms
obtained from Hopei, Hupeh, Kiangsi and Yunnan Provinces. During
recent
years. Additional specimens of dendroids ranging from Upper Cambrian
to
Lower Silurian have been found from different localities in the
provinces of
Liaoning, Shansi, Inner Mongolia, Sikang, Szechuan, Kueichou and
Chekiang.
It is this recently acquired material forwarded to the writer for
examination by many collectors which forms the subject of the
present
account. The majority of the specimens were collected from the Yehli
formation (Tremadocian) of the Taitzeho valley, Liaoning and from
the
Ichang
formation (Tremadocian) of the Changyang district, W.Hupedh.

253.
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Palaeontologia Sinica (Whole Number 145, New Series B No.9)Lower
Triassic
Ammonoids from Western Kwangsi, China
¹ãÎ÷Î÷²¿ÏÂÈýµþ¼Í¾Õʯ In Chinese and English bilingual
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1959/210x280mm/355 pages + 44 plates/Hardcover/$120

While taking geological investigations in Kwangsi from 1940-44, the
writer
and his colleagues of the Institute of Geology, Academia Sinica,
discovered
several fossil localities in the Triassic rocks in the western part
of
that
province, where the ammonoids are not only rich in individuals but
also
rich
in genera and species. The fossils are exclusively an ammonoid
fauna.
Among
the hundreds of specimens in the collections there are only a few
specimens
of small pelecypods and nautiloids. The lower Triassic rocks in
western
Kwangsi are composed largely of thin-bedded or nodular limestones
attaining
a thickness of about 100 metres, in which the fossils are very rare.
However, at many places the limestones become thick-bedded and
impure,
in
which the ammonoids are rich. They can easily be taken out from the
rocks
and most of them are fairly well preserved.
This report deals with the materials collected from twelve
localities
in
five districtsof western Kwangsi: the Linglo, the Fengshan, the
Tiengno, the
Tunglan and the Tientung districts. The ammonoids described and
illustrated
amount to 204 species in 59 genera, which are grouped in 23
families,
of
which more than two-thirds are new formes The study of these
ammonoids
reveals that the fauna is closely related to that of India and that
of
Albania in the Tethys Sea on the one hand, and is more closely
related
to
that of Timor on the other. The Triassic ammonoids of Ussuri land
and
those
of Eastern Siberia also show close connection with the fauna of
Kwangsi.
Although the faunas of these regions bear general resemblance,
difficulties
are usually met with when making precise correlation. The discovery
of
Lower
Triassic ammonoids in Kwangsi is of particular importance, for they
link the
fauna of these distant regions. It is also found that many forms
characteristic of early period persisted much longer in the Kwangsi
province
and some genera appear earlier in this region. From the study of
these
ammonoids it is also recognized that the Lower Trias in Kwangsi can
be
subdivided into four divisions or groups. In ascending order they
are
as
follows: the Gyronitan, the Flemingitan, the Owenitan and the
Columbitan in
the scheme of Spath¡¯s classification. His lowest division, the
Otoceratan,
is not confirmed, whilst his uppermost division, the Prohungaritan
or
Olenikitan, is not junstified.

254.
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Palaeontologia Sinica (Whole Number 149 New Series B No.10)Permian
Fusulinids of Kwangsi, Kueichow and Szechuan
Öйú¹ÅÉúÎïÖ¾-¹ãÎ÷¡¢¹óÖݼ°ËÄ´¨¶þµü¼ÍµÄ¹jÀà In Chinese
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Sheng Jinzhang/1963/230x300mm/247/Hardcover/$46

During the past six years, we have obtained many large collections
of
fusulinids from the marine Permian of Kwangsi, Kueichow and
Szechuan,
which
form the subject of the present account. The fusulinids described
and
illustrated comprise 148 species and varieties belonging to 34
genera,
which
are grouped in 9 subfamilies of 5 families, of which two genera and
one
subgenus and more than one-third species and varieties are new forms.
FUSULINIDEA 1. Ozawainellidae 2. Schubertellidae 3. Schwagerinidae
VERBEEKINIDEA 4. Verbeekinidae 5. Neoschwagerinidae

255.
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Palaeontologia sincia(whole Number 152 New Series B Number
11)Ordovician
Trilobite Faunas of Central and Southwestern China
»ªÖм°Î÷ÄϰÂÌÕ¼ÍÈýÒ¶³æ¶¯ÎïȺ In Chinese and English bilingual
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Lu Yen-Hao/1975/230x310mm/463 pages+46 plates/Paperback/$120

The Ordovician trilobites of central and southwestern China here
described
contain 187 species in 2 subgenus, 75 genera, 22 subfamilies and 30
families, of which 103 species, 4 subspecies, 11 genera, 2
subfamilies
and 2
families are new. They were collected from six regions, namely (1)
Western
Hupeh, (2) South Szechuan,(3) Northern Kueichou,(4) Huayinshan
Region,
central Szechuan, (5) western Szechuan and (6) southern Shensi. On
the
basis
of stratigraphical successions and faunal characters, fossil zones
are
distinguished in the Ordovician strata of each region.

256.
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Palaeontologia Sinica ( Whole Number 154 New Series B, Number 12)
Late
Permian Cephalopods of South China
»ªÄÏÍí¶þµþÊÀÍ·×ãÀà In Chinese with English summary
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Zhao Jinko/1978/180x260mm/194 pages with 103 figures +34
plates/Hardcover/$33

Marine Permian rocks are widely spread and well developed in south
China,
containing various kinds of fossils. Although fusulinids, corals and
brachiopods have been made largely known, so far as the cephalopods
are
concerned, they were found at very few localities. Since the
liberation
of
China, extensive geological investigations have been carried out and
numerous cephalopods have been collected, putting the responsibility
at
us
for identification. The materials of Upper Permian cephalopods upon
which
the present study is made came from more than 80 localities in 12
provinces
and autonomous regions of South China. Among these localities the
writers
visited more than 20 sections to collect more cephalopods,
particularly
ammonoids. It also should be mentioned that our study is of primary
nature,
much detailed work is hoped.

257.
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Palaeontologia Sinica (Whole Number 157 New Series B, Number
14)Devonian
Stromatoporoids from Central and Eastern Parts of Guangxi, China
Öйú¹ÅÉúÎïÖ¾£¨×ܺŵÚ157²á ÐÂÒÒÖÖµÚ14ºÅ£©¹ãÎ÷Öв¿¶«²¿ÄàÅè¼Í²ã¿×³æ
(Used
book)
In Chinese
*********************************************************************
********************************************************************
Yang Jingzhi/1979/185x260mm/89 pages + 46 plates/Hardcover/$20

Stromatoporoids are widely distributed in the calcareous rocks of
the
Devonian system in central and eastern parts of Guangxi. Here are
described
a total number of 185 species in 32 different genera, in which 5 new
genera,
Argostroma, Cubodictyon. Climacostroma, Glyptostroma and Atopostroma
and 110
new species and 3 new subspecies are established. 1.
Clathrodictyidae
Kuhn,
1939 2. Actinostromatidae Nicholson, 1886 3. Stromatoporidae
Winchell,
1867
4. Idiostromatidae Nicholson, 1886

258.
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Palaeontologia Sinica ( Whole Number 152 New Series B Number
15)Beiliuan
(Middle Middle Devonian) Brachiopods from South Guizhou and Central
Guangxi
Ç­ÄϹðÖÐÖÐÄàÅèÊÀ±±Á÷ÆÚÍó×㶯Îï In Chinese with English summary
*********************************************************************
*********************************************************************
**********
Wang Yu & Zhu Ruifang/1979/180x260mm/95 pages + 34 plates/Hardcover/
$34

The brachiopods dealt with in this monograph were collected at 7
localities
in southern Guizhou and central Guangxi. From north to south these
localities are: 1. Houershan, about 10 miles east of Dushan City,
Guizhou;
2. Sipai commune, Luzhai County; 3. Qijian, Tongmu commune; 4.
Laohuling; 5.
Liufengshan,
6 miles south-west of Miaohuang village, Xiangzhou County; 7.
Dafengmen; 8
miles north-east of Ertang commune, Wuxuan County; 6. Huanglingtou,
Baima
commune, Pingnan County and 2 miles north of Beiliu City. Localities
2-7 are
situated along the western flank of the Dayao Mountains, Guangxi.
(See
Fig.
1 ). A brief account is here given of the 7 sections mentioned above.

259.
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palaeontologia Sinica(Whole Number 159, New series B No.16) (out of
print)
Cambrian Trilobite Fauna of Southwestern China
Î÷ÄϵØÇøº®Îä¼ÍÈýÒ¶³æ¶¯ÎïȺ In Chinese with English summary
*********************************************************************
*****************************************************
Zhang wentang & Lu
Yanhao/1980/185x260mm/497pages+134plates/Hardcover/$90

The Cambrian trilobites described and discussed in this monograph,
were
collected from the Cambrian formations in the Yangtze platform, or
geographically speaking in southwestern China including eastern and
southeastern Yunnan, Guizhou, Sichuan, southern Shaanxi, Hubei and
western
Hunan. The field works were carried out in 1956, 1962-1967 and
1970-1973
respectively. In the meantime many Cambrian sections including the
type
sections have been measured in the Gorge district of Yangtze,
western
Hubei
and in eastern Yunnan and northern Guizhou, and immense Cambrian
trilobites
have been collected there, which enable us to advance our knowledge
of
the
Cambrian faunal successions; the component parts of the trilobite
faunas in
Redlichian province; the distribution, ontogeny, phylogeny and
ecology
of
redlichid trilobites; the taxonomy of Eodiscina, Redlichiina and
Oryctocephalacea; The relation between biogeographical province and
ecological province; the correlation between two major Cambrian
faunal
provinces of the world etc. Since the early Lower Cambrian deposits
are
wanting in North China platform, the fully developed and richly
trilobite
fossiliferous Early Cambrian succession in southwestern China, which
has
been assigned to four stages, may be used as a correlation standard
for
the
Lower Cambrian of China and for the Lower Cambrian of the whole
Redlichian
province as well. The specimens of trilobites described and figured
in
this
monograph are kept in the Museum of the Nanjing Institute of Geology
and
Paleontology, Academia Sinica.

260.
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*
Palaeontologica Sinica (Whole Number 161 New Series B, Number 17 )
Late
Mesozoic Conchostracans from Zhejiang, Anhui and Jiangsu Provinces
ËÕÕãÍîÖÐÉú´úºóÆÚÒ¶Ö«½é»¯Ê¯ In Chinese with English summary
*********************************************************************
*********************************************************************
*
Chen Pieji/1982/185x260mm/117 pages + 47 plates/Hardcover/$35

In SE China, Late Mesozoic volcanie rocks and red deposits were
extensively
distributed, ostracods, peleeypods, gastropods, fish and plant
fossils,
especially abundant conchostracans were found to occur in the
variegated
sedimentary intercalations of the volcanic deposits of the Kienteh
Group.
The fossil Conchostracans dealt with in this monograph contain 115
species
in 21 genera, 9 families, of which 71 species, 5 genera, and 1
family
are
new to science. They were mainly collected from four areas, namely
(1)
Zhejiang, (2) Southern Anhui, (3) Nanjing-Wuhu area, and (4)
Xiaotian
district, Westen Anhui.

261.
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***
Palaeontologia Sinica (Whole Number 163 New Series B, Number
18)Pliocene
Ostracode Fauna of Leizhou Peninsula and Northern Hainan Island,
Guangdong
Province
¹ã¶«À×ÇíµØÇøÉÏÐÂÊÀ½éÐÎÀදÎïȺ In Chinese with English summary
*********************************************************************
*********************************************************************
***
Nanjing Institute of Geology and Palaeontology/1982/185x260mm/134
pages+ 23
plates/Hardcover/$25

The marine Pliocene ostracodes in association with foraminifera,
lamellibranches and gastrapods are found richly in the Wanglougang
formation
from the Leizhou Peninsula and northern Hainan Island, but they are
not
so
much in the underlying Foluo formation as in the above one.The
Wanglougang
formation consists mainly of grey, lightgrey mudstone, sandy
mudstone,
siltpelite, siltstone, along with interealated beds of argillaceous
sandstone and gravelly sandstone, and in the upper and the lower
parts
of
this formation appear thn-bedded mustone and calcareous mudstone.
The
foluo
formation is composed of yellow, grey-yellow, grey-green gritstone,
gravelly
sandstone, arper are obtained from the Wanglougang formation. Both
formations are overlain by Quaternary deposits, therefore all
samples
under
study are collected from boreholes.
The ostracode fauna from the above mentioned formations contains 65
genera
and 166 species belonging to Superfamilies Bairdiacea and Cytheracea
and
Family Cytherellidae, among which 3 genera and 52 species are
described
as
new to science.
1. Podocopina Sars, 1866
(1) Bairdiacea Sars, 1888
(2) Cypridacea Baird, 1845
(3) Cytheracea Baird, 1850
2. Platycopina Sars, 1866
(1) Cytherellidae Sars, 1866

262.
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***
Palaeontologia Sinica(Whole No.164, New series B No.19)The
Fusulinids
of the
Maping Limestone of the Upper Carboniferous from YiShan, GuangXi
¹ãÎ÷ÒËɽµØÇøÍíʯ̿ÊÀÂíÆ½×éµÄÜðÀà In Chinese with English summary
*********************************************************************
*********************************************************************
***
Chen Xu & Wang Jianhua/1983/185x260mm/139 pages+25 plates/Hardcover/
$26

The materials dealt with here were collected by prof. Sheng
Jinzhang,Hou
Youtang, Wu Wangshi and Zhang Linxin etc. From the Maping limestone
at
Desheng and Beishan in the Yishan district, Northern Guangxi in the
winter
of 1956. The fusulinids described and illustrated in this paper
comprise 172
species and 26 subspecies belonging to 21 genera and subgenera,
which
are
grouped into 8 subfamilies. Among them 38 species and 4 subspecies
are
new
forms. A list of these genera and species is given in the Chinese
text
on
pages 29-117. The Maping formation in Yishan is composed all of
limestone
containing fusulinids.The succession is quite normal. So far this
formation
has been known to be widely distributed in South China and probably
more
fully developed in the provinces of Guangxi and Guizhou

263.
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Palaeontologia Sinica ( Whole Number 170 New Series B, Number 21)
Early
Mesozoic Fossil Insects From South China
»ªÄÏÖÐÉú´úÔçÆÚµÄÀ¥³æ In Chinese with English summary
*********************************************************************
******************************************
Lin Qibin/1986/180x260mm/12 pages + 20 plates/Hardcover/$28

1. Introduction; 2.Fossil insects of Early Mesozoic; 3.Biological
characters
of the Early Mesozoic insect fossil fauna south China; 4.
Description
of
Species: (1) Order Ephemeroptera, (2) Order Blattoidea Brunner,
1882;
(3)Order Orthoptera: Family Elcanidae Handlirsch, 1906; (4)Order
Heteroptera; (5)Order Homoptera; (6)Order Plecoptera: (7)Family
Osmylitidae
O. Martynova; (8)Family Plecoptera incertae sedis; (9)Order
Coleoptera;
(10)Order Mecoptera: Family Orthophlebiidae Handlirsch; (11)Order
Trichoptera: Family Necrotaulidae Handlirsch; (12)Order Diptera

264.
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Palaeontologia Sinica ( Whole No.172 New Series B No.22)Yukiangian
(Early
Emsian, Devonian) Brachiopods of The Nanning-Liujing District,
Central
Guangxi, Southern China
¹ãÎ÷ÄÏÄþ-Áù¾°¼äÄàÅè¼ÍÓô½­ÆÚÍó×㶯Îï In Chinese with English summary
*********************************************************************
*************************
Wangyu and Rongjiayu/1986/180x260mm/282 pages with 119 figures + 96
plates/Hardcover/$38

The geologic history of the Devonian in the Nanning Distriet,
Central
Guangxi, Southern China, is developed from analysis of the strata
and
fossils, with special emphasis on the systematic description of the
brachioplds, conodonts and corals. Devonian rocks are widely
distributed and
well exposed in the vicinity of Daliancun Village, Nanning and in
the
area
between the Wuhe and Liujing ( formerly Luching) railway stations of
the
Xiang (Hunan)-Gui (Guangxi) Railway, especially in the Luujing area,
Hengxian County , Central Guangxi (Text-figs. 1,3,4), This region is
herein
called the Nanning-Liujing District. Most of our Eollections have
been
gathered from the Liujing area. Detailed stratigraphic sections and
biostratigraphic data are presented, from which faunal assemblages,
based
mainly on brachiopods, ate given in detail. The age of the
brachiopods
with
reference to evidence provided by conodonts and dacryoconariids is
discussed. Paleozoogeographic and community ecologic conclusions are
also
tentatively drawn

265.
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Palaeontologia Sinica (Whole Number 174, New Series B, Number 23)
Bryozoans
from Late Devonian and Early Carboniferous of Central Hunan
ºþÄÏÖв¿ÍíÄàÅèÊÀ¼°Ôçʯ̿ÊÀ̦޺¶¯Îï In Chinese with English summary
*********************************************************************
*******************************************************************
Yang Jingzhi/1988/185x260mm/197 pages + 40 plates/Hardcover/$45

In the present paper a total number of 127 species and subspecies in
36
genera are described, among which 100 new species and subspecies,
and 3
new
genera i. e. Europora, Coelotubulipora and Euthyrhombopora are
erected.
Discussion and revision of some generic definitions are made and the
evolutional trnds of some genera are tentatively explained.

266.
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Palaeontologia Sinica( Whole Number 177 New Series B Number 24)
Carboniferous and Early Early Permian Rugosa From Western Guizhou
and
Eastern Yunnan SW.China
Ç­Î÷µá¶«Ê¯Ì¿¼ÍºÍÔç¶þµþÊÀÔçÆÚµÄËÄÉäɺº÷ In Chinese with English summary
*********************************************************************
*************************
Wu Wangshi/1989/185x260mm/230 pages + 63 plates/Hardcover/$39

The fully developed marine Carboniferous and early Early Permian
rocks
in
Western Guizhou and Eastern Yunnan, SW. China are represented by
several
hundred meters to more than 1,000 m of limestones and argillaceous
limestones, containing abundant faunas of rugose corals in
association
with
brachiopods, and others. The Carboniferous and early Early Permian
rugose
corals here described and illustrated were collected by the authors
and
their colleagues of Nanjing Instate of Geology and Paleontology,
Academia
Sinica from Weining, Shuicheng, Panxian and Pu'an Counties of
Guizhou
Province and ZhanYi County of Yunnan Province in 1963, 1973 and
1981.
They
have been assigned to 215 species (including 105 new species and 13
new
subspecies) in 95 genera (including 8 new genera and 1 new subgenus)
and 24
families, providing the knowledge of their faunal succession,
evolutional
stages and biological community of the Carboniferous and early Early
Permian
in the concerned areas.

267.
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Palaeontologia Sinica ( Whole number 180, New Series B , Number 25)
The
Cambrian Trilobites of western Zhejiang
Õã½­Î÷²¿º®Îä¼ÍÈýÒ¶³æ¶¯ÎïȺ In Chinese with English summary
*********************************************************************
*****************************************
Lu Yanhao and Lin Huanling/1989/180x260mm/287 pages+28
plates/Paperback/$45

The Cambrian trilobites of western Zhejiang represent the typical
Southeast
China Faunal Province, one of the Oriental Faunal Realms. They are
quite
different from those of the Atlantic or the Acado-Baltic Faunal
Province,
one of the Occidental Faunal Realms contemporaneous and
corresponding
to the
Southeast China Faunal Province, though many pelagic genera and
species
of
the agnostics and a few nonagnostid trilobites occur in both
provinces.
The
Agnostida described here includes 10 families and subfamilies, 32
genera and
subgenera, 57 species and 22 undetermined species, among which 1
subgenus
and 20 species are new; the non-agnostic trilobites med species,
including 1
new subfamily and 17 new species. Stratigraphically, the Cambrian
System of
western Zhebrian strata of W. Zhejiang, Central China, NW China, N.
and
NE
China, Kazakhstan, Australia, Scandinavia and N. America is given.

268.
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Palaeontologia Sinica (Whole Number 179 New Series B, Number 26)
Silurian
Graptiolites from Chengkou, Sichuan
ËÄ´¨³Ç¿ÚÖ¾Áô¼Í±Êʯ In Chinese
*********************************************************************
****************************************
Ge Meiyu/1990/185x260mm/157 pages + 23 plates/Hardcover/$25

Silurian graptolite-bearing strata are well developed in Chengkou,
south of
the Daba Mountain in Sichuan Province. The graptolite sequence is
one
of the
most complete in Central China. In 1944, Yang Jingzhi in his paper "
The
Cambrian and Ordovician sections of Tapashan , NE Sichuan", Only
assigned
these strata to the Silurian without making detailed study of the
Silurian
graptolites.
In the autumn of 1965, Liu Yingkai and his colleagues of the 2nd
Geological
Survey and Prospecting Team of Geological Bureau of Sichuan, Zhu
Zhaoling,
Xu Hankui and Yuan Kexing of Nanjing Institute of Geology and
Palaeontology,
Academia Sinica and the writer studied systematically the Silurian
strata
and collected a large number of Silurian graptolites from Chengkou.
In
addition, in 1965, Liu Yingkai and his colleagues collected many
Silurian
graptolites from Taiyanghe of Enshi, Hubei. All the specimens are
described
by the writer in this paper. 155 species and subspecies belonging to
27
genera are recognized. Of them one subfamily one genus, 14 species
and
3
subspecies are new.

269.
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Palaeontologia Sinica ( Whole number 180, New Series B , Number
27)Carboniferous Cephalopods of Xinjiang
н®Ê¯Ì¿¼ÍÍ·×ãÀà In Chinese with English summary
*********************************************************************
***********************************
Liang Xiluo/1999/185x260 mm/171 pages + 40 plates/Hardcover/$28

In total, the sephalopods described here in comprise 96 species in
45
genera, icluding 21 nautiloid species in 15 genera (5 species are
new)
and
75 ammonoid species in 30 genera (20 species are new). Consideration
of
the
present and previous stadies permits of a more comprehensive
discussion
of
the cephalopod faunas especially ammonoids.
1. Nautiloidea (1) Orthoceratida Kuhn, 1940 (2) Nautilida Agassiz,
1847
(3)
Actinocerida Teichert, 1933 2. Ammonoidea (1) Prolecanitida Miller
et
Furnish, 1954 (2) Goniatitida Hyatt, 1884

270.
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Palaeontologia Sinica (Whole Number 181 New Series B, Number 28)
Early
and
Middle Ordovician Graptolites from Wuning, Northwestern Jiangxi,
China
½­Î÷ÎäÄþϰÂÌÕͳ¶¥²¿ºÍÖаÂÌÕͳµÄ±Êʯ In Chinese with English summary
*********************************************************************
*********************************************************************
*******
Chinese with English summary/1991/185x260mm/147 pages + 35
plates/Hardcover/$30

Ordovician strata are well developed in northwestern Jiangxi. The
sequence
has been studied since the 1930s, but no comprehensive work on the
faunas
has been carried out. This paper completes the first detailed
description of
the graptolites from the uppermost Ningkou and Hulo formations in
Wuning,
Northwestern Jiangxi of Southeast China. The material which forms
the
basis
of the paper was collected by the writer and Miss Zhang Xinn bed by
bed
in
the summer of 1963 from 140 beds at Xinkailing, a small village
about
4km to
the north of the Wuning county, The section is 29.7 m in thickness,
spanning
the Nicholsonograptus and Nemagratus gracilis zones. The graptolite
fauna
includes 115 species belonging to 33 genera. Among them three
genera,
i.e.
Wuninograptus, Protabrograptus and Xiphograptus, have been described
before
.. Most specimens are preserved as flattened rhabdosomes although a
few
species are represented by relief material.

271.
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Palaeontologia Sinica (Whole Number 182 New Series B, Number 29)
Upper
Ordovician Graptolites of Central China Reion
Öйú¹ÅÉúÎïÖ¾£­»ªÖÐÇøÉϰÂÌÕͳ±Êʯ In Chinese with English summary
*********************************************************************
*************************************************
Mu Enzhi/1993/185x260mm/393 pages + 66 plates/Hardcover/$68

The Upper Ordovician is extensively distributed in the Central China
Region,
containing rich and varied graptolites. During the recent several
decades, a
great amount of stratigraphical and graptolitic data have been
accumulated.
However, due to the limit of space, this book only adopts more than
27
sections to discuss the problem on the stratigraphical stratify,
division of
graptolite zones and their correlation of the Upper Ordovician in
the
Central China Region and boundary between Ordovician and Silurian .
This
book also deals with the problem on the biostratigraphical division
of
the
Upper Ordovician. Here described are the graptolites from the Upper
Ordovician of the Central China Region, including 33 genera and 192
species
or subspecies; 2 new genera and 69 new species or subspecies are
erected. On
the basis of the description, also discussed are the problem on the
characteristics of Late Ordovician graptolite fauna, classification
of
certain graptolites and the reticulated structure of the rhabdosome.
The
Late Ordovician palaeographic maps of the Central China Region have
been
published in separate papers.

272.
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Palaeontologia Sinica ( Whole number 184, New Series B , Number
30)Trilobites from Middle Upper Cambrian (Changshan Stage) of North
and
Northeast China
»ª±±¼°¶«±±Äϲ¿ÉϺ®Îäͳ³¤É½½×ÈýÒ¶³æ In English
*********************************************************************
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*************
Qian Yiyuan/1994/180x260mm/190 pages+34 plates/Paperback/$28

The upper limit of the Changshan Formation had been traditionally
put
at the
top of the Kaolishania pustulosa zone before 1983. After studying
the
trilobites material from Luotuolingzi of Benxi, Lu and Qian (1983)
suggested
to erect the Acanthometopus zone for the uppermost zone for the
uppermost
zone of Changshan Formation. Thus its upper limit should be extended
to
the
top of the Acanthometopus zone instead of Kaolishania pustulosa
zone.
At the
named locality of the Acanthometopyus zone in the Luotuolingzi
section
are
contained only the zonal fossil and Trianguraspis (gen.nov.). At
Baiyundong
section of Tienshifu, the latter is associated with Elaphraella,
Mansuyia,
and Shirakiella are all the leading fossils of Changshan Formation.
Owing to
this case, the Acanthometopus zone is reasonable to be considered to
put in
Changshan instead of Fengshan Formation, and the upper limit of
Changshan
Formation is corresponding to be drawn at the top of the zone.

273.
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Palaeontologia Sinica ( Whole number 184, New Series B , Number
31)Mesozoic
and Cenozoic Scleractinian Corals From Xizang(Tibet)
Î÷²ØÖС¢ÐÂÉú´úʯɺº÷ In Chinese with English summary
*********************************************************************
************************************************************
Liao Weihua/1994/185x260mm/252 pages+ 68 plates, 100
figures/Hardcover/$32

The Mesozoic and Early Cenozoic marine strata are well developed in
Xizang,
with very rich scleractinian corals. For a long time little was
known
about
these corals from Xizang. Since 1951, a large number of
scleractinians
have
been found from various localities therein. The scleractinian corals
dealt
with in this monograph were collected mainly by the comprehensive
Scientific
Expedition to the Qinghai-Tibetan Plateau of the Chinese Academy of
Sciences. the Geological Institute of Xizang, the 4th Geological
Team
of
Xizang, the Regional Geological Survey Team of Qinghai and the 3rd
Regional
Geological Survey Team of Sichuan. The fossil scleractinians
described
here
comprise 108 genera and 221 species(including some new species)

274.
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Palaeontologia Sinica (Whole Number 188, New Series B, No.
32)Cretaceous
Bivalves of the Region of Songhuajiang and Liaohe Rivers in
Northeast
China
ËÉÁɵØÇø°×ÛѼÍË«¿ÇÀ໯ʯ In Chinese with English summary
*********************************************************************
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**********
Gu Zhiwei/1999/185x260mm/114 pages +21 plates/Hardcover/$49

Chinese edition with English summary and brief description of new
species,
subgenus and genus in English 23 genera, 65 species are described,
among
which 13 species are new to science.
1. Pteriomorphia Beurlen, 1944 2. Palaeoheterodonta Newell, 1965 3.
Heterodonta Neumayr, 1844

275.
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Palaeontologia Sinica (Whole Number 189, New Series B, No. 33)
Typical
Pacific Graptolite Fauna From The Ningkuoan of Early Ordovician in
Chongyi,
JiangXi
In Chinese with English summary
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Li Jijin/2000/185x260mm/188 pages + 30 plates/Hardcover/$38

The graptolite strata of the Ordovician in the hongyi area of
Jiangxi
were
first discovered by Zhang Qianshen and others(1964). Subsequently,
the
Early
Ordovician graptolite strata were report by Xiao Chengxie and
others(1975)
from Niupiwan-Niupilong at Guobu of Chongyi. From August to
November,
1978,
Xiao Chengxie, Xia Tianliang, Wang Zhaoyun and Zhou Chonggui made a
detailed
survey and mapping of the Ordovician Zhangmuqu section at Guobu and
Baishi'ao section at Sishun, with a systematic collection of
graptolites; in
1982, Xiao Chengxie, Chen Hongye and Xie Wenwei make a further
investigation
into the Baishi'ao section at Geobu, Baishi'ao at Sishun, etc.,
making
observation on the Ordovician section and supplementary collection
of
graptolites. Later, the writers selected the better-preserved
graptolite
specimens from those collected in abundance by Xiao Chengxie and
others
over
the past years, with a systematic description of the graptolites
from
the
Ningkuoan of Early Ordovician Assigned to 45 genera, 7 subgenera,
168
species and subspecies, including 3 new species. The Ningkuoan
graptolites
in the Chongyi area had been reported for several times(Yang et al.,
1983;
Li, 198; Xiao et al., 1985 erected two new subgenera, namely
Oncograptus
(Proncograptus) and Cardiograptus (Procardiograptus), and some new
species.
Some of the above-mentioned graptolites are revised in the book. As
a
whole,
the Early Ordovician strata in Chongyi area belongs to the
graptolitic
facies with rich graptolies, especially those of the Ningkuoan,
Whick
are
more abundant, with more genera and species forming a complete
graptolite
sequence, and may be divided into 10 graptolite zones, providing
valuable
material for the precise correlation of the Ningkuoan graptolite
zones
with
those of the same time in the world. On the other hand, the
discovery
of
Isograptus together with its allied genera is of most essential
significance
to the exploration into some curcial problems such as the evolution,
classification of graptolites. Statistics of the diversity of the
graptolite
fauna indicates that the high diversity just conincides with the
major
development stage of Isograptus and its allied genera, while the
fauna
with
a lower diversity appeared in the replacement stage of the
replacement
stage
of the faunas, in which the Anisograpti fauna, for example, was
replaced by
the Dichograpti fauna. Statistical data on changes of the graptolite
fauna
indicate that the fauna with a greater change appeared in Xinchang
and
Ningkuo stages and the Ningkuo and Hulo stages respectively; the
latter
is
also the boundary between Lower and Middle Ordovician boundary
between
Llanvirnian and Llandelian, which represents the most distinct
boundary
in
the development stage of organisms. In addition, this book also
makes a
detailed statistical analysis on the ningkuoan graptolite fauna in
different
places of the cirum-Pacific region, with their genera and species
tabulated
in a list for correlation. The common presence of many identical and
some
comparable in this and other place shows the close relationship
among
them.
It also has been found thast in this region the Ningkuoan graptolite
fauna
is the most abundant among those of the circum-Pacific region.
Moreover,
this graptolite fauna can be taken as a typical representative of
the
Ningkuoan graptolites of the Pacific fauna.

276.
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Paleontologia Sinica (Series C. Vol.1, Fascicle I)Tertiary
Vertebrates
from
Mongolia
ÃɹŵÚÈý¼Í¼¹×µ¶¯Îﻯʯ In English
*********************************************************************
******************
Max Schlosser/1934/230x290mm/119 pages + 6 plates/Hardcover/$150

1. Preface 2. Description of the Fauna (1) Mammalia (2) Aves (3)
Reptilia
(4) Amphibia (5) Pisces 3. The Local distribution of the vertebrates
described above and their relations to other fossil faunas (1)
Tertiary
vertebrates (2) Zoogeographical results (3) Morphologic and
phylogenetic
results 4. Explanations of the plates

277.
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***
Paleontologia Sinica (Seriess C Vol.1 Fascicle S)On a New Fossil
Porcupine
from Honan with Some Remarks about the Development of the Hystridae
ºÓÄÏäųغÀÖí¶¯Îﻯʯ In English
*********************************************************************
*********************************************************************
***
Einar Lonnberg Stockholm/1924/230x290mm/15 pages + 1
plates/Hardcover/$50

278.
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***********
Palaeontologia Sinica (Series C. Volume 1 Fascicle 2)Fossil Primates
from
China
ÖйúÁ鳤ÀදÎﻯʯ In English
*********************************************************************
***********
Max Schlosser In Munich/1924/285x230mm/14 pages + 1
plates/Hardcover/$50

279.
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**************
Palaeontologia Sinica (Series C. Vol. II, Fascicle I)Jungtertiare
Carnivoren
Chinas
ÖйúµÚÈý¼ÍºóÆÚ֮ʳÈâÊÞÀ໯ʯ In German
*********************************************************************
***************
Otto Zdansky/1924/230x290mm/149 pages + 33 plates/Hardcover/$220

280.
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*****
Paleontologia Sinica (Series C. Vol. 2 , Fascicle 3)Fossile Hirsche
Chinas
Öйú֮¹À໯ʯ In German
*********************************************************************
******
Otto Zdansky/1925/230x290mm/88 pages + 16 plates/Hardcover/$180

1. Vorwort 2. Die Hirsche der Hipparion-Fauna 3. Die Hirsche des
jungsten
Tertiars 4. Die Hirsche des Loss 5. Die Hirsche des Jungsten
Quartars
6.
Litteraturverzeichnis 7. Verzeichnis der in dieser Arbeit erwahnten
Fundorte
8. Register

281.
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Palaeontologia Sinica (Series C. Vol.IV. Fasc. 1)Die Familie
Giraffidae
Mit
Besonderer Berucksichtigung Der Fossilen Formaen Aus China
Öйú±±²¿Ö®÷è÷빿ƻ¯Ê¯ In German
*********************************************************************
******************************************************************
Birger Bohlin/1926/230x290mm/178 pages+11 plates/Paperback/$150

1. Vorwort 2. Unterfamilie Palaeotragina 3. Unterfamilie Giraffina
4.
Unterfamilie Okapiina 5. Unterfamilie Sivatheriina 6.
Zusammenfassung
7.
Litteraturverzeichnis

282.
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******
Palaeontologia Sinica (Series C. Vol.IV. Fase.2)Die Hipparionen
Nord-Chinas
Öйú±±·½Ö®ÈýÖºÂí»¯Ê¯ In German
*********************************************************************
******
Ivar Sefve/1927/230x290mm/91 pages +6 plates/Paperback/$55

1. Vorwort 2. Beschreibung der Schadel und des Gebisses von 3.
Beschreibung
der Extremitatenknochen von 4. Ubersicht der Chinesischen
Hipparionarten
5. Beschreibung von Proboscidipparion sinense n. g. n.sp. 6. Die
chinesischen Hipparien 7. Tabellarische Ubersicht 8.
Literaturverzeichnis 9.
Erklarung der Tafeln

283.
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Paleontologia Sinica (Series C. vol. V, Fascicle I)Weitere
Bemerkungen
¨¹ber
fossile Cerviden aus China
Öйú¹À໯ʯз¢¼ûÖ®ÌØáç In German
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*********************************
Otto Zdansky/1927/230x290mm/19 pages + 1 plates/Hardcover/$50

284.
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Paleontologia Sinica (Secies C. Volume IX, Fascicle 1) Fossil
Mammals
From
the Late Cenozoic of Northern China
Öйú±±²¿ÐÂÉú´úºóÆÚÖ®²¸È鶯Îﻯʯ In English
*********************************************************************
*****************************************
P. Teilhard De Chardin/1931/220x290mm/66 pages + 10
plates/Paperback/$90

1. Introduction 2. A Study of the Rodents 3. A Study of the Lower
Pliocene
Antilopidae 4. Complimentary Observations on the fauna and the
Stratigraphy
of Some Interesting Localities 5. Index of Localities 6. Sketch Map
of
W.
Shansi and N. Shensi 7. Bibliography 8. Explanations of Plates

285.
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Paleontologia Sinica (Secies C, Volume IX, Fascicle 2) Miscellaneous
Mammalian Fossils from Shansi and Honan
ɽÎ÷ºÓÄÏÖ®²¸È鶯Îﻯʯ(one copy) In English
*********************************************************************
***************************************
C. C.Young/1935/220x290mm/42 pages + 7 plates/Paperback/$75

1. Introductory Note 2. Description of the Species (1) Shouyang-
Yutze
area
(2) Taiku area (3) Yushe and Chinhsien area (4) Fushan area (5) The
fossil
localities of Pinglu in S. Shansi (6) The Mammal fossils collected
in
the
Mienchih-Hsinan area 3. Bibliography 4. Explanation of the Plates

286.
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***************
Paleontologia Sinica (Series C. Volume IX, Fascicle 3) Fossil
Proboscidea
from China
ÖйúÏóÀ໯ʯ(one copy) In English
*********************************************************************
***************
A. Tindell Hopwood/1935/220x290mm/108 pages + 8 plates/Paperback/$180

1. Preface 2. Introduction 3. Description of species (1) Trilophodon
connexus (2) Trilophodon wimani (3) Trilophodon spectabilis (4)
Serridentinus mongoliensis (5) Serridentinus gobiensis (6)
Serridentinus
florescens (7) Platybelodon grangeri (8) Tetralophodon exoletus (9)
Tetralophodon(?) sinensis
(10) Mastodon americanus (11) Mastodon borsoni (12) Mastodon sp.
Ondet
(13)
Pentalophodon sinensis (14) ? Pentalophodon sinensis (15)
Mastodontoidea
incertae sedis (16) Stegodon officinalis (17) Stegodon zdanskyi (18)
Stegodon orientalis (19) Stegodon orientalis grangeri (20) Stegodon
sinensis
(21) Stegodon aff. Bombifrons (22) Archidiskodon cf planifrons (23)
Paleoloxodon tokunagai (24) Paleoloxodon cf namadicus (25) Mammuthus
primigenius
4. The accompanying fauna and the Age of the Deposits 5. List of
works
consulted  6. Explanation of Plates

287.
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Paleontologia Sinica (Series C, Volume IX, Fascicle 4) Cavicornier
Der
Hipparion-fauna Nord-Chinas
Öйú±±²¿ÈýÖºÂíÁtÖ®¶´½ÇÀ໯ʯ (one copy) In German
*********************************************************************
*****************************
Birger Bohlin/1935/220x290mm/166 pages+ 20 Plates/Paperback/$280

1. Vorwort 2. Unterfamilie Ovibovinoe 3. Genus Tragocerus Gaudry 4.
Genus
Gazella Lichtenstein 5. Genus Tragoreas Schlosser 6. Paleoryx-
ahnliche
Antilopen 7. Verzeichnis der Fundorte 8. Litteraturverzeichnis

288.
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Paleontologia Sinica (Series C, Volume XII, Pascicle 1) On the
Mammalian
Remains from the Archaeological Site of Anyang
°²ÑôÒóÐæÖ®²¸È鶯ÎïȺ(one copy) In English
*********************************************************************
***************************************************
P. Teilhard De Chardin/1936/220x290mm/61 pages + 8 plates/Paperback/
$78

1. Introduction 2. Description of species (1) Order Carnivora Vicq
d'Azyr
(2) Order Cetacea Blumenbach (3) Order Rodentia Vicq d'Azyr (4)
Order
Ungulata
(5) Order Proboscidea Illiger (6) Order Primates L. 3. Conclusion 4.
Bibliography 5. Explanation of Plates

289.
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Paleontologia Sinica (Series C, Volume XIII, Fascicle 1) The
Proboscididans
of South-Eastern Shansi
ɽÎ÷¶«Äϲ¿Ö®ÏóÀ໯ʯ In English
*********************************************************************
******************************
P. Teilhard De Chardin/1937/220x290mm/58 pages + 13
plates/Paperback/$70

1. Preface 2. Introduction to the Proboscidians (1) Family
Paleomastodontidae Andrews (2) Family Mastodontidae (3) Family
Stegodontidae
(4) Family Elephantidae 3. Appendix Description of an Archidiskodon
Tokunagai Mandible from Hopei 4. Conclusions 5. List of the
Localities
6.
Bibliography
7. Explanation of Plates

290.
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Palaeontologia Sinica (New Series C, No.1, Whole Series No.102) The
Pliocene
Camelidae, Giraffidae, and Cervidae of South Eastern Shansi (one
copy)
ɽÎ÷¶«Äϲ¿ÉÏÐÂÍ³Ö®ÂæÍÕ÷è÷ë¹¼°Â¹»¯Ê¯ In English
*********************************************************************
*********************************************************************
*********
By P.Teilhard de Chardin & M.
Trassaert/1937/220x300mm/68pages+4plates/Hardcover/$90

We have described the Poliocene Proboscidians of South Eastern
Shansi
in
palaeontogia Sinica, series C, Volume ¢ú¢ó, Fascicle 1 of he old
series. The
Present memoir deals with the Camelidea ,and Cervide collected
mostly
by PP.
Licent in the same area during period between 1934 and 1937
Detailed explanations on the stratigraphy of the Late Cenozoic
lacustrine
beds of S.E. shansi have already been given in the preface of the
above
mentioned memoir on the Proboscidians and will not be repeated here.
It
has
been made clear there that the Pliocene series of South Eastern
Shansi
consists of lacustrine deposits covering apparently the
Pontian(Zone¢ñ),the
Middle Pliocene (Zone¢ó) . the latter zone being regarded here as
final
Pliocene rather than Early Plenistocene. The nationas in the text
are
the
same as those given in the previously mentioned work. For instance ,
the
number of the specimens refer to the catalogue numbers of the
Hoangho-Paiho
Museum (Tinetsin), the figures being printed in italics for the
illustrated
specimens . All measurements in the present memoir are made in
millimetres

291.
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Paleontologia Sinica (New Series C, No.5, Whole Series No.114) The
Fossils
from Locality 12 of Choukoutien (One copy)
In English
*********************************************************************
**************************************************
P. Teilhard De Chardin/1938/220x290mm/47 pages + 1 plates/Paperback/
$78

1. Introduction 2. Description of species (1) Myotis sp. (2) Canis
sp.
(3)
Ursus cf. angustidens Zd (4) Meles sp.nov (5) Mustela sp (6)
Machairodus
(7) Felis cf. pardus L. (8) Cf. lynx L (9) Sciurus sp. (10)
Cricetinus
varians Zd (11) Cricetulus sp. (12) Epimys rattus L. (13) Gerbillus
sp
(14)
Siphneus (15) Postschizotherium cf. chardini v. K (16) Rhinoceros
sp.
(17)
Perissodactyle ind (18) Sus sp. (19) Cervicornia (or Bovidae) (20)
Cynocephalus cf. wimani Schl. (21) Cynocephalus (or Macacus) 3. Non
mammalian remains 4. Conclusions and comparisons with Locality 18 5.
Referecens 6. Explanation of Plate

292.
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Paleontologia Sinica (New Series C, No.6, Whole Series No. 115)
Cavicornia
of South-Eastern Shansi (One Copy)
In English
*********************************************************************
*******************************************
P. Teilhard De Chardin/1938/220x290mm/98 pages + 4 plates/Paperback/
$98

1. Introduction 2. Description of Forms (1) Group Gazellinae (2)
Group
Pseudotraginae (3) Group Tragelaphinae (4) Group Ovicaprinae (5)
Group
Ovibovinae
(6) Group Bovinae 3. Conclusion 4. List of the Localities 5.
Bibliography 6.
Explanation of Plate

293.
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Palaeontologia Sinica (Whole Number 137 New Series C. No. 14) Fossil
Fishes
from Locality 14 of Choukoutien
Öйú¹ÅÉúÎïÖ¾-ÖܿڵêµÚÊ®ËĵصãÓ㻯ʯ In Chinese with English summary
*********************************************************************
**************************************
Liu Huiting/1954/300x230mm/18 pages + 8 plates/Paperback/$98

The fossil fishes described here have been excavated from locality
14
of
Choukoutien in 1951 by the Laboratory of Vertebrate Palaeontology.
In
1936
Prof. H. C. Chang described two species, Barbus brevicephalus Chang
and
Barbus Szechuanensis Tchang from the same locality. The former is an
extinct
species and the latter is living in Szechuan province. Through the
latter
excavation a considerable number of specimens have been collected by
us. The
study of the new material reveals that, in addition to the
previsionally
described two species, there are one additional species of the genus
Barbus
and one new species of the genus Matsya (M. hsichihi) were present
in
this
fauna. And there are a number of teeth and heap of eggs.

294.
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Palaeontologia Sinica (Whole Number 141, New Series C No.15)
Devonian
Fishes
from Wutung Series Near Nanking, China
ÄϾ©¸½½üÎåͨϵÄàÅè¼ÍÓ㻯ʯ In Chinese with English summary
*********************************************************************
***********************************************
By Liu Tung-sen/1958/230x300mm/40pages+10plates/Paperback/$45

The fossil fish materials described in this paper contain a part of
the
collection made by P¡¯an Kiang of the Geological Museum of the
Ministry
of
Geology. While making geological reconnaissances around Nanking in
1953, at
Lai-ku-tai, a small hill near Lungtan about 30 km east of city, a
few
broken
Pterichthyes plates identified by, H.T.Liu were discovered from the
grayish
black shales at the upper part of the Wutung Weries.
The discovery of the Pterichthyes (Antiarchi) remains, which shows
itself
most probably to be a Devenian form, from the Wutung Series is quite
interesting and important from both the points of view of
palaeontology
and
stratigraphy. Since the Wutung series has long been admitted as
Lower
Carboniferous in age according to palaeobotanical researches,
therefore,
before the Devonian age of the Wutung Series is warranted,
scrupulous
and
intensive studies of better fish materials areneeded. So in 1955
another
excavation was made under the auspices of the original discoverer.
This
time
several well preserved nearly complete Pterichthyes and a great
number
of
isolated plates of it were successfully found. Together with these
fish
plated there are a few scales of Dipnoian and Crossopterygian and
many
plant
remains. The present paper deals with the Pterichthyes of the
collection
only.
In undertaking this work, the authors had constantly referred to
Professor
Erik Aison Stensios various works on the Pterichthyes fished which
are
most
valuable and useful to them. Therefore throughout this work, the
anatomical
nomenclatures of the Pterichthyes follow Prof. Stensios designation
in
his
monography ¡°on the Placodermi of the Upper Devonian of East
Greenland¡± of
1948.

295.
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Palaeontologia Sinica (Whole Number 147 New Series C No. 17 The
Chinese
Kannemeyerids
ÖйúµÄ¿ÏÊÏÊÞÀà In Chinese and English bilingual
*********************************************************************
*****************
Sun Ailin/1963/225x300mm/109 pages + 8 plates/Hardcover/$58

This paper comprises results of the systematic investigation of the
large
collection of kannemeyerid materials discovered from various
localities
in
Shansi Province during the field seasons of 1955, 1956, 1958 and
1959.
Two
genera and five species including three new ones are described. On
the
basis
of morphological study and their comparison with the other known
genera
of
the group, the conclusion is arrived at that the two Chinese genera
of
kannemeyerids have the closest phylogenetic relationship with the
south
African genus Kannemeyeria. Among the evolutional trends shown in
the
dicynodonts, it is found that the two known Chinese genera of small
dicynodonts, that is, Dicynodon sinkianensis and Shansiodon, possess
certain
advanced features characteristic of the kannemeyerids. Therefore,
Shansiodon
has to be grouped with the Kannemeyeriidae, and Dicynodon
sinkianensis,
while it may be retained within the Dicynodontidae, has to be
considered as
distinct generically and the name Jimusaria is proposed. According
to
the
evolutional level reached by the Chinese kannemeyerids and the
analysis
of
the composition of the fauna, the geological age of fossil horizon
of
upper
Er-Ma-Ying formation is late early Triassic to early middle Triassic.
1. Abstract 2. Preface 3. Materials 4. Systematic Description (1)
Sinokannemeyeria Young (2) Parakannemeyeria Sun (3) Materials of
uncertain
specific affinity 5. Morphological comparison 6. Discussion on some
phyletic
problems of Chinese kannemeyerids and other genera 7. Geological
horizon and
age of the Chinese kannemeyerids

296.
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Palaeontologia Sinica (Whole Number 150, New Series C No.18) Fossil
Turtles
Of China
Öйú¹ê±îÀ໯ʯ In Chinese with English summary
*********************************************************************
***************
Ye Xiangkui/1963/303x225mm/112 pages+21 plates/Paperback/$58

1. Preface 2. Description of species (1) Suborder Amphichelydia (2)
Suborder
Pleurodira (3) Suborder Cryptodira (4) Dermatemydidae indet (5)
Emydidae
indet (6) Suborder Trionychoidea 3. Conclusion

297.
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Palaeontologia Sinica (Whole Number 153, New Series C, No. 20)
Mammalian
Fauna from the Paleocene of Nanxiong Basin, Guangdong
¹ã¶«ÄÏÐÛ¹ÅÐÂÊÀ²¸È鶯ÎïȺ In Chinese
*********************************************************************
*********************************************************
Zhou Mingzhun/1977/180x260mm/100 pages.+26 plates/Hardcover/$48

The contents of this memoir consist of five parts:
1) A summary of the continental Lower Tertiary of the Nanxiong
basin,
N.
Guangdong;
2) Sstratigraphical considerations of the Paleocene mammalian
localities and
fossiliferous horizons;
3)Notes on the age and characteristies of the Shanghu mammalian
fauna;
4)Systematic descriptions of the mammalian taxa known from the
Shanghu
Member of Paleocene Lofochai Formation; and
5) Osteology of the pantodont genus Bemalambda. The Lower Tertiary
of
the
Nanxiong Basin includes and upper part, the Danya Formation, of
probable
Eocene age, and a lower part, the Lofochai formation, of Formation,
of
provable Eocene age, and a lower part, the Lofochai formation, of
Paleocene
age, The latter is further divisible into an Upper or Nonshan Member
and a
Lower or Shanghu Member. Lithologically the Paleocene strata are
quite
similar to and hardly distinguishable from Nanxion Formation of late
Cretaceous age. Both consist dominantly of dark purplish red beds of
marly
sandstones, sandy marls and marls. The mammalian fossils described
in
this
paper were all from the Shanghu Member of the Paleocene Lofochai
formation
in which four fossiliferous beds or "zones"are present. With the
exception
of the uppermost "zone", the fossils from the lower three beds are
considered to represent a single local fauna, namely the Shanghu
Fauua.
It
is tentatively assigned to the Middle Paleocene, with Torrejonian of
the
North American as the nearest correlative.
In all 13 mammalian species representing 7 families and 4 orders are
described. Diagnoses of most of the new genera and species had been
given as
a preliminary note published in 1973 (Vet. Palasiatica, vol. 11, no
1;
pp.
31-35). Most of the mammals described are new forms. Those of the
Anagalidae, Mesonychidae, Esthonychidae and Bemalambdidae are among
the
earliest known representatives of the respective groups, and those
of
the
Hyopsodontidae, and Periptychidae(?), are known for the first time
in
Asia.

298.
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Palaeontologia Sinica (Whole Number 155, New Series C, No.
21)Gongwangling
Pleistocene Mammalian Fauna of Lantian.
In Chinese
*********************************************************************
**********************************************
Hu Changkang & Qi Tao/1978/180x260mm/64 pages+15 plates/Hardcover/$45

Mammalian fossils associated with the hominid skull cap collected
from
Gongwangling reddish clays of Lantian, shaanxi were preliminarily
studied in
1965 (Chow et al., 1965). Subsequently, the locality was further
excavated
in the summer field seasons of 1965and 1966, and more mammalian
remains
were
acquired )Woo et al.,1966). In this paper, all the Gongwangling
mammalian
remains are described in detail by the authors; their characters,
chronolgy
and relationships to other mammalian faunas are also discussed. The
locality
is situated at the northern slope of the hill of Gongwangling, which
is
a
spur of an extensive loess platform at the northern foot of the
Qinling
range on the southern side of the Ba He (River), a large tributary
entering
the Wei He (River) near Xian (See Fig. 1).

299.
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Palaeontologia sinica (Whole Number 160 New Series C, Number 22) The
Early
Tertiary Fossil Fishes from Sanshui and its Adjacent Basin, Guangdong
¹ã¶«ÈýË®ÅèµØ¼°½üÁÚÅèµØÔçµÚÈý¼ÍÓ㻯ʯ In Chinese with English summary
*********************************************************************
*********************************************************************
******
Wang Jiangke/1981/185x260mm/89 pages + 10 plates/Hardcover/$45

This paper consists of the following 4 parts: 1) The taxonomy and
description of the early tertiary fossil fishes from Sanshui Basin
and
the
adjacent districts; 2) The horizon and age of the Early tertiary
fossil
fishes from Sanshui Basin; 3) The ecological niches of the fossil
fishes; 4)
The problem of the origin of Cyprinidae. The specimens from Sanshui
Basin
and the adjacnt districts (including Longgui Basin and Dongguan
Basin)
are
mostly well preserved and have been ascribed to 2 orders, 3
families, 8
genera and 15 species, of which there are 10 new species.

300.
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Palaeontologia Sinica (Whole Number 162, New Series C, Number 23)
The
Dinosaurian Remains From Sichuan Basin, China
Öйú¹ÅÉúÎïÖ¾¡ªËÄ´¨ÅèµØÙªÂ޼ͿÖÁú»¯Ê¯ In Chinese with English summary
*********************************************************************
*************************************************
Dong Zhiming&Zhou Shiwu/1983/193x267mm/145 pages+44
plates/Hardcover/$45

The Sichuan (Basin) is a large sedimentary basin depositing the
continental
sediments of Mesozoic. The thickness of deposits is more than three
thousand
meters, composed mainly of purplish red mudstone. These sediments
present
characteristic of the fluviolacustrue facies. Rich and varied
remains
of the
dinosaurs have been found in the basin. These dinosaur-bearing
formations
are continuous from Late. Triassic to Early Cretaceous.
1.Saurischia Seeley, 1888 (1)Sauropodomorpha Huene, 1932 (2)
Theropoda
Marsh
1881 2.Ornithischia Seeley, 1888 (1)Ornithopoda Marsh, 1871
(2)Stegosauria
(Marsh 1877)

301.
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Palaeontologia Sinica (Whole Number 173, New Series C, No. 24)A
Paleocene
Edentate from Nanxiong Basin, Guangdong
¹ã¶«ÄÏÐÛ¹ÅÐÂÊÀƶ³ÝÄ¿»¯Ê¯ In Chinese with English summary
*********************************************************************
********************************************
Ding Suyin/1987/180x260mm/102 pages +14 plates/Hardcover/$48

The discovery of the succession of the Paleocene faunas in China
during
the
last twenty years has been well-known since the Paleocene fossil
remains
were first reported by Young and Chow in 1962. More than 60 genera
and
130
species of Paleocene mammals have been described up to now. The most
spectacular discovery among them is the well-preserved skeleton of
an
edentate-like mammal, Ernanodon, the study of which led to the
present
memoir. The specimen was collected from the Late Paleocene deposits
(Datang
Member of the Nongshan Formation), Nanxiong Basin, Guangdong
Province,
during a harvest field season in 1973 by a team of IVPP. The list of
the
mammalian fossils collected from the same member with Ernanodon is
cited as
following: Edentata has long been considered as an order of mammals
mainly
confined to the South American continent. Ernanodon, the earliest
known
relative of this order from outside of that continent , has
attracted
not
only much scientific interest but also arguments, since the
preliminary
report was published )Ding, 1979). Together with undescribed
notoungulates,
it raises difficult questions for the current popular hypotheses of
the
origin and the distribution of some mammals largely confined to
South
America, At the beginning of the study, even some time later, it
would
never
have been thought of an edentate because of the zoogeographic
barrier.
It
was not recognized as an edentate until comparing with
Palaeanodonts,
especially with the original specimens of that group, of North
American
Paleogene edentate-like mammals. The main part of this memoir
consists
of
the description and the discussion of the systematics of Ernanodon
which are
given as detailed as possible. In agreement with recognizing a
suborder
for
palaeanodont as Pholidots (Emry, 1970), the new suborder Ernanodonta
is
erected. The fossils, as well as the Living families of the
Edentata,
are
briefly introduced in Chinese text to the readers who are not
familiar
with
the order Edentata. The functional analysis of the cranial and the
postcranial skeleton, strongly indication scratch-digging, are also
included.

302.
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Palaeontologia Sinica (Whole Number 175, New Series C, No. 25)The
Chinese
Hipparionine Fossils
In Chinese with English summary
*********************************************************************
*************************
Qiu Zhanxiang & Huang Weilong/1987/180x260mm/248 pages+ 47
plates/Hardcover/$57

Hipparion is one of the few fossil vertebrate genera that were
recognized by
pioneer paleontologists while paleontology was still in its infancy.
The
ubiquitous nature of the hipparionine fossils gave rise to the term
"Hipparion fauna"in the Old World. On the other Hand, the earlier
evolutionists, like T. H. Huxley and B. O. Kovalewsky, found in them
an
ideal form linking the existing horse with its five-toed progenitor.
Both
brought great fame to Hipparion Paradoxically, the richness of the
fossils
caused later much confusion and uncertainty in understanding of that
particular group of animal. In result, after the first outburst of
excitement, the enthusiasm seemed to fade gradually. One of the
remarkable
effects of the postwar scientific boom is the revival of the
interest
in
many of such unsolved problems. A glance over the recent literature
will
suffice to show how fast the interest in hipparionine studies has
been
growing during the last 20 years. China made its important
contribution
to
the study of the hipparionine horses in the first decades of the
present
century, but, unfortunately, it now lags far behind. The confusion
caused by
Sefve's erection of 11 roughly contemporary species remains as
annoying
as
it was half a century ago. None of the Chinese vertebrate
paleontologists
will feel at ease until this matter is properly solved. Bearing the
matter
in mind, the senior author of the present memoir found the
hipparionine
material of the Licent's collection very suitable for a start in
that
direction, while he visited the Tianjin Natural Museum in 1979. The
specimens are well preserved. Most of them are skulls with
associated
lower
jaws and metapodials. What is more important is the fact that there
are
some
new forms evidently from the post-pomtian and pre-nihewanian time
period. As
is well known, the hipparionine fossils from this period are seldom
encountered in the Old World. From literature we know that this
collection
may be part of the material that Teilhard de Chardin planned to
study
and
publish in "Paleontologica Sinica"during the forties of the present
centure,
but he failed in fully realizing it. He succeeded in finishing the
study of
the proboscideans, artiodactyls (without suines),mustelines,
felines,
siphnines and castorids. Among the remainder of this collection the
hipparionines remain untouched. In view of the importance of the
material,
we agreed to initiate immediately a joint plan to study it.
Originally
the
authors of the present memoir did have the intention to confine
their
study
to the specimens of the Licent's collection kept now in the Tianjin
Natural
History Museum. As a matter of fact, the work had been almost
completed
when
the senior author of the present memoir took his two-years' leave
for
West
Germany. While staying in Europe, the senior author had the
opportunity
to
visit Uppsala and saw Sefve's original specimens. Since then it has
been
clear that, without a revision of the Sefve's much confused species,
the
hipparionines from Yushe can not be properly understood. After
returning to
China, the scope or the work was considerably widened, so that all
the
available unstudied materials have been included in the present
volume.
Practically, the work turns now to be a general review and revision
of
all
available Chinese hipparionine materials, which are partly new,
partly
previously described. The specimens to be studied here total 358,
among
which 60 are well preserved skulls and jaws.

303.
*********************************************************************
*******************************************************************
Palaeontologia Sinica (Whole Number 191, New Series C, Number 27)
Early
Pleistocene Mammalian Fauna from Longdan, Dongxiang, Gansu, China
¸ÊËà¶«ÏçÁúµ£Ôç¸üÐÂÊÀ²¸È鶯ÎïȺ In Chinese with English summary
*********************************************************************
*******************************************************************
Qiu Zhanxiang/2004/295x210mm/198 pages + 34 plates/Paperback/$55

This collection includes the fossils from Longdan as well as from
Shitougou,
Keshijian, and Xijia, yielding the same kind of fossils from loess.
Up
to
now about 300 specimens representing 31 mammalian taxa were
gathered.
The
best part of the collection has already been fully prepared: it
includes 165
specimens, among which more than one hundred are well preserved
skulls,
maxillaries and mandibles. The remaining part of the collection is
still
being prepared: it contains mainly limb-bones as well as skull and
jaw
materials of the taxa already adequately represented in the prepared
specimens. This notwithstanding, we deem the available material and
adequate
representation of the Longdan fauna, especially for the large
mammals.

304.
*********************************************************************
******************************************************************
Palaeontologia Sinica( Whole Number 192, New Series C, Number 28)
Fossil
Mammals from Early Eocene Wutu Formation of Shandong Province
Öйú¹ÅÉúÎïÖ¾ ×ܺŵÚ192²á бûÖÖµÚ28ºÅ
ɽ¶«²ýÀÖÎåͼÅèµØÔçʼÐÂÊÀ²¸È鶯ÎïȺ In
Chinese with English summary
*********************************************************************
******************************************************************
By Tong Yongsheng & Wang
Yingwen/2006/185x260mm/201pages+11plates/Paperback/$35

The Wutu Basin is one of the most important Paleogene sedimentary
basins in
China, and is situated 10km east of Changle City, central Shandong
Province.
Prof. C.C. Young (1944) first described a fossil lizard,
Changlosaurus
wutuensis, which possibly came fro the coal beds of the Wutu
Formation
(Young, 1961). The first mammal fossil, Homogalax wutuensis, was
collected
from ¡°the Middle Coal-bearing Member¡± of the Wutu Formation in the
middle
part of Laowanggou by Prof. Li Chuankuei and his colleagues (Chow
and
Li,
1963, 1965). A coryphodont fossil )Heterocoryphodon? Yuntongi
sp.nov.)
was
probably found at the same locality (Li Y-T, 1985). In 1990 we found
some
tooth fragments in the middle part of Laowanggou (Text-fig.1_. Since
then,
we and our colleagues collected numerous mammal fossils in several
field
seasons. Up to date, 51 species belonging to 34 families in 18
orders
were
obtained. These mammals are recorded in this monograph, except that
two
taxa
of plesiadapiformes will be reported separately by Dr.C. Beard of
the
Carnegie Museum of Nature History and the second author of this
book.With 48
illustrations, 33 tables, 11 plates.


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#191 From: John Jackson <strangetruther@...>
Date: Sat Sep 23, 2006 1:32 pm
Subject: Re: [Palaeo-oology] Eggshells in Caves
strangetruther
Offline Offline
Send Email Send Email
 
...and another favourite of David Attenborough - the
"birds nest soup" bird(s), too.

http://en.wikipedia.org/wiki/Swiftlet

Cave-nesting would be a great selector for post-K
survival.

JJ.


--- Alvaro Mones <amones@...> wrote:

> As far as I know Steatornis caripensis
> (Steatornithidae) do.
> Alvaro
>
> *******************************
> Alvaro Mones
> Franzensbadstr. 7 B
> D-86199 Augsburg
> Deutschland/Germany
>
> Tel.: (0049-821) 9985991
> Handy: 0160/979 888 42
> Skype: alvaromones
> E-mail: a-mones@...  amones@...
>   ----- Original Message -----
>   From: Judith Harris
>   To: Palaeo-oology@...
>   Sent: Thursday, 21 September, 2006 21:27
>   Subject: Re: [Palaeo-oology] Eggshells in Caves
>
>
>   Xavier,
>
>   I have never heard of birds nesting in caves but
> that doesn't mean
>   they don't. Just seems unlikely to me--but the
> most unlikely things
>   seem to happen anyway.
>
>   judith harris
>   emerita professor
>   university of colorado museum
>   p.o. box 278
>   chama, nm  87520
>   harrisj@...
>
>
>   On Sep 21, 2006, at 12:30 PM, cogombra wrote:
>
>   >
>   > Prof. Carbonell and I last summer were wandering
> why eggs and nests
>   > have not bee preserved in caves.
>   >
>   > Caves are ideal for birds to nest and for the
> preservation of  their
>   > eggshells.
>   >
>   > As suggested by Prof. Carbonell I read Owls,
> Caves and Fossils by
>   > Prof. Andrews, and I could not find any
> information related to my
>   > question.
>   >
>   > Please,  I would appreciate if somebody could
> help us.
>   >
>   > Respectfully,
>   >
>   > Xavier Panades I Blas
>   >
>   >
>   >
>   >
>   >
>
>


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#189 From: "Alvaro Mones" <amones@...>
Date: Fri Sep 22, 2006 7:32 am
Subject: Re: [Palaeo-oology] Eggshells in Caves
alvaromones
Offline Offline
Send Email Send Email
 
As far as I know Steatornis caripensis (Steatornithidae) do.
Alvaro
 
*******************************
Alvaro Mones
Franzensbadstr. 7 B
D-86199 Augsburg
Deutschland/Germany
 
Tel.: (0049-821) 9985991
Handy: 0160/979 888 42
Skype: alvaromones
E-mail: a-mones@...  amones@...
----- Original Message -----
Sent: Thursday, 21 September, 2006 21:27
Subject: Re: [Palaeo-oology] Eggshells in Caves

Xavier,

I have never heard of birds nesting in caves but that doesn't mean 
they don't. Just seems unlikely to me--but the most unlikely things 
seem to happen anyway.

judith harris
emerita professor
university of colorado museum
p.o. box 278
chama, nm  87520
harrisj@...


On Sep 21, 2006, at 12:30 PM, cogombra wrote:

>
> Prof. Carbonell and I last summer were wandering why eggs and nests
> have not bee preserved in caves.
>
> Caves are ideal for birds to nest and for the preservation of  their
> eggshells.
>
> As suggested by Prof. Carbonell I read Owls, Caves and Fossils by
> Prof. Andrews, and I could not find any information related to my
> question.
>
> Please,  I would appreciate if somebody could help us.
>
> Respectfully,
>
> Xavier Panades I Blas
>
>
>
>
>


#188 From: Judith Harris <harrisj@...>
Date: Thu Sep 21, 2006 7:27 pm
Subject: Re: [Palaeo-oology] Eggshells in Caves
palaeochromis
Offline Offline
Send Email Send Email
 
Xavier,

I have never heard of birds nesting in caves but that doesn't mean
they don't. Just seems unlikely to me--but the most unlikely things
seem to happen anyway.

judith harris
emerita professor
university of colorado museum
p.o. box 278
chama, nm  87520
harrisj@...


On Sep 21, 2006, at 12:30 PM, cogombra wrote:

>
> Prof. Carbonell and I last summer were wandering why eggs and nests
> have not bee preserved in caves.
>
> Caves are ideal for birds to nest and for the preservation of  their
> eggshells.
>
> As suggested by Prof. Carbonell I read Owls, Caves and Fossils by
> Prof. Andrews, and I could not find any information related to my
> question.
>
> Please,  I would appreciate if somebody could help us.
>
> Respectfully,
>
> Xavier Panades I Blas
>
>
>
>
>

#186 From: "cogombra" <cogombra@...>
Date: Thu Sep 21, 2006 6:30 pm
Subject: Eggshells in Caves
cogombra
Offline Offline
Send Email Send Email
 
Prof. Carbonell and I last summer were wandering why eggs and nests
have not bee preserved in caves.

Caves are ideal for birds to nest and for the preservation of  their
eggshells.

As suggested by Prof. Carbonell I read Owls, Caves and Fossils by
Prof. Andrews, and I could not find any information related to my
question.

Please,  I would appreciate if somebody could help us.

Respectfully,

Xavier Panades I Blas

#183 From: John Jackson <strangetruther@...>
Date: Tue Sep 19, 2006 1:15 pm
Subject: Re: [Palaeo-oology] Please, use Palaeooology more often from now on....
strangetruther
Offline Offline
Send Email Send Email
 
I wonder if UK based palaeontologists will be able to
have their own special spelling - with four vowels in
a row? :- palaeoology.

And I was never quite sure - is it:
pally - oo - ology ?

Cheeres,

John J.


--- cogombra <cogombra@...> wrote:

> From: "Gary Rosenberg" <rosenberg@...>
> Reply-To: paleonet@...
> To: <paleonet@...>
> Subject: Re: paleonet Welcome to The
> Palaeo-oological Discussion
> Group
> Date: Fri, 15 Sep 2006 18:16:40 -0400
>
> The Oxford English Dictionary works on an
> evidence-based approach.
> If a
> particular spelling is prevalent among the genuine
> uses of a word,
> the
> OED
> would list that as the primary spelling, taking into
> account regional
> variations such as American versus British
> spellings. If there is
> conflicting usage, an editor presumably will chose
> one as most
> consistent
> with normal patterns in English. All of the
> discussion on this
> listserv
> could be fodder for the determination, since the
> editors routinely
> use
> Internet searches and databases to find uses of
> word. So there is no
> need to
> submit the variant spellings individually; they will
> be considered.
>
> As yet there appear to be only 2 independent uses of
> paleoology and
> its
> cognates: the journal article from 2004, and
> Xavier's announcement
> of
> the
> discussion group, which started this thread. All the
> uses within the
> thread
> are meta-usages, which might influence editors if
> the evidence of
> spelling
> is contradictory, but what will count more is uptake
> in the
> professional
> literature. The OED generally wants at least 6
> independent uses of a
> word
> with some chronological separation for it to qualify
> for listing. So
> Jere,
> start publishing paleooological papers, if that is
> the spelling you
> want to
> prevail. You'll have to get the spellings past the
> journal editors
> too.
> I've
> tried to sneak "shellless" into print for three l's
> in a row, but no
> editor
> has yet let it stand; it always becomes
> "shell-less".
>
> It's interesting to contemplate that as scientists
> describe the world
> biologically, the etymologists are circumscribing
> the geographical
> and
> chronological distributions of our words. They even
> have analogs to
> Lazarus
> taxa, searching for interdatings as well as first
> and last
> occurrences.
>
> Gary
>
>
>
>
>
>
>
>
>
> Yahoo! Groups Links
>
>
>
>
>
>
>


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#182 From: "cogombra" <cogombra@...>
Date: Tue Sep 19, 2006 8:16 am
Subject: Please, help with the definition of Palaeooology...
cogombra
Offline Offline
Send Email Send Email
 
Hi everybody,

Robert Hunter has suggested that we entry a definition of palaeooology
in the wikipwedia dictionary...Any suggestions for a definition waht
to say etc...


From: "Robert Huber" <robert.huber@...>
Reply-To: paleonet@...
To: <paleonet@...>
Subject: RE: paleonet Welcome to The Palaeo-oological Discussion Group
Date: Tue, 19 Sep 2006 09:23:03 +0200

Maybe the paleooologists should start with an wikipedia entry?

#181 From: "cogombra" <cogombra@...>
Date: Mon Sep 18, 2006 9:18 pm
Subject: Please, use Palaeooology more often from now on....
cogombra
Offline Offline
Send Email Send Email
 
From: "Gary Rosenberg" <rosenberg@...>
Reply-To: paleonet@...
To: <paleonet@...>
Subject: Re: paleonet Welcome to The Palaeo-oological Discussion
Group
Date: Fri, 15 Sep 2006 18:16:40 -0400

The Oxford English Dictionary works on an evidence-based approach.
If a
particular spelling is prevalent among the genuine uses of a word,
the
OED
would list that as the primary spelling, taking into account regional
variations such as American versus British spellings. If there is
conflicting usage, an editor presumably will chose one as most
consistent
with normal patterns in English. All of the discussion on this
listserv
could be fodder for the determination, since the editors routinely
use
Internet searches and databases to find uses of word. So there is no
need to
submit the variant spellings individually; they will be considered.

As yet there appear to be only 2 independent uses of paleoology and
its
cognates: the journal article from 2004, and Xavier's announcement
of
the
discussion group, which started this thread. All the uses within the
thread
are meta-usages, which might influence editors if the evidence of
spelling
is contradictory, but what will count more is uptake in the
professional
literature. The OED generally wants at least 6 independent uses of a
word
with some chronological separation for it to qualify for listing. So
Jere,
start publishing paleooological papers, if that is the spelling you
want to
prevail. You'll have to get the spellings past the journal editors
too.
I've
tried to sneak "shellless" into print for three l's in a row, but no
editor
has yet let it stand; it always becomes "shell-less".

It's interesting to contemplate that as scientists describe the world
biologically, the etymologists are circumscribing the geographical
and
chronological distributions of our words. They even have analogs to
Lazarus
taxa, searching for interdatings as well as first and last
occurrences.

Gary

#180 From: "cogombra" <cogombra@...>
Date: Mon Sep 18, 2006 9:17 pm
Subject: Is there any record of fossil snail eggs?
cogombra
Offline Offline
Send Email Send Email
 
From: "Gary Rosenberg" <rosenberg@...>
To: <cogombra@...>
Subject: Re: paleonet Welcome to The Palaeo-oological Discussion
Group
Date: Mon, 18 Sep 2006 13:18:50 -0400


Plain Text Attachment [ Scan and Save to Computer | Save to Yahoo!
Briefcase ]

Hi Xavier,

I've sent a reply to list. But I also had something to mention to
you.
I've
seen fossil snail eggs in Pleistocene deposits from Jamaica, and
what
might
be fossil ant eggs. The snail eggs are preserved because they have
calcareous shells (in members of the family Sagdidae). I broke open
some of
the eggs and found an intact protoconch in one. Have there been
published
reports of fossil snail eggs?

Thanks,
Gary

#179 From: "cogombra" <cogombra@...>
Date: Fri Sep 15, 2006 9:48 am
Subject: Houde, P. 1988.
cogombra
Offline Offline
Send Email Send Email
 
Hi,

If you wish a PDF copy ofthe below paper that mention ratite eggshells
with pictures etc and any other from the same authors.

Visit his website:

http://biology-web.nmsu.edu/houde/phoude.htm



Houde, P.  1988.  Paleognathous birds from the early Tertiary of the
Northern Hemisphere (R. A. Paynter, Jr. ed.) Publications of the
Nuttall Ornithological Club, No. 22, Cambridge MA, 148 pp. pdf

#178 From: Konstantin Mikhailov <konstm@...>
Date: Thu Sep 14, 2006 4:52 am
Subject: Re: [Palaeo-oology] A PDF paper of a fossiled nest
parataxonomy
Offline Offline
Send Email Send Email
 

It would be appreciated!


Вы писали 13 сентября 2006 г., 0:14:55:


>

Anybody fancy a copy of this one?



Mikulá¹ R. & Zasadil B.2004. A

probable fossil bird nest, ?Eocavum isp., from the Miocene wood of the

Czech Republic. In: Mikulá¹ R. /ed./ ( 2004):  Abstract Book. 4th

International Bioerosion Workshop. Prague, August 30-September 3, 2004.

-  Institute of Geology, Academy of Sciences,  Praha, p. 49-51.






 





-- 


  Konstantin Mikhailov                         mailto:konstm@...


#177 From: "cogombra" <cogombra@...>
Date: Wed Sep 13, 2006 7:44 pm
Subject: FW: Re: We must Help Dr. K.R. Rai with his eye sickness please, answer!!!!
cogombra
Offline Offline
Send Email Send Email
 
Dear everybody,

My dear friend Dr. K.R. Rai (the first local ethnic Nepali that
obtained a PhD in his country) has suffered "Central Vein of retina
Occlusion."

Unless, he is operated quite soon (over the next months) he will
lose his vision totally over the next years (see email from his son
below).

As you could understand it is very important that Dr. K.R. Rai
carries on educating his own people and his own scientific career.

They live in a very poor area, and cannot afford the treatment is
not likely available in Nepal.

Please, I would appreciate if you could Dr. K.R. Rai in anyway such
as charities, etc..

Respectfully,

Xavier



From: "Bishwahang Kirat" <bishwahang.kirat@...>
To: "Xavier Panades I Blas" <cogombra@...>
Subject: Re: We must Help Dr. K.R. Rai with his eye sickness please,
answer!!!!
Date: Wed, 13 Sep 2006 16:19:06 +0545

Dear Xavier Bro,
The Problem with my dad is "Central Vein of retina Occlusion"(in
Short.CVRO).
It was all due to sudden rise in his Blood Pressure(BP), due to
which his
Viens in eye was ruptured and the blood got clotted in the retina.
Hence his
vision is very low, about 10% and now he is going on treatment to
save the
vision he has now.
The Optuculist says there aint treatment for this and he will loose
his all
vision within some years. But i havent told my dad that.But i think
there
must be some medical treatment cos, medical science has devloped so
much.
What if we could replace the Retina of Eye? Is It possible.

#176 From: Judith Harris <harrisj@...>
Date: Wed Sep 13, 2006 1:04 am
Subject: Re: [Palaeo-oology] A PDF paper of a fossiled nest
palaeochromis
Offline Offline
Send Email Send Email
 
I just realized that what you sent me was a copy of this abstract
with photos. What a great fossils. Also after reading this through I
know that it is silicified wood.

Thanks so much.

Judith Harris
harrisj@...



On Sep 12, 2006, at 2:14 PM, cogombra wrote:

> Anybody fancy a copy of this one?
>
>
> Mikulá¹ R. & Zasadil B.2004. A
> probable fossil bird nest, ?Eocavum isp., from the Miocene wood of the
> Czech Republic. In: Mikulá¹ R. /ed./ ( 2004):  Abstract Book. 4th
> International Bioerosion Workshop. Prague, August 30-September 3,
> 2004.
> -  Institute of Geology, Academy of Sciences,  Praha, p. 49-51.
>
>
>
>
>
>

#175 From: Judith Harris <harrisj@...>
Date: Wed Sep 13, 2006 1:01 am
Subject: Re: [Palaeo-oology] A PDF paper of a fossiled nest
palaeochromis
Offline Offline
Send Email Send Email
 
Yes please I would love to see this even if only in abstract.

Judith

Judith Harris
harrisj@...



On Sep 12, 2006, at 2:14 PM, cogombra wrote:

> Anybody fancy a copy of this one?
>
>
> Mikulá¹ R. & Zasadil B.2004. A
> probable fossil bird nest, ?Eocavum isp., from the Miocene wood of the
> Czech Republic. In: Mikulá¹ R. /ed./ ( 2004):  Abstract Book. 4th
> International Bioerosion Workshop. Prague, August 30-September 3,
> 2004.
> -  Institute of Geology, Academy of Sciences,  Praha, p. 49-51.
>
>
>
>
>
>

#174 From: ecoroma@...
Date: Tue Sep 12, 2006 11:35 pm
Subject: Re: [Palaeo-oology] Hans-Volker Karl, Gottfried Tichy & Roland Müller 2006
ecoroma@...
Send Email Send Email
 
Xavier, please, I want one of this.
Thanks again

Eduardo


Mensaje citado por: cogombra <cogombra@...>:

> Anybody interested in the PDF copy of the below publication?
>
>
> Thank you to Karl Hans-Volker
>
> Hans-Volker Karl, Gottfried Tichy & Roland Müller
> Prähistorische Vogel-und Eischalenfragmente der Wüste Sulze bei Erfurt
> Vogelwarte 44, 2006: 183190
> © DO-G, IfV, MPG 2006
>
> It is a paper on prehistoric bird egg shells from Thuringia in Germany
> (archeozoological results).
>
>
>
>
>
>
>
>
> Yahoo! Groups Links
>
>
>
>
>



Eduardo Corona-M.
Laboratorio de Arqueozoología &
Seminario Relaciones Hombre -Fauna
(http://www.geocities.com/shofaun),
Instituto Nacional de Antropología e Historia
México

-------------------------------------------------
www.correo.unam.mx
UNAMonos Comunicándonos

#173 From: ecoroma@...
Date: Tue Sep 12, 2006 11:36 pm
Subject: Re: [Palaeo-oology] A PDF paper of a fossiled nest
ecoroma@...
Send Email Send Email
 
ooops!
an another one of this-
Thanks

Eduardo


Mensaje citado por: cogombra <cogombra@...>:

> Anybody fancy a copy of this one?
>
>
> Mikulá¹ R. & Zasadil B.2004. A
> probable fossil bird nest, ?Eocavum isp., from the Miocene wood of the
> Czech Republic. In: Mikulá¹ R. /ed./ ( 2004):  Abstract Book. 4th
> International Bioerosion Workshop. Prague, August 30-September 3, 2004.
> -  Institute of Geology, Academy of Sciences,  Praha, p. 49-51.
>
>
>
>
>
>
>
>
> Yahoo! Groups Links
>
>
>
>
>



Eduardo Corona-M.
Laboratorio de Arqueozoología &
Seminario Relaciones Hombre -Fauna
(http://www.geocities.com/shofaun),
Instituto Nacional de Antropología e Historia
México

-------------------------------------------------
www.correo.unam.mx
UNAMonos Comunicándonos

#172 From: "Charles Deeming" <charlie@...>
Date: Tue Sep 12, 2006 8:27 pm
Subject: Re: [Palaeo-oology] A PDF paper of a fossiled nest
charles_deeming
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Yes please!!
 
Charles
 
----- Original Message -----
From: cogombra
Sent: Tuesday, September 12, 2006 9:14 PM
Subject: [Palaeo-oology] A PDF paper of a fossiled nest

Anybody fancy a copy of this one?


Mikulá¹ R. & Zasadil B.2004. A
probable fossil bird nest, ?Eocavum isp., from the Miocene wood of the
Czech Republic. In: Mikulá¹ R. /ed./ ( 2004):  Abstract Book. 4th
International Bioerosion Workshop. Prague, August 30-September 3, 2004.
-  Institute of Geology, Academy of Sciences,  Praha, p. 49-51.






#171 From: "cogombra" <cogombra@...>
Date: Tue Sep 12, 2006 8:14 pm
Subject: A PDF paper of a fossiled nest
cogombra
Offline Offline
Send Email Send Email
 
Anybody fancy a copy of this one?


Mikulá¹ R. & Zasadil B.2004. A
probable fossil bird nest, ?Eocavum isp., from the Miocene wood of the
Czech Republic. In: Mikulá¹ R. /ed./ ( 2004):  Abstract Book. 4th
International Bioerosion Workshop. Prague, August 30-September 3, 2004.
-  Institute of Geology, Academy of Sciences,  Praha, p. 49-51.

#170 From: "cogombra" <cogombra@...>
Date: Tue Sep 12, 2006 6:15 pm
Subject: Hans-Volker Karl, Gottfried Tichy & Roland Müller 2006
cogombra
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Anybody interested in the PDF copy of the below publication?


Thank you to Karl Hans-Volker

Hans-Volker Karl, Gottfried Tichy & Roland Müller
Prähistorische Vogel-und Eischalenfragmente der Wüste Sulze bei Erfurt
Vogelwarte 44, 2006: 183190
© DO-G, IfV, MPG 2006

It is a paper on prehistoric bird egg shells from Thuringia in Germany
(archeozoological results).

#169 From: Konstantin Mikhailov <konstm@...>
Date: Tue Sep 12, 2006 11:12 am
Subject: Re: [Palaeo-oology] Re: I have a copy of Sahni, A., Kumar, G., Bajpai, S., and Srinivasan, S. 1990
parataxonomy
Offline Offline
Send Email Send Email
 

 Sahni, A., Kumar, G., Bajpai, S., and Srinivasan, S. 1990. A review 

of Late Pleistocene ostriches (Struthio sp. in India. Man and  Environment, 15(1):41-47.


I would also appreciate a copy to: 

konstm@...



Thank you!

Konstantin Mikhailov



Вы писали 11 сентября 2006 г., 20:47:51:


>

--- In Palaeo-oology@..., "cogombra" <cogombra@y...> 

wrote:

>

> Thank to Prof. Sahni and R. Patnaik for the PDF copy of the below 

> paper...

> Does anybody fancy a copy?

> Sahni, A., Kumar, G., Bajpai, S., and Srinivasan, S. 1990. A review 

of 

> Late Pleistocene ostriches (Struthio sp. in India. Man and 

> Environment, 15(1):41-47.

>

I would also appreciate a copy to: 

tommy.tyrberg@...


Tommy Tyrberg





 





-- 


  Konstantin Mikhailov                         mailto:konstm@...


#168 From: "Alvaro Mones" <amones@...>
Date: Tue Sep 12, 2006 7:36 am
Subject: Fw: Tertiary Bird egg and nests from SouthCentral and America
alvaromones
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> Dear Xavier,
> I couldn't find references to South American Tertiary avian nests or eggs
> but bellow I send you some references that I have not seen in your
> bibliographical listing (there is a lot of abstracts of congress that I'm
> not including). I think that this addenda may be of interest to some
> colleagues in the palaeoo/o-ooöology (or what so ever) list.
> Cheers,
> Alvaro
>
> Azevedo, S. A. K. de, V. G. da Silva & J. Ferigolo. 1994. Um ovo de
> quelônio do Neocretáceo brasileiro. Anais da Academia Brasileira de
> Ciências, 66(2):255. Rio de Janeiro.
>
> Azevedo, S. A., V. Gallo & J. Ferigolo. 2000. A possible chelonian egg
> from the Brazilian late Cretaceous. Anais da Academia Brasileira de
> Ciências, 72(2):187-193, figs. 1-5. Rio de Janeiro.
>
> Borgomanero, G. & G. Leonardi. 1981. Um ovo de dinossauro de
> Aix-en-Provence (França) e fragmentos de ovos fósseis de outras
> procedéncias conservados em Curitiba, Paraná. Atas 3° Simpósio Regional de
> Geologia (Curitiba), 2:213-225, láms. 1-3.
>
> Campos, D. de A. & R. J. Bertini. 1985. Ovos de dinossauro da Formação
> Uberaba, Cretáceo superior do Estado de Minas Gerais. 9° Congresso
> Brasileiro de Paleontologia (Fortaleza, 1985), Resumos das Comunicações,
> p. 19.
>
> Carpenter, K. 1999. Eggs, nests, and baby dinosaurs. A look at dinosaur
> reproduction. Pp. xi + 1-336, láms. 1-13, figs. Indiana University Press,
> Bloomington.
>
> Casadío, S. T. Manera, A. Parras, C. Montalvo & G. Cornachione. 2000.
> Primer registro en superficie de sedimentitas continentales del Cretácico
> superior en la cuenca dle Colorado, sureste de La Pampa. Revista de la
> Asociación Geológica Argentina, 55(1-2):129-133, figs. 1-2. Buenos Aires.
>
> Casadío, S., T. Manera, A. Parras & C. I. Montalvo. 2002. Huevos de
> dinosaurios (Faveoloolithidae) del Cretácico superior de la cuenca del
> Colorado, Provincia de La Pampa, Argentina. Ameghiniana, 39(3):285-293,
> figs. 1-4. Buenos Aires.
>
> Chiappe, L. M. & R. A. Coria. 2004. Auca Mahuevo, un extraordinario sitio
> de nidificación de dinosaurios saurópodos del Cretácico tardío, Neuquén,
> Argentina. Ameghiniana, 41(4):591-596, figs. 1-5. Buenos Aires.
>
> Chiappe, L. M. & L. Dingus. 2001. Walking on eggs. The astonishing
> discovery of thousands of dinosaur eggs in the badlands of Patagonia. Pp.
> 1-[221], 8 pls., 39 figs. Scribner, New York.
>
> Faccio, G. 1994. Un inusual huevo multicáscara de dinosaurio.
> Paleociencias del Uruguay, (Serie Didáctica)2:15. Montevideo.
>
> Faccio, G. & J. Montaña. 1994. Registro fósil in situ de huevos de
> dinosaurios del Cretácico superior de Durazno y la presencia de
> Faveoloolithidae (Zhao et Ding 1976) en huevos de dinosaurios del Uruguay.
> Paleociencias del Uruguay, (Serie Didáctica)2:16-18. Montevideo.
>
> Gobbo-Rodrigues, S. R., A. W. A. Kellner, D. de A. Campos, L. B. de
> Carvalho & S. A. K. de Azevedo. 2005. New information on theropod eggs
> from the late Cretaceous Bauru Group, Brazil. 2° Congresso
> Latino-Americano de Paleontologia de Vertebrados (Rio de Janeiro,
> 10-12.08.2005), Boletim de Resumos, p. 124.
>
> Grellet-Tinner, G. 2000. Phylogenetic interpretation of eggs and eggshells
> of Paleognathae. First International Symposium of Dinosaur Eggs and Babies
> (Isona, 2000), Extended Abstracts, pp. 61-75, figs. 1-12.
>
> Grellet-Tinner, G. 2005. Membrana testacea of titanosaurid dinosaur eggs
> from auca Mahuevo (Argentina): implications for exceptional preservation
> of soft tissue in Lagerstätten. JVP, 25(1):99-106, figs. 1-4.
>
> Grellet-Tinner, G. & L. M. Chiappe. 2004. Dinosaur eggs and nesting:
> Implications for understanding the origin of birds, in Currie, P.J., E. B.
> Koppelhus, M. A. Shugar & J. L. Wright (eds.): Feathered dragons: Studies
> on the transition from dinosaurs to birds, pp. 185-214, figs. 1-18.
> Indiana University Press, Bloomington.
>
> Grellet-Tinner, G., L. M. Chiappe & R. Coria. 2004. Eggs of titanosauroid
> sauropods from the upper Cretaceous of Auca Mahuevo (Argentina). Canadian
> Journal of Earth Sciences, 41(8):949-960, figs. 1-4.
>
> Grellet-Tinner, G., L. M. Chiappe, M. Norell & D. Bottjer. 2006. Dinosaur
> eggs and nesting behaviors: A paleobiological investigation.
> Palaeogeography, Palaeoclimatology, Palaeoecology, 232(2-4):294-321, figs.
> 1-10.
>
> López-Martínez, N. 2003. Dating dinosaur oodiversity: chronostratigraphic
> control of late Cretaceous oospecies succession. Palaeovertebrata,
> 32(2-4):121-148, lám. 1., figs. 1-5. Montpellier.
>
> Manera de Bianco, T. 1996. Nueva localidad con nidos y huevos de
> dinosaurios (Titanosauridae) del Cretácico superior, Cerro Blanco,
> Yaminué, Río Negro, Argentina. Publicación Especial, 4:59-67, figs. 1-10.
> Asociación Paleontológica Argentina, Buenos Aires.
>
> Manera de Bianco, T. 2000. Un nuevo tipo de cáscara de huevo del Cretácico
> superior del Cerro Blanco, Yaminue, Provincia de Río Negro, Argentina.
> Ameghiniana Resúmenes, 37(4 Suplemento):24R. Buenos Aires.
>
> Manera de Bianco, T. & G. Köhler. 2003. Primer registro de cáscaras de
> huevo de la oofamilia Spheroolithidae (Zhao, 1979) en Yaminué (Cretácico
> superior), Provincia de Río Negro, Argentina. Ameghiniana Resúmenes, 40(4,
> Suplemento):62R. Buenos Aires.
>
> Manera, T. C. I, Montalvo, S. Casadío & A. M. Parras. 1999. Huevos de
> dinosaurios del Cretácico superior en el departamento Hucal, Provincia de
> la Pampa, Argentina. Jornadas Pampeanas de Ciencias Naturales, 7(Santa
> Rosa, 1-3.12.1999), p. 46.
>
> Manera, T., A. Parras, C. Montalvo & S. Casadío. 2000. Parataxonomía de
> huevos de dinosaurios del Cretácico superior, cuenca del Colorado, La
> Pampa, Argentina. Ameghiniana Resúmenes, 37(4 Suplemento):75R. Buenos
> Aires.
>
> Powell, J. E. 1996. Nuevos datos sobre huevos de dinosaurios del Cretácico
> superior de Río Negro, Argentina. Ameghiniana, 33(4):470. Buenos Aires.
>
> Ribeiro C. M. M. 2002. Ovo e fragmentos de cascas de ovos de dinossauros,
> provenientes da região de Peirópolis, Uberaba, Minas Gerais. Arquivos do
> Museu Nacional, 60(3):223-228, figs. 1-2. Rio de Janeiro.
>
> Ribeiro, C. M. M. & L. C. Ribeiro. 2000. Nuevo hallazgo de huevo fósil y
> fragmentos de cáscaras de huevos en la Formación Marília (Cretácico
> tardío), Uberaba, Minas Gerais, Brasil. Ameghiniana Resúmenes, 37(4
> Suplemento):27R-28R. Buenos Aires.
>
> Ribeiro, C. M. M., I. de S. Carvalho & W. R. Nava. 2006. Ovos de
> crocodilomorfos da Formação Araçatuba (Bacia Bauru, Cretáceo superior),
> Brasil, in Gallo, V., P. M. Brito, H. M. A. Silva & F. J. Figueiredo
> (eds.): Paleontologia de Vertebrados: Grandes temas e contribuições
> científicas, pp. 285-292, figs. 1-2. Editora Interciência, Rio de Janeiro.
>
> Schweitzer, M. H., F. D. Jackson, L. M. Chiappe, J. O. Calvo & D. E.
> Rubilar. 2001. Cretaceous avian eggs and embryos from Argentina. JVP,
> 21(3, supplement):99A.
>
> Schweitzer, M. H., F. D. Jackson, L. M. Chiappe, J. G. Schmitt, J. O.
> Calvo & D. E. Rubilar. 2002. Late Cretaceous avian eggs with embryos from
> Argentina. JVP, 22(1):191-195, figs. 1-3.
>
> Sigé, B. 1968. Dents de micromammifères et fragments de coquilles d'oeufs
> de dinosauriens dans la faune de vertébrés du Crétacé supérieur de Laguna
> Umayo (Andes péruviennes). Comptes Rendus hebdomadaires des Séances de
> l'Academie des Sciences, (D)267():1495-1498. Paris.
>
> Valais, S. de, S. Apesteguía & D. Udrizar Sauthier. 2003. Nuevas
> evidencias de dinosaurios de la Formación Puerto Yeruá (Cretácico),
> Provincia de Entre Ríos, Argentina. Ameghiniana, 40(4):631-635, figs. 1-4.
> Buenos Aires.
>
> Vicalvi, M. A., C. S. Ferreira, I. de S. Carvalho & S. M. dos Anjos. 1993.
> Fragmentos de ovos de dinossauros na Formação Itapecuru, Maranhão: uma
> discussão. Anais da Academia Brasileira de Ciências, 65(2):218. Rio de
> Janeiro.
>
> *******************************
> Alvaro Mones
> Franzensbadstr. 7 B
> D-86199 Augsburg
> Deutschland/Germany
>
> Tel.: (0049-821) 9985991
> Handy: 0160/979 888 42
> Skype: alvaromones
> E-mail: a-mones@...  amones@...
>
>
>
> ----- Original Message -----
> From: "Xavier Panades I Blas" <cogombra@...>
> To: <a-mones@...>; <alvaromones@...>; <amones@...>
> Sent: Monday, 11 September, 2006 14:13
> Subject: Tertiary Bird egg and nests from SouthCentral and America
>
>
>>
>> Alvaro no encuentro ninguna publi que diga que se han encontrado Tertiary
>> Bird egg and nests from SouthCentral and America...Dame una ayuda por
>> favor!
>>
>>
>> Respectfully,
>>
>> Xavier Panades I Blas
>> 55, Marksbury Road
>> Bedminster
>> Bristol BS3 5JY
>> England (EC)
>>
>> http://www.acs.bolton.ac.uk/~xp1pls/
>>
>>
>>
>

#167 From: Xavier Panades I Blas <cogombra@...>
Date: Mon Sep 11, 2006 8:52 pm
Subject: Re: [Palaeo-oology] Our field of work, Paleooology, to be legalised by the Oxford English Dictionary
cogombra
Offline Offline
Send Email Send Email
 
Hi,
 
We are witnessing and contributing to the legal and official Birth of a new science by accident like evolution...And I am in the middle...
Excellent, I am glad that his is getting somewhere...
 
I am very busy I wll try to update the publication list soon...You keep on sending cites!

Judith Harris <harrisj@...> wrote:
I am definitely in favor of this. One of my dearest students, 
friends, and colleagues, Karl Hirsch, was a great paleoologist.

Judith


judith harris
emerita professor
university of colorado museum
p.o. box 278
chama, nm  87520
harrisj@...


On Sep 11, 2006, at 7:34 AM, cogombra wrote:

> Dear Everybody,
>
>
> Palaeoology, Paleooology, and Paleoöology will likely be a term in
> the Oxford English Dictionary.
>
> Thanks to Gary...
>
>
> From: "Gary Rosenberg" <rosenberg@...>
> Reply-To: paleonet@...
> To: <paleonet@...>
> Subject: Re: paleonet Welcome to The Palaeo-oological Discussion
> Group
> Date: Mon, 11 Sep 2006 08:57:14 -0400
>
> I'm an adviser to the Oxford English Dictionary, and have forwarded
> the message to the appropriate editor. I'd guess they'd standardize
> it to palaeoology if the word and its cognates continue to be used.
> The first occurrence may be
>
> Estudios Geologicos 60, no.3-6 (2004) p. 179: "Most sites contain
> bony remains, but there are also paleoichnological and paleoological
> sites, with dinosaur and other reptilian tracks and eggshells."
>
> Gary Rosenberg
>
> >>> jlipps@... 09/10/06 05:54PM >>>
> palaeooobiology
>
> I like this word.    You should nominate it for the Oxford English
> Dictionary.   But you spelled it with only 2 "o" earlier in the
> email.   Which is correct.   I hope it's the 3 "o" version, although
> a purist would insist on a hyphen, I'd guess, between no. 1 and no.
> 2.
>
>
>
>
>
>
>
>



#166 From: "tommytyrberg" <tommytyrberg@...>
Date: Mon Sep 11, 2006 4:47 pm
Subject: Re: I have a copy of Sahni, A., Kumar, G., Bajpai, S., and Srinivasan, S. 1990
tommytyrberg
Offline Offline
Send Email Send Email
 
--- In Palaeo-oology@..., "cogombra" <cogombra@y...>
wrote:
>
> Thank to Prof. Sahni and R. Patnaik for the PDF copy of the below
> paper...
>
> Does anybody fancy a copy?
>
>
> Sahni, A., Kumar, G., Bajpai, S., and Srinivasan, S. 1990. A review
of
> Late Pleistocene ostriches (Struthio sp. in India. Man and
> Environment, 15(1):41-47.
>
I would also appreciate a copy to:
tommy.tyrberg@...

Tommy Tyrberg

#165 From: Judith Harris <harrisj@...>
Date: Mon Sep 11, 2006 2:40 pm
Subject: Re: [Palaeo-oology] Our field of work, Paleooology, to be legalised by the Oxford English Dictionary
palaeochromis
Offline Offline
Send Email Send Email
 
I am definitely in favor of this. One of my dearest students,
friends, and colleagues, Karl Hirsch, was a great paleoologist.

Judith


judith harris
emerita professor
university of colorado museum
p.o. box 278
chama, nm  87520
harrisj@...


On Sep 11, 2006, at 7:34 AM, cogombra wrote:

> Dear Everybody,
>
>
> Palaeoology, Paleooology, and Paleoöology will likely be a term in
> the Oxford English Dictionary.
>
> Thanks to Gary...
>
>
> From: "Gary Rosenberg" <rosenberg@...>
> Reply-To: paleonet@...
> To: <paleonet@...>
> Subject: Re: paleonet Welcome to The Palaeo-oological Discussion
> Group
> Date: Mon, 11 Sep 2006 08:57:14 -0400
>
> I'm an adviser to the Oxford English Dictionary, and have forwarded
> the message to the appropriate editor. I'd guess they'd standardize
> it to palaeoology if the word and its cognates continue to be used.
> The first occurrence may be
>
> Estudios Geologicos 60, no.3-6 (2004) p. 179: "Most sites contain
> bony remains, but there are also paleoichnological and paleoological
> sites, with dinosaur and other reptilian tracks and eggshells."
>
> Gary Rosenberg
>
> >>> jlipps@... 09/10/06 05:54PM >>>
> palaeooobiology
>
> I like this word.    You should nominate it for the Oxford English
> Dictionary.   But you spelled it with only 2 "o" earlier in the
> email.   Which is correct.   I hope it's the 3 "o" version, although
> a purist would insist on a hyphen, I'd guess, between no. 1 and no.
> 2.
>
>
>
>
>
>
>
>

#164 From: "cogombra" <cogombra@...>
Date: Mon Sep 11, 2006 1:34 pm
Subject: Our field of work, Paleooology, to be legalised by the Oxford English Dictionary
cogombra
Offline Offline
Send Email Send Email
 
Dear Everybody,


Palaeoology, Paleooology, and Paleoöology will likely be a term in
the Oxford English Dictionary.

Thanks to Gary...


From: "Gary Rosenberg" <rosenberg@...>
Reply-To: paleonet@...
To: <paleonet@...>
Subject: Re: paleonet Welcome to The Palaeo-oological Discussion
Group
Date: Mon, 11 Sep 2006 08:57:14 -0400

I'm an adviser to the Oxford English Dictionary, and have forwarded
the message to the appropriate editor. I'd guess they'd standardize
it to palaeoology if the word and its cognates continue to be used.
The first occurrence may be

Estudios Geologicos 60, no.3-6 (2004) p. 179: "Most sites contain
bony remains, but there are also paleoichnological and paleoological
sites, with dinosaur and other reptilian tracks and eggshells."

Gary Rosenberg

  >>> jlipps@... 09/10/06 05:54PM >>>
palaeooobiology

I like this word.    You should nominate it for the Oxford English
Dictionary.   But you spelled it with only 2 "o" earlier in the
email.   Which is correct.   I hope it's the 3 "o" version, although
a purist would insist on a hyphen, I'd guess, between no. 1 and no.
2.

#163 From: Palaeo-oology@...
Date: Sun Sep 10, 2006 9:27 pm
Subject: File - Palaeo-oological publications
Palaeo-oology@...
Send Email Send Email
 
ANDREWS C.W , 1911. - Notes on some fragments of the fossil egg-shell of a large
struthiuos brid from Southern Algeria with remarks on some pieces of the
egg-shell of an ostrich from Northern India , Verh.V Intern. Orn. Kongress ,
Berlin , 1910 , p. 169-171 .
ANDREWS R.C , 1923 .- Les œufs de Dinosaures , L'Illustration n° 4217 , p. 669.
ANTUNES  M. T , TAQUET P. &   RIBEIRO V. , 1998. - Upper Jurassic  Dinosaur and
Crocodile eggs from Paimogo nesting site ( Lourinha , Portugal ) , Memorias de
Academias de Ciencias de Lisboa , vol.37 , p. 83-100.
BAJPAI S. , SAHNI A. &  SRINIVASAN S. , 1993. - Ornithoid eggshells from Deccan
Intertrappean  beds near Anjar ( Kachchh ) ,Western India , Current Science ,
vol. 64 , p. 42- 45.
BIDWELL E. , 1910 .- Remarks on some fragments of egg-shell of a fossil ostrich
from India , Ibis , sér.9 , vol.4 , p. 759-761 .
BONAPARTE J.F , 1978.- El Mesozoico de America del Sur y sus tetrapodos, Opera
lilloana , 26 , 596 p.
BONAPARTE J.F  &  VINCE M. , 1979. - El hallazgo el primer nido de dinosaurios
triasicos  ( Saurischia ; Prosauropoda  ) , Triasico Superior  de Patagonia  ,
Ameghiniana , vol.16 , p.173- 182.
BRANDT A. Von , 1873. - Ueber ein grosses fossiles Vogelei  aus der Umgegend von
Cherson , Bulletin  Academy of Science , St. Petersburg , vol.18 , p. 158-161.
BRANDT A. Von , 1874. - On a large fossil egg from the neighbourhood of Cherson
, Ibis , vol.3 , p.4 .
BRANDT A. Von , 1885 .- Ueber das Schicksal des Eies von Struthiolithus
chersonensis , Zool. Anz. vol.8 , p. 191 .
BRAZATTI T. & CALLIGARIS R. , 1995. - Studio preliminare di reperti ossei di
dinosauri del Carso Triestino , Ani. Mus. Civ . Stor. Nat. Trieste vol.46 , p.
221-226.
BRAY E. S. , 1998. - Dinosaur eggshell Boletuoolithus carlylensis , oogen.nov.,
from the Lower Cretaceous Cedar Mountain Formation of Utah , p. 221-223 In :
LUCAS S.G ? KIRKLAND J.I. & ESTEP J.W  ( Eds.) , Lower and Middle cretaceous
Terrestrial Ecosysems , New-Mexico Museum of natural History and Science
Bulletin n°14.
BRAY E. S &  LUCAS S. G. , 1997. - Theropod dinosaur eggshell from the Upper
Jurassic of New Mexico p. 41-43 , In : LUCAS S.G , WILLIAMSON T.E.& MORGAN G.S.
( Eds.) , New's Mexico Fosil record  1. New Mexico Museum of Natural History
Bulletin n°11 .
BROWN B. &  SCHLAIKJER E.M, 1940. -The structure and relationships of
Protoceratops, Acad.Sci.Ann., vol.40, p. 133- 266.
BUFFETAUT E. & LE LOEUFF J. , 1994 . - The discovery of dinosaur eggshells in
nineteenth-century France In Dinosaur eggs and babies , K.Carpenter , K.F Hirsch
and J.R Horner ( Eds.) , p.31-34 , Cambridge University Press , U.K.
CALVO J. O , ENGELLAND S., HEREDIA S. E & SALGADO L. , 1997. - First record of
dinosaur eggshells ( ? Sauropoda -Megaoolithidae ) from the Neuquen , Patagonia
, Argentina , Gaia , vol.14 , p. 381-389.
CARPENTER K.  & ALF K., 1994 .- Global distribution of dinosaur eggs , nests and
babies In Dinosaur eggs and babies , K.Carpenter , K.F Hirsch and J.R Horner (
Eds.) , p.15-30 , Cambridge University Press , U.K .
CASE T.J., 1978. - Speculations on the growth rate and reproduction in some
Dinosaurs .Paleobiology vol.4 , p. 320-328.
CHATTERJEE S. &  KUROCHKIN N. E. , 1994. - A new embryonic  bird from the
Cretaceous of Mongolia , Journal of Vertebrate Paleontology , vol. 14 (
supplement ) , 20A.
CHIAPPE L. M., CORIA R. A., DINGUS L., JACKSON F., CHINSAMY A. & FOX M. , 1998.
- Sauropod dinosaur embryos from the late Cretaceous of Patagonia , Nature ,
vol.396 ,p. 258-259.
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SOCHAVA A .V. , 1970. - Microtexture do Dinosaur egg shells from the Lower
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1137-1140.
SOCHAVA A.V , 1972. - The skeleton of an embryo in Dinosaur egg ,
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the Cretaceous beds of Mongolia, American Mus.Novitates ,vol.173 , p.1- 4.
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1 , p. 295-312.
SUNIL BAJPAI , SRINIVASAN S. & SAHNI A. , 1997. - Fossil turtle   eggshells from
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49 ( Feb.1997 ) , p. 209-213 .
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THULBORN A., 1991. - The discovery of Dinosaur eggs , Modern Geology vol.16 , p.
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Palasiatica vol.37 , n°4 , p. 278-284

#162 From: ecoroma@...
Date: Fri Sep 8, 2006 2:57 pm
Subject: Re: [Palaeo-oology] I have a copy of Sahni, A., Kumar, G., Bajpai, S., and Srinivasan, S. 1990
ecoroma@...
Send Email Send Email
 
Dear Xavier,
yeah, I would like!
Thanks

Eduardo


Mensaje citado por: cogombra <cogombra@...>:

> Thank to Prof. Sahni and R. Patnaik for the PDF copy of the below
> paper...
>
> Does anybody fancy a copy?
>
>
> Sahni, A., Kumar, G., Bajpai, S., and Srinivasan, S. 1990. A review of
> Late Pleistocene ostriches (Struthio sp. in India. Man and
> Environment, 15(1):41-47.
>
>
>
>
>
>
> Yahoo! Groups Links
>
>
>
>
>
>



Eduardo Corona-M.
Laboratorio de Arqueozoología &
Seminario Relaciones Hombre -Fauna
(http://www.geocities.com/shofaun),
Instituto Nacional de Antropología e Historia
México

-------------------------------------------------
www.correo.unam.mx
UNAMonos Comunicándonos

#161 From: Judith Harris <harrisj@...>
Date: Fri Sep 8, 2006 2:48 pm
Subject: Re: [Palaeo-oology] Copies of different papers
palaeochromis
Offline Offline
Send Email Send Email
 
An amazing compilation. Thanks for the link.

Judith

judith harris
emerita professor
university of colorado museum
p.o. box 278
chama, nm  87520
harrisj@...


On Sep 8, 2006, at 8:04 AM, cogombra wrote:

> Do you fancy a PDF copy of the below papers? (just go to
> http://www2.nrm.se/ve/birds/sape/litt001.html.en and put in the
> field find eggs and you will find lots of publications...below some
> examples)
>
> Bibi, F., Shabel, A., Kraatz, B. & Stidham, T. 2006. New fossil
> ratite (Aves: Palaeognathae) eggshell discoveries from the Late
> Miocene Baynunah Formation of the United Arab Emirates, Arabian
> Peninsula. Palaeontologia Electronica Vol 9, Issue 1; 2A, 13 p. PDF
> http://www.paleo.erdw.ethz.ch/2006_1/eggshell/eggs.pdf
>
> Bajpai, S., Sahni, A. & Srinivasan, S. 1993. Ornithoid eggshells
> from Deccan intertrappean beds near Anjar (Kachchh) western India.
> Current Science (Bangalore) 64(1):42-45. HTML
> http://www.ias.ac.in/j_archive/currsci/64/1/42-45/viewpage.html
>
> Allen, J, A. 1899. Abstract from Farrington O. C. A fossil Egg from
> South Dakotas in Field Columb. Mus. 1899. 191. Auk 16:370. DejaVu
> PDF
> http://elibrary.unm.edu/sora/Auk/v016n04/p0370-p0370.pdf
>
> Bird, M. I., Turney, C. S. M., Fifield, L. K., Smith, M. A., Miller,
> G. H., Roberts, R. G. & Magee 2003. Radiocarbon dating of organic-
> and carbonate-carbon in Genyornis and Dromaius eggshell using
> stepped combustion and stepped acidification. Quaternary Science
> Reviews 22:1805-1811. PDF
> http://uow.edu.au/science/eesc/staff/cturney/docs/4Eggshells.pdf
>
> Bradbury, W. C. 1919. Some notes on the egg of Aepyornis maximus.
> Condor 21:97-101. DejaVu PDF
> http://elibrary.unm.edu/sora/Condor/files/issues/v021n03/p0097-
> p0101.pdf
>
> Chandler, R. M. & Wall, P. 2002. The first record of bird eggs from
> the early Oligocene (Orellan) of North America. Proceedings of the
> 6th Fossil Resource Conference. Geologic Resource Division Technical
> Report NPS/NRGRD/GRDTR-01. HTML
> http://www2.nature.nps.gov/geology/paleontology/pub/fossil_conference
> _6/chandler.htm
>
> Clarke, S. J. 2005. Isoleucine epimerisation and stable isotope
> ratio studies of cassowary, megapode and aepyornis eggshells:
> biogeochemical and palaeonenvironmental implications. PhD Thesis,
> University of Wollongong. PDF
> http://www.library.uow.edu.au/adt-NWU/public/adt-NWU20050405.124008/
>
>
> Gill, B. J. 2000. Morphometrics of moa eggshell fragments (Aves:
> Dinornithiformes) from Late Holocene dune-sands of the Karikari
> Peninsula, New Zealand. Journal of the Royal Society of New Zealand
> 30(2):131-145. PDF
> http://www.rsnz.org/publish/jrsnz/2000/7.pdf
>
>
> Grellet-Tinner, G. & Dyke, G. J. 2005. The eggshell of the Eocene
> bird Lithornis. Acta Palaeontologica Polonica 50(4):831-835. PDF
> http://app.pan.pl/acta50/app50-831.pdf
>
>
>
>
>
>
>
>

#160 From: "cogombra" <cogombra@...>
Date: Fri Sep 8, 2006 2:04 pm
Subject: Copies of different papers
cogombra
Offline Offline
Send Email Send Email
 
Do you fancy a PDF copy of the below papers? (just go to
http://www2.nrm.se/ve/birds/sape/litt001.html.en and put in the
field find eggs and you will find lots of publications...below some
examples)

Bibi, F., Shabel, A., Kraatz, B. & Stidham, T. 2006. New fossil
ratite (Aves: Palaeognathae) eggshell discoveries from the Late
Miocene Baynunah Formation of the United Arab Emirates, Arabian
Peninsula. Palaeontologia Electronica Vol 9, Issue 1; 2A, 13 p. PDF
http://www.paleo.erdw.ethz.ch/2006_1/eggshell/eggs.pdf

Bajpai, S., Sahni, A. & Srinivasan, S. 1993. Ornithoid eggshells
from Deccan intertrappean beds near Anjar (Kachchh) western India.
Current Science (Bangalore) 64(1):42-45. HTML
http://www.ias.ac.in/j_archive/currsci/64/1/42-45/viewpage.html

Allen, J, A. 1899. Abstract from Farrington O. C. A fossil Egg from
South Dakotas in Field Columb. Mus. 1899. 191. Auk 16:370. DejaVu
PDF
http://elibrary.unm.edu/sora/Auk/v016n04/p0370-p0370.pdf

Bird, M. I., Turney, C. S. M., Fifield, L. K., Smith, M. A., Miller,
G. H., Roberts, R. G. & Magee 2003. Radiocarbon dating of organic-
and carbonate-carbon in Genyornis and Dromaius eggshell using
stepped combustion and stepped acidification. Quaternary Science
Reviews 22:1805-1811. PDF
http://uow.edu.au/science/eesc/staff/cturney/docs/4Eggshells.pdf

Bradbury, W. C. 1919. Some notes on the egg of Aepyornis maximus.
Condor 21:97-101. DejaVu PDF
http://elibrary.unm.edu/sora/Condor/files/issues/v021n03/p0097-
p0101.pdf

Chandler, R. M. & Wall, P. 2002. The first record of bird eggs from
the early Oligocene (Orellan) of North America. Proceedings of the
6th Fossil Resource Conference. Geologic Resource Division Technical
Report NPS/NRGRD/GRDTR-01. HTML
http://www2.nature.nps.gov/geology/paleontology/pub/fossil_conference
_6/chandler.htm

Clarke, S. J. 2005. Isoleucine epimerisation and stable isotope
ratio studies of cassowary, megapode and aepyornis eggshells:
biogeochemical and palaeonenvironmental implications. PhD Thesis,
University of Wollongong. PDF
http://www.library.uow.edu.au/adt-NWU/public/adt-NWU20050405.124008/


Gill, B. J. 2000. Morphometrics of moa eggshell fragments (Aves:
Dinornithiformes) from Late Holocene dune-sands of the Karikari
Peninsula, New Zealand. Journal of the Royal Society of New Zealand
30(2):131-145. PDF
http://www.rsnz.org/publish/jrsnz/2000/7.pdf


Grellet-Tinner, G. & Dyke, G. J. 2005. The eggshell of the Eocene
bird Lithornis. Acta Palaeontologica Polonica 50(4):831-835. PDF
http://app.pan.pl/acta50/app50-831.pdf

#159 From: hvkarl@...
Date: Fri Sep 8, 2006 12:53 pm
Subject: Re: [Palaeo-oology] I have a copy of Sahni, A., Kumar, G., Bajpai, S., and Srinivasan, S. 1990
hvkarl
Offline Offline
Send Email Send Email
 
Yes, cordially Hans: hvkarl@...


Von: Palaeo-oology@...
Gesendet: 08.09.06 14:47:18
An: Palaeo-oology@...
Betreff: [Palaeo-oology] I have a copy of Sahni, A., Kumar, G., Bajpai, S., and Srinivasan, S. 1990

Thank to Prof. Sahni and R. Patnaik for the PDF copy of the below
paper...

Does anybody fancy a copy?


Sahni, A., Kumar, G., Bajpai, S., and Srinivasan, S. 1990. A review of
Late Pleistocene ostriches (Struthio sp. in India. Man and
Environment, 15(1):41-47.





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