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ON NEW MATERIAL OF STEGODON WITH RECOLLECTIONS OF THE CLASSIFICATION OF STEGODON IN china

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古脊椎动物学报(中英文） 1995年第3期 229-230页

作者： Zong Guanfu(Institulc of vertebrate paleontology and paleoanthropology, the Chincse academy ofScicnces beijing. 100044)

The genus Slegodon is an Asiatic endemic and includes about 2o species, ofwhich about three are discovered in china. The chronologically earliest known re-cord of the genus (as Stegodon bombijrons) is;upper Miocene from the Dhok-Pathanof the Siwa1ik. It flourished in Pliocene and Pleistocene of south and south-weatof china as well as south-east Asia, and survived until early Holocene and thechronologica1ly latest record is 5oOo years B. P. from Jinhua, Zhejiang (Ma et al.,l 992).

关键词： china Late Cenozoic Stegodon

The Shanghuang Mammalian Fauna, Middle Eocene of Jiangsu:History of Discovery and Significance

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古脊椎动物学报(中英文） 1996年第3期 209-214页

作者： Qi Tao K. Christopher Beard Wang Banyue Mary R. Dawson Guo Jianwei Li Chuankui(institute of vertebrate paleontology and paleoanthropology, chinese academy of sciences beijing 100044)(Section of vertebrate paleontology, Carnegie Museam of Natural Histo

A Paleogene mammalian fauna, here named the Shanghuang fauna, was discov ered near the village of Shanghuang, close to Liyang City, Jiangsu Province, china (Fig.1). At present, rouglily sixty species of fossil mammals have been recognied in the Shanghuang fauna. Many of these mammal taxa are new to science, and others represent new occurrences for the Eocene of china. Particularly well represented in the Shanghuang fauna are micromammals (including marsupials, insectivores, rodents,lagomorphs, primates, and bats) that have seldom if ever been found in other Eocene Asian localities. Biostratigraphic correlations suggest that the Shanghuang fauna repre sents the Irdinmanhan and early Sharamurunian Land Mammal Ages and is likely to be about 45 million years old. Ongoing study of the Shanghuang manunal fauna promlses to shed new insight into the phylogeny and historical biogeography of numer ous higherlevel mammalian taxa. Here, we provide a history of field activities at Shanghuang and an overview of mammalian diversity at Shanghuang.

关键词： Jiangsu Middle Eocene Shanghuang Mammalian Fauna

A zooarchaeological study of bone assemblages from the Ma'anshan Paleolithic site

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Science china Earth sciences 2010年第3期53卷 395-402页

作者： ZHANG Yue1,2,3, WANG ChunXue1,2, ZHANG ShuangQuan1,2 & GAO Xing1,2 1 institute of vertebrate paleontology and paleoanthropology, chinese academy of sciences, beijing 100044 2 Joint Laboratory of Human Evolution and Archaeometry, chinese academy of sciences, beijing 100044 3 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing 210008 institute of vertebrate paleontology and paleoanthropology Chinese Academy of Sciences Beijing China Joint Laboratory of Human Evolution and Archaeometry Chinese Academy of Sciences Beijing China State Key Laboratory of Palaeobiology and Stratigraphy Nanjing China

Ten thousands of bone fragments were recovered from the Ma’anshan Paleolithic site, of which 4358 pieces can be identified to skeletal elements or species. In this research, the bone assemblages are quantified based on elements of MNI, MNE, and MAU. Then bone surface modifications and skeletal element profiles of the bone assemblages are studied to understand shlepping behaviors and reveal the technique of disarticulating and defleshing the animals’ bodies, etc. Based on the analyses of bone assemblages and the comparative study with the ethnoarchaeological as well as experimental data, it is assumed that later hominids at the site made fuller use of the game animals than the earlier hominids. Incorporating the lines of evidence from chronological dating, paleoenvironment, and polished bone tools between the two cultural layers, here we propose three hypotheses suggesting that the changes of environment, the migrations of the hominids from the North, or the demographic pulses may cause such a behavioral difference. However, it is yet to be determined which hypothesis can better explain the changes.

关键词： Ma’anshan site zooarchaeology Paleolithic hominid behavior

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EARLY DEVONIAN FISHES FROM GUIJIATUN AND XUJIACHONG FORMATIONS OF QUJING,YUNNAN,AND RELATED BIOSTRATIGRAPHIC PROBLEMS

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古脊椎动物学报(中英文） 1994年第1期 15-20页

作者： Zhu Min Wang Junqing Fan Junhang (institute of vertebrate paleontology and paleoanthropology, Academia Sinica beijing 100044)

Lower Devonian stratigraphy of Qujing in eastern Yunnan is a non-marine strato-type in South china and can be subdivided into Xishancun, Xitun, Guijiatun and Xujiachong Formations in ascending order. This sequence is rich in fossils of early vertebrates, bivalves, ostracods and plants. With the early vertebrates, the aspects of Xishancun and Xitun Formations are fairly definite while those of Guijiatun and Xujiachong Formations are equivocal, restraining the establishment of complete early Devonian biostratigraphic succession. In the paper, the new discoveries of early vertebrates from Guijiatun and Xujiachong Formations have been described, i. e.,galeaspid Gantarostraspis geni in Xujiachong Formation, and antiarchs Yunnanolepis chii, Procondylolepis qujingensis and crossopterygian Youngolepis sp. in Guijiatun Formation.

关键词： Qujing, Yunnan early Devonian fishes biostratigraphy

QUATERNARY STRATIGRAPHY AND MAMMAL FOSSILS OF YIHE AND SHUHE RIVER DRAINAGES

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古脊椎动物学报(中英文） 1996年第4期 330-331页

作者： YOU Yuzhu(institute of vertebrate paleontology and paleoanthropology, chinese academy of sciences beijing 100044)XU Shubin(Commission of Preservation of Ancient Monument of Linyi, Shangdong Province Linyi 276000)

The present paper represents the recent advance of research on Quatermary stratigraphyand mammal fossils in Yihe and Shuhe River drainages, Shandong Province. Based on theLithologic observations and various assemblages of mammal fossils, the Plesistocene stratacan be divided into three parts in sequence , which are listed from oldat to youngest asfollows:

关键词： Yi and Shu River drainage quaternary stratigraphy mammalian fossil

LATE MESOZOIC FISH FAUNA FROM WESTERN LIAONING, china

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古脊椎动物学报(中英文） 1995年第3期 191-193页

作者： Jin Fan Zhang Jiangyong Zhou Zhonghe(institute of vertebrate Poleonxology and paleoanthropology, the Chinesc academy of sciences beijing 100044)

Large samples of fossil fishes were collected from the Late Mesozoic non-ma-rine Jehol Group (including the Yixian, Jiufotang, Shahai and Fuxin formations inascending order) at 25 localities in western Liaoning, china (Fig.1, Table 1). Thenew material enriches the composition of the Jehol fish fauna greatly. Our preli-minary study indicates that this fish fauna is dominated by sturgeons (Peipiaosteidae:Yanosteus longidorsalis and Peipiaosteus pani), paddlefishes (Polyodontidae: Protopse-phurus liui), diversified lycopterids (Lycoptera dagidi, L. muroii, L. sinensis, ***, and Jinanichthys longiccphalus), osteoglossids (Paralycoptera sp.),and possibly osteoglossomorphs (Huashia sp., ?Nieerkunia and an indeterminatefish); it also includes palaeonisciforms, amiiforms (Sinamia sp.), and a teleost incer-tae sedis (Longdeichthys luoiiaxiaensis)

关键词： Western Liaoning Latest Jurassic-Early Cretaceous Fish Fauna

A REVIEW OF MESOZOIC OSTEOGLOSSOMORPH FISH LYCOPTERA LONGICEPHALUS

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古脊椎动物学报(中英文） 1994年第1期 55-59页

作者： Zhang Jingangyong Jin Fan Zhou Zhonghe(institute of vertebrate paleontology and paleoanthropology, Academia sinica beijing 100044)

In the present paper the anatomical charctrters and morphologival variatin of lyciotera longicarpjalus found from western lianing are reviewed, lycoptera long-icephalus Liu et al. 1963 is emended to Jinanichthys longicephalus (Liu et al. )Li-aosiichthys Su 1992 is considered as a synonym of Jinanichthys. The evolutionary trend and systematic of jinanichthys are discussed.

关键词： Liaoning Late Jurassic to Early Cretaceous Osteoglossomorpha Morphology Systematic position

Track Fading and Its Applications in Archaeology, Tectonics and Geothermal Chronology in china

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Journal of Earth Science 2013年第4期24卷 645-651页

作者：郭士伦袁万明陈宝流黄慰文刘顺生 Department of Nuclear Physics China Institute of Atomic Energy School of Earth sciences and Resourses China University of Geosciences Department of Radioisotopes China Institute of Atomic Energy institute of vertebrate paleontology and paleoanthropology Chinese Academy of Sciences Guangzhou institute of Geochemistry Chinese Academy of Sciences

Track fading is a basic phenomenon in track science and has been the source of informa- tion in geosciences. This article summarizes the knowledge of track fading and gives some examples of successful applications of track fading in archaeology, tectonics and geothermal chronology in china. The applications of track fading are classified into 5 modes：（1） mode of complete fading （annealing）; （2） mode of partial fading; （3） use of the dependence of track fading on time and temperature; （4） use of the differences of track fading between coexisting minerals; and （5） use of fading-reduced track length. Track fading mechanisms hints that scientists in geothermal chronology should adopt microprobes for quantitative elemental analysis to determine the detailed chemical compositions of each mineral grain or at least of the grains from each position of geological structures in order that one becomes well aware of the relation between the track fading behavior and chemical compositions of the mineral used.

关键词： track fading archaeology tectonics geothermal chronology.

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Use-wear evidence confirms the earliest hafted chipped-stone adzes of Upper Palaeolithic in northern china

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chinese Science Bulletin 2010年第3期55卷 268-275页

作者： ZHANG XiaoLing1,2,3, SHEN Chen1,2,4 GAO Xing1,2 CHEN FuYou1,2 & WANG ChunXue1,2,3 1institute of vertebrate paleontology and paleoanthropology, chinese academy of sciences, beijing 100044, china 2Laboratory of Human Evolution and Archaeometry, chinese academy of sciences, beijing 100044, china 3Graduate University of chinese academy of sciences, beijing 100049, china 4The Royal Ontario Museum, Toronto M5S 2C6, Canada institute of vertebrate paleontology and paleoanthropology Chinese Academy of Sciences Beijing China Laboratory of Human Evolution and Archaeometry Chinese Academy of Sciences Beijing China Graduate University of chinese academy of sciences Beijing China The Royal Ontario Museum Toronto Canada

Chipped-stone "adze-shaped objects" (ASOs) were identified from a few Upper Palaeolithic sites in northern china. Its morpho- logical form resembles to ground-stone type-specific adze, but the function of the ASO has never been assessed. The objective of this study is to investigate the use function of this particular tool type recovered from the Hutouliang site in the Nihewan Basin of northern china. In this study, the lithic use-wear analysis is applied to examining microscopically edge-damages and sur- face-rounding of the tools in order to assess how they were employed. The result suggests that the ASO might have been used as woodworking tools with a hafted shaft, providing evidence for the appearance of the earliest hafted chipped-stone adzes prior to 10000 years ago in northern china. This study also demonstrates that the use-wear technique is an innovated and effective analytic appraoch to the study of stone tool functions that has been conventionally treated by typo-technological analyses. Stone tool use-patterns revealed by use-wear evidence would shed new insights on prehistoric adaptive strategies of modern human in northern china.

关键词：旧石器时代晚期中国北方磨损证据石材加工工具木工工具中国网站技术分析

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