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    15 March 2002, Volume 40 Issue 01
    A NEW NAMURIAN PALAEOMSCON) FISH FROM ZHONGWEI, NINGXIA
    LU Li-Wu
    2002, 40(01):  1-8. 
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    CYMBOSPONDYLUS FROM THE UPPER TRIASSIC OF GUIZHOU, CHINA
    Ll Chun, YOU Hai-Lu
    2002, 40(01):  9-16. 
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    A new species of Cymbospondylus is named and described on the basis of tm) well-preserved skulls from the Late Triassic Wayao Member of the Falang Formation at Guanling, Guizhou Province. The prominent character of the new species is the teeth on the lower jaw, which only exist on anterior half of the dentary. Furthermore, it has large maxilla and relativelv, has the smallest orbit in the known ichthyosaurs. This is the latest occurrence of the genus Cymbospondylus, which is previously known only from the Middle Triassic of North America and Europe.
    CREODONT (MAMMALIA) REMAINS FROM THE EARLY OLIGOCENE OF ULANTATAL, NEI MONGOL
    HUANG Xue-Shi, ZHU Bao-Cheng
    2002, 40(01):  17-22. 
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    A new creodont, Hyaenodon neimongoliensis sp. nov. found in 1980' s by the authors is briefly described in the present paper. This is the only named species of the order in the Early Oligocene Ulantatal Fauna (Huang, 1998) .
    A PORCUPNE FROM LATE MIOCENE OF LINXIA BASIN, GANSU, CHNA
    WANG Ban-Yue, QIU Zhan-Xiang
    2002, 40(01):  23-33. 
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    In China the living porcupines are known to be distributed in Tibet and the area south to the Yangtze River, not beyond N 35°. The distribution of Quaternary fossil porcupines is known to be much wider than that of today, reaching Benxi in Northeastern China (north to N 41°) . However, our knowledge of the Chinese Neogene porcupines is limited to two species from south China: H. Zhengi from Pliocene of Sichuan and Guangxi, and Hystrix sp. from late Miocene of Lufeng of Yunnan. So far no fossil porcupines have ever been reported from Gansu Province. The discovery of the new porcupine from Linxia, Gansu, not only widened the distribution of the Neogene porcupines in China , but also shed new light on the evolutionary history of the fossil porcupines .
    TYE FIRST APPEARANCE OF TINOSAURUS FOSSIL IN THE QUATERNARY
    LI Yong-Xiang, XUE Xiang-Xu
    2002, 40(01):  34-41. 
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    Some Tinosaurus fossils were collected from the Quaternary caves of Luonan County,Shaanxi Province, which are well-preserved row of teeth and dentary. The dentary is stronger and has the vertical grooves between teeth on external side of ramus caused by wear of opposing upper teeth. The teeth are reducing in size from back to front. It is the first report of Tinosaurus in the Quintenary and made the record of this genus extended from early Tertiary to the Quaternary The specimens from the area show the characters of Tinosaurus well, and compared with other species of the genera they show some differences. So we record it as a new species: T. luonanensis sp. nov.
    PLEISTOCENE VERTEBRATE FAUNA FROM WUYUN CAVE OF TIANDONG COUNTY,GUANGXI
    CHEN Geng-Jiao, WANG Wei, MO Jin-You, HUANG Zhi-Tao, TIAN Feng,- HUANG Wei-Wen
    2002, 40(01):  42-51. 
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    An assemblage Of vertebrate remains is collected from Wuyun Cave,Tiandong County,Guangxi Province.It contains the following species:Neotetracus cf.N.sinensis, Soriculus sp., Crocidura sp ., Anourosorex sp., Scotomanes sp.,Hipposideros sp.Macaca sp.Prebytis sp. 1~2,Pongo pygmaeus weidenreichi, Sciurotamias sp., Callosciurus sp. Belomvs sp., Typhlomys cinereus, Atherurus cf. A. macrourus,Hystnx subcnstata,Mus cf.M. Pahari, Hapalomys delacouri, Chiropodomys cf. C. gliroides,Leopoldamys sp., Niviventer sp. 1~3, Rattus sp., Cuon cf. C. jacanicus antiquus , Arctonyx collaris , Ursus thibetanus, Ailuropoda melanoleuca baconi, Felis tigirs, Felis pardus, Felis teilhardi, Paradoxurus sp., Stegodon orientalis, Elephas maximus, Tapirus sinensis, Megatapirus augustus, Rhinoceros sinensis, Sus scrofa, ? Muntiacus sp., Cervus sp. I -e 2, Capricornis sumatraensis, Bovinae gen. et sp. indet. and Alligator cf. A. sinensis. The Wuyun Cave assemblage should belong to a typical Ailuropoda- Stegodon Fauna from South China based on its composition. The age seems to be not so early as Early Pleistocene because of lacking of ancient elements, such as Ailuropoda microta, Tapirus peii, Stegodon preorientalis etc . Generally, this fauna is comparable in age with those of Late Pleistocene from South China. H0Mever, some slightly primitive features of Paradoxurus sp., Typhlomys cinereus and Tapirus sinensis indicate an earlier age, which is of Middle Pleistocene or early late Pleistocene. Judging from the analysis of habitat type of different animals, the environment should be subtropical-tropical climate with forest, open ground and water bodies.
    THE AGE AND CORRELATION OF SOME DEVONIAN FISH-BEARING BEDS OF EAST YUNNAN, CHINA
    LIU Yu-Hai
    2002, 40(01):  52-69. 
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    LATE NEOGENE MACROMAMMALIAN ASSEMBLAGES FROM LINGTAI, GANSU PROVINCE, CHINA
    CHEN Guan-Fang
    2002, 40(01):  70-79. 
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