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《EARTH SCIENCE》 1995-05
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A NEW EARLY PLEISTOCENE MAMMALIA FAUNA FROM ZHOUKOUDIAN

Cheng Jie(Department of Geology and Mineral Resources,China University of Geosciences, Beijing 100083)Cao Boxun(Faculty of Earth Sciences,China University of Geosciences,Wuhan 430074)Tian Mingzhong;Li Longyin(Department of Geology and Mineral Resources,Ch  
A new cave-fissure site in the north slope of the Taipingshan Hill at Zhoukoudian was discovered by Cao Boxun et al.from China University of Geosciences(Wuhan)in 1985.It is about 2km from the Locality 1. Its thick deposits are rich in fossil mammals.During 1992-1993, more than 400mammalia fossils were gained by the first author by screen-washing and identified including 30 speciesbelonging to 23 genera. They mainly are Crocidura sp.,Lepus sp.,Hypolagus of .brachypus,Alilipus zhoukoudianensis sp.nov.,Sciurotamias praecox,Spermophilus? sp.,Allocricetus ehiki, Cricetinus uarians,Cricetulus obscurus, Hyperacrius yenshanensis, Alticola sp.,Allophaiomys of.pliocaenicus, Proedromys of bedfordi, Lasiopodomys probrandti, Apodemus dominans,A. latronum,Niviventer preconfucianus, Mus of musculus, Cardinomys nihewanicus. The east cave fauna mainly consists of the early and middle EarlyPleistocene species and contains a few members of late Early Pleistocene and Middle-Late Pleistocene.Sothe east cave fauna may correlate with the Nihewan fauna(middle Early Pleistocene )in age,and in later than the Locality 18 at Huiyu (early Early Pleistocene)as well as earlier than the Gongwangling fauna of Lantian (late Early pleistocene).Based on the study on the east cave in magnetostratigraphy, the age ofits deposits ranges 1.67~0.97MaB.P..
【Fund】: 地质矿产部(2-1-93-269),北京市地矿局项目资助
【CateGory Index】: Q915.663.1
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