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Chronological sequence of the early Pleistocene Gigantopithecus faunas from cave sites in the Chongzuo, Zuojiang River area, South China

文献类型：期刊论文

作者Jin, Changzhu1; Wang, Yuan1; Deng, Chenglong2; Harrison, Terry3; Qin, Dagong4; Pan, Wenshi4; Zhang, Yingqi1; Zhu, Min1; Yan, Yaling1
刊名QUATERNARY INTERNATIONAL
出版日期2014-12-15
卷号354页码:4-14
ISSN号1040-6182
DOI10.1016/j.quaint.2013.12.051
文献子类Article
英文摘要Since 2004, five new early Pleistocene cave sites with Gigantopithecus blacki and other fossil mammals have been discovered in the Chongzuo, Zuojiang River area, Guangxi Zhuang Autonomous Region (Guangxi ZAR), South China. These sites include Baikong Cave of Liyu Mountain, Juyuan Cave of Boyue Mountain, Sanhe and Queque Caves of Wuming Mountain, and Wuming Cave of Mulan Mountain. The present study provides a preliminary account of these newly discovered Gigantopithecus faunas, and discusses their taxonomic composition, evolutionary trends and chronology based on recent biostratigraphic and geochronological studies. Combining faunal and paleomagnetic data, the Gigantopithecus faunas from the Zuojiang River area can be divided into three temporal stages during the early Pleistocene. The early stage (2.6-1.8 Ma) is represented by the Baikong and Boyue faunas, which include some Neogene relics (e.g., Sinomastodon, Hesperotherium, Dicoryphochoerus, Dorcabune and Cervavitus) and several species that make their first appearance during the Pleistocene (e.g., Sinicuon dubius, Pachycrocuta licenli, Ailuropoda microta, Sinomastodon jiangnanensis, Stegodon huananensis and Tapirus sanyuanensis). The middle stage (1.8-1.2 Ma) is represented by the Sanhe fauna, which is characterized by the appearance of Ailuropoda wulingshanensis, Cuon antiquus, and Tapirus sinensis. The late stage (1.2-0.8 Ma) is represented by the Queque fauna, which is characterized by a marked decrease in Neogene relics and the appearance of a few species that are more typical of the middle Pleistocene (e.g., Ailuropoda baconi and Stegodon orientalis). Evolutionary trends in the early Pleistocene Gigantopithecus faunas include a gradual increase in dental size in some of the typical taxa, such as G. blacki, Ailuropoda and Tapirus, and the successive turnover of representative species, such as A. microta e A. wulingshanensis e A. baconi. Thus far, Eleven G. blacki sites of early Pleistocene age have been recorded in southern China, and these are primarily concentrated in Guangxi ZAR, where more than 70% of early Pleistocene G. blacki cave sites are known. Given this temporal and geographic distribution it is possible to infer that Guangxi ZAR represents an important early evolutionary and zoogeographic center for G. blacki. (C) 2014 Elsevier Ltd and INQUA. All rights reserved.
WOS关键词BUBING BASIN ; MAMMALIAN FOSSILS ; HUMAN ORIGINS ; GUANGXI ; BLACKI ; TEETH ; HOMO ; ASIA ; GOMPHOTHERIIDAE ; SINOMASTODON
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000345523300002
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构Program of Chinese Academy of Sciences(KZZD-EW-03) ; Program of Chinese Academy of Sciences(KZZD-EW-03) ; National Natural Science Foundation of China(41072013 ; National Natural Science Foundation of China(41072013 ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; Program of China Geological Survey(1212011220519) ; Program of China Geological Survey(1212011220519) ; 41174054 ; 41174054 ; 41202017) ; 41202017) ; Program of Chinese Academy of Sciences(KZZD-EW-03) ; Program of Chinese Academy of Sciences(KZZD-EW-03) ; National Natural Science Foundation of China(41072013 ; National Natural Science Foundation of China(41072013 ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; Program of China Geological Survey(1212011220519) ; Program of China Geological Survey(1212011220519) ; 41174054 ; 41174054 ; 41202017) ; 41202017) ; Program of Chinese Academy of Sciences(KZZD-EW-03) ; Program of Chinese Academy of Sciences(KZZD-EW-03) ; National Natural Science Foundation of China(41072013 ; National Natural Science Foundation of China(41072013 ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; Program of China Geological Survey(1212011220519) ; Program of China Geological Survey(1212011220519) ; 41174054 ; 41174054 ; 41202017) ; 41202017) ; Program of Chinese Academy of Sciences(KZZD-EW-03) ; Program of Chinese Academy of Sciences(KZZD-EW-03) ; National Natural Science Foundation of China(41072013 ; National Natural Science Foundation of China(41072013 ; National Key Basic Research Program of China(2012CB821900) ; National Key Basic Research Program of China(2012CB821900) ; Program of China Geological Survey(1212011220519) ; Program of China Geological Survey(1212011220519) ; 41174054 ; 41174054 ; 41202017) ; 41202017)
源URL[http://ir.iggcas.ac.cn/handle/132A11/84912]  
专题中国科学院地质与地球物理研究所
通讯作者Jin, Changzhu
作者单位1.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Key Lab Vertebrate Evolut & Human Origins, Beijing 100044, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.NYU, Ctr Study Human Origins, Dept Anthropol, New York, NY 10003 USA
4.Peking Univ, Sch Life Sci, Beijing 100871, Peoples R China
推荐引用方式
GB/T 7714		 Jin, Changzhu,Wang, Yuan,Deng, Chenglong,et al. Chronological sequence of the early Pleistocene Gigantopithecus faunas from cave sites in the Chongzuo, Zuojiang River area, South China[J]. QUATERNARY INTERNATIONAL,2014,354:4-14.
APA Jin, Changzhu.,Wang, Yuan.,Deng, Chenglong.,Harrison, Terry.,Qin, Dagong.,...&Yan, Yaling.(2014).Chronological sequence of the early Pleistocene Gigantopithecus faunas from cave sites in the Chongzuo, Zuojiang River area, South China.QUATERNARY INTERNATIONAL,354,4-14.
MLA Jin, Changzhu,et al."Chronological sequence of the early Pleistocene Gigantopithecus faunas from cave sites in the Chongzuo, Zuojiang River area, South China".QUATERNARY INTERNATIONAL 354(2014):4-14.

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