IVPP-IR  > 中科院古脊椎所(2000年以后)
The Early Pleistocene Gigantopithecus-Sinomastodon fauna from Juyuan karst cave in Boyue Mountain, Guangxi, South China
Wang, Yuan1,2; Jin, Changzhu1; Pan, Wenshi3; Qin, Dagong3; Yan, Yaling1; Zhang, Yingqi1; Liu, Jinyi1; Dong, Wei1; Deng, Chenglong4
2017-04-01
发表期刊QUATERNARY INTERNATIONAL
卷号434页码:4-16
文章类型Article
摘要As one of the most important Quaternary mammalian faunas in southern China, the Gigantopithecus-Sinomastodon fauna has received much attention. The large-primate fossil teeth newly collected from Juyuan karst cave in Boyue Mountain, Guangxi Zhuang Autonomous Region of southern China, can be identified as Gigantopithecus blacki. The morphology and size of these G. blacki teeth differ from those of the middle Pleistocene Gigantopithecus teeth which hold evidently larger dental dimensions and more complex crenulations from Hejiang Cave also in Guangxi and Tham Khuyen Cave in Vietnam. However, the G. blacki teeth from Juyuan Cave are relatively similar to those from Early Pleistocene Mohui Cave and Liucheng Gigantopithecus Cave both in Guangxi, which suggests that the three cave sites have similar age. The Juyuan fauna associated with Gigantopithecus blacki, consisting of 45 mammalian species (such as Sino mastodon yangziensis, Ailuropoda wulingshanensis, Stegodon huananensis, and Rhinoceros fusuiensis), is a typical Early Pleistocene Gigantopithecus-Sinomastodon fauna of southern China. The Juyuan fauna is mostly similar to Mohui fauna, also implying their contemporaneity. Paleomagnetic analyses demonstrate that the fossil-bearing sediments in Juyuan Cave are dominated by normal polarity. Combining the faunal analysis and magnetostratigraphic evidence, the Juyuan sediments can be best correlated with the Olduvai normal subchron, giving an estimated age of 1.8 Ma. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
关键词Gigantopithecus Blacki Gigantopithecus-sinomastodon Fauna Chongzuo Guangxi Juyuan Cave Of Boyue Mountain Early Pleistocene
WOS标题词Science & Technology ; Physical Sciences
DOI10.1016/j.quaint.2015.11.071
关键词[WOS]BUBING BASIN ; YANLIANG CAVE ; CHUIFENG CAVE ; MAMMAL FAUNA ; GIANT PANDA ; MOHUI CAVE ; CHONGZUO ; BLACKI ; SEQUENCE ; REMAINS
收录类别SCI ; SSCI
语种英语
项目资助者Program of Chinese Academy of Sciences(KZZD-EW-03) ; National Natural Science Foundation of China(41202017 ; State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS)(143109) ; 41372001)
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号WOS:000399509100002
引用统计
文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/7448
专题中科院古脊椎所(2000年以后)
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, Nanjing Inst Geol & Paleontol, State Key Lab Paleobiol & Stratig, Nanjing 210008, Jiangsu, Peoples R China
3.Peking Univ, Sch Life Sci, Beijing 100871, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Wang, Yuan,Jin, Changzhu,Pan, Wenshi,et al. The Early Pleistocene Gigantopithecus-Sinomastodon fauna from Juyuan karst cave in Boyue Mountain, Guangxi, South China[J]. QUATERNARY INTERNATIONAL,2017,434:4-16.
APA Wang, Yuan.,Jin, Changzhu.,Pan, Wenshi.,Qin, Dagong.,Yan, Yaling.,...&Deng, Chenglong.(2017).The Early Pleistocene Gigantopithecus-Sinomastodon fauna from Juyuan karst cave in Boyue Mountain, Guangxi, South China.QUATERNARY INTERNATIONAL,434,4-16.
MLA Wang, Yuan,et al."The Early Pleistocene Gigantopithecus-Sinomastodon fauna from Juyuan karst cave in Boyue Mountain, Guangxi, South China".QUATERNARY INTERNATIONAL 434(2017):4-16.
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
查看访问统计
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Wang, Yuan]的文章
[Jin, Changzhu]的文章
[Pan, Wenshi]的文章
百度学术
百度学术中相似的文章
[Wang, Yuan]的文章
[Jin, Changzhu]的文章
[Pan, Wenshi]的文章
必应学术
必应学术中相似的文章
[Wang, Yuan]的文章
[Jin, Changzhu]的文章
[Pan, Wenshi]的文章
相关权益政策
中科院和国家自然科学...
收藏/分享
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。