Early Paleogene stratigraphic sequences, mammalian evolution and its response to environmental changes in Erlian Basin, Inner Mongolia, China
Wang YuanQing1; Meng Jin2; Beard, Christopher K.3; Li Qian1; Ni XiJun1; Gebo, Daniel L.4; Bai Bin1; Jin Xun1; Li Ping1; wangyuanqing@ivpp.ac.cn
刊名SCIENCE CHINA-EARTH SCIENCES
2010-12-01
卷号53期号:12页码:1918-1926
关键词Erlian Basin Paleogene Mammal Faunal Turnover Biochronology Environmental Response
ISSN号1674-7313
文献子类Article
英文摘要Paleogene strata in the Huheboerhe area, Erlian Basin, Inner Mongolia, China have been subdivided into three lithological units: the Nomogen Formation, the Arshanto Formation, and the Irdin Manha Formation. At least 12 mammal-bearing horizons have been recognized in these formations, of which 4 in the Nomogen Formation, 6 in the Arshanto Formation, and 2 in the Irdin Manha Formation. Recent investigation proved that the "Houldjin Formation" recognized in this area by the Central Asiatic Expeditions (CAE) of the American Museum Natural History in the 1920s is actually the Irdin Manha Formation, while the "Irdin Manha Formation" of CAE is the Arshanto Formation. A recent paleomagnetic study suggests that the upper part of the Nomogen Formation is early Eocene in age and the Arshanto Formation is mainly early Eocene rather than middle Eocene as previously thought. The Gashatan, Bumbanian, and Arshantan land mammal ages are correlated respectively to the Thanetian, the early Ypresian, and the middle Ypresian through earliest Lutetian of the Geological Time Scale. These land mammal ages are also correlated with the late Tiffanian through Clarkforkian, the early Wasatchian, and the middle-late Wasatchian and most of the Bridgerian of the North American Land Mammal Ages. During the early Paleogene, the mammalian history of the Erlian Basin was dominated by the appearance of new mammalian families and the replacement of a variety of genera and species, corresponding to the gradual climatic changes during this time period. The abrupt emergence of several modern mammalian orders at the beginning of the Eocene is probably related to extreme climatic warming in relation to the Paleocene-Eocene Thermal Maximum.
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WOS关键词NEI-MONGOL ; PALEOCENE ; EOCENE ; BOUNDARY ; TURNOVER ; TERTIARY ; STRATA ; GLIRES ; FAUNA ; ASIA
WOS研究方向Geology
语种英语
WOS记录号WOS:000284845600017
公开日期2013-11-27
内容类型期刊论文
源URL[http://119.78.100.205/handle/311034/4508]  
专题古脊椎动物与古人类研究所_图书馆1
古脊椎动物与古人类研究所_古低等脊椎动物研究室
古脊椎动物与古人类研究所_古哺乳动物研究室
通讯作者wangyuanqing@ivpp.ac.cn
作者单位1.Chinese Acad Sci, Lab Evolutionary Systemat Vertebrates, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
2.Amer Museum Nat Hist, Div Paleontol, New York, NY 10024 USA
3.Carnegie Museum Nat Hist, Sect Vertebrate Paleontol, Pittsburgh, PA 15213 USA
4.No Illinois Univ, Dept Anthropol, De Kalb, IL 60115 USA
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Wang YuanQing,Meng Jin,Beard, Christopher K.,et al. Early Paleogene stratigraphic sequences, mammalian evolution and its response to environmental changes in Erlian Basin, Inner Mongolia, China[J]. SCIENCE CHINA-EARTH SCIENCES,2010,53(12):1918-1926.
APA Wang YuanQing.,Meng Jin.,Beard, Christopher K..,Li Qian.,Ni XiJun.,...&wangyuanqing@ivpp.ac.cn.(2010).Early Paleogene stratigraphic sequences, mammalian evolution and its response to environmental changes in Erlian Basin, Inner Mongolia, China.SCIENCE CHINA-EARTH SCIENCES,53(12),1918-1926.
MLA Wang YuanQing,et al."Early Paleogene stratigraphic sequences, mammalian evolution and its response to environmental changes in Erlian Basin, Inner Mongolia, China".SCIENCE CHINA-EARTH SCIENCES 53.12(2010):1918-1926.
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