中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The evidence of fossil carbon isotopes of the climatic event at the beginning of Quaternary

文献类型:期刊论文

作者Deng, T; Xue, XX; Dong, JS; Deng, T (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China.
刊名CHINESE SCIENCE BULLETIN
出版日期1999-03-01
卷号44期号:5页码:477-480
关键词Climatic Event Quaternary Ungulate Carbon Isotope
ISSN号1001-6538
文献子类Article
英文摘要Tooth enamel of mammalian fossils can efficiently preserve the original carbon isotopic composition when they lived. The ungulate fossils, especially equids in the early Early Pleistocene Bajiazui fauna from Qingyang, Gansu are studied. According to the enriched relation of carbon isotopes between mammalian tooth enamel and grass diets, the fractions of C-3 and C-4 plants in this region at that time are reconstructed, which indicates that C-3 grass occupied a dominant position. Because C-3 grass adapts itself to cold and damp climates, our analytic results show that the time of the Bajiazui fauna was in a critical state between a glacial stage beginning and a summer monsoon retreat, and it was a refection to the turning cold event of the global climate at the beginning of the Quaternary.; Tooth enamel of mammalian fossils can efficiently preserve the original carbon isotopic composition when they lived. The ungulate fossils, especially equids in the early Early Pleistocene Bajiazui fauna from Qingyang, Gansu are studied. According to the enriched relation of carbon isotopes between mammalian tooth enamel and grass diets, the fractions of C-3 and C-4 plants in this region at that time are reconstructed, which indicates that C-3 grass occupied a dominant position. Because C-3 grass adapts itself to cold and damp climates, our analytic results show that the time of the Bajiazui fauna was in a critical state between a glacial stage beginning and a summer monsoon retreat, and it was a refection to the turning cold event of the global climate at the beginning of the Quaternary.
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WOS关键词HORSES
WOS研究方向Science & Technology - Other Topics
语种英语
WOS记录号WOS:000080126600021
公开日期2013-11-27
源URL[http://119.78.100.205/handle/311034/3964]  
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
通讯作者Deng, T (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China.
作者单位1.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
2.NW Univ Xian, Dept Geol, Xian 710069, Peoples R China
推荐引用方式
GB/T 7714
Deng, T,Xue, XX,Dong, JS,et al. The evidence of fossil carbon isotopes of the climatic event at the beginning of Quaternary[J]. CHINESE SCIENCE BULLETIN,1999,44(5):477-480.
APA Deng, T,Xue, XX,Dong, JS,&Deng, T .(1999).The evidence of fossil carbon isotopes of the climatic event at the beginning of Quaternary.CHINESE SCIENCE BULLETIN,44(5),477-480.
MLA Deng, T,et al."The evidence of fossil carbon isotopes of the climatic event at the beginning of Quaternary".CHINESE SCIENCE BULLETIN 44.5(1999):477-480.

入库方式: OAI收割

来源:古脊椎动物与古人类研究所

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