IVPP-IR  > 中科院古脊椎所(2000年以后)
Middle Pleistocene climate and habitat change at Zhoukoudian, China, from the carbon and oxygen isotopic record from herbivore tooth enamel
Gaboardi, M; Deng, T; Wang, Y; Gaboardi, M (reprint author), Florida State Univ, Dept Geol Sci, 108 Carraway Bldg, Tallahassee, FL 32306 USA.
2005-05-01
发表期刊QUATERNARY RESEARCH
ISSN0033-5894
卷号63期号:3页码:329-338
文章类型Article
摘要The Pleistocene deposits at Zhoukoudian, often referred to as the "Peking Man" site, contain dental remains from a diverse group of herbivores, including Equus sanmeniensis, Cervus elaphus, Cervus nippon, Megaloceros pachyosteus, Sus lydekkeri, and Dicerorhinus choukoutienensis. The carbon and oxygen isotopic compositions of structural carbonate within the enamel of these teeth are used to reconstruct the paleodiet and paleoenvironment of the mammals. The δC-13 values of enamel from Zhoukoudian range from -2.3&PTSTHOUSND; to -13.0&PTSTHOUSND;, indicating that these mammals consumed between ∼ 25% and 100% C-3 plants. The presence of significant amounts of C-4 plants in the diets of some herbivore species indicates that at the onset of the Middle Pleistocene local habitats included mixed C-3/C-4 vegetation. By approximately 470,000 yr ago, C-3 plants dominated the diets of herbivores studied, suggesting that the abundance of C-4 flora had decreased in the area. For all deer analyzed in this study, the values of δC-13 and δO-18 decrease substantially from about 720,000 to 470,000 yr ago. This trend may be due to a strengthening of the winter monsoon during the Middle Pleistocene. © 2005 University of Washington. All rights reserved.; The Pleistocene deposits at Zhoukoudian, often referred to as the "Peking Man" site, contain dental remains from a diverse group of herbivores, including Equus sanmeniensis, Cervus elaphus, Cervus nippon, Megaloceros pachyosteus, Sus lydekkeri, and Dicerorhinus choukoutienensis. The carbon and oxygen isotopic compositions of structural carbonate within the enamel of these teeth are used to reconstruct the paleodiet and paleoenvironment of the mammals. The δC-13 values of enamel from Zhoukoudian range from -2.3&PTSTHOUSND; to -13.0&PTSTHOUSND;, indicating that these mammals consumed between ∼ 25% and 100% C-3 plants. The presence of significant amounts of C-4 plants in the diets of some herbivore species indicates that at the onset of the Middle Pleistocene local habitats included mixed C-3/C-4 vegetation. By approximately 470,000 yr ago, C-3 plants dominated the diets of herbivores studied, suggesting that the abundance of C-4 flora had decreased in the area. For all deer analyzed in this study, the values of δC-13 and δO-18 decrease substantially from about 720,000 to 470,000 yr ago. This trend may be due to a strengthening of the winter monsoon during the Middle Pleistocene. © 2005 University of Washington. All rights reserved.
关键词Zhoukoudian Pleistocene Carbon Isotopes Oxygen Isotopes Homo Erectus Paleomonsoon Paleoecology
WOS标题词Science & Technology ; Physical Sciences
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关键词[WOS]NORTHERN CHINA ; PEKING-MAN ; LOESS PLATEAU ; SITE ; TEETH ; PRECIPITATION ; VARIABILITY ; CHRONOLOGY ; PHOSPHATE ; APATITES
收录类别SCI
语种英语
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号WOS:000228947300010
引用统计
文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/3555
专题中科院古脊椎所(2000年以后)
古哺乳动物研究室
通讯作者Gaboardi, M (reprint author), Florida State Univ, Dept Geol Sci, 108 Carraway Bldg, Tallahassee, FL 32306 USA.
作者单位1.Florida State Univ, Dept Geol Sci, Tallahassee, FL 32306 USA
2.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
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Gaboardi, M,Deng, T,Wang, Y,et al. Middle Pleistocene climate and habitat change at Zhoukoudian, China, from the carbon and oxygen isotopic record from herbivore tooth enamel[J]. QUATERNARY RESEARCH,2005,63(3):329-338.
APA Gaboardi, M,Deng, T,Wang, Y,&Gaboardi, M .(2005).Middle Pleistocene climate and habitat change at Zhoukoudian, China, from the carbon and oxygen isotopic record from herbivore tooth enamel.QUATERNARY RESEARCH,63(3),329-338.
MLA Gaboardi, M,et al."Middle Pleistocene climate and habitat change at Zhoukoudian, China, from the carbon and oxygen isotopic record from herbivore tooth enamel".QUATERNARY RESEARCH 63.3(2005):329-338.
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