Environment and ecology of East Asian dinosaurs during the Early Cretaceous inferred from stable oxygen and carbon isotopes in apatite
Amiot, Romain1,2,3; Wang, Xu4; Zhou, Zhonghe1; Wang, Xiaolin1; Lecuyer, Christophe2,3; Buffetaut, Eric5; Fluteau, Frederic6; Ding, Zhongli4; Kusuhashi, Nao7; Mo, Jinyou8
刊名JOURNAL OF ASIAN EARTH SCIENCES
2015-02-01
卷号98页码:358-370
关键词Dinosaurs Reptiles Early Cretaceous East Asia Stable isotopes Climate Ecology
ISSN号1367-9120
DOI10.1016/j.jseaes.2014,11.032
文献子类Article
英文摘要During the cold Late Barremian-Early Albian interval, terrestrial environments in East Asia were populated by rich and diverse vertebrate faunas characterized by a strong provincialism. The latitudinal gradient of temperature and the existence of geographic barriers likely accounted for some aspects of this heterogeneous distribution of faunas. Other factors, however, such as local environmental conditions and interactions within vertebrate communities, which could have influenced their distribution, have not yet been fully identified and understood. Therefore, new and published oxygen and carbon isotope compositions of apatite from Chinese and Thai reptiles (dinosaurs, crocodilians and turtles) have been analyzed and interpreted in terms of ecology, local air temperature and precipitation amounts. Differences in carbon and oxygen isotope compositions between various groups of sympatric plant-eating dinosaurs (sauropods, ornithopods and ceratopsians) indicate food resources partitioning among them most likely to avoid competition. Mid-latitude environments, where the Jehol Biota flourished, were submitted to cool temperate climatic conditions with Mean Air Temperature (MAT) of 10 +/- 4 degrees C and Mean Annual Precipitations (MAP) of about 600 mm/yr compatible with the existence of forest environments. By contrast, sub-tropical regions, characterized by MAT of about 20-25 degrees C were either submitted to high amounts of seasonal precipitations (of about 1200 mm/yr in Thailand) or to significant aridity (MAP of about 400 mm/yr in South China). This difference in precipitation regime between Thailand and South China may be attributed to the occurrence of the Coastal Cordillera extending along the East margin of the South China block. These mountain ranges likely prevented humid air masses from the Pacific to penetrate some parts of South China, thus generating a "rain shadow effect". Mosaic environments characterizing East Asia during the Late Early Cretaceous may have acted as a cradle for the origination of advanced dinosaur taxa that subsequently radiated over Eurasia and North America during the Late Cretaceous. (C) 2014 Elsevier Ltd. All rights reserved.
WOS关键词MESOZOIC WOOD GENUS ; BONE PHOSPHATE ; TOOTH ENAMEL ; JEHOL-BIOTA ; TERRESTRIAL PALEOCLIMATES ; PALEOMAGNETIC CONSTRAINTS ; DELTA-O-18 RECORD ; BIOGENIC APATITES ; MARINE-SEDIMENTS ; OSTRICH EGGSHELL
WOS研究方向Geology
语种英语
出版者PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号WOS:000348955800028
资助机构National Basic Research Program of China Grant(2012CB821900) ; National Basic Research Program of China Grant(2012CB821900) ; CNRS PICS program "DINASIA" ; CNRS PICS program "DINASIA" ; special INSU grant ; special INSU grant ; National Basic Research Program of China Grant(2012CB821900) ; National Basic Research Program of China Grant(2012CB821900) ; CNRS PICS program "DINASIA" ; CNRS PICS program "DINASIA" ; special INSU grant ; special INSU grant ; National Basic Research Program of China Grant(2012CB821900) ; National Basic Research Program of China Grant(2012CB821900) ; CNRS PICS program "DINASIA" ; CNRS PICS program "DINASIA" ; special INSU grant ; special INSU grant ; National Basic Research Program of China Grant(2012CB821900) ; National Basic Research Program of China Grant(2012CB821900) ; CNRS PICS program "DINASIA" ; CNRS PICS program "DINASIA" ; special INSU grant ; special INSU grant
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/86923]  
专题中国科学院地质与地球物理研究所
通讯作者Amiot, Romain
作者单位1.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Key Lab Vertebrate Evolut & Human Origins, Beijing 100044, Peoples R China
2.Univ Lyon 1, CNRS, UMR 5276, F-69622 Villeurbanne, France
3.Ecole Normale Super Lyon, F-69622 Villeurbanne, France
4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
5.Ecole Normale Super, Geol Lab, CNRS, UMR 8538, F-75231 Paris 05, France
6.Inst Phys Globe Paris, F-75005 Paris, France
7.Ehime Univ, Grad Sch Sci & Engn, Dept Earths Evolut & Environm, Matsuyama, Ehime 7908577, Japan
8.Nat Hist Museum Guangxi, Nanning 530012, Peoples R China
9.Mahasarakham Univ, Palaeontol Res & Educ Ctr, Maha Sarakham, Thailand
推荐引用方式
GB/T 7714
Amiot, Romain,Wang, Xu,Zhou, Zhonghe,et al. Environment and ecology of East Asian dinosaurs during the Early Cretaceous inferred from stable oxygen and carbon isotopes in apatite[J]. JOURNAL OF ASIAN EARTH SCIENCES,2015,98:358-370.
APA Amiot, Romain.,Wang, Xu.,Zhou, Zhonghe.,Wang, Xiaolin.,Lecuyer, Christophe.,...&Xu, Xing.(2015).Environment and ecology of East Asian dinosaurs during the Early Cretaceous inferred from stable oxygen and carbon isotopes in apatite.JOURNAL OF ASIAN EARTH SCIENCES,98,358-370.
MLA Amiot, Romain,et al."Environment and ecology of East Asian dinosaurs during the Early Cretaceous inferred from stable oxygen and carbon isotopes in apatite".JOURNAL OF ASIAN EARTH SCIENCES 98(2015):358-370.
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