期刊
EARTH AND PLANETARY SCIENCE LETTERS
卷 380, 期 -, 页码 1-11出版社
ELSEVIER SCIENCE BV
DOI: 10.1016/j.epsl.2013.08.027
关键词
stable carbon isotope; latest Miocene; C-4 expansion; Asian interior
资金
- National Basic Research Program of China (973 Program) [2013CB956400]
- Strategic Priority Research Program of the Chinese Academy of Sciences [XDB03020500]
- National Nature Science Foundation of China [41290251, 41272203]
The Cenozoic era is marked by dramatic climatic and ecological changes. The timing of the emergence and the subsequent expansions of C-4 grasses are prominent biological events on Earth. In China, thick Cenozoic deposits in the Tarim and Junggar Basins, which are located in the Asian interior, provide important geological archives for studying paleoenvironmental changes. Here we use carbon isotope compositions of organic matter to reconstruct the history of ecologic evolution during the late Cenozoic in the Tarim and Junggar Basins. The results show that there is a shift to slightly higher delta C-13 values at 5.3 Ma indicating a change in terrestrial ecosystems in the Asian interior driven by an increased regional aridity rather than decreasing atmospheric pCO(2) levels. The weakened water vapor transportation related to the retreat of Paratethys Ocean and the enhanced rain shadow effect of mountain uplift during the latest Miocene mostly triggered this event. (C) 2013 Elsevier B.V. All rights reserved.
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