δ18O and δ13C records from a Cenozoic sedimentary sequence in the Lanzhou Basin, Northwestern China: Implications for palaeoenvironmental and palaeoecological changes
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- 作者：Baofeng Li ; libf11@lzu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Donghuai Sun ; Xin Wang ; Yuebao Zhang ; Wenwei Hu ; Fei Wang ; Zaijun Li ; Zhiwei Ma ; Baiqing Liang
- 关键词：Aridification ; Palaeoecosystem ; Pedogenic carbonate ; Oxygen and carbon isotopes
- 刊名：Journal of Asian Earth Sciences
- 出版年：2016
- 出版时间：1 August 2016
- 年：2016
- 卷：125
- 期：Complete
- 页码：22-36
- 全文大小：2296 K
文摘
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Cenozoic δ18O and δ13C records of pedogenic carbonate from northwestern China.
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Drying of the Lanzhou Basin began at ∼33 Ma due to the retreat of the Tethys Sea.
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Asian inland aridity was further enhanced at ∼22 and ∼3.5 Ma.
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C4 plants expanded within the Lanzhou Basin after ∼3.5 Ma.