A Late-Eocene palynological record from the Hoh Xil Basin, northern Tibetan Plateau, and its implications for stratigraphic age, paleoclimate and paleoelevation
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- 作者：Yunfa Miaoa ; Fuli Wub ; c ; wufuli@itpcas.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Hong Changd ; Xiaomin Fangb ; c ; Tao Denge ; Jimin Sunf ; Chunsheng Jinf
- 关键词：Tibetan Plateau ; Palynology ; Late Eocene ; Paleoclimate ; Paleoelevation
- 刊名：Gondwana Research
- 出版年：2016
- 出版时间：March 2016
- 年：2016
- 卷：31
- 期：Complete
- 页码：241-252
- 全文大小：3336 K
文摘
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Hoh Xil Basin is crucial for studying Tibetan paleoclimate and paleoelevation.
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Age of sedimentary Yaxicuo Group at Hoh Xil Basin still remains under debate.
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Late Eocene is inferred based on palynological morphologies and assemblages.
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Hoh Xil Basin was dry and no higher than 2000 m a.s.l. during the Late Eocene.