A persistent Holocene wetting trend in arid central Asia, with wettest conditions in the late Holocene, revealed by multi-proxy analyses of loess-paleosol sequences in Xinjiang, China
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- 作者：Fahu Chena ; b ; fhchen@lzu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Jia Jiaa ; jiaj@lzu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Jianhui Chena ; Guoqiang Lia ; Xiaojian Zhanga ; Haichao Xiea ; Dunsheng Xiaa ; Wei Huanga ; Chengbang Ana
- 关键词：Holocene ; Loess-paleosol sequence ; Moisture trend ; Wettest late Holocene
- 刊名：Quaternary Science Reviews
- 出版年：2016
- 出版时间：15 August 2016
- 年：2016
- 卷：146
- 期：Complete
- 页码：134-146
- 全文大小：2631 K
文摘
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The Holocene paleosol was formed after ∼6 ka BP in Xinjiang, China, the core area of ACA.
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A persistent Holocene wetting trend was found in the core area of ACA, with the wettest conditions in the late Holocene.
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The moisture dynamics in the core area of ACA may have close link with the westerlies, AO, NAO, and CGT during Holocene.