Diatom-inferred salinity changes from the Yushe paleolake indicate an aridification during the Plioc

来源 :The 23rd International Diatom Symposium (第23届国际硅藻大会) | 被引量 : 0次 | 上传用户：xhbtbyrr

【摘要】

：

The global climate changed significantly during the Pliocene-Pleistocene transition,and a worldwide aridification occurred.In order to investigate the influence

【作者】

：

Ya-Meng Li David K.Ferguson Qi Zhao Yu-Fei Wang Rui-Xia Wang Cheng-Sen Li

【机构】

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InstituteofGeologyandPaleontology,LinyiUniversity,Linyi,ShandongProvince,China;StateKeyLaboratoryofS

【出处】

：

The 23rd International Diatom Symposium (第23届国际硅藻大会)

【发表日期】

：

2014年9期

【关键词】

：

diatoms aridification paleolimnology Pliocene-Pleistocene transition Zhangcun No

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The global climate changed significantly during the Pliocene-Pleistocene transition,and a worldwide aridification occurred.In order to investigate the influence of the aridification during the Pliocene-Pleistocene transition in the East Asian interior, diatom assemblages from the Upper Zhangcum Formation, North China, deposited during 2.77-2.52 Ma BP were analyzed, and the lake salinity was reconstructed using diatom-environment transfer functions.

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Diatom-inferred salinity changes from the Yushe paleolake indicate an aridification during the Plioc

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