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Diatom-inferred salinity changes from the Yushe paleolake indicate an aridification during the Plioc
【机 构】
:
Institute of Geology and Paleontology,Linyi University,Linyi,Shandong Province,China
【出 处】
:
The 23rd International Diatom Symposium (第23届国际硅藻大会)
【发表日期】
:
2014年期
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