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Diatom-inferred salinity changes from the Yushe paleolake indicate an aridification during the Pliocene-Pleistocene transition in north China [期刊论文]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2015-01-01, 417
Li Y.-M.;  Ferguson D.K.;  Zhao Q.;  Wang Y.-F.;  Wang R.-X.;  Li C.-S.
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