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- W2389008450 abstract "At the 560-415 cm section of sediment core Q14B in Qinghai lake,δ18O of ostracod being heavier than of inorganic carbonate,indicates the higher temperature of lake surface water than of lake bottom water.The minor difference between ostracod δ18O and inorganic carbonate δ18O reflects the situation of shallow lake water induced by the cold and dry climate.The changing range of ostracod δ18O is in excess of that of inorganic carbonate δ18O,which possibly proves that the changing range of bottom water temperature exceeds that of surface water.When lacustrine carbonate δ18O is used to study the climatic and/or environmental evolution,it is of importance to test the single carbonate mineral δ18O." @default.
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- W2389008450 date "2011-01-01" @default.
- W2389008450 modified "2023-09-26" @default.
- W2389008450 title "Environmental Significance of Oxygen Isotopic Composition Disparity between Co-existing Ostracod and Inorganic Precipitated Carbonate Minerals:Evidence from Qinghai Lake" @default.
- W2389008450 hasPublicationYear "2011" @default.
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