Re-examination of the temperature-dependent relationship between delta 18Odiatoms and delta 18Olake...
Re-examination of the temperature-dependent relationship between delta 18Odiatoms and delta 18Olake water and implications for paleoclimate inferences
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English
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The oxygen isotope composition ( delta 18O) of diatoms is commonly used for paleoclimate reconstruction. There is, however, no consensus regarding the equilibrium isotopic fractionation factor between diatom silica and the water in which it is precipitated. We re-examined the temperature-dependent relationship between delta 18Odiatoms and delta 18O...
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Re-examination of the temperature-dependent relationship between delta 18Odiatoms and delta 18Olake water and implications for paleoclimate inferences
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TN_cdi_proquest_miscellaneous_902364902
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_902364902
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0921-2728
DOI
10.1007/s10933-010-9436-2
