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- W2021199037 abstract "The oxygen isotope composition (δ18O) 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 δ18Odiatoms and δ18Olake water from Lake Annecy (France). A temperature coefficient of −0.16‰/°C (R 2 = 0.51) was determined, supporting findings from previous calibration studies. However, regression lines obtained from different calibration studies, though displaying similar slopes, were shifted. In this manuscript, we propose that several factors, including selected variables (temperature, δ18Olake water), analytical techniques, the impact of diagenetic processes and biological effects, may influence the silica-water fractionation factor for diatom silica. The similar magnitude of the diatom-temperature coefficients determined across studies is promising, supporting its use as a valuable tool for interpreting variations in δ18O values from fossil lacustrine diatoms in temperate lakes. With respect to paleoclimatic applications, the temperature-dependent relationship yielded uncertainties of ±3°C on reconstructed temperatures and ±0.5‰ on δ18Olake water." @default.
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- W2021199037 date "2010-04-22" @default.
- W2021199037 modified "2023-10-18" @default.
- W2021199037 title "Re-examination of the temperature-dependent relationship between δ18Odiatoms and δ18Olake water and implications for paleoclimate inferences" @default.
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- W2021199037 doi "https://doi.org/10.1007/s10933-010-9436-2" @default.
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