Articles | Volume 19, issue 11
https://doi.org/10.5194/bg-19-2759-2022
https://doi.org/10.5194/bg-19-2759-2022
Research article
 | 
02 Jun 2022
Research article |  | 02 Jun 2022

A modern snapshot of the isotopic composition of lacustrine biogenic carbonates – records of seasonal water temperature variability

Inga Labuhn, Franziska Tell, Ulrich von Grafenstein, Dan Hammarlund, Henning Kuhnert, and Bénédicte Minster

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Revised manuscript accepted for BG
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Cited articles

Andersson, S., Rosqvist, G., Leng, M. J., Wastegård, S., and Blaauw, M.: Late Holocene climate change in central Sweden inferred from lacustrine stable isotope data, J. Quaternary Sci., 25, 1305–1316, https://doi.org/10.1002/jqs.1415, 2010. a, b, c
Andrews, J. E., Coletta, P., Pentecost, A., Riding, R., Dennis, S., Dennis, P. F., and Spiro, B.: Equilibrium and disequilibrium stable isotope effects in modern charophyte calcites: implications for palaeoenvironmental studies, Palaeogeogr. Palaeocl., 204, 101–114, https://doi.org/10.1016/S0031-0182(03)00725-9, 2004. a, b
Apolinarska, K., Pełechaty, M., and Pronin, E.: Discrepancies between the stable isotope compositions of water, macrophyte carbonates and organics, and mollusc shells in the littoral zone of a charophyte-dominated lake (Lake Lednica, Poland), Hydrobiologia, 768, 1–17, https://doi.org/10.1007/s10750-015-2524-6, 2016. a, b, c
Beck, W. C., Grossman, E. L., and Morse, J. W.: Experimental studies of oxygen isotope fractionation in the carbonic acid system at 15, 25, and 40 C, Geochim. Cosmochim. Ac., 69, 3493–3503, https://doi.org/10.1016/j.gca.2005.02.003, 2005. a
Bova, S., Rosenthal, Y., Liu, Z., Godad, S. P., and Yan, M.: Seasonal origin of the thermal maxima at the Holocene and the last interglacial, Nature, 589, 548–553, https://doi.org/10.1038/s41586-020-03155-x, 2021. a
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This study presents the isotopic composition of recent biogenic carbonates from several lacustrine species which calcify during different times of the year. The authors demonstrate that when biological offsets are corrected, the dominant cause of differences between species is the seasonal variation in temperature-dependent fractionation of oxygen isotopes. Consequently, such carbonates from lake sediments can provide proxy records of seasonal water temperature changes in the past.
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