Comparative clumped isotope temperature relationships in freshwater carbonates

Abstract Lacustrine, riverine and spring carbonates represent archives of terrestrial climates and their geochemistry has been used to study palaeoenvironments. Clumped isotope thermometry is an emerging tool that has been applied to freshwater carbonates. Limited work has been done to evaluate comparative relationships between clumped isotopes and temperature in different types of modern freshwater carbonates. This study assembles an extensive calibration data set with 135 samples of modern freshwater carbonates from 96 sites and constrains the relationship between independent observations of water temperature and the clumped isotopic composition of carbonates (denoted by Δ 47 ), including new measurements, and recalculates published data in accordance with current community‐defined standard values. For temperature reconstruction, the study reports a composite freshwater calibration and material‐specific calibrations for biogenic carbonates (freshwater gastropods and bivalves), fine‐grained carbonate (e.g. micrites), biologically mediated carbonates (microbialites and tufas) and travertines. Material‐specific calibration trends show a convergence of slopes that are in agreement with recently published syntheses, but statistically significant differences in intercepts occur between some materials (e.g. some biogenics, fine‐grained carbonates). These differences may arise due to unresolved seasonal biases, kinetic isotope effects and/or varying degrees of biological influence. The impact of different calibrations is shown through application to new data for glacial and deglacial age travertines from Austria and published data sets. While material‐specific calibrations may yield more accurate results for biogenic and fine‐grained carbonate samples, the use of material‐specific and the composite freshwater calibrations generally produces values within 1.0–1.5°C of each other, and typically fall within calibration uncertainty given limitations of precision.

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Publication Details

Journal
The Depositional Record
Published
2024-10-06
DOI
https://doi.org/10.1002/dep2.312
Citations
4
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
1.51
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article

Comparative clumped isotope temperature relationships in freshwater carbonates

Aradhna Tripati, Priyadarsi Debajyoti Roy, James M. Russell, Cristian Román‐Palacios et al.
4 citations
The Depositional Record
Geology and Paleoclimatology Research
1.51
article

Comparative clumped isotope temperature relationships in freshwater carbonates

Aradhna Tripati, Priyadarsi Debajyoti Roy, James M. Russell, Cristian Román‐Palacios, Bryce Mitsunaga, Jamie Lucarelli, Daniel Ibarra, Majie Fan, Martin Dietzel, Robert B. Dunbar, Darrell S. Kaufman, J. A. Mering, Andrew S. Cohen, Stefan V. Lalonde, Ronny Boch, Lenin D. Chari, Ben Elliott, Huashu Li, Xingqi Liu, Robert A. Eagle, John Wilson, Alexandrea Arnold, Fengming Chang, Lin Li, hyn Victoria Petrys
article en
4 citations

Abstract

Abstract Lacustrine, riverine and spring carbonates represent archives of terrestrial climates and their geochemistry has been used to study palaeoenvironments. Clumped isotope thermometry is an emerging tool that has been applied to freshwater carbonates. Limited work has been done to evaluate comparative relationships between clumped isotopes and temperature in different types of modern freshwater carbonates. This study assembles an extensive calibration data set with 135 samples of modern freshwater carbonates from 96 sites and constrains the relationship between independent observations of water temperature and the clumped isotopic composition of carbonates (denoted by Δ 47 ), including new measurements, and recalculates published data in accordance with current community‐defined standard values. For temperature reconstruction, the study reports a composite freshwater calibration and material‐specific calibrations for biogenic carbonates (freshwater gastropods and bivalves), fine‐grained carbonate (e.g. micrites), biologically mediated carbonates (microbialites and tufas) and travertines. Material‐specific calibration trends show a convergence of slopes that are in agreement with recently published syntheses, but statistically significant differences in intercepts occur between some materials (e.g. some biogenics, fine‐grained carbonates). These differences may arise due to unresolved seasonal biases, kinetic isotope effects and/or varying degrees of biological influence. The impact of different calibrations is shown through application to new data for glacial and deglacial age travertines from Austria and published data sets. While material‐specific calibrations may yield more accurate results for biogenic and fine‐grained carbonate samples, the use of material‐specific and the composite freshwater calibrations generally produces values within 1.0–1.5°C of each other, and typically fall within calibration uncertainty given limitations of precision.

The Depositional RecordVol. 11(1)
University of Southern California (US), Planetary Science Institute (US), University of Arizona (US), Pacific Northwest National Laboratory (US), University of California, Los Angeles (US), Université de Bretagne Occidentale (FR), The University of Texas at Arlington (US), Chinese Academy of Sciences (CN), Northern Arizona University (US), Brown University (US), University of Bristol (GB), Graz University of Technology (AT), Institute of Oceanology (CN), GSI Environmental (United States) (US), Center for Creative Leadership (US), Institut Universitaire Européen de la Mer (FR), Universidad Nacional Autónoma de México (MX), Capital Normal University (CN), Stanford University (US)
Life below water
Openalex Percentile: Top 19%
Geology and Paleoclimatology Research
1.51
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