Combined clumped isotope measurements resolve kinetic biases in carbonate formation temperatures
- 1Institute of Geosciences, Goethe University Frankfurt, Frankfurt am Main, Germany
- 2Institute of Geology and Mineralogy, University of Cologne, Cologne, Germany
- 3Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA, USA
- 4Senckenberg Biodiversity and Climate Research Centre (SBiK-F), Frankfurt am Main, Germany
- 5U.S. Geological Survey, Reston, VA, USA
- 6Institute of Geosciences, Johannes Gutenberg University Mainz, Mainz, Germany
- 7GEOMAR Helmholtz Centre for Ocean Research, Kiel, Germany
- 8School of Geography, Earth and Environmental Sciences, University of Plymouth, Plymouth, UK
Reaction kinetics involved in the precipitation of carbonates can introduce large scatter and inaccuracies in the temperatures derived from their δ18O and ∆47 values. Advances in mass spectrometry instrumentation recently enabled high-precision analysis of the 18O–18O clumping in carbonate minerals (∆48), despite the relatively low natural abundance of 12C18O18O, the main isotopologue contributing to the ∆48 signal (1). Measurements of ∆48, when combined with ∆47, can yield additional insights into kinetic effects and the carbonate formation environment (2).
Here we report high-precision ∆47 and ∆48 values of speleothem carbonates, modern coral skeletons, a brachiopod, and a belemnite. We constrained equilibrium in ∆47 vs ∆48 space by anchoring empirically derived ∆47 vs temperature and ∆48 vs temperature relationships to a Devils Hole mammillary calcite, known to be precipitated at extremely slow rates at a constant 33.7(±0.8) °C and water oxygen isotope composition. Our results, compared to theoretical predictions, provide the most substantial evidence to date that the isotopic disequilibrium commonly observed in speleothems and scleractinian coral skeletons is inherited from the dissolved inorganic carbon pool of their parent solutions. Data from an ancient belemnite imply it precipitated near isotopic equilibrium and confirm the warmer-than-present temperatures at Early Cretaceous southern high latitudes. The presence of similar kinetic departure in a brachiopod but not in a belemnite suggests that the current discrepancy between belemnite and brachiopod-based temperature estimates in the geologic record is most likely related to a greater kinetic bias in the isotopic composition of brachiopod shells.
We demonstrate that the combined clumped isotope method makes it possible to identify carbonates that did not precipitate in thermodynamic equilibrium from their parent water. Our results highlight the potential that the combined clumped isotope analyses hold for accurate paleoclimate reconstructions and the identification of the kinetic fractionation processes dominant in carbonate (bio)mineralisation.
(1) Fiebig et al. (2019), https://doi.org/10.1016/j.chemgeo.2019.05.019
(2) Guo, W. (2020), https://doi.org/10.1016/j.gca.2019.07.055
How to cite: Bajnai, D., Guo, W., Löffler, N., Methner, K., Krsnik, E., Coplen, T. B., Gischler, E., Hansen, M., Henkel, D., Price, G. D., Raddatz, J., Scholz, D., and Fiebig, J.: Combined clumped isotope measurements resolve kinetic biases in carbonate formation temperatures, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3051, https://doi.org/10.5194/egusphere-egu2020-3051, 2020.
