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^(13)C^(18)O clumping in speleothems: Observations from natural caves and precipitation experiments

Daëron, M. and Guo, W. and Eiler, J. and Genty, D. and Blamart, D. and Boch, R. and Drysdale, R. and Maire, R. and Wainer, K. and Zanchetta, G. (2011) ^(13)C^(18)O clumping in speleothems: Observations from natural caves and precipitation experiments. Geochimica et Cosmochimica Acta, 75 (15). pp. 3303-3317. ISSN 0016-7037. https://resolver.caltech.edu/CaltechAUTHORS:20110816-134745462

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Abstract

The oxygen isotope composition of speleothems is an important proxy of continental paleoenvironments, because of its sensitivity to variations in cave temperature and drip water δ^(18)O. Interpreting speleothem δ^(18)O records in terms of absolute paleotemperatures and δ^(18)O values of paleo-precipitation requires quantitative separation of the effects of these two parameters, and correcting for possible kinetic isotope fractionation associated with precipitation of calcite out of thermodynamic equilibrium. Carbonate clumped-isotope thermometry, based on measurements of Δ_47 (a geochemical variable reflecting the statistical overabundance of ^(13)C^(18)O bonds in CO_2 evolved from phosphoric acid digestion of carbonate minerals), potentially provides a method for absolute speleothem paleotemperature reconstructions independent of drip water composition. Application of this new technique to karst records is currently limited by the scarcity of published clumped-isotope studies of modern speleothems. The only modern stalagmite reported so far in the literature yielded a lower Δ_47 value than expected for equilibrium precipitation, possibly due to kinetic isotope fractionation. Here we report Δ_47 values measured in natural speleothems from various cave settings, in carbonate produced by cave precipitation experiments, and in synthetic stalagmite analogs precipitated in controlled laboratory conditions designed to mimic natural cave processes. All samples yield lower Δ_47 and heavier δ^(18)O values than predicted by experimental calibrations of thermodynamic equilibrium in inorganic calcite. The amplitudes of these isotopic disequilibria vary between samples, but there is clear correlation between the amount of Δ_47 disequilibrium and that of δ^(18)O. Even pool carbonates believed to offer excellent conditions for equilibrium precipitation of calcite display out-of-equilibrium δ^(18)O and Δ_47 values, probably inherited from prior degassing within the cave system. In addition to these modern observations, clumped-isotope analyses of a flowstone from Villars cave (France) offer evidence that the amount of disequilibrium affecting Δ_47 in a single speleothem can experience large variations at time scales of 10 kyr. Application of clumped-isotope thermometry to speleothem records calls for an improved physical understanding of DIC fractionation processes in karst waters, and for the resolution of important issues regarding equilibrium calibration of Δ_47 in inorganic carbonates.


Item Type:Article
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http://dx.doi.org/10.1016/j.gca.2010.10.032DOIUNSPECIFIED
http://www.sciencedirect.com/science/article/pii/S0016703711001761PublisherUNSPECIFIED
Additional Information:© 2011 Elsevier Ltd. Received 14 December 2009; accepted 26 October 2010. Associate editor: Edwin A. Schauble. Available online 21 March 2011. We are grateful to the Versaveau family and Fritz Geissler for supporting this work and granting us access to the Villars and Katerloch caves. We also wish to thank Philippe Orengo (Laboratoire des Sciences du Climat et de l’Environnement) for his help in the field and in setting up the synthetic precipitation experiments; and Julius Nouet (Université de Paris-Sud) for X-ray diffraction analyses. We would also like to thank Hagit Affek and two anonymous reviewers for their thoughtful comments. This work was supported by the National Science Foundation, by the Division of Geological and Planetary Sciences at the California Institute of Technology, and by the Gordon and Betty Moore Foundation through the Caltech Tectonics Observatory. MD is grateful to Jean-Philippe Avouac, the Tectonics Observatory and the Comissariat à l’Energie Atomique for post-doctoral grants. The Australian Research Council offered financial support (DP0773700; DP110102185) to the Corchia project, and the Institut National des Sciences de l’Univers similarly supported this work through the ECLIPSE program. This is LSCE contribution #4470.
Group:Caltech Tectonics Observatory
Funders:
Funding AgencyGrant Number
NSFUNSPECIFIED
Caltech Division of Geological and Planetary SciencesUNSPECIFIED
Gordon and Betty Moore FoundationUNSPECIFIED
Caltech Tectonics ObservatoryUNSPECIFIED
Comissariat à l’Energie Atomique UNSPECIFIED
Australian Research CouncilDP0773700
Australian Research CouncilDP110102185
Institut National des Sciences de l’Univers ECLIPSE programUNSPECIFIED
Other Numbering System:
Other Numbering System NameOther Numbering System ID
LSCE contribution4470
Issue or Number:15
Record Number:CaltechAUTHORS:20110816-134745462
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20110816-134745462
Official Citation:M. Daeron, W. Guo, J. Eiler, D. Genty, D. Blamart, R. Boch, R. Drysdale, R. Maire, K. Wainer, G. Zanchetta, 13C18O clumping in speleothems: Observations from natural caves and precipitation experiments, Geochimica et Cosmochimica Acta, Volume 75, Issue 12, 15 June 2011, Pages 3303-3317, ISSN 0016-7037, DOI: 10.1016/j.gca.2010.10.032.
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:24891
Collection:CaltechAUTHORS
Deposited By: Jason Perez
Deposited On:16 Aug 2011 23:14
Last Modified:03 Oct 2019 03:00

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