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“Clumped-isotope” geochemistry—The study of naturally-occurring, multiply-substituted isotopologues

Eiler, John M. (2007) “Clumped-isotope” geochemistry—The study of naturally-occurring, multiply-substituted isotopologues. Earth and Planetary Science Letters, 262 (3-4). pp. 309-327. ISSN 0012-821X. doi:10.1016/j.epsl.2007.08.020. https://resolver.caltech.edu/CaltechAUTHORS:20121113-132813708

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Abstract

Clumped isotope geochemistry is concerned with the state of ordering of rare isotopes in natural materials. That is, it examines the extent to which rare isotopes (D, ^(13)C, ^(15)N, ^(18)O, etc.) bond with or near each other rather than with the sea of light isotopes in which they swim. Abundances of isotopic ‘clumps’ in natural materials are influenced by a wide variety of factors. In most cases, their concentrations approach (within ca. 1%, relative) the amount expected for a random distribution of isotopes. Deviations from this stochastic distribution result from: enhanced thermodynamic stability of heavy-isotope ‘clumps’; slower kinetics of reactions requiring the breakage of bonds between heavy isotopes; the mass dependence of diffusive and thermo-gravitational fractionations; mixing between components that differ from one another in bulk isotopic composition; biochemical and photochemical fractionations that may reflect combinations of these simpler physical mechanisms; and, in some cases, other processes we do not yet understand. Although clumped isotope geochemistry is a young field, several seemingly promising applications have already emerged. Most importantly, it appears that proportions of ^(13)C–^(18)O bonds in carbonate minerals are sensitive to their growth temperatures, independent of bulk isotopic composition. Thus, ‘clumped isotope’ analysis of ancient carbonates can be used as a quantitative paleothermometer that requires no assumptions about the δ^(18)O of waters from which carbonates grew. This approach has been used to reconstruct marine temperatures across the Phanerozoic (reaching back to the Silurian), terrestrial ground temperatures across the Cenozoic, thermal histories of aqueously altered meteorites, among other applications. Clumped isotope geochemistry is also placing new constraints on the atmospheric budget and stratospheric photochemistry of CO_2, and should be capable of placing analogous new constraints on the budgets of other atmospheric gases. Finally, this field could be extended to encompass sulfates, volatile hydrocarbons, organic moieties and other materials.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1016/j.epsl.2007.08.020 DOIUNSPECIFIED
http://www.sciencedirect.com/science/article/pii/S0012821X07005109PublisherUNSPECIFIED
Additional Information:© 2007 Elsevier B.V. Accepted 13 August 2007. Available online 28 August 2007. Editor: A.N. Halliday.
Subject Keywords:isotopes
Issue or Number:3-4
DOI:10.1016/j.epsl.2007.08.020
Record Number:CaltechAUTHORS:20121113-132813708
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20121113-132813708
Official Citation:John M. Eiler, “Clumped-isotope” geochemistry—The study of naturally-occurring, multiply-substituted isotopologues, Earth and Planetary Science Letters, Volume 262, Issues 3–4, 30 October 2007, Pages 309-327, ISSN 0012-821X, 10.1016/j.epsl.2007.08.020. (http://www.sciencedirect.com/science/article/pii/S0012821X07005109)
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:35439
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:13 Nov 2012 21:40
Last Modified:09 Nov 2021 23:15

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