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Constraints from clumped isotope analyses of a stalagmite on maximum tropical temperature change through the late Pleistocene

Meckler, A. N. and Adkins, J. F. and Eiler, J. M. and Cobb, K. M. (2009) Constraints from clumped isotope analyses of a stalagmite on maximum tropical temperature change through the late Pleistocene. Geochimica et Cosmochimica Acta, 73 (13). A863. ISSN 0016-7037. https://resolver.caltech.edu/CaltechAUTHORS:20130729-134243287

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Abstract

We analyzed modern and ancient speleothems from caves in Northern Borneo (4°N, 115°W) for their carbonate isotopologue, or 'clumped isotope', compositions. Although this method of paleothermometry appears to exhibit a common calibration in a variety of carbonates, speleothems have so far proven to be difficult archives for this technique. Most samples measured to date are out of equilibrium, yielding apparent temperatures that are too high [1,2].


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1016/j.gca.2009.05.011DOIArticle
http://www.sciencedirect.com/science/article/pii/S0016703709002646PublisherArticle
Additional Information:© 2009 Published by Elsevier Ltd.
Issue or Number:13
Record Number:CaltechAUTHORS:20130729-134243287
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20130729-134243287
Official Citation:Goldschmidt Abstracts 2009 – M, Geochimica et Cosmochimica Acta, Volume 73, Issue 13, Supplement, June 2009, Pages A809-A924, ISSN 0016-7037, http://dx.doi.org/10.1016/j.gca.2009.05.011.
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:39632
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:29 Jul 2013 21:11
Last Modified:03 Oct 2019 05:09

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