Published June 2009
| public
Journal Article
Constraints from clumped isotope analyses of a stalagmite on maximum tropical temperature change through the late Pleistocene
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].
Additional Information
© 2009 Published by Elsevier Ltd.Additional details
- Eprint ID
- 39632
- DOI
- 10.1016/j.gca.2009.05.011
- Resolver ID
- CaltechAUTHORS:20130729-134243287
- Created
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2013-07-29Created from EPrint's datestamp field
- Updated
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2021-11-09Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences (GPS)