- Abstract:
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Terrestrial chemical weathering of silicate minerals is a fundamental component of the global cycle of carbon and other elements. Past changes in temperature, rainfall, ice cover, sea-level and physical erosion are thought to affect weathering but the relative impact of these controls through time remains poorly constrained. This problem could be addressed if the nature of past weathering could be constrained at individual sites. In this study, we investigate the use of speleothems as local ...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Accepted manuscript
- Files:
-
-
(pdf, 1.3MB)
-
- Publisher copy:
- 10.1016/j.epsl.2017.04.014
-
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- Funding agency for:
- Pogge von Strandmann, PAE
- Publisher:
- Elsevier Publisher's website
- Journal:
- Earth and Planetary Science Letters Journal website
- Volume:
- 469
- Pages:
- 64-74
- Publication date:
- 2017-04-28
- Acceptance date:
- 2017-04-09
- DOI:
- ISSN:
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1385-013X
- Pubs id:
-
pubs:692264
- URN:
-
uri:20b2d255-a520-4f89-b0c1-14879fe2fedb
- UUID:
-
uuid:20b2d255-a520-4f89-b0c1-14879fe2fedb
- Local pid:
- pubs:692264
- Keywords:
- Copyright holder:
- Elsevier
- Copyright date:
- 2017
- Notes:
- © 2017 Elsevier B.V. All rights reserved. This is the accepted manuscript version of the article. The final version is available online from Elsevier at: http://dx.doi.org/10.1016/j.epsl.2017.04.014
Journal article
Lithium isotopes in speleothems: Temperature-controlled variation in silicate weathering during glacial cycles
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+ Natural Environment Research Council
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