Published August 2006
| public
Journal Article
Biogeochemistry of neoproterozoic low latitude glaciations
Abstract
The Neoproterozoic (c.a. 1000–540 Ma) was a time of great change. Eukaryotes radiated through the ocean, while metazoans originated and diversified. The rock record preserves multiple negative excursions of over 15% in the carbonate ^(13)C/^(12)C, at least three of which are associated with global low-latitude glaciations.
Additional Information
© 2006 Elsevier Ltd. Available online 21 August 2006.Additional details
- Eprint ID
- 47185
- Resolver ID
- CaltechAUTHORS:20140714-142024179
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2014-07-14Created from EPrint's datestamp field
- Updated
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2021-11-10Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences