CaltechAUTHORS
Published August 2006 | Version public
Journal Article Metadata-only

Biogeochemistry of neoproterozoic low latitude glaciations

Creators

  • 1. ROR icon University of Southern California
  • 2. ROR icon California Institute of Technology
  • 3. ROR icon Guangzhou Institute of Geochemistry

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

Identifiers

Eprint ID
47185
Resolver ID
CaltechAUTHORS:20140714-142024179

Dates

Created
2014-07-14
Created from EPrint's datestamp field
Updated
2021-11-10
Created from EPrint's last_modified field

Caltech Custom Metadata

Caltech groups
Division of Geological and Planetary Sciences (GPS)