- Abstract:
-
The mismatch between the 100 and 400 k.y. components of Pleistocene climate and the relative power of those terms from the eccentricity of the Earth's orbit remains a challenge to the Milankovitch hypothesis. Coccolithophores have the potential to respond to parameters of orbital forcing other than insolation, and, as a critical component of the ocean carbon cycle, can act to modify the climate response. The first direct comparison of coccolith fraction Sr/Ca, alkenone abundance and automated...
Expand abstract - Publication status:
- Published
- Publisher copy:
- 10.1016/j.epsl.2006.10.016
-
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- Journal:
- EARTH AND PLANETARY SCIENCE LETTERS
- Volume:
- 253
- Issue:
- 1-2
- Pages:
- 83-95
- Publication date:
- 2007-01-15
- DOI:
- ISSN:
-
0012-821X
- URN:
-
uuid:fab1750a-cb5b-403f-97b4-34e924341f9b
- Source identifiers:
-
82675
- Local pid:
- pubs:82675
- Language:
- English
- Keywords:
- Copyright date:
- 2007
Journal article
Coccolith chemistry reveals secular variations in the global ocean carbon cycle?
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