Coccolith chemistry reveals secular variations in the global ocean carbon cycle?
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...
Main Authors: | Rickaby, R, Bard, E, Sonzogni, C, Rostek, F, Beaufort, L, Barker, S, Rees, G, Schrag, D |
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Format: | Journal article |
Language: | English |
Published: |
2007
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