Opening the gateways for diatoms primes Earth for Antarctic glaciation

The abrupt onset of Antarctic glaciation during the Eocene–Oligocene Transition (?33.7 Ma, Oi1) is linked to declining atmospheric pCO2 levels, yet the mechanisms that forced pCO2 decline remain elusive. Biogenic silicon cycling is inextricably linked to both long and short term carbon cycling throu...

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Bibliographic Details
Published in:Earth and Planetary Science Letters
Main Authors: Egan, Katherine E., Rickaby, Rosalind E.M., Hendry, Katharine R., Halliday, Alex N.
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Online Access:https://eprints.soton.ac.uk/359551/