Eocene/Oligocene ocean de-acidification linked to Antarctic glaciation by sea-level fall
Eocene/Oligocene ocean de-acidification linked to Antarctic glaciation by sea-level fall
One of the most dramatic perturbations to the Earth system during the past 100 million years was the rapid onset of Antarctic glaciation near the Eocene/Oligocene epoch boundary (34 million years ago). This climate transition was accompanied3 by a deepening of the calcite compensation depth
Publication Date:
24/04/2008
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