Revised age calibrations for the Eocene/Oligocene boundary of ODP Site 199-1218

The ocean depth at which the rate of calcium carbonate input from surface waters equals the rate of dissolution is termed the calcite compensation depth. At present, this depth is ~4,500 m, with some variation between and within ocean basins. The calcite compensation depth is linked to ocean acidity...

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Bibliographic Details
Main Authors: Coxall, Helen, Wilson, Paul A, Pälike, Heiko, Lear, Caroline H, Backman, Jan
Format: Dataset
Language:English
Published: PANGAEA 2005
Subjects:
Age
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.769838
https://doi.org/10.1594/PANGAEA.769838