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...
Main Authors: | , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2005
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Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.769838 https://doi.pangaea.de/10.1594/PANGAEA.769838 |