Stable carbon and oxygen isotope ratios of benthic foraminifera from Paleocene to Oligocene sediments

Benthic oxygen and carbon isotopic results from a depth transect on Maud Rise, Antarctica, provide the first evidence for Warm Saline Deep Water (WSDW) in the Paleogene oceans. Distinct reversals occur in the oxygen isotopic gradient between the shallower Hole 689B (Eocene depth ~1400 m; present-day...

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Bibliographic Details
Main Authors: Kennett, James P, Stott, Lowell D
Format: Other/Unknown Material
Language:English
Published: PANGAEA 1990
Subjects:
113-689B
113-690B
DRILL
Drilling/drill rig
Joides Resolution
Leg113
Ocean Drilling Program
ODP
South Atlantic Ocean
Antarc*
Antarctic
Antarctica
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.726317
https://doi.org/10.1594/PANGAEA.726317

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