Benthic (C. wuellerstorfi) δ¹⁸O, δ¹³C and Cd/Ca in sediment core NEAP 4K across the last deglaciation
We present evidence that the characteristic chemical signature (based on coupled benthic foraminiferal Cd/Ca and d13C) of Antarctic Intermediate waters (AAIW) penetrated throughout the intermediate depths of the Atlantic basin to the high-latitude North Atlantic during the abrupt cooling events of t...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2005
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.832162 https://doi.org/10.1594/PANGAEA.832162 |