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...

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Bibliographic Details
Main Authors: Rickaby, Rosalind E M, Elderfield, Henry
Format: Dataset
Language:English
Published: PANGAEA 2005
Subjects:
AGE
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.832162
https://doi.org/10.1594/PANGAEA.832162