Changes in bottom water corrosiveness and carbonate ion concentrations in the sub-Antarctic Atlantic during the last glacial period

The glacial climate system transitioned rapidly between cold (stadial) and warm (interstadial) conditions in the Northern Hemisphere. This variability, referred to as Dansgaard-Oeschger variability, is widely believed to arise from perturbations of the Atlantic Meridional Overturning Circulation. Ev...

Full description

Bibliographic Details
Main Authors: Gottschalk, Julia, Skinner, Luke C, Misra, Sambuddha, Waelbroeck, Claire, Menviel, Laurie, Timmermann, Axel
Format: Dataset
Language:English
Published: PANGAEA 2015
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.841244
https://doi.org/10.1594/PANGAEA.841244