Planktonic foraminifera oxygen isotope and trace metal data ODP Hole 172-1056A, 46-54 ka BP

Salinity increase in the subtropical gyre system may have pre-conditioned the North Atlantic Ocean for a rapid return to stronger overturning circulation and high-latitude warming following meltwater events during the Last Glacial period. Here we investigate the Gulf Stream - subtropical gyre system...

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Bibliographic Details
Main Authors: Hoogakker, Babette A A, Downy, Frances, Andersson, Maria A, Chapman, Mark R, Elderfield, Henry, McCave, I Nick, Lenton, Timothy M, Gruetzner, Jens
Format: Dataset
Language:English
Published: PANGAEA 2013
Subjects:
Ocean Drilling Program
ODP
North Atlantic
Planktonic foraminifera
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.856558
https://doi.org/10.1594/PANGAEA.856558

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