Regional seawater δ18O records and global δ18O seawater-stack over the mid-Pleistocene transition

High-resolution seawater δ18O records, derived from coupled benthic foraminifera Mg/Ca and δ18O analyses, can be used to evaluate how global ice volume changed during the Mid-Pleistocene Transition (MPT, ~1250-600 ka ago). However, such seawater δ18O records are also influenced by regional hydrograp...

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Bibliographic Details
Main Authors: Ford, Heather L, Raymo, Maureen E
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2019
Subjects:
Benthic foraminifera
Mg/Ca
mid-Pleistocene transition
δ18Obenthic
δ18Oseawater
Pacific
Rosenthal
North Atlantic
Online Access:https://dx.doi.org/10.1594/pangaea.908121
https://doi.pangaea.de/10.1594/PANGAEA.908121

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