Decreased Deep Water Oxygenation in the Western North Pacific During the Plio‐Pleistocene Transition

Abstract The deep North Pacific, a vast respired carbon reservoir, likely plays a key role in the Plio‐Pleistocene CO2 decline and global cooling, but evidence for this is lacking. Here, oxygenation change in the upper deep western North Pacific between 5.3 and 1.0 million years ago (Ma) is reconstr...

Full description

Saved in:
Bibliographic Details
Main Authors: Man Zhao, Guodong Jia
Format: Article
Language:English
Published: Wiley 2025-07-01
Series:Geophysical Research Letters
Online Access:https://doi.org/10.1029/2025GL116177
Tags: Add Tag
No Tags, Be the first to tag this record!