Does δ18O of O2 record meridional shifts in tropical rainfall?

Marine sediments, speleothems, paleo-lake elevations, and ice core methane and δ¹⁸O of O₂ (δ¹⁸Oatm) records provide ample evidence for repeated abrupt meridional shifts in tropical rainfall belts throughout the last glacial cycle. To improve understanding of the impact of abrupt events on the global...

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Bibliographic Details
Main Authors: Seltzer, Alan M., Buizert, Christo, Baggenstos, Daniel, Brook, Edward J., Ahn, Jinho, Yang, Ji-Woong, Severinghaus, Jeffrey P.
Format: Text
Language:English
Published: Copernicus Publications 2017
Subjects:
Online Access:https://dx.doi.org/10.7892/boris.106567
https://boris.unibe.ch/106567/