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...
Main Authors: | , , , , , , |
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Format: | Text |
Language: | English |
Published: |
Copernicus Publications
2017
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Subjects: | |
Online Access: | https://dx.doi.org/10.7892/boris.106567 https://boris.unibe.ch/106567/ |