Lake sediments as continental δ18O records from the glacial/post-glacial transition ...
As in polar ice, 18O variations of precipitation are recorded in carbonate sediments formed in lakes (lake marl). We have analyzed many late-glacial profiles from Europe, There are strong l8O variations which coincide with well-known pollen zone boundaries and which indicate that abrupt, drastic cli...
Main Authors: | , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
University of Bern
1984
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Subjects: | |
Online Access: | https://dx.doi.org/10.48350/158751 https://boris-portal.unibe.ch/handle/20.500.12422/43362 |