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...

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Bibliographic Details
Main Authors: Siegenthaler, U., Eicher, U., Oeschger, H., Dansgaard, W.
Format: Article in Journal/Newspaper
Language:English
Published: University of Bern 1984
Subjects:
Online Access:https://dx.doi.org/10.48350/158751
https://boris-portal.unibe.ch/handle/20.500.12422/43362