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...
| Published in: | Annals of Glaciology |
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| Main Authors: | , , , |
| Format: | Conference Object |
| Language: | English |
| Published: |
International Glaciological Society
1984
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| Subjects: | |
| Online Access: | https://boris.unibe.ch/158751/1/lake-sediments-as-continental-18o-records-from-the-glacialpost-glacial-transition.pdf https://boris.unibe.ch/158751/ |
| Summary: | 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 climatic changes occurred in the late glacial period. These events are a major warming around 13 ka BP (pollen zone boundary Oldest Dryas/Bölling) and a marked cold phase between about 10.8 and 10 ka BP (Younger Dryas). Comparison of the δ18O records of European lake sediments and of Greenland ice cores reveal a striking similarity which indicates that climatic changes in the late glacial and early postglacial were parallel in Greenland and in Europe. First results from North American lake-sediment profiles do not exhibit similar δ18O variations. This pattern of climatic changes was probably caused by retreating and readvancing polar water in the high-latitude North Atlantic Ocean, as discussed by Ruddiman and McIntyre (1981). |
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