Biostratigraphic Evidence of the Allerød-Younger Dryas-Preboreal Oscillation in Northern Iceland
Basal sediments of Lake Torfadalsvatn, northern Iceland, record changes in terrestrial and limnic environments in the period 11,300-9000 14C yr B.P. These changes were probably forced by climate and connected with displacements of the marine polar front and sea-ice margin. Pollen, spores, green alga...
Published in: | Quaternary Research |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Academic Press
1995
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Online Access: | https://lup.lub.lu.se/record/b19ad92d-2392-44ae-9088-05f0cda585ee https://doi.org/10.1006/qres.1995.1085 |