A chronology of environmental changes in the Lake Vättern basin from deglaciation to its final isolation

During and after deglaciation, Lake Vättern developed from a proglacial lake situated at the westernmost rim of the Baltic Ice Lake (BIL), into a brackish water body connecting the North Sea and the Baltic Sea, and finally into an isolated freshwater lake. Here we present geochemical and mineralogic...

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Bibliographic Details
Published in:Boreas
Main Authors: Swärd, Henrik, O'Regan, Matt, Björck, Svante, Greenwood, Sarah L., Kylander, Malin E., Mörth, Carl-Magnus, Pearce, Christof, Jakobsson, Martin
Format: Article in Journal/Newspaper
Language:English
Published: John Wiley & Sons Inc. 2018
Subjects:
Geology
Southern Lake
Ice Sheet
Online Access:https://lup.lub.lu.se/record/54387fe4-bb45-452f-8f89-2aaa3ea6723c
https://doi.org/10.1111/bor.12288

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