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

• 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
• Other Authors: Vetenskapsrådet
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2017
• Subjects: Southern Lake; Ice Sheet
• Online Access: http://dx.doi.org/10.1111/bor.12288; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12288; https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12288

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 mineralog...