Ice-free intervals continuing into Marine Isotope Stage 3 at Sokli in the central area of the Fennoscandian glaciations

Ice-free intervals continuing into Marine Isotope Stage 3 at Sokli in the central area of the Fennoscandian glaciations

An unusually long and continuous Late Quaternary sedimentary sequence has been preserved in a sedimentary basin formed in the Sokli Carbonatite Massif in eastern-central Finnish Lapland. A nearly complete sediment recovery from the central Sokli basin combined with palynological results from sedimen...

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Bibliographic Details
Main Authors: K.F. Helmens, P.W. Johansson, M.E. Räsänen, H. Alexanderson, K.O. Eskola
Format: Article
Language:English
Published: Geological Society of Finland 2007-06-01
Series:Bulletin of the Geological Society of Finland
Subjects:
glacial geology
sediments
stratigraphy
pollen analysis
paleobotany
climate change
interstadial environment
interglacial environment
chronology
Pleistocene
Sokli
Lapland Province
Finland
Online Access:http://www.geologinenseura.fi/bulletin/Volume79/Helmens_etal_2007.pdf

Internet

http://www.geologinenseura.fi/bulletin/Volume79/Helmens_etal_2007.pdf

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