Postglacial emergence and the Tapes transgression, north‐central Kola Peninsula, Russia

The history of postglacial emergence on the Murman coast, Kola Peninsula, is reconstructed based on twelve new radiocarbon ages from three marine sections and regional shoreline observations. Two pronounced shore levels are recognized below the Late Weichselian marine limit. The lower shoreline (11...

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Bibliographic Details
Published in:Boreas
Main Authors: SNYDER, JEFFREY A., KORSUN, SERGEY A., FORMAN, STEVEN L.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1996
Subjects:
Geology
Archeology
Ecology, Evolution, Behavior and Systematics
Barents Sea
Kola Peninsula
glacier
kola peninsula
Online Access:http://dx.doi.org/10.1111/j.1502-3885.1996.tb00834.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1996.tb00834.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1996.tb00834.x
Description
Summary:The history of postglacial emergence on the Murman coast, Kola Peninsula, is reconstructed based on twelve new radiocarbon ages from three marine sections and regional shoreline observations. Two pronounced shore levels are recognized below the Late Weichselian marine limit. The lower shoreline (11 ‐16 m a.s.l.) is associated with a transgression dated to 6200–6600 BP, correlative to the Tapes transgression on the Norwegian coastline. The upper shoreline (36–47 m a.s.l.) is not yet dated directly but probably correlates to the Main (Younger Dryas) shoreline. Strandline elevations descend eastward along the Murman coast. Observed emergence trends suggest the greatest regional Late Weichselian glacier load over the west‐central Kola Peninsula rather than in the southern Barents Sea.

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