The Late Weichselian and Holocene relative sea-level change and isolation basin stratigraphy at the Umba settlement, southern coast of Kola Peninsula
https://doi.org/10.15356/0373-2444-2013-1-73-88
Abstract
The lacustrine-marine (from three lakes) and marine-lacustrine transition (isolation contact) in sediment cores from six lake basins situated 12.0–41.0 m a.s.l. in Umba settlement area, South coast of Kola Peninsula, NW Russia, was identifi ed based on lithological and diatom analysis, radiocarbon dated, and used to construct a relative sea-level (RSL) curve for the Late Weichselian – Holocene. Three lake basins show both transgressive (periglacial lake-transition – marine) and regressive (marine-transition – lacustrine) facies succession, six lake basins show regressive (marine-transition – lacustrine) facies succession indicating a postglacial history of continuous emergence.
About the Authors
V. V. Kolka
Geological Institute, Kola Science Centre, RAS
Russian Federation
Russian Federation
V. Ya. Yevzerov
Geological Institute, Kola Science Centre, RAS
Russian Federation
Russian Federation
J. J. Møller
University of Tromsø
Norway
Norway
G. D. Corner
University of Tromsø
Norway
Norway
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Review
For citations:
Kolka V.V., Yevzerov V.Ya., Møller J.J., Corner G.D. The Late Weichselian and Holocene relative sea-level change and isolation basin stratigraphy at the Umba settlement, southern coast of Kola Peninsula. Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya. 2013;(1):73-88. (In Russ.) https://doi.org/10.15356/0373-2444-2013-1-73-88
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