Holocene climate of the Kola Peninsula; evidence from the oxygen isotope record of diatom silica

Holocene climate variability was studied in a lake sediment record covering the last c. 9000 years from Lake Chuna on the Kola Peninsula, north-west Russia, using the oxygen isotope composition of diatom silica (delta(18)O(diatom)). The evaporation of the lake waters is likely to be minimal, and thu...

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Bibliographic Details
Main Authors: Jones, VJ, Leng, MJ, Solovieva, N, Sloane, HJ, Tarasov, P
Format: Article in Journal/Newspaper
Language:unknown
Published: PERGAMON-ELSEVIER SCIENCE LTD 2004
Subjects:
LAKE-LEVEL CHANGES
VEGETATION HISTORY
NORTHERN SWEDEN
ATMOSPHERIC CIRCULATION
BIOGENIC SILICA
TREE-LIMIT
RUSSIA
PRECIPITATION
POLLEN
RECONSTRUCTION
Arctic
Chuna
Kola Peninsula
Fennoscandia
glacier
kola peninsula
North-West Russia
Northern Sweden
Online Access:http://discovery.ucl.ac.uk/11107/

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