Stable isotope records for the last 10 000 years from Okshola cave (Fauske, northern Norway) and regional comparisons

The sensitivity of terrestrial environments to past changes in heat transport is expected to be manifested in Holocene climate proxy records on millennial to seasonal timescales. Stalagmite formation in the Okshola cave near Fauske (northern Norway) began at about 10.4 ka, soon after the valley was...

Full description

Bibliographic Details
Main Authors: H. Linge, S.-E. Lauritzen, C. Andersson, J. K. Hansen, R. Ø. Skoglund, H. S. Sundqvist
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2009
Subjects:
Online Access:https://doaj.org/article/464b83b51dc04bc89b9fff6280de6a89