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...
Main Authors: | , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2009
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Subjects: | |
Online Access: | https://doaj.org/article/464b83b51dc04bc89b9fff6280de6a89 |