Holocene Hydroclimate Variability in Central Scandinavia Inferred from Flood Layers in Contourite Drift Deposits in Lake Storsjön-Reference-Cited by-同舟云学术

Holocene Hydroclimate Variability in Central Scandinavia Inferred from Flood Layers in Contourite Drift Deposits in Lake Storsjön

Published:2018-02-06 Issue:1 Volume:1 Page:2
ISSN:2571-550X
Container-title:Quaternary
language:en
Short-container-title:Quaternary

Author:

Labuhn Inga,Hammarlund Dan^ORCID,Chapron Emmanuel,Czymzik Markus,Dumoulin Jean-Pascal,Nilsson Andreas,Régnier Edouard,Robygd Joakim,von Grafenstein Ulrich

Funder

Vetenskapsrådet

Publisher

MDPI AG

Subject

Earth and Planetary Sciences (miscellaneous),Earth-Surface Processes

Link

http://www.mdpi.com/2571-550X/1/1/2/pdf

Reference126 articles.

1. Holocene glacier fluctuations of Flatebreen and winter-precipitation changes in the Jostedalsbreen region, western Norvay, based on glaciolacustrine sediment records

2. Rapid hydrological changes during the Holocene revealed by stable isotope records of lacustrine carbonates from Lake Igelsjön, southern Sweden

3. Holocene vegetation and climate history on a continental-oceanic transect in northern Fennoscandia based on pollen and plant macrofossils

4. Chironomids as a tool for inferring Holocene climate: an assessment based on six sites in southern Scandinavia

5. Late Holocene climate change in central Sweden inferred from lacustrine stable isotope data

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