Woody vegetation, fuel and fire track the melting of the Scandinavian ice-sheet before 9500 cal yr BP

Abstract New studies indicate the presence of early Holocene ice-free areas far north in Scandinavia. Post-glacial fire and vegetation were investigated based on sedimentary charcoal and pollen from two small lakes in northern Sweden. Accumulation of organic sediment started around 10,900 and 9200 c...

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Published in:Quaternary Research
Main Authors: Carcaillet, Christopher, Hörnberg, Greger, Zackrisson, Olle
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2012
Subjects:
Online Access:http://dx.doi.org/10.1016/j.yqres.2012.08.001
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spelling crcambridgeupr:10.1016/j.yqres.2012.08.001 2024-10-13T14:08:07+00:00 Woody vegetation, fuel and fire track the melting of the Scandinavian ice-sheet before 9500 cal yr BP Carcaillet, Christopher Hörnberg, Greger Zackrisson, Olle 2012 http://dx.doi.org/10.1016/j.yqres.2012.08.001 http://api.elsevier.com/content/article/PII:S0033589412000920?httpAccept=text/xml http://api.elsevier.com/content/article/PII:S0033589412000920?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400008917 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 78, issue 3, page 540-548 ISSN 0033-5894 1096-0287 journal-article 2012 crcambridgeupr https://doi.org/10.1016/j.yqres.2012.08.001 2024-09-18T04:01:05Z Abstract New studies indicate the presence of early Holocene ice-free areas far north in Scandinavia. Post-glacial fire and vegetation were investigated based on sedimentary charcoal and pollen from two small lakes in northern Sweden. Accumulation of organic sediment started around 10,900 and 9200 cal yr BP, showing that both lake valleys were ice-free extremely early given their northerly location. Fire events started after 9600 cal yr BP and became less common around the ‘8.2-ka event’. Woody vegetation provided fuel that contributed to fires. The first vegetation in our pollen record consisted of Hippophae , Dryas , grasses and sedges. Subsequently broadleaved trees ( Betula , Salix ) increased in abundance and later Pinus , Alnus , ferns and Lycopodium characterized the vegetation. Pollen from Larix , Picea and Malus were also found. The change in vegetation composition was synchronous with the decrease in lake-water pH in the region, indicating ecosystem-scale processes; this occurred during a period of net global and regional warming. The changes in fire frequency and vegetation appear independent of regional trends in precipitation. The reconstructed fire history and vegetation support the scenario of early ice-free areas far north in Scandinavia during early Holocene warming, creating favorable conditions for woody plants and wildfires. Article in Journal/Newspaper Ice Sheet Northern Sweden Cambridge University Press Malus ENVELOPE(-65.734,-65.734,-66.229,-66.229) Quaternary Research 78 3 540 548
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract New studies indicate the presence of early Holocene ice-free areas far north in Scandinavia. Post-glacial fire and vegetation were investigated based on sedimentary charcoal and pollen from two small lakes in northern Sweden. Accumulation of organic sediment started around 10,900 and 9200 cal yr BP, showing that both lake valleys were ice-free extremely early given their northerly location. Fire events started after 9600 cal yr BP and became less common around the ‘8.2-ka event’. Woody vegetation provided fuel that contributed to fires. The first vegetation in our pollen record consisted of Hippophae , Dryas , grasses and sedges. Subsequently broadleaved trees ( Betula , Salix ) increased in abundance and later Pinus , Alnus , ferns and Lycopodium characterized the vegetation. Pollen from Larix , Picea and Malus were also found. The change in vegetation composition was synchronous with the decrease in lake-water pH in the region, indicating ecosystem-scale processes; this occurred during a period of net global and regional warming. The changes in fire frequency and vegetation appear independent of regional trends in precipitation. The reconstructed fire history and vegetation support the scenario of early ice-free areas far north in Scandinavia during early Holocene warming, creating favorable conditions for woody plants and wildfires.
format Article in Journal/Newspaper
author Carcaillet, Christopher
Hörnberg, Greger
Zackrisson, Olle
spellingShingle Carcaillet, Christopher
Hörnberg, Greger
Zackrisson, Olle
Woody vegetation, fuel and fire track the melting of the Scandinavian ice-sheet before 9500 cal yr BP
author_facet Carcaillet, Christopher
Hörnberg, Greger
Zackrisson, Olle
author_sort Carcaillet, Christopher
title Woody vegetation, fuel and fire track the melting of the Scandinavian ice-sheet before 9500 cal yr BP
title_short Woody vegetation, fuel and fire track the melting of the Scandinavian ice-sheet before 9500 cal yr BP
title_full Woody vegetation, fuel and fire track the melting of the Scandinavian ice-sheet before 9500 cal yr BP
title_fullStr Woody vegetation, fuel and fire track the melting of the Scandinavian ice-sheet before 9500 cal yr BP
title_full_unstemmed Woody vegetation, fuel and fire track the melting of the Scandinavian ice-sheet before 9500 cal yr BP
title_sort woody vegetation, fuel and fire track the melting of the scandinavian ice-sheet before 9500 cal yr bp
publisher Cambridge University Press (CUP)
publishDate 2012
url http://dx.doi.org/10.1016/j.yqres.2012.08.001
http://api.elsevier.com/content/article/PII:S0033589412000920?httpAccept=text/xml
http://api.elsevier.com/content/article/PII:S0033589412000920?httpAccept=text/plain
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400008917
long_lat ENVELOPE(-65.734,-65.734,-66.229,-66.229)
geographic Malus
geographic_facet Malus
genre Ice Sheet
Northern Sweden
genre_facet Ice Sheet
Northern Sweden
op_source Quaternary Research
volume 78, issue 3, page 540-548
ISSN 0033-5894 1096-0287
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1016/j.yqres.2012.08.001
container_title Quaternary Research
container_volume 78
container_issue 3
container_start_page 540
op_container_end_page 548
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