The use of quantitative models to assess long-term climate–vegetation dynamics – A case study from the northern Scandinavian Mountains

Quantitative vegetation models combined with fossil pollen records have large potentials for assessing long-term vegetation dynamics. In this study, vegetation cover as a function of July temperatures was modelled for the Dividalen valley area situated in the northern Scandinavian Mountains. Site-sp...

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Published in:The Holocene
Main Authors: Sjögren, Per, Karlsen, Stein Rune, Jensen, Christin
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 2015
Subjects:
Online Access:http://dx.doi.org/10.1177/0959683615580196
http://journals.sagepub.com/doi/pdf/10.1177/0959683615580196
http://journals.sagepub.com/doi/full-xml/10.1177/0959683615580196
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spelling crsagepubl:10.1177/0959683615580196 2023-05-15T16:01:07+02:00 The use of quantitative models to assess long-term climate–vegetation dynamics – A case study from the northern Scandinavian Mountains Sjögren, Per Karlsen, Stein Rune Jensen, Christin 2015 http://dx.doi.org/10.1177/0959683615580196 http://journals.sagepub.com/doi/pdf/10.1177/0959683615580196 http://journals.sagepub.com/doi/full-xml/10.1177/0959683615580196 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 25, issue 7, page 1124-1133 ISSN 0959-6836 1477-0911 Paleontology Earth-Surface Processes Ecology Archeology Global and Planetary Change journal-article 2015 crsagepubl https://doi.org/10.1177/0959683615580196 2022-04-14T04:41:32Z Quantitative vegetation models combined with fossil pollen records have large potentials for assessing long-term vegetation dynamics. In this study, vegetation cover as a function of July temperatures was modelled for the Dividalen valley area situated in the northern Scandinavian Mountains. Site-specific pollen deposition values of the two dominating tree species pine and birch were simulated and compared with empirical fossil pollen values. The applied vegetation model could not explain the forest dynamics prior to 7400 cal. BP, although after this date, the forest seemed to have received a modern structure, and summer temperatures could potentially explain the long-term variations in forest cover. The most extensive forest cover occurred c. 7400–3800 cal. BP, corresponding to July temperatures of 0.5–1°C above the present. The approach proved sensitive to both site location and data quality. Careful site-selection is of importance for the application, and pollen accumulation rates are to be preferred as pollen percentage values proved problematic. Article in Journal/Newspaper Dividalen SAGE Publications (via Crossref) Dividalen ENVELOPE(19.547,19.547,68.881,68.881) The Holocene 25 7 1124 1133
institution Open Polar
collection SAGE Publications (via Crossref)
op_collection_id crsagepubl
language English
topic Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
spellingShingle Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
Sjögren, Per
Karlsen, Stein Rune
Jensen, Christin
The use of quantitative models to assess long-term climate–vegetation dynamics – A case study from the northern Scandinavian Mountains
topic_facet Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
description Quantitative vegetation models combined with fossil pollen records have large potentials for assessing long-term vegetation dynamics. In this study, vegetation cover as a function of July temperatures was modelled for the Dividalen valley area situated in the northern Scandinavian Mountains. Site-specific pollen deposition values of the two dominating tree species pine and birch were simulated and compared with empirical fossil pollen values. The applied vegetation model could not explain the forest dynamics prior to 7400 cal. BP, although after this date, the forest seemed to have received a modern structure, and summer temperatures could potentially explain the long-term variations in forest cover. The most extensive forest cover occurred c. 7400–3800 cal. BP, corresponding to July temperatures of 0.5–1°C above the present. The approach proved sensitive to both site location and data quality. Careful site-selection is of importance for the application, and pollen accumulation rates are to be preferred as pollen percentage values proved problematic.
format Article in Journal/Newspaper
author Sjögren, Per
Karlsen, Stein Rune
Jensen, Christin
author_facet Sjögren, Per
Karlsen, Stein Rune
Jensen, Christin
author_sort Sjögren, Per
title The use of quantitative models to assess long-term climate–vegetation dynamics – A case study from the northern Scandinavian Mountains
title_short The use of quantitative models to assess long-term climate–vegetation dynamics – A case study from the northern Scandinavian Mountains
title_full The use of quantitative models to assess long-term climate–vegetation dynamics – A case study from the northern Scandinavian Mountains
title_fullStr The use of quantitative models to assess long-term climate–vegetation dynamics – A case study from the northern Scandinavian Mountains
title_full_unstemmed The use of quantitative models to assess long-term climate–vegetation dynamics – A case study from the northern Scandinavian Mountains
title_sort use of quantitative models to assess long-term climate–vegetation dynamics – a case study from the northern scandinavian mountains
publisher SAGE Publications
publishDate 2015
url http://dx.doi.org/10.1177/0959683615580196
http://journals.sagepub.com/doi/pdf/10.1177/0959683615580196
http://journals.sagepub.com/doi/full-xml/10.1177/0959683615580196
long_lat ENVELOPE(19.547,19.547,68.881,68.881)
geographic Dividalen
geographic_facet Dividalen
genre Dividalen
genre_facet Dividalen
op_source The Holocene
volume 25, issue 7, page 1124-1133
ISSN 0959-6836 1477-0911
op_rights http://journals.sagepub.com/page/policies/text-and-data-mining-license
op_doi https://doi.org/10.1177/0959683615580196
container_title The Holocene
container_volume 25
container_issue 7
container_start_page 1124
op_container_end_page 1133
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