Holocene development and permafrost history of two mires in Tavvavuoma, Northern Sweden

Two peat cores from two mires with different characteristics, but both containingpermafrost features and located in the eastern part of the Tavvavuoma mire complex innorthernmost Sweden, were analysed for macrofossils and geochemical properties. Local vegetationsequences and changes in geochemical p...

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Bibliographic Details
Main Author: Prėskienis, Vilmantas
Format: Bachelor Thesis
Language:English
Published: Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK) 2013
Subjects:
Ice
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-92709
id ftstockholmuniv:oai:DiVA.org:su-92709
record_format openpolar
spelling ftstockholmuniv:oai:DiVA.org:su-92709 2023-05-15T16:11:55+02:00 Holocene development and permafrost history of two mires in Tavvavuoma, Northern Sweden Prėskienis, Vilmantas 2013 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-92709 eng eng Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK) http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-92709 info:eu-repo/semantics/openAccess plant macrofossils palsa peat plateau peatland development Tavvavuoma permafrost Holocene soil carbon content Student thesis info:eu-repo/semantics/bachelorThesis text 2013 ftstockholmuniv 2023-02-23T21:36:55Z Two peat cores from two mires with different characteristics, but both containingpermafrost features and located in the eastern part of the Tavvavuoma mire complex innorthernmost Sweden, were analysed for macrofossils and geochemical properties. Local vegetationsequences and changes in geochemical properties of peat were used to reconstruct development ofthe studied mires during the Holocene. The study includes measurements of water/ice content, bulkdensity, loss-on-ignition and C/N ratio. Radiocarbon dates for peatland inception and permafrostaggradation are available. The main purpose of the study is to verify permafrost history in thepeatlands. The results of the macrofossil analysis and values of C/N ratio indicate nutrient poor tointermediate fen environments in both studied mires until recently. Signs of permafrost upheavalwhich caused formation of xerophilic peat can be proved only since late 1950’s. The study resultscorroborate with other studies from Northern Fennoscandia and infer peatland initiation soon afterthe deglaciation of the area and permafrost-free conditions throughout entire Holocene untilrecently. Bachelor Thesis Fennoscandia Ice Northern Sweden palsa Peat Peat plateau permafrost Stockholm University: Publications (DiVA) Tavvavuoma ENVELOPE(20.860,20.860,68.520,68.520)
institution Open Polar
collection Stockholm University: Publications (DiVA)
op_collection_id ftstockholmuniv
language English
topic plant macrofossils
palsa
peat plateau
peatland development
Tavvavuoma
permafrost
Holocene
soil carbon content
spellingShingle plant macrofossils
palsa
peat plateau
peatland development
Tavvavuoma
permafrost
Holocene
soil carbon content
Prėskienis, Vilmantas
Holocene development and permafrost history of two mires in Tavvavuoma, Northern Sweden
topic_facet plant macrofossils
palsa
peat plateau
peatland development
Tavvavuoma
permafrost
Holocene
soil carbon content
description Two peat cores from two mires with different characteristics, but both containingpermafrost features and located in the eastern part of the Tavvavuoma mire complex innorthernmost Sweden, were analysed for macrofossils and geochemical properties. Local vegetationsequences and changes in geochemical properties of peat were used to reconstruct development ofthe studied mires during the Holocene. The study includes measurements of water/ice content, bulkdensity, loss-on-ignition and C/N ratio. Radiocarbon dates for peatland inception and permafrostaggradation are available. The main purpose of the study is to verify permafrost history in thepeatlands. The results of the macrofossil analysis and values of C/N ratio indicate nutrient poor tointermediate fen environments in both studied mires until recently. Signs of permafrost upheavalwhich caused formation of xerophilic peat can be proved only since late 1950’s. The study resultscorroborate with other studies from Northern Fennoscandia and infer peatland initiation soon afterthe deglaciation of the area and permafrost-free conditions throughout entire Holocene untilrecently.
format Bachelor Thesis
author Prėskienis, Vilmantas
author_facet Prėskienis, Vilmantas
author_sort Prėskienis, Vilmantas
title Holocene development and permafrost history of two mires in Tavvavuoma, Northern Sweden
title_short Holocene development and permafrost history of two mires in Tavvavuoma, Northern Sweden
title_full Holocene development and permafrost history of two mires in Tavvavuoma, Northern Sweden
title_fullStr Holocene development and permafrost history of two mires in Tavvavuoma, Northern Sweden
title_full_unstemmed Holocene development and permafrost history of two mires in Tavvavuoma, Northern Sweden
title_sort holocene development and permafrost history of two mires in tavvavuoma, northern sweden
publisher Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK)
publishDate 2013
url http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-92709
long_lat ENVELOPE(20.860,20.860,68.520,68.520)
geographic Tavvavuoma
geographic_facet Tavvavuoma
genre Fennoscandia
Ice
Northern Sweden
palsa
Peat
Peat plateau
permafrost
genre_facet Fennoscandia
Ice
Northern Sweden
palsa
Peat
Peat plateau
permafrost
op_relation http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-92709
op_rights info:eu-repo/semantics/openAccess
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