The role of the circumarctic forest–tundra ecotone for Arctic biodiversity

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dc.creator Hofgaard, Annika
dc.creator Harper, Karen A., 1969-
dc.creator Golubeva, Elena
dc.date.accessioned 2020-09-28T13:32:48Z
dc.date.available 2020-09-28T13:32:48Z
dc.date.issued 2012-10-10
dc.identifier.issn 1488-8386
dc.identifier.uri http://library2.smu.ca/xmlui/handle/01/29416
dc.description Accepted Version en_CA
dc.description.abstract The arctic forest–tundra ecotone (FTE), which links species communities of the boreal forest with those of the arctic tundra, is expected to respond swiftly to climate change with a profound reduction of tundra as the dominating scenario. With its circumarctic expanse and up to several hundred kilometres in width, the zone occupies a large part of the vegetated surface at high latitudes. Relocation and structural changes of the ecotone vegetation will affect not only plant but also animal and other biological diversity. A large number of arctic species are dependent on the forest–tundra ecotone in terms of food and habitat during parts of their life cycle or annual migration. In the ‘Arctic Species Trend Index’, developed to provide trends in arctic vertebrates, more than half of the species and data are from the forest–tundra ecotone. However, in assessments of arctic biodiversity, only the northernmost tundra-dominated areas of the ecotone are included. This is unfortunate and somewhat problematic since the treed part that serves as a source of seeds for new seedlings and saplings in the tundra-dominated part is excluded. This inconsistency hampers monitoring efficiency and biodiversity conservation efforts. During the International Polar Year, a large international research project on the forest–tundra ecotone established numerous sites around the circumpolar north where causes and consequences of vegetation change were analyzed. This network of sites and data forms an excellent basis for necessary monitoring of the spatial and temporal complexity of forest encroachment into tundra and its relation to arctic biodiversity. en_CA
dc.description.provenance Submitted by Sherry Briere (sherry.briere@smu.ca) on 2020-09-28T13:32:48Z No. of bitstreams: 1 Harper_Karen_A_article_2012_a.pdf: 1093759 bytes, checksum: ad4013fee838487ba2da6d0cb6084399 (MD5) en
dc.description.provenance Made available in DSpace on 2020-09-28T13:32:48Z (GMT). No. of bitstreams: 1 Harper_Karen_A_article_2012_a.pdf: 1093759 bytes, checksum: ad4013fee838487ba2da6d0cb6084399 (MD5) Previous issue date: 2012-05-23 en
dc.language.iso en en_CA
dc.publisher Taylor & Francis en_CA
dc.relation.uri https://doi.org/10.1080/14888386.2012.700560
dc.rights This is an Accepted Manuscript of an article published by Taylor & Francis in Biodiversity on 10 October, 2012, available online: http://www.tandfonline.com/10.1080/14888386.2012.700560.
dc.subject.lcsh Biodiversity -- Arctic regions
dc.subject.lcsh Ecotones -- Arctic regions
dc.subject.lcsh Taiga ecology -- Arctic regions
dc.subject.lcsh Tundra ecology -- Arctic regions
dc.subject.lcsh Climatic changes -- Arctic regions
dc.title The role of the circumarctic forest–tundra ecotone for Arctic biodiversity en_CA
dc.type Text en_CA
dcterms.bibliographicCitation Biodiversity 13, 174-181. (2012) en_CA
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This is an Accepted Manuscript of an article published by Taylor & Francis in Biodiversity on 10 October, 2012, available online: http://www.tandfonline.com/10.1080/14888386.2012.700560.
 
Published Version: https://doi.org/10.1080/14888386.2012.700560
 
 

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