Tundra Fire and Vegetation Change along a Hillslope on the Seward Peninsula, Alaska, U.S.A

A 1977 tundra fire burned a hillslope where prefire soils and vegetation ranged from poorly drained moist tussock-shrub tundra on the lower slopes to well-drained dwarf shrub tundra on the back slope and very poorly drained wet sedge meadow on the flat crest. We sampled the vegetation on this slope...

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Published in:	Arctic, antarctic, and alpine research Vol. 36; no. 1; pp. 1 - 10
Main Authors:	Racine, Charles, Jandt, Randi, Meyers, Cynthia, Dennis, John
Format:	Journal Article
Language:	English
Published:	Taylor & Francis 01.02.2004 Institute of Arctic and Alpine Research
Subjects:	Climate change Deciduous shrubs Lichens Permafrost Sedges Shrubs Sloping terrain Subshrubs Tundras Vegetation USA, Alaska
ISSN:	1523-0430, 1938-4246
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Abstract	A 1977 tundra fire burned a hillslope where prefire soils and vegetation ranged from poorly drained moist tussock-shrub tundra on the lower slopes to well-drained dwarf shrub tundra on the back slope and very poorly drained wet sedge meadow on the flat crest. We sampled the vegetation on this slope before the fire and at 8 sites following the fire at irregular intervals from 1 yr to 25 yr. During the first decade after the fire, short-term recovery was dominated by bryophytes, sedges, and grasses from both regrowing sedge tussocks and seedlings. However, during the second and third decade, and by 24 yr after the fire, evergreen (Ledum palustre) and deciduous shrubs (mainly Salix pulchra willow) expanded dramatically so that shrub cover was generally higher than before the fire. Labrador tea has increased by vegetative means on the poorly drained lowest 3 tussock-shrub tundra sites. Upslope on the better-drained and more severely burned tussock-shrub and dwarf shrub tundra sites, willows became established from seed mainly during the first 10 yr after the fire and, based on their relatively large size (0.5–1 m tall) and cover, have grown rapidly during the past 15 to 20 yr. There has been very little or no recovery of Sphagnum moss and fruticose lichens after 24 yr at any site, except for Sphagnum moss in the wet meadow site. The permafrost active layer thickness has diminished to prefire levels at the lower slope tussock-shrub tundra sites but is much greater or degraded completely on the steeper slope, corresponding with the distribution of willow shrub colonization. These changes in tundra vegetation and permafrost following fire suggest that such fires could accelerate the predicted effects of climate warming on ecosystems in the Arctic.
AbstractList	A 1977 tundra fire burned a hillslope where prefire soils and vegetation ranged from poorly drained moist tussock-shrub tundra on the lower slopes to well-drained dwarf shrub tundra on the back slope and very poorly drained wet sedge meadow on the flat crest. We sampled the vegetation on this slope before the fire and at 8 sites following the fire at irregular intervals from 1 yr to 25 yr. During the first decade after the fire, shortterm recovery was dominated by bryophytes, sedges, and grasses from both regrowing sedge tussocks and seedlings. However, during the second and third decade, and by 24 yr after the fire, evergreen (Ledum palustre) and deciduous shrubs (mainly Salix pulchra willow) expanded dramatically so that shrub cover was generally higher than before the fire. Labrador tea has increased by vegetative means on the poorly drained lowest 3 tussock-shrub tundra sites. Upslope on the better-drained and more severely burned tussock-shrub and dwarf shrub tundra sites, willows became established from seed mainly during the first 10 yr after the fire and, based on their relatively large size (0.5-1 m tall) and cover, have grown rapidly during the past 15 to 20 yr. There has been very little or no recovery of Sphagnum moss and fruticose lichens after 24 yr at any site, except for Sphagnum moss in the wet meadow site. The permafrost active layer thickness has diminished to prefire levels at the lower slope tussock-shrub tundra sites but is much greater or degraded completely on the steeper slope, corresponding with the distribution of willow shrub colonization. These changes in tundra vegetation and permafrost following fire suggest that such fires could accelerate the predicted effects of climate warming on ecosystems in the Arctic. A 1977 tundra fire burned a hillslope where prefire soils and vegetation ranged from poorly drained moist tussock-shrub tundra on the lower slopes to well-drained dwarf shrub tundra on the back slope and very poorly drained wet sedge meadow on the flat crest. We sampled the vegetation on this slope before the fire and at 8 sites following the fire at irregular intervals from 1 yr to 25 yr. During the first decade after the fire, short-term recovery was dominated by bryophytes, sedges, and grasses from both regrowing sedge tussocks and seedlings. However, during the second and third decade, and by 24 yr after the fire, evergreen (Ledum palustre) and deciduous shrubs (mainly Salix pulchra willow) expanded dramatically so that shrub cover was generally higher than before the fire. Labrador tea has increased by vegetative means on the poorly drained lowest 3 tussock-shrub tundra sites. Upslope on the better-drained and more severely burned tussock-shrub and dwarf shrub tundra sites, willows became established from seed mainly during the first 10 yr after the fire and, based on their relatively large size (0.5-1 m tall) and cover, have grown rapidly during the past 15 to 20 yr. There has been very little or no recovery of Sphagnum moss and fruticose lichens after 24 yr at any site, except for Sphagnum moss in the wet meadow site. The permafrost active layer thickness has diminished to prefire levels at the lower slope tussock-shrub tundra sites but is much greater or degraded completely on the steeper slope, corresponding with the distribution of willow shrub colonization. These changes in tundra vegetation and permafrost following fire suggest that such fires could accelerate the predicted effects of climate warming on ecosystems in the Arctic. A 1977 tundra fire burned a hillslope where prefire soils and vegetation ranged from poorly drained moist tussock-shrub tundra on the lower slopes to well-drained dwarf shrub tundra on the back slope and very poorly drained wet sedge meadow on the flat crest. We sampled the vegetation on this slope before the fire and at 8 sites following the fire at irregular intervals from 1 yr to 25 yr. During the first decade after the fire, short-term recovery was dominated by bryophytes, sedges, and grasses from both regrowing sedge tussocks and seedlings. However, during the second and third decade, and by 24 yr after the fire, evergreen ( Ledum palustre ) and deciduous shrubs (mainly Salix pulchra willow) expanded dramatically so that shrub cover was generally higher than before the fire. Labrador tea has increased by vegetative means on the poorly drained lowest 3 tussock-shrub tundra sites. Upslope on the better-drained and more severely burned tussock-shrub and dwarf shrub tundra sites, willows became established from seed mainly during the first 10 yr after the fire and, based on their relatively large size (0.5-1 m tall) and cover, have grown rapidly during the past 15 to 20 yr. There has been very little or no recovery of Sphagnum moss and fruticose lichens after 24 yr at any site, except for Sphagnum moss in the wet meadow site. The permafrost active layer thickness has diminished to prefire levels at the lower slope tussock-shrub tundra sites but is much greater or degraded completely on the steeper slope, corresponding with the distribution of willow shrub colonization. These changes in tundra vegetation and permafrost following fire suggest that such fires could accelerate the predicted effects of climate warming on ecosystems in the Arctic.
Author	Meyers, Cynthia Racine, Charles Jandt, Randi Dennis, John
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Cites_doi	10.14430/arctic2133 10.2307/2261664 10.1175/1520-0442(2001)014<0336:SSIIAT>2.0.CO;2 10.1046/j.1365-2486.2000.00337.x 10.1023/A:1005504031923 10.2307/2680083 10.2307/1939337 10.1029/98JD02400 10.2307/1935679 10.2307/1938338 10.2307/1551412 10.1038/35079180 10.1080/15230430.1999.12003306 10.2307/3546421 10.1080/07038992.2001.10854894
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References	Racine (I1523-0430-36-1-1-RACINE3) 1987; 19 Chapin III (I1523-0430-36-1-1-CHAPIN1) 1995; 76 McFadden (I1523-0430-36-1-1-MCFADDEN1) 1998; 103 Serreze (I1523-0430-36-1-1-SERREZE1) 2000; 46 Bret-Harte (I1523-0430-36-1-1-BRETHARTE1) 2001; 82 Vavrek (I1523-0430-36-1-1-VAVREK1) 1999; 31 Fetcher (I1523-0430-36-1-1-FETCHER1) 1984; 65 Racine (I1523-0430-36-1-1-RACINE2) 1985; 38 Hastings (I1523-0430-36-1-1-HASTINGS1) 1989; 12 Sturm (I1523-0430-36-1-1-STURM2) 2001b; 14 Landhausser (I1523-0430-36-1-1-LANDHAUSSER1) 1993; 81 Wein (I1523-0430-36-1-1-WEIN1) 1973; 54 Rupp (I1523-0430-36-1-1-RUPP1) 2000; 6 Hobbie (I1523-0430-36-1-1-HOBBIE1) 1999; 84 Silapaswan (I1523-0430-36-1-1-SILAPASWAN1) 2001; 27 Sturm (I1523-0430-36-1-1-STURM1) 2001a; 411
References_xml	– volume: 38 start-page: 194 issn: 0004-0843 year: 1985 ident: I1523-0430-36-1-1-RACINE2 publication-title: Arctic doi: 10.14430/arctic2133 – volume: 81 start-page: 665 issn: 0022-0477 year: 1993 ident: I1523-0430-36-1-1-LANDHAUSSER1 publication-title: Journal of Ecology doi: 10.2307/2261664 – volume: 14 start-page: 336 issn: 1520-0442 year: 2001b ident: I1523-0430-36-1-1-STURM2 publication-title: Journal of Climate doi: 10.1175/1520-0442(2001)014<0336:SSIIAT>2.0.CO;2 – volume: 6 start-page: 541 issn: 1354-1013 year: 2000 ident: I1523-0430-36-1-1-RUPP1 publication-title: Global Change Biology doi: 10.1046/j.1365-2486.2000.00337.x – volume: 46 start-page: 159 issn: 0165-0009 year: 2000 ident: I1523-0430-36-1-1-SERREZE1 publication-title: Climatic Change doi: 10.1023/A:1005504031923 – volume: 82 start-page: 18 issn: 0012-9658 year: 2001 ident: I1523-0430-36-1-1-BRETHARTE1 publication-title: Ecology doi: 10.2307/2680083 – volume: 76 start-page: 694 issn: 0012-9658 year: 1995 ident: I1523-0430-36-1-1-CHAPIN1 publication-title: Ecology doi: 10.2307/1939337 – volume: 103 start-page: 28947 issn: 0148-0227 year: 1998 ident: I1523-0430-36-1-1-MCFADDEN1 publication-title: Journal of Geophysical Research doi: 10.1029/98JD02400 – volume: 54 start-page: 845 issn: 0012-9658 year: 1973 ident: I1523-0430-36-1-1-WEIN1 publication-title: Ecology doi: 10.2307/1935679 – volume: 65 start-page: 1332 issn: 0012-9658 year: 1984 ident: I1523-0430-36-1-1-FETCHER1 publication-title: Ecology doi: 10.2307/1938338 – volume: 19 start-page: 461 issn: 0004-0851 year: 1987 ident: I1523-0430-36-1-1-RACINE3 publication-title: Arctic and Alpine Research doi: 10.2307/1551412 – volume: 411 start-page: 546 issn: 0028-0836 year: 2001a ident: I1523-0430-36-1-1-STURM1 publication-title: Nature doi: 10.1038/35079180 – volume: 31 start-page: 254 issn: 1523-0430 year: 1999 ident: I1523-0430-36-1-1-VAVREK1 publication-title: Arctic, Antarctic, and Alpine Research doi: 10.1080/15230430.1999.12003306 – volume: 12 start-page: 304 issn: 0105-9327 year: 1989 ident: I1523-0430-36-1-1-HASTINGS1 publication-title: Holarctic Ecology – volume: 84 start-page: 417 issn: 0030-1299 year: 1999 ident: I1523-0430-36-1-1-HOBBIE1 publication-title: Oikos doi: 10.2307/3546421 – volume: 27 start-page: 542 issn: 0703-8992 year: 2001 ident: I1523-0430-36-1-1-SILAPASWAN1 publication-title: Canadian Journal of Remote Sensing doi: 10.1080/07038992.2001.10854894
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SubjectTerms	Climate change Deciduous shrubs Lichens Permafrost Sedges Shrubs Sloping terrain Subshrubs Tundras Vegetation
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Title	Tundra Fire and Vegetation Change along a Hillslope on the Seward Peninsula, Alaska, U.S.A
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