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Long-term warming effects on root morphology, root mass distribution, and microbial activity in two dry tundra plant communities in northern Sweden

Björk, Robert G., 1974 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för växt- och miljövetenskaper,Department of Plant and Environmental Sciences,Department of Plant and Environmental Sciences, Göteborg University, Gothenburg, Sweden
Majdi, Hooshang (författare)
Department of Ecology, Swedish University of Agricultural Sciences, Uppsala, Sweden,Biologi
Klemedtsson, Leif, 1953 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för växt- och miljövetenskaper,Department of Plant and Environmental Sciences,Department of Plant and Environmental Sciences, Göteborg University, Gothenburg, Sweden
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Lewis-Jonsson, Lotta, 1982 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för växt- och miljövetenskaper,Department of Plant and Environmental Sciences,Department of Plant and Environmental Sciences, Göteborg University, Gothenburg, Sweden
Molau, Ulf, 1951 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för växt- och miljövetenskaper,Department of Plant and Environmental Sciences,Department of Plant and Environmental Sciences, Göteborg University, Gothenburg, Sweden
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 (creator_code:org_t)
2007-10-12
2007
Engelska.
Ingår i: New Phytologist. - : Wiley. - 0028-646X .- 1469-8137. ; 176:4, s. 862-873
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • center dot Effects of warming on root morphology, root mass distribution and microbial activity were studied in organic and mineral soil layers in two alpine ecosystems over > 10 yr, using open-top chambers, in Swedish Lapland. center dot Root mass was estimated using soil cores. Washed roots were scanned and sorted into four diameter classes, for which variables including root mass (g dry matter (g DM) m(-2)), root length density (RLD; cm cm(-3) soil), specific root length (SRL; m g DM-1), specific root area (SRA; m(2) kg DM-1), and number of root tips m(-2) were determined. Nitrification (NEA) and denitrification enzyme activity (DEA) in the top 10 cm of soil were measured. center dot Soil warming shifted the rooting zone towards the upper soil organic layer in both plant communities. In the dry heath, warming increased SRL and SRA of the finest roots in both soil layers, whereas the dry meadow was unaffected. Neither NEA nor DEA exhibited differences attributable to warming. center dot Tundra plants may respond to climate change by altering their root morphology and mass while microbial activity may be unaffected. This suggests that carbon may be incorporated in tundra soils partly as a result of increases in the mass of the finer roots if temperatures rise.

Ämnesord

NATURVETENSKAP  -- Biologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences (hsv//eng)
NATURVETENSKAP  -- Biologi -- Ekologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences -- Ecology (hsv//eng)

Nyckelord

Arctic
climate change
nitrogen
root biomass
root length density
soil layers
specific root area
specific root length
NORWAY SPRUCE STAND
ENVIRONMENTAL MANIPULATIONS
NITROGEN
MINERALIZATION
ARCTIC TUNDRA
FOREST SOIL
FINE ROOTS
RESPONSES
GROWTH
FIELD
NITRIFICATION
Arctic

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