Soil microbial respiration in arctic soil does not acclimate to temperature.
about
Living roots magnify the response of soil organic carbon decomposition to temperature in temperate grasslandThermal adaptation of decomposer communities in warming soils.Temperature sensitivity of soil respiration rates enhanced by microbial community response.Biotic interactions mediate soil microbial feedbacks to climate change.Stronger warming effects on microbial abundances in colder regions.Vascular plants promote ancient peatland carbon loss with climate warmingSimilar temperature responses suggest future climate warming will not alter partitioning between denitrification and anammox in temperate marine sediments.The Role of Microbial Community Composition in Controlling Soil Respiration Responses to TemperatureTemperature response of soil respiration largely unaltered with experimental warming.Organic matter flow in the food web at a temperate heath under multifactorial climate change.Plant-soil interactions in a changing world.Positive climate feedbacks of soil microbial communities in a semi-arid grassland.Thermal acclimation in widespread heterotrophic soil microbes.Soil microbial responses to warming and increased precipitation and their implications for ecosystem C cycling.Temperature responses of carbon monoxide and hydrogen uptake by vegetated and unvegetated volcanic cindersThe sensitivity of soil respiration to soil temperature, moisture, and carbon supply at the global scale.Effects of Soil Temperature and Moisture on Soil Respiration on the Tibetan PlateauShifts in microbial trophic strategy explain different temperature sensitivity of CO2 flux under constant and diurnally varying temperature regimes.Microbial functional potential and community composition in permafrost-affected soils of the NW Canadian Arctic.Temperature adaptation of bacterial communities in experimentally warmed forest soils.Temperature sensitivity and enzymatic mechanisms of soil organic matter decomposition along an altitudinal gradient on Mount Kilimanjaro.How interactions between microbial resource demands, soil organic matter stoichiometry, and substrate reactivity determine the direction and magnitude of soil respiratory responses to warming.Input of easily available organic C and N stimulates microbial decomposition of soil organic matter in arctic permafrost soil.Microbial physiology and soil CO2 efflux after 9 years of soil warming in a temperate forest - no indications for thermal adaptations.Does declining carbon-use efficiency explain thermal acclimation of soil respiration with warming?Ectomycorrhizal fungi slow soil carbon cycling.Environmental parameters altered by climate change affect the activity of soil microorganisms involved in bioremediation.High arctic heath soil respiration and biogeochemical dynamics during summer and autumn freeze-in - effects of long-term enhanced water and nutrient supply.Soil organic matter turnover is governed by accessibility not recalcitranceIntegrating microbial ecology into ecosystem models: challenges and prioritiesTemperature and soil organic matter decomposition rates - synthesis of current knowledge and a way forwardDirect and indirect effects of climate change on soil microbial and soil microbial-plant interactions: What lies ahead?Microbial temperature sensitivity and biomass change explain soil carbon loss with warmingReduction of the temperature sensitivity of soil organic matter decomposition with sustained temperature increaseChanges in Arctic marine bacterial carbon metabolism in response to increasing temperatureLong-term experimentally deepened snow decreases growing-season respiration in a low- and high-arctic tundra ecosystemActivity of temperate grassland plants and symbiotic fungi during the winter - implications for community structure and carbon cycling in a changing climateAdaptation of soil microbial communities to temperature: comparison of fungi and bacteria in a laboratory experimentResponses to increases in temperature of heterotrophic micro-organisms in soils from the maritime AntarcticHow do enzymes catalysing soil nitrogen transformations respond to changing temperatures?
P2860
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P2860
Soil microbial respiration in arctic soil does not acclimate to temperature.
description
2008 nî lūn-bûn
@nan
2008 թուականի Յուլիսին հրատարակուած գիտական յօդուած
@hyw
2008 թվականի հուլիսին հրատարակված գիտական հոդված
@hy
2008年の論文
@ja
2008年論文
@yue
2008年論文
@zh-hant
2008年論文
@zh-hk
2008年論文
@zh-mo
2008年論文
@zh-tw
2008年论文
@wuu
name
Soil microbial respiration in arctic soil does not acclimate to temperature.
@ast
Soil microbial respiration in arctic soil does not acclimate to temperature.
@en
type
label
Soil microbial respiration in arctic soil does not acclimate to temperature.
@ast
Soil microbial respiration in arctic soil does not acclimate to temperature.
@en
prefLabel
Soil microbial respiration in arctic soil does not acclimate to temperature.
@ast
Soil microbial respiration in arctic soil does not acclimate to temperature.
@en
P2093
P1433
P1476
Soil microbial respiration in arctic soil does not acclimate to temperature.
@en
P2093
David W Hopkins
Iain P Hartley
Martin Sommerkorn
Philip A Wookey
P304
P356
10.1111/J.1461-0248.2008.01223.X
P407
P50
P577
2008-07-08T00:00:00Z