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Community adaptation to temperature explains abrupt soil bacterial community shift along a geothermal gradient on Iceland

Weedon, James T. (författare)
Vrije Universiteit Amsterdam
Bååth, Erland (författare)
Lund University,Lunds universitet,MEMEG,Biologiska institutionen,Naturvetenskapliga fakulteten,BECC: Biodiversity and Ecosystem services in a Changing Climate,Centrum för miljö- och klimatvetenskap (CEC),Mikrobiologisk ekologi,Forskargrupper vid Lunds universitet,Department of Biology,Faculty of Science,Centre for Environmental and Climate Science (CEC),Microbial Ecology,Lund University Research Groups
Rijkers, Ruud (författare)
Vrije Universiteit Amsterdam
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Reischke, Stephanie (författare)
Lund University,Lunds universitet,Biologiska institutionen,Naturvetenskapliga fakulteten,Mikrobiologisk ekologi,Forskargrupper vid Lunds universitet,Department of Biology,Faculty of Science,Microbial Ecology,Lund University Research Groups
Sigurdsson, Bjarni D. (författare)
Agricultural University of Iceland
Oddsdottir, Edda (författare)
Icelandic Forest Research
van Hal, Jurgen (författare)
Vrije Universiteit Amsterdam
Aerts, Rien (författare)
Vrije Universiteit Amsterdam
Janssens, Ivan A. (författare)
University of Antwerp
van Bodegom, Peter M. (författare)
Leiden University
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 (creator_code:org_t)
Elsevier BV, 2023
2023
Engelska 11 s.
Ingår i: Soil Biology and Biochemistry. - : Elsevier BV. - 0038-0717. ; 177
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Understanding how and why soil microbial communities respond to temperature changes is important for understanding the drivers of microbial distribution and abundance. Studying soil microbe responses to warming is often made difficult by concurrent warming effects on soil and vegetation and by a limited number of warming levels preventing the detection of non-linear effects. A unique area in Iceland, where soil temperatures have recently increased due to geothermic activity, created a stable warming gradient in both grassland (dominated by Agrostis capillaris) and forest (Picea sitchensis) vegetation. By sampling soils which had been subjected to four years of temperature elevation (ambient (MAT 5.2 °C) to +40 °C), we investigated the shape of the response of soil bacterial communities to warming, and their associated community temperature adaptation. We used 16S rRNA amplicon sequencing to profile bacterial communities, and bacterial growth-based assays (3H-Leu incorporation) to characterize community adaptation using a temperature sensitivity index (SI, log (growth at 40 °C/4 °C)). Despite highly dissimilar bacterial community composition between the grassland and forest, they adapted similarly to warming. SI was 0.6 (equivalent to a minimum temperature for growth of between −6 and −7 °C) in both control plots. Both diversity and community composition, as well as SI, showed similar threshold dynamics along the soil temperature gradient. There were no significant changes up to soil warming of 6–9 °C above ambient, beyond which all indices shifted in parallel, with SI increasing from 0.6 to 1.5. The consistency of these responses provide evidence for an important role for temperature as a direct driver of bacterial community shifts along soil temperature gradients.

Ämnesord

LANTBRUKSVETENSKAPER  -- Lantbruksvetenskap, skogsbruk och fiske -- Markvetenskap (hsv//swe)
AGRICULTURAL SCIENCES  -- Agriculture, Forestry and Fisheries -- Soil Science (hsv//eng)

Nyckelord

Bacterial growth
Geothermic gradient
Soil bacterial community
Temperature adaptation
Threshold

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