Arctic soil respiration and microbial community structure driven by silicon and calcium
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Arctic soil respiration and microbial community structure driven by silicon and calcium. / Stimmler, Peter; Priemé, Anders; Elberling, Bo; Goeckede, Mathias; Schaller, Joerg.
I: Science of the Total Environment, Bind 838, Nr. 2, 156152, 2022.Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
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T1 - Arctic soil respiration and microbial community structure driven by silicon and calcium
AU - Stimmler, Peter
AU - Priemé, Anders
AU - Elberling, Bo
AU - Goeckede, Mathias
AU - Schaller, Joerg
N1 - CENPERM[2022] Publisher Copyright: © 2022 Elsevier B.V.
PY - 2022
Y1 - 2022
N2 - Global warming is most pronounced in the Arctic region. Greenhouse gas (GHG) release from Arctic soils increase due to global warming. By this, the Arctic may change from currently being a carbon sink to a future source. To improve accurate predictions of future GHG release from Arctic soils, it is important to unravel factors controlling both the microbial community structure and activity. Soil microbial activity is important for Arctic greenhouse gas production, but depends on soil conditions such as salinity being increased by calcium (Ca) and decreased by amorphous silica (Si) potentially enhancing water availability. In the Arctic, climate changes may alter salinity by changing Si and Ca concentrations upon permafrost thaw as a result of global warming with Si potentially decreasing and Ca potentially increasing salinity. Here, we show that higher Si concentration increased and higher Ca concentrations decreased the microbial CO2 production for both a salt-poor and a salt-rich soil from Greenland. In the salt-rich soil, Si amendment increased CO2 production and the abundance of gram-negative bacteria. However, the bacterial community became dominated by spore-forming gram-positive Firmicutes and Actinobacteria. The CO2 release from soils was directly affected by the abundance of bacteria and fungi, and their community structure. Our results highlight the importance of the soil Si and Ca concentration on organic carbon turnover by strongly changing microbial abundance and community structure, with consequences for CO2 release in the Arctic. Consequently, Ca and Si and their relation to Arctic soil microbial community structure has to be considered when estimating pan-Arctic carbon budgets.
AB - Global warming is most pronounced in the Arctic region. Greenhouse gas (GHG) release from Arctic soils increase due to global warming. By this, the Arctic may change from currently being a carbon sink to a future source. To improve accurate predictions of future GHG release from Arctic soils, it is important to unravel factors controlling both the microbial community structure and activity. Soil microbial activity is important for Arctic greenhouse gas production, but depends on soil conditions such as salinity being increased by calcium (Ca) and decreased by amorphous silica (Si) potentially enhancing water availability. In the Arctic, climate changes may alter salinity by changing Si and Ca concentrations upon permafrost thaw as a result of global warming with Si potentially decreasing and Ca potentially increasing salinity. Here, we show that higher Si concentration increased and higher Ca concentrations decreased the microbial CO2 production for both a salt-poor and a salt-rich soil from Greenland. In the salt-rich soil, Si amendment increased CO2 production and the abundance of gram-negative bacteria. However, the bacterial community became dominated by spore-forming gram-positive Firmicutes and Actinobacteria. The CO2 release from soils was directly affected by the abundance of bacteria and fungi, and their community structure. Our results highlight the importance of the soil Si and Ca concentration on organic carbon turnover by strongly changing microbial abundance and community structure, with consequences for CO2 release in the Arctic. Consequently, Ca and Si and their relation to Arctic soil microbial community structure has to be considered when estimating pan-Arctic carbon budgets.
KW - Carbon cycle
KW - Greenhouse gas emissions
KW - Halo-tolerance
KW - Microbial community structure
KW - Permafrost
KW - Salinity
KW - Silica
U2 - 10.1016/j.scitotenv.2022.156152
DO - 10.1016/j.scitotenv.2022.156152
M3 - Journal article
C2 - 35609699
AN - SCOPUS:85131042761
VL - 838
JO - Science of the Total Environment
JF - Science of the Total Environment
SN - 0048-9697
IS - 2
M1 - 156152
ER -
ID: 309281247