Full TGIF Record # 315286
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DOI:10.1016/j.soilbio.2020.107826
Web URL(s):https://www.sciencedirect.com/science/article/pii/S0038071720301231
    Last checked: 11/05/2020
    Access conditions: Item is within a limited-access website
https://www.sciencedirect.com/science/article/pii/S0038071720301231/pdfft
    Last checked: 11/05/2020
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Publication Type:
i
Refereed
Author(s):Zhang, Jing; Ekblad, Alf; Sigurdsson, Bjarni D.; Wallander, H^Doakan
Author Affiliation:Zhang: Department of Biology, Lund University, Lund, Sweden and Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China; Ekblad: School of Science and Technology, Örebro University, Örebro, Sweden; Sigurdsson: Faculty of Natural Resources and Environmental and Forest Sciences, Agricultural University of Iceland, Hvanneyri, Borgarnes, Iceland; Wallander: Department of Biology, Lund University, Lund, Sweden
Title:The influence of soil warming on organic carbon sequestration of arbuscular mycorrhizal fungi in a sub-arctic grassland
Source:Soil Biology & Biochemistry. Vol. 147, August 2020, p. 44205.
Publishing Information:Amsterdam, The Netherlands: Elsevier
# of Pages:9
Related Web URL:https://www.sciencedirect.com/science/article/pii/S0038071720301231#abs0010
    Last checked: 11/05/2020
    Notes: Abstract only
Keywords:Author-Supplied Keywords: Arbuscular mycorrhizal fungi; Geothermal warming; Fungal biomass; Fungal necromass; Glomalin-related soil protein; Ingrowth mesh bags
Abstract/Contents:"A substantial portion of grassland photosynthates is allocated belowground to arbuscular mycorrhizal fungi (AMF), but controversy remains about whether this carbon (C) contributes to soil organic carbon (SOC) under warming. The goal of this study was to investigate how AMF biomass and C sequestered by AMF (CNew) re influenced by soil warming. We estimated the AMF biomass and CNew, assumed to be mostly AMF necromass, in mycelial ingrowth bags buried for 1, 2, or 3 years in soil under warming (~+0.5-16.4 °C). The AMF biomass had a positive, curvilinear response to warming gradients after one year of burial. About 107 g C m-2 of CNew accumulated over the three years and ~12% of this C was from glomalin-related soil protein. Modelling suggested the production rate of AMF biomass was 153 g C m-2 yr-1 with a rapid (36-65 days) turnover while AMF necromass turnover was much slower (1.4 ± 0.2 yr-1). Warming duration (7-9 years vs. > 50 years) did not have significant influence on AMF biomass or CNew (P > 0.05). Our results suggest that AMF are more tolerant to increases in temperature than other microbes or fine roots. The dramatic loss of soil C and stable soil aggregates under warming found earlier at this site were not attributed to a decrease in AMF biomass or CNew. Despite a low AMF standing biomass, its contribution to SOC may be substantial."
Language:English
References:72
Note:Tables
Graphs
ASA/CSSA/SSSA Citation (Crop Science-Like - may be incomplete):
Zhang, J., A. Ekblad, B. D. Sigurdsson, and H. Wallander. 2020. The influence of soil warming on organic carbon sequestration of arbuscular mycorrhizal fungi in a sub-arctic grassland. Soil Biol. Biochem. 147:p. 44205.
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DOI: 10.1016/j.soilbio.2020.107826
Web URL(s):
https://www.sciencedirect.com/science/article/pii/S0038071720301231
    Last checked: 11/05/2020
    Access conditions: Item is within a limited-access website
https://www.sciencedirect.com/science/article/pii/S0038071720301231/pdfft
    Last checked: 11/05/2020
    Requires: PDF Reader
    Access conditions: Item is within a limited-access website
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