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Deforestation for agriculture increases microbial carbon use efficiency in subarctic soils

GND
1202564755
ORCID
0000-0003-3625-104X
Zugehörigkeit
Thünen Institute of Climate-Smart Agriculture, Bundesallee 68, Brunswick, Germany
Schroeder, Julia;
GND
1239600119
ORCID
0000-0001-7181-7331
Zugehörigkeit
Thünen Institute of Climate-Smart Agriculture, Bundesallee 68, Brunswick, Germany
Peplau, Tino;
ORCID
0000-0003-0679-1045
Zugehörigkeit
Department of Evolutionary Biology and Environmental Studies, University of Zurich, Winterthurerstrasse 190, Zurich, Switzerland
Pennekamp, Frank;
ORCID
0000-0003-3652-2946
Zugehörigkeit
Research and Development Centre, Central Experimental Farm, Agriculture and Agri-Food Canada, 960 Carling Ave, Ottawa, Canada
Gregorich, Edward;
GND
1019148403
ORCID
0000-0003-4861-0214
Zugehörigkeit
Thünen Institute of Biodiversity, Bundesallee 65, Brunswick, Germany
Tebbe, Christoph C.;
GND
1025492234
ORCID
0000-0003-3108-8810
Zugehörigkeit
Thünen Institute of Climate-Smart Agriculture, Bundesallee 68, Brunswick, Germany
Poeplau, Christopher

Agriculture is likely to expand poleward with climate change, encouraging deforestation for agriculture in subarctic regions, which alters soil physical, chemical and biological properties and potentially affects microbial metabolic efficiency. Deciphering how and by which mechanisms land-use change affects microbial carbon use efficiency (CUE) will enable the development of mitigation strategies to alleviate C losses. We assessed CUE using 18O-labelled water in a paired-plot approach on soils collected from 19 farms across the subarctic region of Yukon, Canada, comprising 14 pairs of forest-to-grassland conversion and 15 pairs of forest-to-cropland conversion. Microbial CUE significantly increased following conversion to grassland and cropland. Land-use conversion resulted in a lower estimated abundance of fungi, while the archaeal abundance increased. Interestingly, structural equation modelling revealed that increases in CUE were mediated by a rise in soil pH and a decrease in soil C:N ratio rather than by shifts in microbial community composition, i.e. the ratio of fungi, bacteria and archaea. Our findings indicate a direct control of abiotic factors on microbial CUE via improved nutrient availability and facilitated conditions for microbial growth. Overall, this implies that to a certain extent CUE can be managed to achieve a more efficient build-up of stabilised soil organic C (SOC), as reflected in increased mineral-associated organic C under agricultural land use. These insights may also help constrain SOC models that generally struggle to predict the effects of deforestation, something that is likely to take place more frequently in the subarctic.

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