Microbial community composition shapes enzyme patterns in topsoil and subsoil horizons along a latitudinal transect in Western Siberia

• Main Authors: Schnecker, Jörg, Wild, Birgit, Takriti, Mounir, Alves, Ricardo J. Eloy, Gentsch, Norman, Gittel, Antje, Hofer, Angelika, Klaus, Karoline, Knoltsch, Anna, Lashchinskiy, Nikolay, Mikutta, Robert, Richter, Andreas
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Oxford : Pergamon-Elsevier Science Ltd 2015
• Subjects: extracellular enzymes; plfa; tundra; boreal forests; steppe; permafrost; soil organic-matter; mycorrhizal fungi; forest soils; decomposition; nitrogen; carbon; dynamics; litter; depth; ectomycorrhizal; Dewey Decimal Classification500 | Naturwissenschaften; Dewey Decimal Classification500 | Naturwissenschaften570 | Biowissenschaften, Biologie; Dewey; Tundra; Siberia
• Online Access: https://dx.doi.org/10.15488/484; http://www.repo.uni-hannover.de/handle/123456789/508

Soil horizons below 30 cm depth contain about 60% of the organic carbon stored in soils. Although insight into the physical and chemical stabilization of soil organic matter (SUM) and into microbial community composition in these horizons is being gained, information on microbial functions of subsoil microbial communities and on associated microbially-mediated processes remains sparse. To identify possible controls on enzyme patterns, we correlated enzyme patterns with biotic and abiotic soil parameters, as well as with microbial community composition, estimated using phospholipid fatty acid profiles. Enzyme patterns (i.e. distance-matrixes calculated from these enzyme activities) were calculated from the activities of six extracellular enzymes (cellobiohydrolase, leucine-amino-peptidase, N-acetylglucosaminidase, chitotriosidase, phosphatase and phenoloxidase), which had been measured in soil samples from organic topsoil horizons, mineral topsoil horizons, and mineral subsoil horizons from seven ecosystems along a 1500 km latitudinal transect in Western Siberia. We found that hydrolytic enzyme activities decreased rapidly with depth, whereas oxidative enzyme activities in mineral horizons were as high as, or higher than in organic topsoil horizons. Enzyme patterns varied more strongly between ecosystems in mineral subsoil horizons than in organic topsoils. The enzyme patterns in topsoil horizons were correlated with SUM content (i.e., C and N content) and microbial community composition. In contrast, the enzyme patterns in mineral subsoil horizons were related to water content, soil pH and microbial community composition. The lack of correlation between enzyme patterns and SUM quantity in the mineral subsoils suggests that SOM chemistry, spatial separation or physical stabilization of SUM rather than SUM content might determine substrate availability for enzymatic breakdown. The correlation of microbial community composition and enzyme patterns in all horizons, suggests that microbial community composition shapes enzyme patterns and might act as a modifier for the usual dependency of decomposition rates on SUM content or C/N ratios.