| Literature DB >> 34314543 |
Lea-Rebekka Tonjer1, Ella Thoen1, Luis Morgado1,2, Synnøve Botnen1, Sunil Mundra1,3, Line Nybakken4, Anders Bryn5, Håvard Kauserud1.
Abstract
Climate change causes upward shift of forest lines worldwide, with consequences on soil biota and carbon (C) sequestration. We here analyse compositional changes in the soil biota across the forest line ecotone, an important transition zone between different ecosystems. We collected soil samples along transects stretching from subalpine mountain birch forests to alpine heath. Soil fungi and micro-eukaryotes were surveyed using DNA metabarcoding of the 18S and ITS2 markers, while ergosterol was used to quantify fungal biomass. We observed a strong shift in the soil biota across the forest line ecotone: Below the forest line, there were higher proportions of basidiomycetes and mucoromycetes, including ectomycorrhizal and saprotrophic fungi. Above, we observed relatively more root-associated ascomycetes, including Archaeorhizomycetes, ericoid mycorrhizal fungi and dark septate endophytes. Ergosterol and percentage C content in soil strongly and positively correlated with the abundance of root-associated ascomycetes. The predominance of ectomycorrhizal and saprotrophic fungi below the forest line likely promote high C turnover, while root-associated ascomycetes above the forest line may enhance C sequestration. With further rise in forest lines, there will be a corresponding shift in the belowground biota, likely leading to enhanced release of soil C. This article is protected by copyright. All rights reserved.Entities:
Keywords: climate change; forest line; mycorrhiza; saprotroph; soil carbon; soil fungi; treeline
Year: 2021 PMID: 34314543 DOI: 10.1111/mec.16095
Source DB: PubMed Journal: Mol Ecol ISSN: 0962-1083 Impact factor: 6.185