
Microcosm‐based analyses of Scots pine seedling growth, ectomycorrhizal fungal community structure and bacterial carbon utilization profiles in boreal forest humus and underlying illuvial mineral horizons
Author(s) -
Heisalo Jussi,
Jørgensen Kirsten S.,
Sen Robin
Publication year - 2001
Publication title -
fems microbiology ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.377
H-Index - 155
eISSN - 1574-6941
pISSN - 0168-6496
DOI - 10.1111/j.1574-6941.2001.tb00827.x
Subject(s) - biology , rhizosphere , botany , scots pine , ectomycorrhiza , pisolithus , humus , mycorrhiza , ecology , soil water , symbiosis , genetics , bacteria , pinus <genus>
We report on the identity of indigenous mycorrhiza forming fungi and rhizosphere/mycorrhizosphere bacterial community carbon source utilization profiles of Scots pine ( Pinus sylvestris L.) seedlings grown in boreal forest humus (O) or illuvial (B) mineral horizon containing microcosm growth systems. Based on rDNA (ITS)‐RFLP analyses, a total of 10 fungal RFLP taxa were identified from pre‐morphotyped mycorrhizas on 7‐month‐old seedling roots. Hierarchical cluster analysis, including corresponding RFLPs of known fungal species, confirmed root colonization by eight mycorrhizal species. In the O horizon, roots were colonized by e.g. Suillus bovinus , Suillus variegatus , Cenococcum geophilum , Piloderma croceum , Thelephora terrestris and Russula vinicolor . Mycobiont diversity in the mineral B horizon was lower but included Piceirhiza bicolorata and both Suillus species which produced extensive extramatrical mycelium. In comparison to non‐colonized soils, rhizosphere and mycorrhizosphere compartments supported significantly higher numbers of bacteria (mean range 10 8 –10 11 cells g −1 fresh weight (fw)). Specific rhizosphere/mycorrhizosphere ‘niche’‐linked bacterial communities were detected following multivariate analyses (PCA and CA) of bacterial carbon utilization profiles (Biolog® GN microplate). Distinct preferences for amino and carboxylic acids were identified in mineral B horizon rhizospheres whereas a wider range of carbon sources were utilized in the fungal‐dominated mycorrhizospheres irrespective of soil types.