5 ) was associated with highly significant increases in the relative abundance of Ascomycota classes Sordariomycetes and Dothideomycetes, which increased by 329% and 433% (respectively) in the deeper soils and by 182% and 198% (respectively) in the surface soils (Fig. 6 B).
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Conversion of boreal forests to agricultural systems: soil microbial responses along a land-conversion chronosequence.
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