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Fast growing softwood species such as pine are preferred for biomass-based heat as well as electricity production and stored in large quantities. A newly established outdoor pile of freshly cut pine-wood chips was monitored to analyze exothermic processes. Inside the pile, a mean temperature increase of up to 44 °C was measured after six days of piling which was paralleled by a decrease of O2-concentration and an increase of CO2-concentration. Thereafter four additional CO2 maxima were observed, while O2-concentration remained at ambient concentration. The fungal community structure remained almost unchanged after four weeks, while the bacterial community structure was characterized by continuous shifts over time. The rapid heating in the early stage of storage corresponded to high relative abundance of microbial strains belonging to the genera Pseudomonas, Luteibacter and Caulobacter, ascomycetous genera Sphaeropsis and Cadophora and basidiomycetous order Polyporales and genus Sistotremastrum. The late stage was composed by a broader diversity of microorganisms, and heating processes inside the wood pile were attributed mainly to physicochemical processes. Taken together, these observations suggest that the early bacterial and fungal communities are key players in exothermic processes and were replaced by a broader diversity of highly adapted microorganisms.
Forefields of receding glaciers are unique and sensitive environments representing natural soil chronosequences, where sulfate availability is assumed to be a limiting factor. Bacterial mineralization of organosulfur is an important sulfate-providing process in soils. We analyzed the diversity of sulfonate-desulfurizing (desulfonating) bacteria in the Damma glacier forefield on the basis of the key gene asfA by terminal restriction fragment length polymorphism and clone libraries. The community structure and sequence diversity of desulfonating bacteria differed significantly between forefield soils deglaciated in the 1990s and the 1950s. Soil age had a strong effect on the desulfonating rhizosphere communities of Agrostis rupestris, but only a slight impact on the ones from Leucanthemopsis alpina. AsfA affiliated to Polaromonas sp. was predominantly found in the more recent ice-free soils and the corresponding rhizospheres of A. rupestris, while a group of unidentified sequences was found to be dominating the matured soils and the corresponding rhizospheres of A. rupestris. The desulfonating bacterial diversity was not affected by varying levels of sulfate concentrations. The level of asfA diversity in recently deglaciated soils suggests that desulfonating bacteria are a critical factor in sulfur cycling, with defined groups dominating at different stages of soil formation.