Abstract
Soil microbes and invertebrates are essential for nutrient cycling, and microbial biomass in soil determines the rate of organic matter turnover. Although soil microbial biomass carbon constitutes only a small percentage of soil organic carbon, e.g. 1.19% in coniferous forest soil (Martikainen and Palojärvi 1990), the contribution of soil microbes to nutrient mineralization is notable. Living trees require a constant supply of mineral nutrients which are formed in the decomposition process carried out by microbes. Consequently, microbes play a major role in silviculture and timber production. In boreal coniferous forests, litter tends to accumulate on the forest floor indicating slow microbial litter decomposition. The rate of decomposition is not limited by the amount of soil organic carbon, which is present in large amounts; in fact the quality of organic matter is more important to decomposers than the quantity. A significant proportion of the soil organic carbon is recalcitrant, and microbial biomass may be limited by the forms of organic carbon present rather than by the absolute amount (Wardle 1992).
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Pietikäinen, J., Fritze, H. (1996). Soil Microbial Biomass: Determination and Reaction to Burning and Ash Fertilization. In: Goldammer, J.G., Furyaev, V.V. (eds) Fire in Ecosystems of Boreal Eurasia. Forestry Sciences, vol 48. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-8737-2_29
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DOI: https://doi.org/10.1007/978-94-015-8737-2_29
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