6 Conclusions
Soil microorganisms, particularly the rhizosphere flora of higher plants, remarkably affect the phosphorus bioavailability in soils. Microbially derived carboxylic acids mobilize calcium phosphates as well as iron- and aluminum-bound phosphorus. Microbial mineralization of organic matter is essential for nutrient cycling in soils and phosphatases enhance the use of organic P compounds by higher plants. Plants, especially in nutrient-poor habitats like forest ecosystems, often depend on symbiotic relations with microorganisms like mycorrhizal fungi. However, rhizosphere flora also decomposes P-mobilizing substances derived from plant roots. Microorganisms can be powerful competitors for growth-limiting nutrients like P, but microbial turnover can also make P available for higher plants. The difficulty in quantifying all these complex and partially contrary processes is a substantial weak point in mathematical P-utilization models as well as in the use of P-mobilizing microbes as biofertilizers. The investigation of these complex effects with modern methods, which cover also the large majority of noncultivable microorganisms, is an important aim for further research.
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Deubel, A., Merbach, W. (2005). Influence of Microorganisms on Phosphorus Bioavailability in Soils. In: Varma, A., Buscot, F. (eds) Microorganisms in Soils: Roles in Genesis and Functions. Soil Biology, vol 3. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-26609-7_9
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