Abstract
The major resources of plant mineral nutrients in all soils exist as complex molecular aggregates from which they must be released before they become available for utilization by the vegetation. Since the rate of nutrient release often limits the primary productivity of an ecosystem, it is of fundamental importance to understand the major processes involved through decomposition and mineralization in the maintenance of nutrient cycling phenomena.
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Read, D.J., Mitchell, D.T. (1983). Decomposition and Mineralization Processes in Mediterranean-Type Ecosystems and in Heathlands of Similar Structure. In: Kruger, F.J., Mitchell, D.T., Jarvis, J.U.M. (eds) Mediterranean-Type Ecosystems. Ecological Studies, vol 43. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-68935-2_12
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