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      Fungal biomass development in a chronosequence of land abandonment

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          Ecosystem properties and forest decline in contrasting long-term chronosequences.

          During succession, ecosystem development occurs; but in the long-term absence of catastrophic disturbance, a decline phase eventually follows. We studied six long-term chronosequences, in Australia, Sweden, Alaska, Hawaii, and New Zealand; for each, the decline phase was associated with a reduction in tree basal area and an increase in the substrate nitrogen-to-phosphorus ratio, indicating increasing phosphorus limitation over time. These changes were often associated with reductions in litter decomposition rates, phosphorus release from litter, and biomass and activity of decomposer microbes. Our findings suggest that the maximal biomass phase reached during succession cannot be maintained in the long-term absence of major disturbance, and that similar patterns of decline occur in forested ecosystems spanning the tropical, temperate, and boreal zones.
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            Changes in soil fungal:bacterial biomass ratios following reductions in the intensity of management of an upland grassland

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              Bacterial and fungal abundance and biomass in conventional and no-tillage agroecosystems along two climatic gradients

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                Author and article information

                Journal
                Soil Biology and Biochemistry
                Soil Biology and Biochemistry
                Elsevier BV
                00380717
                January 2006
                January 2006
                : 38
                : 1
                : 51-60
                Article
                10.1016/j.soilbio.2005.04.017
                2cc53545-82b6-4c05-9073-1c34d12f6b78
                © 2006

                http://www.elsevier.com/tdm/userlicense/1.0/

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