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      LONG-TERM CONSEQUENCES OF DISTURBANCE ON NITROGEN DYNAMICS IN AN ARID ECOSYSTEM

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      Ecology
      Wiley-Blackwell

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          Biological feedbacks in global desertification.

          Studies of ecosystem processes on the Jornada Experimental Range in southern New Mexico suggest that longterm grazing of semiarid grasslands leads to an increase in the spatial and temporal heterogeneity of water, nitrogen, and other soil resources. Heterogeneity of soil resources promotes invasion by desert shrubs, which leads to a further localization of soil resources under shrub canopies. In the barren area between shrubs, soil fertility is lost by erosion and gaseous emissions. This positive feedback leads to the desertification of formerly productive land in southern New Mexico and in other regions, such as the Sahel. Future desertification is likely to be exacerbated by global climate warming and to cause significant changes in global biogeochemical cycles.
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            Nitrogen Saturation in Northern Forest Ecosystems

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              On the Spatial Pattern of Soil Nutrients in Desert Ecosystems

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                Author and article information

                Journal
                Ecology
                Ecology
                Wiley-Blackwell
                0012-9658
                January 1999
                January 1999
                : 80
                : 1
                : 150-160
                Article
                10.1890/0012-9658(1999)080[0150:LTCODO]2.0.CO;2
                4d635841-0101-48ce-8a79-6944694ac666
                © 1999

                http://doi.wiley.com/10.1002/tdm_license_1.1

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