An Overview of the Implications of Global Change for Natural and Managed Terrestrial Ecosystems

dc.contributor.authorWalker, Brian H.en_US
dc.contributor.authorSteffen, Willen_US
dc.date.accessioned2009-07-31T15:00:32Z
dc.date.available2009-07-31T15:00:32Z
dc.date.issued1997en_US
dc.date.submitted2008-10-31en_US
dc.date.submitted2008-10-31en_US
dc.description.abstract"Global change is the net effect of individual and interactive effects of changes in land use, atmospheric composition, biological diversity, and climate. A synthesis of the past six years' activities of the Global Change and Terrestrial Ecosystems project of the IGBP (International Geosphere-Biosphere Programme) deals with global change effects as ecosystem responses and living with global change. Ecosystem responses are considered in terms of changes in function and vegetation composition/structure. Field experiments of elevated CO2 effects on aboveground biomass show, on average, a positive effect on biomass, ranging from -20% to +80%. Some early predictions of CO2 effects (C3 vs. C4 plants, N-fixers, C:N in litter) are not generally supported, and it is necessary to consider the interactive effects of changes in CO2, temperature, and nitrogen. Dynamic global vegetation models involving transient changes show that biomes will not shift as intact entities. Significant changes in vegetation, especially in high latitudes, are likely over the next century, and changes in disturbance regimes will be most important. Based on forecast changes in land use, vegetation structure, and ecosystem physiology, the terrestrial biosphere will probably become a source rather than a sink for carbon over the next century. "Because of land use change, the terrestrial biosphere of the 21st century will probably be further impoverished in species richness and substantially reorganized. More natural ecosystems will be in an early successional state or converted to production systems. The biosphere will be generally weedier and structurally simpler, with fewer areas in an ecologically complex old-growth state. "Temperate crop production will probably increase slightly because of CO2 increases (5-7% for wheat for average field conditions), but crop production in the tropics may decline in some areas. Land use change will have the greatest effect on pastures and rangelands; due to a required >2% annual increase in crop production to meet the expanding human population, there will be increased incursion of cropland into rangelands."en_US
dc.identifier.citationjournalEcology and Societyen_US
dc.identifier.citationmonthDecemberen_US
dc.identifier.citationnumber2en_US
dc.identifier.citationvolume1en_US
dc.identifier.urihttps://hdl.handle.net/10535/3389
dc.subjectglobal changeen_US
dc.subjectagricultureen_US
dc.subjectclimateen_US
dc.subjectland tenure and useen_US
dc.subject.sectorAgricultureen_US
dc.subject.sectorLand Tenure & Useen_US
dc.titleAn Overview of the Implications of Global Change for Natural and Managed Terrestrial Ecosystemsen_US
dc.typeJournal Articleen_US
dc.type.publishedpublisheden_US

Files

Original bundle

Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
30.pdf
Size:
402.59 KB
Format:
Adobe Portable Document Format

Collections