Soil Crust
photo by Minerva Bloom6 067
Organic Abstract of Red Rock Soil Crust in Arizona. Photo study by Minerva Bloom. Crusts contribute to a number of functions in the environment. Because they are concentrated in the top 1 to 4 mm of soil, they primarily effect processes that occur at the land surface or soil-air interface. These include soil stability and erosion, atmospheric nitrogen fixation, nutrient contributions to plants, soil-plant-water relations, infiltration, seedling germination, and plant growth. The lands where crusts occur is used for a wide range of purposes--from grazing and recreation to military uses, and in some places, crops. Ultimately, land managers need to know how the functions of crusts change under different practices. Where the functions of crusts are impaired or eliminated because of land use practices, and are essential to the health of the ecosystem, land managers need guidelines to adapt their practices to protect or restore the functions of crusts.
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A soil crust is a layer of soil whose particles cohere because of organic material including live organisms and what they produce. Soil crusts develop most commonly in arid and semi-arid environments by biological organisms from diverse lineages binding together inorganic and organic portions of the soils. Organisms may include eukaryotic algae and fungi and prokaryotic bacteria including Crinalium epipsammum, a species of cyanobacteria that works with green algae to form crusts on coastal dunes.
Belnap, Jayne, et al. 2001. Biological Soil Crusts: Ecology and Management. U. S. Department of Interior, Bureau of Land Management and U. S. Geological Survey. Technical Reference 1730-2. 118p. [1]
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