Desert Biology 1974
DOI: 10.1016/b978-0-12-135902-7.50009-1
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Desert Soils

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Cited by 8 publications
(4 citation statements)
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“…This crust may later be colonized by biological elements to form a microbiotic crust (Scott 1982). Alternatively, a rain-impacted soil crust (Fuller 1974) bonded by silicon or carbonate may become stabilized by a layer of filamentous blue-green algae.…”
Section: Microbiota and Ecosystem Processesmentioning
confidence: 99%
“…This crust may later be colonized by biological elements to form a microbiotic crust (Scott 1982). Alternatively, a rain-impacted soil crust (Fuller 1974) bonded by silicon or carbonate may become stabilized by a layer of filamentous blue-green algae.…”
Section: Microbiota and Ecosystem Processesmentioning
confidence: 99%
“…The present study can only be considered a first step toward the elucidation of organic compounds in semiarid soils. Fuller (1974) observed from the literature that the relatively low humus content of semiarid soils is due chiefly to the activity of a highly biogenic soil process, and not, as previously supposed, to a low amount of vegetative remains entering the soil. The role of individual compounds within the soil system may become quite significant under these conditions.…”
Section: Discussionmentioning
confidence: 79%
“…Soil biological characteristics are severely affected by the often prevalent calcic (CaCOrenriched "petrocalcic" or "caliche"), gypsic, and duripan (silicic) horizons, which form hard, cemented layers, mostly impenetrable by plant roots and restrictive to water movement. Excellent reviews of desert soils have been published by Fuller (1974) and Dregne (1976). The latter publication contains informative listings of comparative international desert-soil classification nomenclature.…”
Section: Soilsmentioning
confidence: 99%