1993
DOI: 10.1016/0009-2541(93)90105-r
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Vegetation-induced, subsurface precipitation of carbonate as an aggradational process in the permanent swamps of the Okavango (delta) fan, Botswana

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Cited by 100 publications
(70 citation statements)
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“…As the trees transpire they leave dissolved solutes behind resulting in salinity increase in the groundwater. As a result of this, salt accumulations occur underneath islands and minimize surface water salinity (McCarthy et al 1994). Similar processes are beginning to be identified in other sub-tropical major wetlands, such as the Everglades (e.g., Wetzel et al 2005, Sullivan et al 2010.…”
Section: Introductionmentioning
confidence: 85%
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“…As the trees transpire they leave dissolved solutes behind resulting in salinity increase in the groundwater. As a result of this, salt accumulations occur underneath islands and minimize surface water salinity (McCarthy et al 1994). Similar processes are beginning to be identified in other sub-tropical major wetlands, such as the Everglades (e.g., Wetzel et al 2005, Sullivan et al 2010.…”
Section: Introductionmentioning
confidence: 85%
“…Ecosystem services performed by riparian tree species include primary production which produces food, nutrient cycling (Murkin 1998) and water purification through the process of evapotranspiration (McCarthy et al 1994). Riparian tree species hold the soil together through their roots which helps to reduce erosion due to floods (Carter 1996).…”
Section: Introductionmentioning
confidence: 99%
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“…Once an island nucleus has thus formed, it grows by chemical precipitation, a process driven by the high evapotranspiration by trees on island fringes. The growth of islands is believed to occur by expansion in the soil within the vegetated fringes as a result of the precipitation of calcium carbonate and silica from the groundwater as the salinity of the water rises due to evapotranspirational loss of groundwater (McCarthy et al, 1993a). Evapotranspiration of groundwater also leads to a build-up of the more soluble salts and ultimately the formation of salt crusts (trona) on the islands.…”
Section: Study Areamentioning
confidence: 99%
“…The region is characterized by extremely low local relief, with a maximum relief of no more than 2 to 3 m (e.g. McCarthy et al, 1993a;Gumbricht et al, 2001). The average relief is much lower, and in kilometre-long transects, the standard deviation on elevation is typically around 50 cm.…”
Section: Introductionmentioning
confidence: 99%