1980
DOI: 10.1007/bf01876890
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Human impact on beach and foredune vegetation of North Padre Island, Texas

Abstract: Vehicular and pedestrian traffic decreased top and root production, percent cover, and diversity of vegetation, and modified species composition on beach and foredune areas of Padre Island National Seashore and Nueces County Park. Degradation of vegetal cover was directly related to the type and intensity of traffic; species in heavily trafficked areas represented earlier successional stages than those in comparable undisturbed areas.

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Cited by 15 publications
(12 citation statements)
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“…On the foreshore and at the bases of primary dunes subjected to either long-or short-term heavy vehicular and pedestrian traffic, vegetative growth was inhibited and embryo dune formation was prevented (McAtee and Drawe 1980). This had a pronounced influence on microenvironmental parameters such as average daily wind speed to 1 m above the soil line, evaporation, atmospheric salinity, wind-blown sand, soil salinity, soil pH, soil and air temperatures, bulk density, and soil moisture in the immediate area as well as further landward.…”
Section: Discussionmentioning
confidence: 98%
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“…On the foreshore and at the bases of primary dunes subjected to either long-or short-term heavy vehicular and pedestrian traffic, vegetative growth was inhibited and embryo dune formation was prevented (McAtee and Drawe 1980). This had a pronounced influence on microenvironmental parameters such as average daily wind speed to 1 m above the soil line, evaporation, atmospheric salinity, wind-blown sand, soil salinity, soil pH, soil and air temperatures, bulk density, and soil moisture in the immediate area as well as further landward.…”
Section: Discussionmentioning
confidence: 98%
“…This sand was precipitated out at a greater distance from the tidal areas, not only causing mechanical injury to existing vegetation, but also burying individual plants and causing the deaths of less tolerant species. Species composition differences that decreased diversity and stability among transects at these higher zones (McAtee and Drawe 1980) were attributed partly to this action. The greatest sand deposition occurred at the base of the foredune instead of on the foreshore because the soil of the foreshore was damp from salt spray.…”
Section: Discussionmentioning
confidence: 98%
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