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Padre Island, the longest barrier island in the United States, extends for approximately 182 km along the Texas coast. The island is usually divided into two distinct sections, northern Padre Island and southern Padre Island, which are separated by the Mansfield Ship Channel (Fig. 1). The island was formed on a bed of Pleistocene-age sands and gravel and is subject to annual cycles of sediment deposition from the riv¬ ers of Texas and periods of erosion from the actions of waves, wind, and human activities along its length (Baccus and Horton, 1979). The climate of northern Padre Island has been described as subtropical and semiarid, and precipitation, almost always from rain¬ fall, averages from 74 cm at the extreme northern end of Padre Island National Seashore (PINS) to 66 cm at the southern boundary. Average temperature at PINS is 24°C and evaporation rates are high (Weise and White, 1980).

Community relationships of some small mammals on Padre Island National Seashore, Texas