Ecological Applications · 1996 · 195 citations · 43 references
Life SciencesEcologySoil SciencesSoil EcologySoil ScienceTerrestrial EcologyGrassland EcologyGrazing EcologyGrazing Impacts On SoilGrazing PressureSoil - Vegetation InteractionsSuccession EcologyGrazing Effects On CompositionGrazing Effects On SoilsGrazing-habitat InteractionsNative Species DiversityPost-grazing SuccessionSoil Disturbance PatternsSpecies Composition StabilitySuccessional Species Composition
Grasslands at the Hastings Natural History Reservation (HNHR) and in adjacent Santa Lucia coastal range of Monterey County, California were sampled from 1971 to 1991. Grasslands on HNHR showed two distinct and stable associations: stands with and without historical cultivation (≈ 1865‐1937$). Relict stands dominated by native, perennial grasses (e.g., Nassella pulchra, Poa secunda) are limited to uncultivated, steeper stands, often where soils have more clay. Abandoned agricultural fields have stable compositions dominated by Avena fatua, Bromus mollis, B. diandrus, Erodium spp., Hypochaeris glabra, Vulpia spp., Eremocarpus setigerus, and Amsinckia spp. Patterns in species composition were associated with gradients in soil texture, gopher abundance, and slope. Gophers provide a significant and continuous source of soil disturbance and may slow successional processes in old fields. Where gophers are excluded, aboveground biomass accumulates. Germination and establishment of native perennial grasses (compared to introduced, annual grasses) are reduced on gopher tailings in old fields. Species composition patterns reflecting past cultivation on both grazed and ungrazed stands are apparent. Relict (uncultivated) stands of native grasses persist under many historical levels of grazing. Effects of grazing are often only seen on old fields, and not on relict grasslands. Compared to stands where grazing was removed in 1937, stands currently or recently grazed by cattle show higher soil nitrogen, but reductions in cover of gopher tailings, species diversity, soil phosphate, and sulphate.
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