IMPACT4SOIL OpenAire Crossref Microsoft Academic Graph American Midland Naturalist unspecified 2006-04-24 Nitrogen and phosphorus were identified as nutrients limiting the growth of plants in an herbaceous community on serpentine soil. Potassium, sulfur and calcium additions had little or no effect. Nutrients were added, alone and in combination, to plots in the field and to greenhouse pots of serpentine soil containing the annual grasses, Bromus mollis and Vulpia microstachys. The absence of any effect due to added calcium indicates that calcium deficiency is not a universal explanation of the low primary production on serpentine soils. INTRODUCTION Wherever they are found, serpentine soils support a vegetation that differs from that on surrounding nonserpentine soils in productivity, floristic composition and often physiognomy. It is now clear that a considerable degree of variability in physical and chemical properties is found among soils classified as serpentine. Thus the phenomenon cannot be ascribed to a single cause but rather a family of causes that vary in importance from site to site. Most notable among these are low levels of the major nutrients, nitrogen, phosphorus and potassium, low levels of calcium combined with high magnesium, and high concentrations of the potentially toxic elements, nickel, chromium and cobalt (Proctor and Woodell, 1975). Serpentine outcrops are common in the California Coastal Mountains as part of the Franciscan formation (Page, 1966). Among these is an outcrop supporting an herbaceous plant community contained within the Jasper Ridge Biological Preserve. The low productivity and floristic uniqueness of this grassland has been well-documented by McNaughton (1968). The consequences of its low productivity for foliage canopy development and potential light competition were studied by Turitzin (1978). No one, however, has reported on the causes of its low productivity. The present study was undertaken to analyze nutrient limitations to plant growth on this serpentine soil. MATERIALS AND METHODS The Jasper Ridge Biological Preserve occupies half of a low-lying ridge on the eastern side of the Santa Cruz Mountains in San Mateo Co., Calif. The crest of the ridge, which reaches an elevation of 189 m, supports an extensive area of annual grassland. A serpentine outcrop, obliquely bisecting the ridge, is occupied by a mixture of annuals and herbaceous perennials. The climate is of the Mediterranean type with warm, dry summers and cool, wet winters. Plants are active from October until May. Nutrient limitations to productivity in the field were studied on experimental plots arranged in a randomized complete blocks design (Sokal and Rohlf, 1969). Treatments were applied to nine 0.25m2 square plots arranged in 1 x 2.5 m blocks that included an untreated control plot. Blocks were replicated six times. Nutrient supplements were applied on 12 January and 12 March 1975. On each occasion nitrogen, phosphorus or potassium, or various combinations were added as solutions of reagent grade NH4NO3 (28.6g m2),. NaH2PO4 * H20 (19.4g m-2) and K2S04 (18.5g m2). Calcium applied as powdered agricultural grade gypsum (calcium sulfate, 1OOg m-2) was added in January only. Aboveground biomass contained within a 0.09 m2 quadrat was harvested from the center of each plot during late April. 'Present address: University Honors Program and School of Life and Health Sciences, University of Delaware, Newark 1971 1. 0106 biological sciences 2. Zero hunger 0401 agriculture, forestry, and fisheries 04 agricultural and veterinary sciences 15. Life on land 01 natural sciences Stephen N. Turitzin 1982-01-01 journalpaper Nitrogen and phosphorus were identified as nutrients limiting the growth of plants in an herbaceous community on serpentine soil. Potassium, sulfur and calcium additions had little or no effect. Nutrients were added, alone and in combination, to plots in the field and to greenhouse pots of serpentine soil containing the annual grasses, Bromus mollis and Vulpia microstachys. The absence of any effect due to added calcium indicates that calcium deficiency is not a universal explanation of the low primary production on serpentine soils. INTRODUCTION Wherever they are found, serpentine soils support a vegetation that differs from that on surrounding nonserpentine soils in productivity, floristic composition and often physiognomy. It is now clear that a considerable degree of variability in physical and chemical properties is found among soils classified as serpentine. Thus the phenomenon cannot be ascribed to a single cause but rather a family of causes that vary in importance from site to site. Most notable among these are low levels of the major nutrients, nitrogen, phosphorus and potassium, low levels of calcium combined with high magnesium, and high concentrations of the potentially toxic elements, nickel, chromium and cobalt (Proctor and Woodell, 1975). Serpentine outcrops are common in the California Coastal Mountains as part of the Franciscan formation (Page, 1966). Among these is an outcrop supporting an herbaceous plant community contained within the Jasper Ridge Biological Preserve. The low productivity and floristic uniqueness of this grassland has been well-documented by McNaughton (1968). The consequences of its low productivity for foliage canopy development and potential light competition were studied by Turitzin (1978). No one, however, has reported on the causes of its low productivity. The present study was undertaken to analyze nutrient limitations to plant growth on this serpentine soil. MATERIALS AND METHODS The Jasper Ridge Biological Preserve occupies half of a low-lying ridge on the eastern side of the Santa Cruz Mountains in San Mateo Co., Calif. The crest of the ridge, which reaches an elevation of 189 m, supports an extensive area of annual grassland. A serpentine outcrop, obliquely bisecting the ridge, is occupied by a mixture of annuals and herbaceous perennials. The climate is of the Mediterranean type with warm, dry summers and cool, wet winters. Plants are active from October until May. Nutrient limitations to productivity in the field were studied on experimental plots arranged in a randomized complete blocks design (Sokal and Rohlf, 1969). Treatments were applied to nine 0.25m2 square plots arranged in 1 x 2.5 m blocks that included an untreated control plot. Blocks were replicated six times. Nutrient supplements were applied on 12 January and 12 March 1975. On each occasion nitrogen, phosphorus or potassium, or various combinations were added as solutions of reagent grade NH4NO3 (28.6g m2),. NaH2PO4 * H20 (19.4g m-2) and K2S04 (18.5g m2). Calcium applied as powdered agricultural grade gypsum (calcium sulfate, 1OOg m-2) was added in January only. Aboveground biomass contained within a 0.09 m2 quadrat was harvested from the center of each plot during late April. 'Present address: University Honors Program and School of Life and Health Sciences, University of Delaware, Newark 1971 1. Nutrient Limitations To Plant-Growth In A California Serpentine Grassland 10.2307/2425191 https://doi.org/10.2307/2425191