

Publisher: John Wiley & Sons Inc
E-ISSN: 1939-9170|70|1|105-113
ISSN: 0012-9658
Source: Ecology, Vol.70, Iss.1, 1989-02, pp. : 105-113
Disclaimer: Any content in publications that violate the sovereignty, the constitution or regulations of the PRC is not accepted or approved by CNPIEC.
Abstract
Soils that develop on areas of hydrothermally altered rock in the western Great Basin of Nevada support Sierran conifers, such as Pinus ponderosa, in a desert climate. These soils have low pH (°3.7) and low concentrations of HCO3——extractable P (5.6 mg/g), compared to adjacent brown desert soils supporting sagebrush (Artemisia tridentata) vegetation. The occurrence of Sierran conifers appears to be related to their tolerance of the unusual soil chemistry, high nutrient—use efficiency in growth, high reabsorption of foliar nutrients before leaf abscission, and slow growth rates. Most of these traits appear to be inherent characteristics of evergreen vegetation, and show little acclimation to the nutrient—poor conditions on hydrothermally altered rock. In contrast, plants of the Great Basin sagebrush vegetation are physiologically intolerant of the unusually soils that develop from hydrothermally altered rock and are excluded from such sites.
Related content


Resource‐Use Efficiency and Drought Tolerance In Adjacent Great Basin and Sierran Plants
Ecology, Vol. 72, Iss. 1, 1991-02 ,pp. :






Nutrient Uptake from Enriched Soil Microsites by Three Great Basin Perennials
Ecology, Vol. 75, Iss. 1, 1994-01 ,pp. :