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The Ecology of Plants, Large Mammalian Herbivores, and Drought in Yellowstone National Park
Author(s) -
Frank Douglas A.,
McNaughton Samuel J.
Publication year - 1992
Publication title -
ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.144
H-Index - 294
eISSN - 1939-9170
pISSN - 0012-9658
DOI - 10.2307/1941454
Subject(s) - herbivore , grassland , ecology , shrub , national park , ecosystem , temperate climate , range (aeronautics) , population , habitat , bison bison , biology , materials science , demography , sociology , composite material
The purpose of this study was to examine the effect of abundant native large herbivores on ecosystem function of a spatially and temporally heterogeneous temperate grassland. Net aboveground primary production (ANPP), large herbivore consumption (C), and dung deposit (D), an index of nutrient flow from herbivores to the soil, were measured in grassland ad shrub—grassland habitat on winter, transitional, and summer range used by herbs of elk (Cervus elaphus) and bison (Bison bison) in northern Yellowstone National Park. Temporary exclosures (5—7 per site) were moved ever 4 wk during the snow—free season to determine ANPP and C. Data were collected during 1988, a year of drought and unusually high elk and bison population levels, and 1989, a climatically near—average year, with dramatically fewer elk and bison. All three processes, ANPP, C, and D, varied widely among sites: ANPP range: 16—589 g/m 2 , C range: 0—306 g/m 2 , and D ranged: 0—68 g.m 2 . An average of 45% of ANPP was consumed by herbivores. Production and consumption, and consumption and dung deposition were positively correlated across all sites. In addition, sites were grazed when plants were growing. There was a 19% reduction in ANPP from 1988 to 1989, likely caused by death or injury to plants during the 1988 drought. Drought also appeared to be partially responsible for reductions in elk and bison from 1988 to 1989, which were coincident with declines in C and D. Results indicate direct effects and suggest indirect effects of a single—season drought on grassland function that will persist for several years after the event.