Open AccessNonlinear responses to nitrogen and strong interactions with nitrogen and phosphorus additions drastically alter the structure and function of a high arctic ecosystem
Author(s) -
Arens Seth J. T.,
Sullivan Patrick F.,
Welker Jeffrey M.
Publication year - 2008
Publication title -
journal of geophysical research: biogeosciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2007jg000508
Subject(s) - tundra , ecosystem , arctic vegetation , environmental science , biogeochemical cycle , growing season , shrub , ecosystem respiration , nitrogen , terrestrial ecosystem , nitrogen cycle , ecology , agronomy , chemistry , primary production , biology , organic chemistry
Significant changes in ecosystem CO 2 exchange and vegetation characteristics were observed following multiple additions of nitrogen (N) and factorial additions of N and phosphorus (P) to prostrate dwarf‐shrub, herb tundra in Northwest Greenland. Ecosystem CO 2 exchange and vegetation cover and composition were very sensitive to low rates of N inputs (0.5 g m −2 y −1 ), indicating that even low rates of atmospheric N deposition may alter high arctic ecosystem structure and function. Increasing N addition from 1 to 5 g N m −2 y −1 did not alter CO 2 exchange or vegetation characteristics, suggesting the ecosystem had become N saturated. Factorial additions of both N and P released the ecosystem from N saturation and dramatically increased gross ecosystem photosynthesis (+500%) and ecosystem respiration (+250%), such that the ecosystem switched from a small source of CO 2 to a small sink for CO 2 at midday during the 2005 growing season. Changes in the component fluxes of CO 2 exchange were largely explained by a doubling of the normalized difference vegetation index, a 100% increase in vascular plant cover and dramatic increases in the abundance of several previously rare grass species. Our results clearly demonstrate that high arctic prostrate dwarf‐shrub, herb tundra is highly sensitive to low levels of N addition and that future increases in N deposition or N mineralization will likely lead to change in carbon cycling and vegetation characteristics, but the magnitude of the response will be constrained by P availability.