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Carbon distribution in subalpine forests and meadows of the Olympic Mountains, Washington

January 1, 2000

stimates of C storage in mountainous regions are rare. Forest–meadow ecotones in subalpine ecosystems, which contain a mosaic of forests and meadows, may be particularly sensitive to future changes in climate and are therefore important to include in estimates of terrestrial C storage. In this study, we quantified soil C and ecosystem C pools in subalpine forest and meadow soils of the northeastern (NE, dry climate) and southwestern (SW, wet climate) Olympic Mountains. Carbon concentrations of mineral soil are relatively high in upper horizons, ranging from 43 to 142 g kg−1 in NE soils and 27 to 162 g kg−1 in SW soils. Northeastern meadow soils store more C than NE forests ( P = 0.009), while SW forest soils store more C than SW meadows ( P = 0.038) Ecosystem C storage is greater in forests than in meadows. Under a warmer climatic scenario with drier summers and wetter winters, subalpine C storage may decrease in the NE and increase in the SW, and changes in C storage will be closely related to vegetation distribution, ecosystem productivity, decomposition rates, and local disturbance regimes. Because ecosystem processes and associated C storage differ between high- and low-elevation ecosystems, it is important that data from both high- and low-elevation sites are included in estimates of C storage in terrestrial ecosystems.

Publication Year 2000
Title Carbon distribution in subalpine forests and meadows of the Olympic Mountains, Washington
DOI 10.2136/sssaj2000.6451834x
Authors S.J. Prichard, D. L. Peterson, R.D. Hammer
Publication Type Article
Publication Subtype Journal Article
Series Title Soil Science Society of America Journal
Index ID 1016162
Record Source USGS Publications Warehouse
USGS Organization Forest and Rangeland Ecosystem Science Center