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Decomposition at multiple spatial scales in oak savanna. DeForest, Jared*,1, Noormets, Asko1, Tenney, Gwen1, Chen, Jiquan1, 1 Earth, Ecological, and Environmental Sciences, Toledo, OH ABSTRACT- Accurate measurements of decomposition rates are important to estimate ecosystem C cycling. However, we poorly understand if leaf (cm2) mass loss can be scaled-up to the forest floor (m2), and landscape (km2) scale. Because mass loss can correspond with soil respiration (Rsoil), which is closely linked with ecosystem respiration (RE), we reason mass loss can be estimated at the landscape-scale. We tested our hypothesis in an oak savanna in northwest Ohio from November to February (90 days) to minimize respiration from plants. Rsoil was estimated using a temperature-dependent model and RE was measured by eddy-covariance. Leaf mass loss was measured using litter bags, whereas forest floor mass loss was determined by sequential harvesting. Landscape mass loss was estimated from RE using the relationship between forest floor mass loss and Rsoil. Mass loss (%) from litter bags strongly (r2 = 0.97) correlated with forest floor % mass loss. Moreover, forest floor leaf mass loss (%) was correlated (r2 = 0.88) with Rsoil. Estimates of leaf litter mass loss for 90 days was 14% from litter bags, 40% for forest floor, and 37% at the landscape-scale. Results suggest that short-term decomposition from leaf litter bags may underestimates decomposition by 35% when compared to decomposition in the forest floor. Identifying and understanding the behavior of the respiration sources at different spatial scales will allow the use small-scale measurements for scaling landscape-level C fluxes. Key words: carbon cycling, decomposition, landscape ecology, winter ecology |
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