Changes in Carbon Storage in Wetlands of the United States: 2011-2016
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Wetland soils contain some of the densest stores of carbon in the biosphere. However, there is little understanding of the quantity and distribution of carbon stored in US wetlands, of the potential effects of human disturbance on these stocks, or how these stocks change over time. Soil carbon was measured to a maximum depth ranging from 90 to 120 cm at approximately 1000 probabilistically selected wetland sites in each of the 2011 and 2016 National Wetland Condition Assessment (NWCA); 207 of the same sites were sampled in both survey years. Preliminary analyses of carbon density from the resampled sites show a median increase of 6.0% in the top 10 cm, while lower in the soil profile (30–60 cm and 60–90 cm), median carbon density decreased (-14.4 and -9.1%, respectively). Significant decreases in soil carbon density over time (i.e., 5 years) deeper in the soil profile parallel results from the 2011 NWCA data, where human disturbance was correlated to lower carbon densities in the deepest (60–90 cm and 90–120 cm) soil layers (Nahlik & Fennessy, 2016, NatComm:13835). These data provide the first empirical, unbiased estimates of change in soil carbon for wetlands of the United States, and demonstrate the power of probabilistic surveys for upscaling data collected at a limited number of sites to regional and national scales. Understanding wetland carbon storage at large scales provides critical insight for the effective management of carbon stocks for climate regulation.