Loss in Soil Organic Carbon Storage in Wetlands Across the United States Over a 5-Year Period
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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 wetlands of the United States (U.S.), or how these stocks change over time. The 2011 and 2016 National Wetland Condition Assessment (NWCA) provides one of the most comprehensive, field-based national wetland databases in the U.S., if not the world, that can be used to quantify carbon storage in U.S. wetland soils and monitor those stores over time. Soil carbon was measured using the same soil pit sampling protocols to a depth of 90 cm in three 30-cm depth increments at approximately 1,000 probabilistically-selected wetland sites in each year. Of these, approximately 200 sites were sampled in both the 2011 and 2016 surveys. Total carbon storage (Pg) and mean carbon density (tC ha-1) for the NWCA target wetland area across the U.S. (38.73 Mha) and for various subpopulations were estimated. We found that over the 5-year study period, there was a consistent trend of organic carbon loss from each 30-cm depth increment, resulting in an estimated loss of 1.055 PgC, or 12.0% of the carbon stock originally measured in 2011. Mean carbon densities for 0-90 cm decreased significantly between 2011 and 2016 from 225.21±14.84 to 197.97±17.65 tC ha-1 (p=0.016). Carbon density losses increased with depth, ranging from -8.2% (7.9 tC ha-1) from 0-30 cm to -16.4% (9.6 tC ha-1) in the deepest soils (61-90 cm). The sites sampled in both years showed a similar pattern of soil carbon loss. There is strong evidence that changes in soil carbon are driven by losses in organic-dominated soils, especially from 0-30 cm (with a decrease of 36.02±16.63 tC ha-1, p<0.001). While our study was not designed to identify the mechanisms of carbon loss, we show possible relationships between regions of the U.S. in which wetland soil carbon densities declined, initial carbon density, and deviation from the 30-year climate normals. These data provide the first empirical estimates of soil carbon change for US wetlands and demonstrate the power of probabilistic surveys for upscaling data collected at a limited number of sites to regional and national scales. These data add to our understanding of wetland carbon storage and loss at large scales, providing critical insight for the effective management of carbon stocks for climate regulation.