Punching above their weight: Wetlands moderate nutrient delivery to streams despite comprising just 5% of the conterminous US land area
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Wetlands can mediate the transfer of materials between uplands and streams through interception of upland flows and connectivity to receiving streams. We used geospatial data to classify the connectivity of 6.7 million wetlands to 2.6 million stream segments across the conterminous US (CONUS). We defined a flowpath from each wetland to its receiving stream and classified wetland units based on stream proximity (i.e., riparian vs. non-riparian) and likely dominant flow and soil drainage types along these paths (i.e., surface vs. subsurface flow and poorly vs. well-drained soils). 71% of all wetland areas in the CONUS were classified as riparian, making them the dominant class. Further, we delineated each wetland basin to quantify the land area and upland N each receives. Maps of these basins reveal a profound spatial mismatch between the locations of upland N inputs and of intercepting wetlands across the CONUS. Despite this mismatch, wetlands, which comprise just 5% of the landscape, potentially intercept 25% of the total land area and associated upland N. Regression analysis of TN concentrations from 1,779 CONUS sample sites on wetland-intercepted and wetland-bypassed N inputs showed wetland-intercepted inputs (of any wetland class) did not contribute to instream TN concentrations, suggesting wetlands effectively removed these inputs. Instead, instream TN was associated with the 75% of N inputs that bypassed wetlands. The maps and model produced by this study suggest that wetlands are an underused, yet potentially effective mitigator of upland stressors on streams.