Higher rates of sea level rise result in higher lateral flux of dissolved organic carbon (DOC) from tidal wetlands to coastal waters of the northern Gulf of Mexico
Chris L Osburn, North Carolina State University Raleigh, Raleigh, NC, United States, Ishan Joshi, Louisiana State University, Diana Oviedo-Vargas, Stroud Water Research Center, Avondale, NC, United States, Thomas S S Bianchi, University of Florida, Department of Geological Sciences, Gainesville, United States, Eurico J. D'Sa, Louisiana State University, Department of Oceanography and Coastal Sciences, Baton Rouge, LA, United States, Dong Ko, US Naval Research Laboratory, Monterey, CA, United States, Ana R. Arellano, University of South Florida, College of Marine Science, St. Petersburg, United States, Michael R Shields, Texas A&M University, College Station, TX, United States and Nicholas D Ward, Pacific Northwest National Laboratory, Coastal Sciences Division, Richland, WA, United States
