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

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ADS bibcode
2018AGUFM.B43G2938O
year
2018
Listed Authors
Osburn, C. L.
Joshi, I.
Oviedo-Vargas, D.
Bianchi, T. S.
D'Sa, E. J.
Ko, D.
Arellano, A. R.
Shields, M. R.
Ward, N. D.
Listed Institutions
North Carolina State University Raleigh, Raleigh, NC, United States
Louisiana State University
Stroud Water Research Center, Avondale, NC, United States
Department of Geological Sciences, University of Florida, Ft Walton Beach, FL, United States
Louisiana State Univ, Baton Rouge, LA, United States
US Naval Research Laboratory, Monterey, CA, United States
University of South Florida St. Petersburg, St Petersburg, FL, United States
Texas A&M University, College Station, TX, United States
Marine Sciences Laboratory, Pacific Northwest National Laboratory, Sequim, United States

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