Dissolved Organic Carbon in Coastal Waters: Global Patterns, Stocks and Environmental Physical Controls
- Section for Marine Diversity and Experimental Ecology Department of Ecoscience Aarhus University Roskilde Denmark
- CSIC Instituto de Investigacións Mariñas Vigo Spain
- Centre for Environmental and Marine Studies (CESAM) University of Aveiro Aveiro Portugal
- Departamento Interdisciplinario de Sistemas Costero Marinos Centro Universitario Regional Este Universidad de La República Rocha Uruguay
- Instituto de Oceanografía y Cambio Global (IOCAG) Universidad de Las Palmas de Gran Canaria Las Palmas Spain
- Indian Institute of Science Education and Research Kolkata Kolkata India, Faculty of Applied Sciences UCSI University Kuala Lumpur Kuala Lumpur Malaysia
- Rosenstiel School of Marine, Atmospheric and Earth Science University of Miami Miami FL USA, Monterey Bay Aquarium Research Institute Moss Landing CA USA
- IMEDEA (CSIC‐UIB), Mediterranean Institute for Advanced Studies Esporles Spain
- State Key Laboratory for Marine Environmental Science Institute of Marine Microbes and Ecospheres College of Ocean and Earth Sciences Xiamen University Xiamen China, Fujian Key Laboratory of Marine Carbon Sequestration Xiamen University Xiamen China
- Centro de Estudos do Mar Universidade Federal do Paraná Pontal do Paraná Brazil
- CNR—ISMAR Istituto di Scienze Marine Trieste Italy
- Centre for Coastal Biogeochemistry Faculty of Science and Engineering Southern Cross University Lismore NSW Australia
- National Oceanography Centre Southampton UK
- National Institute of Oceanography and Applied Geophysics (OGS) Trieste Italy, Istituto Centrale Per la Ricerca Scientifica e Tecnologia Applicata al Mare Chioggia Italy
- National Institute of Aquatic Resources Technical University of Denmark Kgs Lyngby Denmark
- Australian Institute of Marine Science Townsville QLD Australia
- Rosenstiel School of Marine, Atmospheric and Earth Science University of Miami Miami FL USA
- Department of Ecoscience Aarhus University Aarhus Denmark
- Fisheries and Aquatic Ecosystems Branch Agri‐Food and Biosciences Institute Belfast UK
- Consiglio Nazionale delle Ricerche (CNR) Istituto di Scienze Marine (ISMAR) Rome Italy, Institute of Marine Sciences Middle East Technical University Erdemli‐Mersin Turkey
- Remote Sensing Laboratory Institute of Oceanology Polish Academy of Sciences Sopot Poland
- ENTROPIE IRD CNRS IFREMER University of Reunion University of New Caledonia Nouméa New Caledonia
- Consiglio Nazionale Delle Ricerche Istituto Per lo Studio Degli Impatti Antropici e Sostenibilità in Ambiente Marino (CNR‐IAS) Oristano Italy
- Asian School of the Environment Nanyang Technological University Singapore Singapore
- Department of Biology Virginia Commonwealth University Richmond VA USA
- King Abdullah University of Science and Technology Thuwal Kingdom of Saudi Arabia, Centro Oceanográfico de Gijón/Xixón Instituto Español de Oceanografía Gijón/Xixón Spain
- Leibniz Institute for Baltic Sea Research Warnemuende Rostock‐Warnemuende Germany
- School of Earth and Environmental Sciences Seoul National University Seoul Korea
- College of Marine Science University of South Florida Saint Petersburg FL USA
- State Key Laboratory of Estuarine and Coastal Research East China Normal University Shanghai China
- Centro de Investigación Mariña‐Universidade de Vigo Vigo Spain
- Pacific Northwest National Laboratory Marine and Coastal Research Laboratory Sequim WA USA
- Faculty of Environmental Earth Science Hokkaido University Hokkaido Japan
- College of Environment and Safety Engineering Fuzhou University Fuzhou China
Dissolved organic carbon (DOC) in coastal waters is integral to biogeochemical cycling, but global and regional drivers of DOC are still uncertain. In this study we explored spatial and temporal differences in DOC concentrations and stocks across the global coastal ocean, and how these relate to temperature and salinity. We estimated a global median coastal DOC stock of 3.15 Pg C (interquartile range (IQR) = 0.85 Pg C), with median DOC concentrations being 2.2 times higher than in open ocean surface waters. Globally and seasonally, salinity was the main driver of DOC with concentrations correlated negatively with salinity, without a clear relationship to temperature. DOC concentrations and stocks varied with region and season and this pattern is likely driven by riverine inputs of DOC and nutrients that stimulate coastal phytoplankton production. Temporally, high DOC concentrations occurred mainly in months with high freshwater input, with some exceptions such as in Eastern Boundary Current margins where peaks are related to primary production stimulated by nutrients upwelled from the adjacent ocean. No spatial trend between DOC and temperature was apparent, but many regions (19 out of 25) had aligned peaks of seasonal temperature and DOC, related to increased phytoplankton production and vertical stratification at high temperatures. Links of coastal DOC with salinity and temperature highlight the potential for anthropogenic impacts to alter coastal DOC concentration and composition, and thereby ecosystem status.
- Sponsoring Organization:
- USDOE
- OSTI ID:
- 2564298
- Journal Information:
- Global Biogeochemical Cycles, Journal Name: Global Biogeochemical Cycles Journal Issue: 5 Vol. 39; ISSN 0886-6236
- Publisher:
- American Geophysical Union (AGU)Copyright Statement
- Country of Publication:
- United States
- Language:
- English
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