Authors

Samuel T. Wilson, University of Hawaiʻi at MānoaFollow
Alia N. Al-Haj, Boston University
Annie Bourbonnais, University of South Carolina
Claudia Frey, Universitat Basel
Robinson W. Fulweiler, Boston University
John D. Kessler, University of Rochester
Hannah K. Marchant, Max Planck In­sti­tute for Mar­ine Mi­cro­bi­o­logy
Jana Milucka, Max Planck In­sti­tute for Mar­ine Mi­cro­bi­o­logy
Nicholas E. Ray, Boston University
Parv Suntharalingham, University of East Anglia
Brett F. Thornton, Stockholms universitet
Robert C. Upstill-Goddard, Newcastle University
Thomas S. Weber, University of Rochester
Damian L. Arévalo-Martínez, GEOMAR - Helmholtz-Zentrum für Ozeanforschung Kiel
Hermann W. Bange, GEOMAR - Helmholtz-Zentrum für Ozeanforschung Kiel
Heather M. Benway, Woods Hole Oceanographic Institution
Daniele Bianchi, University of California, Los Angeles
Alberto V. Borges, Université de Liège
Bonnie X. Chang, University of Washington
Patrick M. Crill, Stockholms universitet
Daniela A. Del Valle, University of Southern Mississippi
Laura Fariás, Centro de Ciencia del Clima y la Resiliencia (CR)2
Samantha B. Joye, University of GeorgiaFollow
Annette Kock, GEOMAR - Helmholtz-Zentrum für Ozeanforschung Kiel
Jabrane Labidi, University of California, Los Angeles
Cara C. Manning, The University of British Columbia
John W. Pohlman, United States Geological Survey
Gregor Rehder, The Leibniz Institute for Baltic Sea Research
Katy J. Sparrow, Florida State UniversityFollow
Philippe D. Tortell, The University of British Columbia
Tina Treude, University of California, Los Angeles
David L. Valentine, University of California, Santa Barbara

Document Type

Article

Publication Date

11-26-2020

Abstract

In the current era of rapid climate change, accurate characterization of climate-relevant gas dynamics-namely production, consumption, and net emissions-is required for all biomes, especially those ecosystems most susceptible to the impact of change. Marine environments include regions that act as net sources or sinks for numerous climateactive trace gases including methane (CH4) and nitrous oxide (N2O). The temporal and spatial distributions of CH4 and N2O are controlled by the interaction of complex biogeochemical and physical processes. To evaluate and quantify how these mechanisms affect marine CH4 and N2O cycling requires a combination of traditional scientific disciplines including oceanography, microbiology, and numerical modeling. Fundamental to these efforts is ensuring that the datasets produced by independent scientists are comparable and interoperable. Equally critical is transparent communication within the research community about the technical improvements required to increase our collective understanding of marine CH4 and N2O. A workshop sponsored by Ocean Carbon and Biogeochemistry (OCB) was organized to enhance dialogue and collaborations pertaining to marine CH4 and N2O. Here, we summarize the outcomes from the workshop to describe the challenges and opportunities for near-future CH4 and N2O research in the marine environment.

Publication Title

Biogeosciences

Volume

17

Issue

22

First Page

5809

Last Page

5828

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