Articles | Volume 18, issue 5
https://doi.org/10.5194/bg-18-1823-2021
https://doi.org/10.5194/bg-18-1823-2021
Research article
 | 
16 Mar 2021
Research article |  | 16 Mar 2021

Warming and ocean acidification may decrease estuarine dissolved organic carbon export to the ocean

Michelle N. Simone, Kai G. Schulz, Joanne M. Oakes, and Bradley D. Eyre

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Cited articles

Admiraal, W.: The ecology of estuarine sediment-inhabiting diatoms, in: Progress in phycological Research, edited by: Round, F. E., and Chapman, D. J., Biopress, Bristol, 269–322, 1984. 
Allen, A., Gillooly, J., and Brown, J.: Linking the global carbon cycle to individual metabolism, Funct. Ecol., 19, 202–213, https://doi.org/10.1111/j.1365-2435.2005.00952.x, 2005. 
Allen, H. L.: Low molecular weight dissolved organic matter in five soft-water ecosystems: a preliminary study and ecological implications: With 3 figures and 2 tables in the text and on 1 folder, Internationale Vereinigung für theoretische und angewandte Limnologie: Verhandlungen, 20, 514–524, 1978. 
Apple, J., Smith, E., and Boyd, T.: Temperature, Salinity, Nutrients, and the Covariation of Bacterial Production and Chlorophyll-a in Estuarine Ecosystems, J. Coast. Res., 2008, 59–75, https://doi.org/10.2112/SI55-005.1, 2008. 
Apple, J. K., del Giorgio, P. A., and Kemp, W. M.: Temperature regulation of bacterial production, respiration, and growth efficiency in a temperate salt-marsh estuary, Aquat. Microb. Ecol., 43, 243–254, https://doi.org/10.3354/ame043243, 2006. 
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Estuaries are responsible for a large contribution of dissolved organic carbon (DOC) to the global C cycle, but it is unknown how this will change in the future. DOC fluxes from unvegetated sediments were investigated ex situ subject to conditions of warming and ocean acidification. The future climate shifted sediment fluxes from a slight DOC source to a significant sink, with global coastal DOC export decreasing by 80 %. This has global implications for C cycling and long-term C storage.
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