Articles | Volume 15, issue 22
https://doi.org/10.5194/bg-15-6819-2018
https://doi.org/10.5194/bg-15-6819-2018
Research article
 | 
16 Nov 2018
Research article |  | 16 Nov 2018

Impact of carbonate saturation on large Caribbean benthic foraminifera assemblages

Ana Martinez, Laura Hernández-Terrones, Mario Rebolledo-Vieyra, and Adina Paytan

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Cited articles

Angell, R. W.: Test morphogenesis (chamber formation) in the foraminifer Spiroloculina hyalina Schulze, J. Foramin. Res., 10, 89–101, 1980. 
Back, W., Hanshaw, B. B., Pyle, T. E., Plummer, L. N., and Weidie, A.: Geochemical significance of groundwater discharge and carbonate solution to the formation of Caleta Xel Ha, Quintana Roo, Mexico, Water Resour. Res., 15, 1521–1535, 1979. 
BCO-DMO: Project: Calcification in low saturation seawater: What can we learn from organisms in the proximity of low pH; undersaturated submarine springs, available at: https://www.bco-dmo.org/project/488852, last access: 12 November 2018. 
Bentov, S., Brownlee, C., and Erez, J.: The role of seawater endocytosis in the biomineralization process in calcareous foraminifera, P. Natl. Acad. Sci. USA, 106, 21500–21504, https://doi.org/10.1073/pnas.0906636106, 2009. 
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Short summary
Our study at low-pH submarine springs suggests that ocean acidification may reduce the number of Caribbean benthic foraminifera, particularly those species that form carbonate shells. This may have subsequent repercussions on the global carbon cycle and marine food webs that depend on benthic foraminifera.
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