Articles | Volume 20, issue 16
https://doi.org/10.5194/bg-20-3423-2023
https://doi.org/10.5194/bg-20-3423-2023
Reviews and syntheses
 | 
17 Aug 2023
Reviews and syntheses |  | 17 Aug 2023

Benthic foraminifera and gromiids from oxygen-depleted environments – survival strategies, biogeochemistry and trophic interactions

Nicolaas Glock

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Cited articles

Alve, E. and Murray, J.: Temporal variability in vertical distributions of live (stained) intertidal foraminifera, Southern England, J. Foramin. Res., 31, 12–24, https://doi.org/10.2113/0310012, 2001. 
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Auten, R. L. and Davis, J. M.: Oxygen toxicity and reactive oxygen species: The devil is in the details, Pediatr. Res., 66, 121–127, https://doi.org/10.1203/PDR.0b013e3181a9eafb, 2009. 
Barras, C., Mouret, A., Nardelli, M. P., Metzger, E., Petersen, J., La, C., Filipsson, H. L., and Jorissen, F.: Experimental calibration of manganese incorporation in foraminiferal calcite, Geochim. Cosmochim. Ac., 237, 49–64, https://doi.org/10.1016/j.gca.2018.06.009, 2018. 
Bernhard, J. M.: Characteristic assemblages and morphologies of benthic foraminifera from anoxic, organic-rich deposits; Jurassic through Holocene, J. Foraminifer. Res., 16, 207–215, https://doi.org/10.2113/GSJFR.16.3.207, 1986. 
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Short summary
Ocean deoxygenation due to climate warming is an evolving threat for organisms that are not well adapted to O2 depletion, such as many pelagic fish species. Other better-adapted organisms, such as some benthic foraminifera species, might benefit from ocean deoxygenation. Benthic foraminifera are a group of marine protists and can have specific adaptations to O2 depletion such as the ability to respire nitrate instead of O2. This paper reviews the current state of knowledge about these organisms.
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