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dc.contributor.authorOmar, Naaman M.
dc.contributor.authorPrášil, Ondřej
dc.contributor.authorMcCain, J. Scott P.
dc.contributor.authorCampbell, Douglas A.
dc.date.accessioned2022-04-25T12:40:33Z
dc.date.available2022-04-25T12:40:33Z
dc.date.issued2022-04-15
dc.identifier.urihttps://hdl.handle.net/1721.1/142037
dc.description.abstractMarine phytoplankton vary widely in size across taxa, and in cell suspension densities across habitats and growth states. Cell suspension density and total biovolume determine the bulk influence of a phytoplankton community upon its environment. Cell suspension density also determines the intercellular spacings separating phytoplankton cells from each other, or from co-occurring bacterioplankton. Intercellular spacing then determines the mean diffusion paths for exchanges of solutes among co-occurring cells. Marine phytoplankton and bacterioplankton both produce and scavenge reactive oxygen species (ROS), to maintain intracellular ROS homeostasis to support their cellular processes, while limiting damaging reactions. Among ROS, hydrogen peroxide (H<sub>2</sub>O<sub>2</sub>) has relatively low reactivity, long intracellular and extracellular lifetimes, and readily crosses cell membranes. Our objective was to quantify how cells can influence other cells via diffusional interactions, using H<sub>2</sub>O<sub>2</sub> as a case study. To visualize and constrain potentials for cell-to-cell exchanges of H<sub>2</sub>O<sub>2</sub>, we simulated the decrease of [H<sub>2</sub>O<sub>2</sub>] outwards from representative phytoplankton taxa maintaining internal [H<sub>2</sub>O<sub>2</sub>] above representative seawater [H<sub>2</sub>O<sub>2</sub>]. [H<sub>2</sub>O<sub>2</sub>] gradients outwards from static cell surfaces were dominated by volumetric dilution, with only a negligible influence from decay. The simulated [H<sub>2</sub>O<sub>2</sub>] fell to background [H<sub>2</sub>O<sub>2</sub>] within ~3.1 &micro;m from a <i>Prochlorococcus</i> cell surface, but extended outwards 90 &micro;m from a diatom cell surface. More rapid decays of other, less stable ROS, would lower these threshold distances. Bacterioplankton lowered simulated local [H<sub>2</sub>O<sub>2</sub>] below background only out to 1.<sub>2</sub> &micro;m from the surface of a static cell, even though bacterioplankton collectively act to influence seawater ROS. These small diffusional spheres around cells mean that direct cell-to-cell exchange of H<sub>2</sub>O<sub>2</sub> is unlikely in oligotrophic habits with widely spaced, small cells; moderate in eutrophic habits with shorter cell-to-cell spacing; but extensive within phytoplankton colonies.en_US
dc.publisherMultidisciplinary Digital Publishing Instituteen_US
dc.relation.isversionofhttp://dx.doi.org/10.3390/microorganisms10040821en_US
dc.rightsCreative Commons Attributionen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_US
dc.sourceMultidisciplinary Digital Publishing Instituteen_US
dc.titleDiffusional Interactions among Marine Phytoplankton and Bacterioplankton: Modelling H2O2 as a Case Studyen_US
dc.typeArticleen_US
dc.identifier.citationMicroorganisms 10 (4): 821 (2022)en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Biology
dc.identifier.mitlicensePUBLISHER_CC
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2022-04-21T21:03:38Z
dspace.date.submission2022-04-21T21:03:38Z
mit.licensePUBLISHER_CC
mit.metadata.statusAuthority Work and Publication Information Neededen_US


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