MIT Libraries logoDSpace@MIT

MIT
View Item 
  • DSpace@MIT Home
  • MIT Open Access Articles
  • MIT Open Access Articles
  • View Item
  • DSpace@MIT Home
  • MIT Open Access Articles
  • MIT Open Access Articles
  • View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.

Diffusional Interactions among Marine Phytoplankton and Bacterioplankton: Modelling H2O2 as a Case Study

Author(s)
Omar, Naaman M.; Prášil, Ondřej; McCain, J. Scott P.; Campbell, Douglas A.
Thumbnail
Downloadmicroorganisms-10-00821.pdf (3.198Mb)
Publisher with Creative Commons License

Publisher with Creative Commons License

Creative Commons Attribution

Terms of use
Creative Commons Attribution https://creativecommons.org/licenses/by/4.0/
Metadata
Show full item record
Abstract
Marine 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.
Date issued
2022-04-15
URI
https://hdl.handle.net/1721.1/142037
Department
Massachusetts Institute of Technology. Department of Biology
Publisher
Multidisciplinary Digital Publishing Institute
Citation
Microorganisms 10 (4): 821 (2022)
Version: Final published version

Collections
  • MIT Open Access Articles

Browse

All of DSpaceCommunities & CollectionsBy Issue DateAuthorsTitlesSubjectsThis CollectionBy Issue DateAuthorsTitlesSubjects

My Account

Login

Statistics

OA StatisticsStatistics by CountryStatistics by Department
MIT Libraries
PrivacyPermissionsAccessibilityContact us
MIT
Content created by the MIT Libraries, CC BY-NC unless otherwise noted. Notify us about copyright concerns.