4.6 Article

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

期刊

MICROORGANISMS
卷 10, 期 4, 页码 -

出版社

MDPI
DOI: 10.3390/microorganisms10040821

关键词

diffusional interactions; hydrogen peroxide; phytoplankton; bacterioplankton

资金

  1. Mount Allison University Rice Memorial Graduate Fellowship
  2. New Brunswick Innovation Foundation STEM Graduate Award
  3. Canada Research Chair in Phytoplankton Ecophysiology
  4. Microbiology Institute of the Czech Academy of Science of the European Union Researcher Mobility program [CZ.02.2.69/0.0/0.0/16_027/0007990]

向作者/读者索取更多资源

Marine phytoplankton have varying sizes and cell suspension densities, which determine their influence on the environment. Hydrogen peroxide plays a crucial role in cell-to-cell exchanges, but its diffusion is limited by intercellular spacing.
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 cooccurring 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 (H2O2) 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 H2O2 as a case study. To visualize and constrain potentials for cell-to-cell exchanges of H2O2, we simulated the decrease of [H2O2] outwards from representative phytoplankton taxa maintaining internal [H2O2] above representative seawater [H2O2]. [H2O2] gradients outwards from static cell surfaces were dominated by volumetric dilution, with only a negligible influence from decay. The simulated [H2O2] fell to background [H2O2] within similar to 3.1 mu m from a Prochlorococcus cell surface, but extended outwards 90 mu m from a diatom cell surface. More rapid decays of other, less stable ROS, would lower these threshold distances. Bacterioplankton lowered simulated local [H2O2] below background only out to 1. 2 mu 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 H2O2 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.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.6
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据