Omar Naaman M, Prášil Ondřej, McCain J Scott P, Campbell Douglas A
Department of Biology, Mount Allison University, Sackville, NB E4L1G7, Canada.
Center Algatech, Laboratory of Photosynthesis, Novohradska 237, CZ 37981 Trebon, Czech Republic.
Microorganisms. 2022 Apr 15;10(4):821. doi: 10.3390/microorganisms10040821.
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 (HO) 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 HO as a case study. To visualize and constrain potentials for cell-to-cell exchanges of HO, we simulated the decrease of [HO] outwards from representative phytoplankton taxa maintaining internal [HO] above representative seawater [HO]. [HO] gradients outwards from static cell surfaces were dominated by volumetric dilution, with only a negligible influence from decay. The simulated [HO] fell to background [HO] within ~3.1 µm from a cell surface, but extended outwards 90 µm from a diatom cell surface. More rapid decays of other, less stable ROS, would lower these threshold distances. Bacterioplankton lowered simulated local [HO] below background only out to 1. µm 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 HO 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.
海洋浮游植物在不同分类群中的大小差异很大,在不同栖息地和生长状态下的细胞悬浮密度也各不相同。细胞悬浮密度和总生物体积决定了浮游植物群落对其环境的总体影响。细胞悬浮密度还决定了浮游植物细胞彼此之间或与同时存在的浮游细菌之间的细胞间距。细胞间距进而决定了同时存在的细胞间溶质交换的平均扩散路径。海洋浮游植物和浮游细菌都能产生和清除活性氧(ROS),以维持细胞内ROS的稳态,支持其细胞过程,同时限制损伤反应。在ROS中,过氧化氢(HO)反应性相对较低,细胞内和细胞外寿命较长,并且很容易穿过细胞膜。我们的目标是以HO为例,量化细胞如何通过扩散相互作用影响其他细胞。为了可视化并限制HO细胞间交换的可能性,我们模拟了从代表性浮游植物分类群向外[HO]的降低,这些分类群维持内部[HO]高于代表性海水[HO]。从静态细胞表面向外的[HO]梯度主要由体积稀释主导,衰变的影响可以忽略不计。模拟的[HO]在距细胞表面约3.1 µm内降至背景[HO],但从硅藻细胞表面向外延伸90 µm。其他不太稳定的ROS的更快衰变会缩短这些阈值距离。浮游细菌仅在距静态细胞表面1. µm范围内将模拟的局部[HO]降低到背景以下,尽管浮游细菌共同作用会影响海水ROS。细胞周围这些小的扩散球意味着,在细胞间距大、细胞小的贫营养环境中,HO不太可能直接进行细胞间交换;在细胞间距较短的富营养环境中交换程度适中;但在浮游植物群落内部交换广泛。