Abstract

The phytoplankton community in the oligotrophic open ocean is numerically dominated by the cyanobacterium Prochlorococcus, accounting for approximately half of all photosynthesis. In the illuminated euphotic zone where Prochlorococcus grows, reactive oxygen species are continuously generated via photochemical reactions with dissolved organic matter. However, Prochlorococcus genomes lack catalase and additional protective mechanisms common in other aerobes, and this genus is highly susceptible to oxidative damage from hydrogen peroxide (HOOH). In this study we showed that the extant microbial community plays a vital, previously unrecognized role in cross-protecting Prochlorococcus from oxidative damage in the surface mixed layer of the oligotrophic ocean. Microbes are the primary HOOH sink in marine systems, and in the absence of the microbial community, surface waters in the Atlantic and Pacific Ocean accumulated HOOH to concentrations that were lethal for Prochlorococcus cultures. In laboratory experiments with the marine heterotroph Alteromonas sp., serving as a proxy for the natural community of HOOH-degrading microbes, bacterial depletion of HOOH from the extracellular milieu prevented oxidative damage to the cell envelope and photosystems of co-cultured Prochlorococcus, and facilitated the growth of Prochlorococcus at ecologically-relevant cell concentrations. Curiously, the more recently evolved lineages of Prochlorococcus that exploit the surface mixed layer niche were also the most sensitive to HOOH. The genomic streamlining of these evolved lineages during adaptation to the high-light exposed upper euphotic zone thus appears to be coincident with an acquired dependency on the extant HOOH-consuming community. These results underscore the importance of (indirect) biotic interactions in establishing niche boundaries, and highlight the impacts that community-level responses to stress may have in the ecological and evolutionary outcomes for co-existing species.

Highlights

  • The open ocean is the largest biome on the surface of the earth, but due to its distance from coastal and deep ocean sediments, is one of the most oligotrophic

  • HOOH diffuses freely across cellular membranes [55], and the heterotrophic HOOH degradation could occur in the cytoplasm, periplasm, or extracellular milieu, perhaps with the same overall effect

  • Densitydependence of HOOH resistance has been observed in Escherichia coli, and catalase-positive E. coli has been shown to crossprotect more vulnerable catalase-negative mutants in co-culture [56]

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Summary

Introduction

The open ocean is the largest biome on the surface of the earth, but due to its distance from coastal and deep ocean sediments, is one of the most oligotrophic. Microbes dominate biomass in this ‘‘wet desert’’ [2] and the most abundant phytoplankter in the tropics and subtropics (,40uN to 40uS latitude) is the unicellular cyanobacterium, Prochlorococcus [3]. This oligotrophic specialist has the smallest cell size (0.4 to 1.2 mm in diameter) and genome (1.7–2.56106 bp) [4,5] of any known photoautotroph. The small cell size results in a superior surface to volume ratio that is believed to provide a key advantage in nutrient scavenging versus larger competitors [6]. As a result of these and other adaptations, Prochlorococcus populations span the entire euphotic zone, often exceeding 105 cells mL21, and due to this numerical dominance have been credited for roughly half of all photosynthesis in the oceans [8,9,10,11,12]

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