Abstract

Eukaryotic phytoplankton contribute to the flow of elements through marine food webs, biogeochemical cycles, and Earth’s climate. Therefore, how phytoplankton die is a critical determinate of the flow and fate of nutrients. While heterotroph grazing and viral infection contribute to phytoplankton mortality, recent evidence suggests that bacteria-derived cues also control phytoplankton lysis. Here, we report exposure to nanomolar concentrations of 2,3,4,5-tetrabromopyrrole (TBP), a brominated chemical cue synthesized by marine γ-proteobacteria, resulted in mortality of seven phylogenetically-diverse phytoplankton species. A comparison of nine compounds of marine-origin containing a range of cyclic moieties and halogenation indicated that both a single pyrrole ring and increased bromination were most lethal to the coccolithophore, Emiliania huxleyi. TBP also rapidly induced the production of reactive oxygen species and the release of intracellular calcium stores, both of which can trigger the activation of cellular death pathways. Mining of the Ocean Gene Atlas indicated that TBP biosynthetic machinery is globally distributed throughout the water column in coastal areas. These findings suggest that bacterial cues play multiple functions in regulating phytoplankton communities by inducing biochemical changes associated with cellular death. Chemically-induced lysis by bacterial infochemicals is yet another variable that must be considered when modeling oceanic nutrient dynamics.

Highlights

  • Produced polyhalogenated organic compounds are pervasive in the marine environment and have been isolated with regularity from marine biota[1], including sponges and associated cyanobacteria[2], macroalgae, invertebrates[3], and bacteria[4,5]

  • Our original investigation of the algicidal activity of P. piscicida exometabolome indicated that this species of bacteria produced at least two separate compounds capable of inducing mortality in Emiliania huxleyi

  • Marine bacteria have been categorized as those that either actively seek nutrient ‘hot spots’ and exploit them leading to enhanced growth[61] or those that are more passive and have strategies to wait to encounter a nutrient windfall[62]

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Summary

Introduction

Produced polyhalogenated organic compounds are pervasive in the marine environment and have been isolated with regularity from marine biota[1], including sponges and associated cyanobacteria[2], macroalgae, invertebrates[3], and bacteria[4,5]. Members of the γ-proteobacteria include the genus Pseudoalteromonas, which constitutes 0.5–6.0% of the bacterial species found globally and are frequently isolated from biofilms covering the surface of marine organisms[12]. Representative species within this genus are motile, rod-shaped, and known to be pathogenic or opportunistic[15]. Pseudoalteromonas spp. are frequently implicated as producers of extracellular products that cause phytoplankton mortality[15,19,20] These bacteria have been found to produce a suite of biologically active metabolites that include a range of polybrominated pyrroles[17]. Additional physiological and biochemical assays are needed to diagnose the underlying molecular targets and mechanisms responsible for algal cell death

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