Abstract

The production and consumption of organic matter by marine organisms plays a central role in the marine carbon cycle. Labile organic compounds (metabolites) are the major currency of energetic demands and organismal interaction, but these compounds remain elusive because of their rapid turnover and concomitant minuscule concentrations in the dissolved organic matter pool. Organic osmolytes are a group of small metabolites synthesized at high intracellular concentrations (mM) to regulate cellular osmolarity and have the potential to be released as abundant dissolved substrates. Osmolytes may represent an essential currency of exchange among heterotrophic prokaryotes and primary and secondary producers in marine food webs. For example, the well-known metabolite dimethylsulfoniopropionate (DMSP) is used as an osmolyte by some phytoplankton and can be subsequently metabolized by 60% of the marine bacterial community, supplying up to 13% of the bacterial carbon demand and 100% of the bacterial sulfur demand. While marine osmolytes have been studied for decades, our understanding of their cycling and significance within microbial communities is still far from comprehensive. Here, we surveyed the genes responsible for synthesis, breakdown, and transport of 14 key osmolytes. We systematically searched for these genes across marine bacterial genomes (n = 897) and protistan transcriptomes (n = 652) using homologous protein profiles to investigate the potential for osmolyte metabolisms. Using the pattern of gene presence and absence, we infer the metabolic potential of surveyed microbes to interact with each osmolyte. Specifically, we identify: (1) complete pathways for osmolyte synthesis in both prokaryotic and eukaryotic marine microbes, (2) microbes capable of transporting osmolytes but lacking complete synthesis and/or breakdown pathways, and (3) osmolytes whose synthesis and/or breakdown appears to be specialized and is limited to a subset of organisms. The analysis clearly demonstrates that the marine microbial loop has the genetic potential to actively recycle osmolytes and that this abundant group of small metabolites may function as a significant source of nutrients through exchange among diverse microbial groups that significantly contribute to the cycling of labile carbon.

Highlights

  • Marine microbes live in a high salinity environment and must maintain cellular mechanisms for rapid response to any small changes in external water potential in order to maintain cellular homeostasis (Bisson and Kirst, 1995)

  • Dimethylsulfoniopropionate (DMSP) was removed from the list of osmolytes considered because the pathways involved in its biosynthesis and breakdown are incomplete in Kyoto Encyclopedia of Genes and Genomes (KEGG)

  • Across the three domains of life, we found that osmolyte metabolic capabilities could be broken down into two main categories: (1) globally ubiquitous, and (2) mosaically present across groups

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Summary

Introduction

Marine microbes live in a high salinity environment and must maintain cellular mechanisms for rapid response to any small changes in external water potential in order to maintain cellular homeostasis (Bisson and Kirst, 1995). Ions are most readily transported by microbes, and their concentrations typically respond first to external salinity changes. Osmolytes are often referred to as compatible solutes as they are small, organic molecules that are highly soluble and can accumulate at high concentrations within the cytoplasm without interfering with cellular function (Stefels, 2000; Roeßler and Muller, 2001). Organic osmolytes are energetically more costly to use than inorganic ions, because they must be either synthesized or actively transported into the cell, many serve multiple functions in addition to their osmotic contributions. With the exception of a few extensively studied osmolytes (e.g., dimethylsulfoniopropionate, DMSP), we know relatively little about osmolyte distributions in the ocean, the role of environmental conditions in controlling intracellular osmolyte abundances and subsequent release into the dissolved phase, or the significance of osmolytes as substrates in the microbial loop

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