Abstract

Vesicomyid clams harbor intracellular sulfur-oxidizing bacteria that are predominantly maternally inherited and co-speciate with their hosts. Genome recombination and the occurrence of non-parental strains were recently demonstrated in symbionts. However, mechanisms favoring such events remain to be identified. In this study, we investigated symbionts in two phylogenetically distant vesicomyid species, Christineconcha regab and Laubiericoncha chuni, which sometimes co-occur at a cold-seep site in the Gulf of Guinea. We showed that each of the two species harbored a single dominant bacterial symbiont strain. However, for both vesicomyid species, the symbiont from the other species was occasionally detected in the gills using fluorescence in situ hybridization and gene sequences analyses based on six symbiont marker genes. Symbiont strains co-occurred within a single host only at sites where both host species were found; whereas one single symbiont strain was detected in C. regab specimens from a site where no L. chuni individuals had been observed. These results suggest that physical proximity favored the acquisition of non-parental symbiont strains in Vesicomyidae. Over evolutionary time, this could potentially lead to genetic exchanges among symbiont species and eventually symbiont displacement. Symbiont densities estimated using 3D fluorescence in situ hybridization varied among host species and sites, suggesting flexibility in the association despite the fact that a similar type of metabolism is expected in all symbionts.

Highlights

  • Vesicomyid bivalves are one of the most abundant groups of chemosynthetic fauna inhabiting deep-sea reducing ecosystems, including hydrothermal vents, whale falls and cold seeps [1,2,3]

  • From a more ecological point of view, we investigated whether sites or host species influence the density of bacterial symbionts measured using 3D fluorescence in situ hybridization (FISH) as the percentage of bacteriocyte volume occupied by symbiont bacteria [19]

  • A single c oxidase subunit I (COI) haplotype was detected in the three L. chuni specimens

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Summary

Introduction

Vesicomyid bivalves are one of the most abundant groups of chemosynthetic fauna inhabiting deep-sea reducing ecosystems, including hydrothermal vents, whale falls and cold seeps [1,2,3]. Vesicomyid bivalves live in symbiosis with sulfur-oxidizing bacteria located in their gills [6,7]. These symbionts produce organic compounds used by the bivalve hosts for their nutrition, and in turn, the bivalve hosts supply the symbionts with oxygen, carbon dioxide and reduced sulfur. Oxygen and carbon dioxide are directly available in the ambient seawater and are transported, through the inhalant siphon, to gills and bacteria therein. Sulfide from the sediment is absorbed in the host through the foot into the hemolymph and transported to the gills [8]

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