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Osvatic, J. T.

Publications and source records attributed to Osvatic, J. T..

2 recordsLinked to original sources

Organosulfur cycling in the multi-partner symbiosis between lucinid bivalves, sulphur-oxidizing symbionts, and Endozoicomonas

Organosulfur compounds play an important role in chemotaxis, stress protection, and nutrition in many marine symbioses. Lucinidae, an ancient and species-rich family of marine bivalves, host chemosynthetic sulphur-oxidising bacteria within gill epithelial cells, and is well-known for its contribution to inorganic sulphur cycling in marine sediments worldwide. Little is known about organosulfur transformations by lucinid-associated microbiota or the hosts potential contribution. Here, we integrated field measurements, genomics, transcriptomics, and experimental assays to investigate organosulfur cycling in three lucinid species from temperate and tropical environments. Concentrations of the osmolyte dimethylsulphoniopropionate (DMSP) in lucinids were typically much higher than in their surrounding environment, and varied with host species and season, but not with symbiont abundance. Indeed, candidate DMSP synthesis DSYB genes were expressed by the animal hosts implying that the host may be the source of DMSP. Furthermore, a newly identified and isolated Candidatus Endozoicomonas endolucinida symbiont was capable of DMSP catabolism to dimethylsulphide (DMS), which could be further syntrophically oxidised by the sulphur-oxidising symbionts that encode methanethiol oxidase genes in their genomes. Finally, incubation experiments supported a combined role of the host and its associated microbiome in organosulfur cycling during stress, with the highest DMSP concentrations measured when holobionts were incubated with antibiotics under anoxic conditions. This study identified a previously unrecognised microbial partner in lucinid symbioses and revealed its potential organosulphur-based metabolic interactions with both the host and the sulphur-oxidising symbionts, highlighting the capacity of these widespread associations to influence global organosulfur cycling.

ecology↗

Novel nitrifying symbiont lineages are vertically inherited and widespread in marine sponges

Ammonia-oxidising archaea and nitrite-oxidising bacteria are common members of marine sponge microbiomes. They derive energy for carbon fixation and growth from nitrification - the oxidation of ammonia to nitrite and further to nitrate - and are proposed to play essential roles in the carbon and nitrogen cycling of sponge holobionts. In this study, we characterise two novel nitrifying symbiont lineages, Ca. Nitrosokoinonia and Ca. Nitrosymbion in the marine sponge Coscinoderma matthewsi using a combination of molecular tools, single-cell imaging techniques, and physiological rate measurements. Both represent a new genus in the ammonia-oxidising archaeal class Nitrososphaeria and the nitrite-oxidising bacterial order Nitrospirales, respectively. Furthermore, we show that larvae of this viviparous sponge are densely colonised by representatives of Ca. Nitrosokoinonia and Ca. Nitrosymbion indicating vertical transmission. In adults, the representatives of both symbiont genera are located extracellularly in the mesohyl. Comparative metagenome analyses and physiological data suggest that ammonia-oxidising archaeal symbionts of the genus Ca. Nitrosokoinonia strongly rely on endogenously produced nitrogenous compounds (i.e., ammonium, urea, nitriles/cyanides, and creatinine) rather than on exogenous ammonium sources taken up by the sponge. Additionally, the nitrite-oxidising bacterial symbionts Ca. Nitrosymbion may reciprocally support the ammonia-oxidisers with ammonia via the utilisation of sponge-derived urea and cyanate. Interestingly, comparative analyses of published environmental 16S rRNA amplicon data revealed that Ca. Nitrosokoinonia and Ca. Nitrosymbion are widely distributed and predominantly associated with marine sponges and corals, suggesting a broad relevance of our findings.

microbiology↗