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Titel Inorganic carbon incorporation and nutritional transfers in the chemosynthetic ectosymbiosis harboured by the Atlantic hydrothermal vent shrimp Rimicaris exoculata
VerfasserIn Julie Ponsard, Marie-Anne Cambon-Bonavita, Magali Zbinden, Gilles Lepoint, André Joassin, Laure Corbari, Bruce Shillito, Philippe Compère
Konferenz EGU General Assembly 2011
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 13 (2011)
Datensatznummer 250047356
 
Zusammenfassung
The hydrothermal vent shrimp Rimicaris exoculata is characterized by its chemoautotrophic bacteria hosted in its gill chambers. It lives in dense swarms of thousands individuals per m2 on the black smoker chimneys of the Mid-Atlantic Ridge (MAR) vent sites, including the Rainbow site (36˚ 13’N MAR) where we sampled. First considered as a monoculture of a single phylotype of sulphide-oxidizing epsilon-proteobacteria (Polz & Cavanaugh, 1995), the R. exoculata symbionts are recognized as forming real bacterial community that includes various phylotypes and metabolisms. Zbinden et al. (2008) and Petersen et al. (2010) have identified genes characteristic of methane–oxidizing and sulphide–oxidizing bacteria in the shrimp gill chambers. Furthermore, they observed the occurrence of intracellular sulphur– and iron–enriched granules in filament and rod bacteria, and identified some methanotrophic–like bacteria cells, suggesting that at least three metabolisms (iron, sulphur and methane oxidation) co–occur within the ectosymbiotic community. On the other hand, Schmidt et al. (2008) also pointed out that several reducing compounds present in the hydrothermal environment (H2, CH4, Fe2+ or SH-) could be used as geochemical energy sources for the shrimp bacterial growth and CO2-fixation. The major aims of the work were to determine the environmental reducing compounds really used by ectosymbiotic bacteria of R. exoculata as energy supply of their metabolism and to highlight the probable transfer of molecules from bacteria to the shrimp tissues. In the experiments, shrimps were incubated alive in small volumes in pressurized aquarium IPOCAMPTM either for 4, 6 or 10 hours with various reducers (H2, CH4, Fe2+, thiosulphate) and in presence of carbon isotope-labelled Na-bicarbonate (NaH13CO3or NaH14CO3). Other experiment was also realized by 1 hour-incubation of shrimps in seawater in presence of 14C-acetate and 3H-lysine. Preferential metabolism and carbon incorporation in the biofilm in the shrimp gill chamber was determined through the quantification of 13C in mass spectrometry and by scintillation counting for 14C. The first data carbon-isotope incorporation allows identifying Fe2+ and thiosulphate as suitable energy sources for the bacteria. They also suggest the presence of an internal energy supply in the bacteria owing the carbon fixation also occurs over several hours in pure seawater. The sulphur granules observed in the bacteria reported by Zbinden et al. (2008) could be the energy source used. The possible transfer of organic molecules from the bacterial symbionts to the host shrimp was also investigated by examining the 13C, 14C and 3H levels in the tissues. The presence of 14C and 3H incorporated from 14C-bicarbonate, 14C-acetate and 3H-lysine confirm the transfer and the higher levels of radioactivity in the gill chamber integuments support a probable tegumental incorporation pathway of dissolved organic molecules rather than a digestive pathway. The authors thank the National Fund for Scientific Research (FNRS-FRIA, Belgium) (conv. FRFC No 2.4.594.07.F, fellowships of Dr L. Corbari and J. Ponsard), and the French Institutes (CNRS and IFREMER) for their financial support. References: Petersen et al., Environmental Microbiology, (2010) 1-15; Polz & Cavanaugh, Proc. Natl. Acad. Sci.., 92 (1995) 7232-7236; Schmidt et al., Mar. Chem., 108 (2008) 18–31; Zbinden et al., Exp. Mar. Biol. and Ecol., 359 (2008) 131–140