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Global distribution of hydrothermal vent shrimp belonging to the genus Rimicaris . The occurrence of these shrimp at two ridge systems: (A) Mid-Atlantic Ridge (colonized by Rimicaris exoculata [black] & Rimicaris cf. exoculata [black-white]) and (B) Central Indian Ridge [colonized by Rimicaris kairei (white)] is indicated in the enlarged maps (for details, see Table 1). 

Global distribution of hydrothermal vent shrimp belonging to the genus Rimicaris . The occurrence of these shrimp at two ridge systems: (A) Mid-Atlantic Ridge (colonized by Rimicaris exoculata [black] & Rimicaris cf. exoculata [black-white]) and (B) Central Indian Ridge [colonized by Rimicaris kairei (white)] is indicated in the enlarged maps (for details, see Table 1). 

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The vent shrimp Rimicaris exoculata thrives around many hydrothermal vent sites along the Mid-Atlantic Ridge (MAR), where it aggregates into dense swarms. In contrast to hydrothermal vent fields at the East Pacific Rise (EPR), where the biomass is dominated by tubeworms, clams, and mussels, this shrimp is one of the major animal species at MAR vent...

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... vent shrimp Rimicaris exoculata dominates the vagile fauna at most Mid-Atlantic Ridge hydrothermal vent sites ( Fig. 1). This species lives within steep chemical and thermal gra- dients, where hot, reduced hydrothermal fluid mixes turbulently with oxygenated seawater. First described by Williams and Rona (1986), this species was observed to colonize black smoker complexes in the rift valley at the TAG site (26 ° 08.3 # N, 44 ° 49.6 # W; depth: 3,620–3,650 m). Rimicaris exoculata was subsequently found at several MAR-vent sites in the depth- range of 2,300–3,900 m (Rainbow, Broken Spur, TAG, Snake Pit, Logatchev, 5 ° S; Fig. 1, Table 1). In comparison with the hydrothermal environment on the East Pacific Rise where tubeworms, clams, and mussels dominate the vent fauna (Van Dover 1995), Rimicaris exoculata is by far one of the most abundant invertebrates at the Mid-Atlantic ridge vents (Williams & Rona 1986, Van Dover 1995, Van Dover et al. 2002, Desbruye ` res et al. 2000, Desbruye ` res et al. 2001). The two MAR-sites where this species has not been observed are the shallower vent fields Menez Gwen (860 m) and Lucky Strike (1,700 m). Although it was first believed that R. exoculata were present at the latter one (Van Dover et al. 1996), the existence of the shrimp at this site has not been reported after further expeditions (Table 1). Dense swarms of Rimicaris cf. exoculata were investigated at recently discovered hydrothermal vent fields along the southern Mid-Atlantic Ridge (Turtle Pits and Red Lion 5 ° S, 3,000m; References in Fig. 1 & Table 1). Recently, the existence of dense shrimp swarms at the active Kairei and Edmond hydrothermal vent fields (Central Indian Ridge, 2,451–3,320-m depth) (Fig. 1, Table 1) was described (Hashimoto et al. 2001a, Hashimoto et al. 2001b). Van Dover et al. (2001) reported that shrimp tissue from these sites is isotopically indistinguishable from those of R. exoculata on the Mid-Atlantic Ridge. Further studies demonstrated that the shrimp found at the Central Indian Ridge are very close to Rimicaris exoculata but still clearly distinguishable by some morphological differences and therefore classified as Rimicaris kairei (Watabe & Hashimoto 2002). The abundance of R. exoculata varies between different sites. For example, at Rainbow, shrimp assemble in depressions between chimney structures (Fig. 2B), whereas at TAG, black smoker complexes were almost entirely covered by dense agglomerations. Contrarily, at Broken Spur, low shrimp biomass was found (Copley et al. 1997). At the site Red Lion an unusual flange growth was investigated that appears to support a thriving shrimp community (Koschinsky et al. 2006). Other chimneys, that lack the flange growth, show a low abundance of Rimicaris cf. exoculata (Koschinsky et al. 2006). It is still unknown to what extent hydrothermal flow rates and composition influence the distribution of R. exoculata . However, they presumably play a role in the adaptation strategies of this species to such extreme environments. In particular, large variations in chemical composition of the endmember fluid have been observed between different MAR sites (Von Damm et al. 2001, Charlou et al. 2002, Douville et al. 2002). Rimicaris exoculata form large aggregations on solid sulfide surfaces around warm vent water emissions (Fig. 2). ...
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... vent shrimp Rimicaris exoculata dominates the vagile fauna at most Mid-Atlantic Ridge hydrothermal vent sites ( Fig. 1). This species lives within steep chemical and thermal gra- dients, where hot, reduced hydrothermal fluid mixes turbulently with oxygenated seawater. First described by Williams and Rona (1986), this species was observed to colonize black smoker complexes in the rift valley at the TAG site (26 ° 08.3 # N, 44 ° 49.6 # W; depth: 3,620–3,650 m). Rimicaris exoculata was subsequently found at several MAR-vent sites in the depth- range of 2,300–3,900 m (Rainbow, Broken Spur, TAG, Snake Pit, Logatchev, 5 ° S; Fig. 1, Table 1). In comparison with the hydrothermal environment on the East Pacific Rise where tubeworms, clams, and mussels dominate the vent fauna (Van Dover 1995), Rimicaris exoculata is by far one of the most abundant invertebrates at the Mid-Atlantic ridge vents (Williams & Rona 1986, Van Dover 1995, Van Dover et al. 2002, Desbruye ` res et al. 2000, Desbruye ` res et al. 2001). The two MAR-sites where this species has not been observed are the shallower vent fields Menez Gwen (860 m) and Lucky Strike (1,700 m). Although it was first believed that R. exoculata were present at the latter one (Van Dover et al. 1996), the existence of the shrimp at this site has not been reported after further expeditions (Table 1). Dense swarms of Rimicaris cf. exoculata were investigated at recently discovered hydrothermal vent fields along the southern Mid-Atlantic Ridge (Turtle Pits and Red Lion 5 ° S, 3,000m; References in Fig. 1 & Table 1). Recently, the existence of dense shrimp swarms at the active Kairei and Edmond hydrothermal vent fields (Central Indian Ridge, 2,451–3,320-m depth) (Fig. 1, Table 1) was described (Hashimoto et al. 2001a, Hashimoto et al. 2001b). Van Dover et al. (2001) reported that shrimp tissue from these sites is isotopically indistinguishable from those of R. exoculata on the Mid-Atlantic Ridge. Further studies demonstrated that the shrimp found at the Central Indian Ridge are very close to Rimicaris exoculata but still clearly distinguishable by some morphological differences and therefore classified as Rimicaris kairei (Watabe & Hashimoto 2002). The abundance of R. exoculata varies between different sites. For example, at Rainbow, shrimp assemble in depressions between chimney structures (Fig. 2B), whereas at TAG, black smoker complexes were almost entirely covered by dense agglomerations. Contrarily, at Broken Spur, low shrimp biomass was found (Copley et al. 1997). At the site Red Lion an unusual flange growth was investigated that appears to support a thriving shrimp community (Koschinsky et al. 2006). Other chimneys, that lack the flange growth, show a low abundance of Rimicaris cf. exoculata (Koschinsky et al. 2006). It is still unknown to what extent hydrothermal flow rates and composition influence the distribution of R. exoculata . However, they presumably play a role in the adaptation strategies of this species to such extreme environments. In particular, large variations in chemical composition of the endmember fluid have been observed between different MAR sites (Von Damm et al. 2001, Charlou et al. 2002, Douville et al. 2002). Rimicaris exoculata form large aggregations on solid sulfide surfaces around warm vent water emissions (Fig. 2). ...
Context 3
... vent shrimp Rimicaris exoculata dominates the vagile fauna at most Mid-Atlantic Ridge hydrothermal vent sites ( Fig. 1). This species lives within steep chemical and thermal gra- dients, where hot, reduced hydrothermal fluid mixes turbulently with oxygenated seawater. First described by Williams and Rona (1986), this species was observed to colonize black smoker complexes in the rift valley at the TAG site (26 ° 08.3 # N, 44 ° 49.6 # W; depth: 3,620–3,650 m). Rimicaris exoculata was subsequently found at several MAR-vent sites in the depth- range of 2,300–3,900 m (Rainbow, Broken Spur, TAG, Snake Pit, Logatchev, 5 ° S; Fig. 1, Table 1). In comparison with the hydrothermal environment on the East Pacific Rise where tubeworms, clams, and mussels dominate the vent fauna (Van Dover 1995), Rimicaris exoculata is by far one of the most abundant invertebrates at the Mid-Atlantic ridge vents (Williams & Rona 1986, Van Dover 1995, Van Dover et al. 2002, Desbruye ` res et al. 2000, Desbruye ` res et al. 2001). The two MAR-sites where this species has not been observed are the shallower vent fields Menez Gwen (860 m) and Lucky Strike (1,700 m). Although it was first believed that R. exoculata were present at the latter one (Van Dover et al. 1996), the existence of the shrimp at this site has not been reported after further expeditions (Table 1). Dense swarms of Rimicaris cf. exoculata were investigated at recently discovered hydrothermal vent fields along the southern Mid-Atlantic Ridge (Turtle Pits and Red Lion 5 ° S, 3,000m; References in Fig. 1 & Table 1). Recently, the existence of dense shrimp swarms at the active Kairei and Edmond hydrothermal vent fields (Central Indian Ridge, 2,451–3,320-m depth) (Fig. 1, Table 1) was described (Hashimoto et al. 2001a, Hashimoto et al. 2001b). Van Dover et al. (2001) reported that shrimp tissue from these sites is isotopically indistinguishable from those of R. exoculata on the Mid-Atlantic Ridge. Further studies demonstrated that the shrimp found at the Central Indian Ridge are very close to Rimicaris exoculata but still clearly distinguishable by some morphological differences and therefore classified as Rimicaris kairei (Watabe & Hashimoto 2002). The abundance of R. exoculata varies between different sites. For example, at Rainbow, shrimp assemble in depressions between chimney structures (Fig. 2B), whereas at TAG, black smoker complexes were almost entirely covered by dense agglomerations. Contrarily, at Broken Spur, low shrimp biomass was found (Copley et al. 1997). At the site Red Lion an unusual flange growth was investigated that appears to support a thriving shrimp community (Koschinsky et al. 2006). Other chimneys, that lack the flange growth, show a low abundance of Rimicaris cf. exoculata (Koschinsky et al. 2006). It is still unknown to what extent hydrothermal flow rates and composition influence the distribution of R. exoculata . However, they presumably play a role in the adaptation strategies of this species to such extreme environments. In particular, large variations in chemical composition of the endmember fluid have been observed between different MAR sites (Von Damm et al. 2001, Charlou et al. 2002, Douville et al. 2002). Rimicaris exoculata form large aggregations on solid sulfide surfaces around warm vent water emissions (Fig. 2). ...
Context 4
... vent shrimp Rimicaris exoculata dominates the vagile fauna at most Mid-Atlantic Ridge hydrothermal vent sites ( Fig. 1). This species lives within steep chemical and thermal gra- dients, where hot, reduced hydrothermal fluid mixes turbulently with oxygenated seawater. First described by Williams and Rona (1986), this species was observed to colonize black smoker complexes in the rift valley at the TAG site (26 ° 08.3 # N, 44 ° 49.6 # W; depth: 3,620–3,650 m). Rimicaris exoculata was subsequently found at several MAR-vent sites in the depth- range of 2,300–3,900 m (Rainbow, Broken Spur, TAG, Snake Pit, Logatchev, 5 ° S; Fig. 1, Table 1). In comparison with the hydrothermal environment on the East Pacific Rise where tubeworms, clams, and mussels dominate the vent fauna (Van Dover 1995), Rimicaris exoculata is by far one of the most abundant invertebrates at the Mid-Atlantic ridge vents (Williams & Rona 1986, Van Dover 1995, Van Dover et al. 2002, Desbruye ` res et al. 2000, Desbruye ` res et al. 2001). The two MAR-sites where this species has not been observed are the shallower vent fields Menez Gwen (860 m) and Lucky Strike (1,700 m). Although it was first believed that R. exoculata were present at the latter one (Van Dover et al. 1996), the existence of the shrimp at this site has not been reported after further expeditions (Table 1). Dense swarms of Rimicaris cf. exoculata were investigated at recently discovered hydrothermal vent fields along the southern Mid-Atlantic Ridge (Turtle Pits and Red Lion 5 ° S, 3,000m; References in Fig. 1 & Table 1). Recently, the existence of dense shrimp swarms at the active Kairei and Edmond hydrothermal vent fields (Central Indian Ridge, 2,451–3,320-m depth) (Fig. 1, Table 1) was described (Hashimoto et al. 2001a, Hashimoto et al. 2001b). Van Dover et al. (2001) reported that shrimp tissue from these sites is isotopically indistinguishable from those of R. exoculata on the Mid-Atlantic Ridge. Further studies demonstrated that the shrimp found at the Central Indian Ridge are very close to Rimicaris exoculata but still clearly distinguishable by some morphological differences and therefore classified as Rimicaris kairei (Watabe & Hashimoto 2002). The abundance of R. exoculata varies between different sites. For example, at Rainbow, shrimp assemble in depressions between chimney structures (Fig. 2B), whereas at TAG, black smoker complexes were almost entirely covered by dense agglomerations. Contrarily, at Broken Spur, low shrimp biomass was found (Copley et al. 1997). At the site Red Lion an unusual flange growth was investigated that appears to support a thriving shrimp community (Koschinsky et al. 2006). Other chimneys, that lack the flange growth, show a low abundance of Rimicaris cf. exoculata (Koschinsky et al. 2006). It is still unknown to what extent hydrothermal flow rates and composition influence the distribution of R. exoculata . However, they presumably play a role in the adaptation strategies of this species to such extreme environments. In particular, large variations in chemical composition of the endmember fluid have been observed between different MAR sites (Von Damm et al. 2001, Charlou et al. 2002, Douville et al. 2002). Rimicaris exoculata form large aggregations on solid sulfide surfaces around warm vent water emissions (Fig. 2). ...

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... Particularly important in explaining these small-scale patterns are the available concentrations of reduced chemical compounds (e.g. hydrogen sulfide, methane and hydrogen) that are involved in chemosynthetic pathways (Jannasch, 1985;Matabos et al., 2008;Schmidt et al., 2008;Luther et al., 2012) as well as those of metals and oxygen (Desbruyères et al., 2000;Cuvelier et al., 2011a;Martins et al., 2011;). Although vital for the hydrothermal fauna, these chemicals can also have deleterious effects, depending on their concentrations (Martins et al., 2011). ...
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Variations in reproductive patterns according to feeding strategies or food supply have been recognized in many animals from various ecosystems. Despite an unusual trophic structure, these relationships remain largely under-studied in chemosynthetic ecosystems. Here, we use Rimicaris shrimps as a study case to explore relations between reproduction, diets and food supply in these environments. For that, we compiled data on presence of reproductive individuals from the past 35 years and compared reproductive outputs of three shrimps differing by their diets and regions. We report distinct reproductive patterns between Rimicaris species according to their trophic regime regardless of variations related to body size. Besides, we observed a reproductive period mostly between January and early April whatever the region. Intriguingly, this periodicity does not correspond to seasonal variations with presence of ovigerous females during either boreal winter or austral summer. These observations contrast with the long-standing paradigm in deep-sea species for which periodic reproductive patterns have always been attributed to seasonal variations of photosynthetic production sinking from surface. Our results suggest the presence of intrinsic basis for biological rhythms in the deep sea, and bring to light the importance of having year-round observations in order to understand life history of vent animals.
... The shrimp Rimicaris exoculata dominates the faunal communities of several hydrothermal sites along the Mid-Atlantic Ridge (MAR) [2][3][4]. This species lives in dense aggregates in quite a warm part of the hydrothermal environment, 3-25°C, with nearly neutral pH [5], and slightly lower oxygen content than deep seawater [6]. It can be retrieved from geochemically contrasting environments. ...
... Both strains seem capable of using several electron donors. The detection, for the first time, of canonical cyc2 iron oxidizing genes (Additional File 12) in both MAGs strengthens the possibility that these epibionts oxidize iron, as suggested by several authors [5,8,14,21,23,24]. It is noteworthy that cyc2 genes, and splits containing them, showed a slightly lower average coverage compared with the remaining Zetaproteobacteria genes for RB_ MAG_00008 (Additional File 13A). ...
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Background Free-living and symbiotic chemosynthetic microbial communities support primary production and higher trophic levels in deep-sea hydrothermal vents. The shrimp Rimicaris exoculata , which dominates animal communities along the Mid-Atlantic Ridge, houses a complex bacterial community in its enlarged cephalothorax. The dominant bacteria present are from the taxonomic groups Campylobacteria , Desulfobulbia (formerly Deltaproteobacteria ), Alphaproteobacteria , Gammaproteobacteria , and some recently discovered iron oxyhydroxide-coated Zetaproteobacteria . This epibiotic consortium uses iron, sulfide, methane, and hydrogen as energy sources. Here, we generated shotgun metagenomes from Rimicaris exoculata cephalothoracic epibiotic communities to reconstruct and investigate symbiotic genomes. We collected specimens from three geochemically contrasted vent fields, TAG, Rainbow, and Snake Pit, to unravel the specificity, variability, and adaptation of Rimicaris –microbe associations. Results Our data enabled us to reconstruct 49 metagenome-assembled genomes (MAGs) from the TAG and Rainbow vent fields, including 16 with more than 90% completion and less than 5% contamination based on single copy core genes. These MAGs belonged to the dominant Campylobacteria , Desulfobulbia , Thiotrichaceae , and some novel candidate phyla radiation (CPR) lineages. In addition, most importantly, two MAGs in our collection were affiliated to Zetaproteobacteria and had no close relatives (average nucleotide identity ANI < 77% with the closest relative Ghiorsea bivora isolated from TAG, and 88% with each other), suggesting potential novel species. Genes for Calvin-Benson Bassham (CBB) carbon fixation, iron, and sulfur oxidation, as well as nitrate reduction, occurred in both MAGs. However, genes for hydrogen oxidation and multicopper oxidases occurred in one MAG only, suggesting shared and specific potential functions for these two novel Zetaproteobacteria symbiotic lineages. Overall, we observed highly similar symbionts co-existing in a single shrimp at both the basaltic TAG and ultramafic Rainbow vent sites. Nevertheless, further examination of the seeming functional redundancy among these epibionts revealed important differences. Conclusion These data highlight microniche partitioning in the Rimicaris holobiont and support recent studies showing that functional diversity enables multiple symbiont strains to coexist in animals colonizing hydrothermal vents.