The giant bathymodioline mussels from vents have been studied as models to understand the adaptation of organisms to deep-sea chemosynthetic environments. These mussels are closely related to minute mussels associated to organic remains decaying on the deep-sea floor. Whereas biological data accumulate for the giant mussels, the small mussels remain poorly studied. Despite this lack of data for species living on organic remains it has been hypothesized that during evolution, contrary to their relatives from vents or seeps, they did not acquire highly specialized biological features. We aim at testing this hypothesis by providing new biological data for species associated with organic falls. Within Bathymodiolinae a close phylogenetic relationship was revealed between the Bathymodiolus sensu stricto lineage (i.e. “thermophilus” lineage) which includes exclusively vent and seep species, and a diversified lineage of small mussels, attributed to the genus Idas, that includes mostly species from organic falls. We selected Idas iwaotakii (Habe, 1958) from this latter lineage to analyse population structure and to document biological features. Mitochondrial and nuclear markers reveal a north-south genetic structure at an oceanic scale in the Western Pacific but no structure was revealed at a regional scale or as correlated with the kind of substrate or depth. The morphology of larval shells suggests substantial dispersal abilities. Nutritional features were assessed by examining bacterial diversity coupled by a microscopic analysis of the digestive tract. Molecular data demonstrated the presence of sulphur-oxidizing bacteria resembling those identified in other Bathymodiolinae. In contrast with most Bathymodiolus s.s. species the digestive tract of I. iwaotakii is not reduced. Combining data from literature with the present data shows that most of the important biological features are shared between Bathymodiolus s.s. species and its sister-lineage. However Bathymodiolus s.s. species are ecologically more restricted and also display a lower species richness than Idas species.
Citation: Thubaut J, Corbari L, Gros O, Duperron S, Couloux A, Samadi S (2013) Integrative Biology of Idas iwaotakii (Habe, 1958), a ‘Model Species’ Associated with Sunken Organic Substrates. PLoS ONE 8(7): e69680. https://doi.org/10.1371/journal.pone.0069680
Editor: Donald James Colgan, Australian Museum, Australia
Received: February 12, 2013; Accepted: June 11, 2013; Published: July 24, 2013
Copyright: © 2013 Thubaut et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: This work was developed in the framework of the European research network DiWood (GDRE-CNRS 225), in collaboration with N. Lebris, was supported by a grant of Fondation pour la Recherche sur la Biodiversité (BioWood AAP-IN-2009-009) and by the ANR TF-DeepEvo (ANR-12-ISV7-0005-01). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Despite the number and variety of studies on organisms from deep-sea chemosynthetic environments, their evolutionary origins and the biological processes explaining their diversity remain poorly resolved . Among these organisms, bathymodioline mussels are studied as a model to elucidate the biological processes in vent and seep environments often designated as ‘extreme’ (e.g. , ). A comparative approach with the most closely related organisms from different environments is, however, required to understand the evolutionary significance of the organisms’ features in such ‘extreme’ environments. Distel et al. (2000)  were the first to show that bathymodioline mussels inhabiting vents and seeps form a monophyletic lineage with the modioline mussels associated with sunken organic substrates. This pioneering phylogenetic result implied the inclusion of the small and poorly-known deep-sea mussels from organic falls in the Bathymodiolinae. Recently, an evolutionary scenario was proposed in which sunken-wood is considered as an “early stage” towards adaptation to more extreme chemosynthetic environments in the deep-sea , . However, a recent molecular phylogenetic study, including more than 20 potentially new species associated with organic remains, suggested a more complex evolutionary scenario in which the history of hydrothermal vent and cold seep species is entangled with that of the small mussels associated with organic remains (Fig. 1) . Lorion et al. (2010)  confirmed that the vent and seep mussels are divided into several distinct lineages, among which the “thermophilus” group (i.e. Bathymodiolus sensus stricto since thermophilus is the type-species of the genus) is the most thoroughly-studied. This clade is closely related to a much more diversified lineage of small mussels, here provisionally attributed to the genus Idas, with most of the species associated with organic remains but also with a few from vents or seeps (Fig. 1). Unfortunately, biological data are scarce for most species within this lineage  and thus the evolutionary significance of biological features observed in vent and seep species is difficult to establish.
Asterisks correspond to nodes with posterior probabilities (PP) obtained from BA analysis and bootstrap values obtained from ML analysis that are higher than 0.90 and 50%, respectively. (modified from ).
One of the most striking feature discovered with these ‘extreme’ environments is symbiotic interactions with chemosynthetic bacteria , interpreted as a key adaptation of bathymodioline mussels to the particular environmental conditions of deep-sea vents and seeps. In Bathymodiolus s.s., chemosynthetic bacteria use reduced compounds such as hydrogen sulphide (H2S) and/or methane (CH4) to gain energy and for carbon fixation from dissolved CO2 or methane providing a source of carbon to their host . Most species within Bathymodiolus s.s. have both sulphur- and methane-oxidising symbionts, (e.g. ). Hydrogen was also recently shown to be an additional energy source for the sulphur-oxidising symbionts of Bathymodiolus (s.s.) puteoserpentis . In all species, bacteria are located within the gill epithelial cells suggesting a tight relationship between metazoan and bacterial partners. Moreover for several Bathymodiolus s.s. species, the digestive tract is reduced – and it has been hypothesized that filter-feeding plays only a minor role in the diet compared to the food supply offered by their symbionts, especially in deeper-dwelling species.
By contrast, for the small species within the sister lineage of Bathymodiolus s.s, data about symbiosis are only available for two cold seep species (Idas modiolaeformis: , ; I. macdonaldi: ) and for three species associated with organic remains (Idas washingtonius on whale bone: –; Idas sp. D on wood falls:  and Idas sp. C on both wood and bone: ). Located on gills, symbiotic bacteria are intracellular in I. washingtonius and I. macdonaldi but extracellular for I. sp. D and I. sp. C. Up to six different bacteria were observed in the gills of the seep species I. modiolaeformis , , meanwhile other species seem to harbour only sulphur-oxidisers. No data are available concerning the anatomy of the digestive tracts of Idas species.
Larval dispersal is a key issue for understanding the evolutionary success of specialized species, because hydrothermal vents and cold seeps are patchily distributed over large distances . In bivalves, larval dispersal capability can be inferred, to a certain extent, from larval shell morphology. Indeed since the size of the prodissoconch I and of the oocyte are correlated, the size of the prodissosconch II relative to that of the prodisoconch I is indicative of the time spent in plankton by larvae . Most bathymodioline species are considered planktotrophic because of their small egg size and prodissoconch morphology. Moreover, evidence for long-distance dispersal is available for several Bathymodiolus s.s. species –. The distribution of organic falls is patchy, but accumulations of vegetal remains are predictably found in the vicinity of tropical islands . Several species associated with wood falls can also prosper on animal remains . Thus, animal remains (notably the carcasses of large marine vertebrates), although not predictably located, are spread throughout the sea floor  and may constitute steps for dispersal among distant locations.
No study has yet documented population connectivity patterns among mussels associated with organic remains. We selected the species Idas iwaotakii to initiate such studies. This species was frequently sampled during the cruises of the Tropical Deep-sea Benthos program . It has been found mainly on wood susbtrates, but also occurs on turtle bones . It is distributed throughout the south-western Pacific. I. iwaotakii is divided into two genetic lineages , . While the first has only been found in Japan and the Philippines, the second was found throughout the Western Pacific (sampled in Japan, Vanuatu and New Caledonia).
To document connectivity patterns in I. iwaotakii, we describe larval development and morphology of prodissoconchs and infer the genetic structure of populations at different geographic scales considering two environmental factors (depth and organic substrate type). We describe the bacteria associated with the gill tissue and describe the structure of the digestive tract to infer the nature of its diet. We also re-evaluate the evolutionary significance of features often presented as adaptation to extreme environments by comparing the biological features revealed here with those available for other species within the same clade (I. modiolaeformis, I. macdonaldi and I. washingtonius) or for species of Bathymodiolus s.s.
Materials and Methods
Specimens were collected during recent cruises of the Tropical Deep-sea Benthos program  off the Solomon Islands (2004), Vanuatu (2005, 2006), the Philippines (2005, 2007), New Caledonia (2008) and Papua New Guinea (2010) . Part of the material has already been used as described in Lorion et al. (2009, 2010) , . The studied organisms are not protected and do not require specific export permits. Research permits were obtained for the EEZ of each country. In the Solomon Islands and Vanuatu, officers from Fisheries departments collaborated on the cruises. In the Philippines and Papua New Guinea, cruises were organised under a Memorandum of Understanding with Bureau of Fisheries and Aquatic Resources and the University of Papua New Guinea respectively. Collecting in New Caledonia was done within the French EEZ with a French vessel and no permit was required at the time of the cruises. Mussels were collected by trawling and dredging between 460 m and 2,307 m depth. Sampling locations include the Philippines (7 specimens), Papua-New Guinea (9 specimens), the Solomon Islands (12 specimens), Vanuatu (48 specimens) and New Caledonia (22 specimens) (Table 1 and Fig. 2). Specimens were preserved in 80% EtOH and are deposited in the collections of the Muséum National d’Histoire Naturelle (MNHN).
Larval shell observation.
The prodissoconchs of 15 specimens (sample ID: MNHN-IM-2009–22278 to MNHN-IM-2009–22292) from New Caledonia were coated with gold-palladium and examined under a JEOL JSM-840A scanning electron microscope (SEM) operating at 80 kV. Shells were subsequently measured and described.
The specimen used to study the localisation of symbiotic bacteria was collected off Vanuatu in association with coconut fibers. Gills were pre-fixed at sea in cacodylate-buffered 2% glutaraldehyde for two hours at room temperature (RT) and briefly rinsed in a fresh volume of the same buffer. Gills were stored at RT in that buffer until they were brought to the laboratory a few weeks later. Samples were then fixed for 45 minutes at RT in 1% osmium tetroxide in the same buffer, rinsed in distilled water and post-fixed with 2% aqueous uranyl acetate for one hour before embedding in Epon-Araldite by the method of Mollenhauer described by Glauert (1975) .
Two specimens (sample ID: MNHN-IM-2009–22293 and MNHN-IM-2009–22294, preservation in 80% ethanol), were chosen for the analysis of the digestive tract structure, both living on turtle bone off New Caledonia. Digestive tracts of specimens (n = 2) were observed in longitudinal sections, and cross sections. Mussels were removed from their shell and whole individuals were first fixed in phosphate-buffered 2% glutaraldehyde for two hours at room temperature, and post-fixed in 1% osmium in phosphate for one hour. Samples were washed with phosphate Sörensen buffer (TPS), dehydrated through a graded ethanol series and then embedded in Spurr’s resin (Spurr, 1969) . Semi-thin (0.5–1 µm) and ultra-thin sections (500 nm) were obtained with a Reichert-Jung ultramicrotome (Ultracut E). Semi-thin sections were stained with toluidine blue (pH 9.0) for observation under a light microscope (LM) (Coolscope, Nikon). Ultra-thin sections were stained with uranium acetate and lead citrate as contrast agents and examined with a Jeol (JEM 2000 FX) transmission electron microscope (TEM).
PCR Amplification, Cloning and Sequencing
DNA was extracted either from the gills of large individuals or from entire specimens using the QIAmp® DNA Micro Kit (Qiagen). For all specimens, a 579 bp fragment of the Cytochrome Oxydase I (COI) mitochondrial gene was amplified using primers LCOI 1490  and H691 5′-GTRTTAAARTGRCGATCAAAAAT-3′ . For selected individuals representing distinct COI haplotypes, a 999 bp fragment of the 28S rRNA nuclear gene corresponding to the domains D1, D2 and D3 was amplified using the primers C1’ (5′-ACCCGCTGAATTTAAGCAT-3′) and C4 (5′-TCGGAGGGAACCAGCTACTA-3′). PCR reactions were performed in a final volume of 25 µL containing approximately 3 ng of template DNA, 1.5 mM of MgCl2, 0.26 mM of each dNTP, 0.3 µM of each primer, 5% DMSO, and 0.75 unit of Taq polymerase (Qbiogene). Amplicons were generated by an initial denaturation step of 4 min at 94°C followed by 35 cycles of denaturation at 94°C for 40 sec, annealing at 50°C for COI and 52°C for 28S for 50 sec, and extension at 72°C for 1 min; and a final elongation at 72°C for 10 min.
The bacterial gene encoding 16S rRNA, used for the characterisation of bacterial communities, was amplified as described in Duperron et al. (2005) . Symbiont diversity was evaluated for six specimens: two from the Philippines, two from Vanuatu (sunken wood) and two from New Caledonia (turtle bone). For each specimen, five PCR products were pooled and purified (Montage PCR kit, Millipore) prior to cloning using the QIAGEN PCR Cloning Kit. Inserts from a total of fifty positive clones were amplified using the plasmid-specific primers M13F and M13R.
PCR products were purified with AMPure XP beads, cycle-sequenced using the ABI BigDye Terminator v3.1 Cycle Sequencing Kit (1/32 reactions), and purified using an EtOH/sodium acetate precipitation. These products were then electrophoresed on an ABI PRISM (R) 3730×l Genetic Analyzer.
Genetic structure of mussel populations.
Sequences were edited using Sequencher 4.1.4 and aligned using the Clustal W module implemented in Mega 4.0 . Sequences were deposited both in BOLD and GenBank (COI: KC861674-KC861725; 28S: KC861726-KC861749 and KC904226-KC904234).
For the COI dataset, for each locality, the number of haplotypes (Hap), the number of segregating sites (Seg), haplotype (Hd) and nucleotide (Pi) diversity were determined using Arlequin 220.127.116.11 . Phylogenetic relationships among haplotypes were constructed using the Median-Joining algorithm  and maximum parsimony post-processing calculation  implemented in Network 18.104.22.168 (http://www.fluxus-engineering.com).
FST was estimated among sampling locations using the formula of Weir and Cockerham (1984)  to assess population genetic structure. These calculations were based both on haplotype frequencies and on their pairwise nucleotide differences. A distribution of FST values under the null hypothesis of spatial genetic homogeneity was drawn from 10,000 datasets simulated by permutations of specimens between south-western localities. Genetic structure was also analysed with an exact test of differentiation using a Markov chain process with a burnin of 1000 steps. An Analysis of Molecular Variance (AMOVA; ) was performed among populations of the south-western part of the sampling region (Papua New Guinea, the Solomon Islands, Vanuatu and New Caledonia). An AMOVA was also assessed in order to evaluate hypothesised patterns of bathymetric genetic structure by using two depth categories (sampling<and >600 m). All tests were performed in Arlequin 22.214.171.124 .
Tajima’s D  and Fu’s FS  statistics were calculated to trace demographic events. Their statistical significance at alpha = 5% was estimated with a permutation test (10,000 replicates). Tests were performed for south-western localities, and for groups of localities among which no structure was detected. The parameters of a demographic expansion model, including the expansion factor (τ), the mutation parameter (θ = 2 µN, where µ is the mutation rate and N is the effective population size) initial (θ0) and actual (θ1) of the south-western populations were estimated using Arlequin. These estimators were used to plot the distribution of the number of pairwise differences between mitochondrial sequences (‘mismatch distributions’) based on Slatkin and Hudson (1991)  for south-western Pacific populations. Under the coalescent model modified from Hudson (1990)  1,000 replicates were carried out to calculate parameters, to define 99% confidence intervals, and to calculate the sum of squared deviations (SSD) of these parameters between the observed and estimated mismatch distribution.
Phylogenetic relationships at the intra-specific level were inferred from COI sequences. A sequence of the species I. macdonaldi (AY649804), which belongs to the same clade as I. iwaotakii, was added to the dataset as an outgroup. A phylogenetic tree based on the neighbour-joining (NJ) method of Kimura two-parameter (K2P) distances was built using MEGA version 4.0 . The bootstrap analysis was based on 1000 replicates.
The sequences obtained for the bacterial 16S fragment were aligned using the Clustal W module implemented by Mega 4.0 . Sequences with ≥99% identity were considered as a single phylotype and a single representative clone from each phylotype was chosen for phylogenetic analysis. Sequences were deposited on GenBank (KC904235-KC904238). Sequences were compared with the NCBI (http://www.ncbi.nlm.nih.gov/) database using BLAST . The most similar BLAST sequences were included in phylogenetic analysis. Phylogenetic reconstructions were performed using maximum likelihood (ML) and Bayesian (BA) analyses.
The most appropriate evolutionary model was estimated using jModelTest 0.1.1. The GTR+I+Γ model was chosen based on AIC. The ML analysis was performed using the software Treefinder  and node support was assessed with 1,000 bootstrap replicates . BA was performed using MrBayes v3.1.2 . Two independent analyses were run in parallel. Each analysis comprised four Markov chains and each chain was run over 8 million generations with a sampling frequency of one tree every hundred generations and a burnin period of 40,000 generations. Convergence between the two analyses was assessed using likelihood curves, standard deviation of split frequencies and potential scale reduction factor .
Genetic Diversity and Phylogenetic Analyses
A total of 50 COI mtDNA sequences of 579 bp were obtained. Moreover, 53 sequences available on Genbank were added to this new dataset for the analyses. Because the three sequences available on Genbank for Japan specimens are 430 bp (AB257520, AB257521 and AB257523)  and haplotype network reconstructions are sensitive to missing data, this analysis was performed on a reduced dataset of 430 bp long, in order to include as many specimens as possible. For each locality, the number of haplotypes (h), the haplotype (Hd) and nucleotide (π) diversities and the number of segregating sites (S) are given in Table 2. Indexes of diversity were low except for nucleotide diversity in populations from Japan, the Philippines and Papua New Guinea (4.467, 2.429 and 2.500 respectively). The neighbour-joining (NJ) tree constructed from unique COI haplotypes splits the specimens into the two clusters detected in previous studies , . The first (A’’) includes specimens from the north-western localities only (two specimens from Japan and seven from the Philippines), and the second (A’) pools all specimens from the south-western localities (Papua New Guinea, the Solomon Islands, Vanuatu and New Caledonia) but also four specimens from Japan and one from the Philippines (Fig. 3).
Left part: K2P neighbour-joining tree of unique COI haplotypes of I. iwaotakii. The localities at which each haplotype have been sampled is figured by a coloured circle (see legend for correspondence between localities and colours), the number of individuals sharing the same COI haplotype at each locality is given in brackets. The grey rectangles underline the haplotypes shared by the two studied regions. The scale bar represents 0.02% estimated base substitutions. The mitochondrial haplotypes of I. iwaotakii are divided in two clades, A’ and A’’, represented by one panel with large dots and the other one with small dots, respectively. Right part: Median-joining networks (MJN) from COI mtDNA data drawn independently for each of the two studied regions (North Western and South Western haplotypes). Size of haplotype circles is proportional to the number of specimens. Colours used to figure the localities within each region are the same of that used for the NJ tree. A small black circle represents a hypothetical haplotype. The haplotypes shared by the two studied regions are underlined using grey circles over haplotype labels.
Two separate median-joining networks were computed for the north-western and south-western regions, as these locations harboured distinct phylogenetic lineages and the sampling effort was very unbalanced between the two regions. In agreement with the NJ analysis, median-joining networks revealed the co-occurrence of both lineages in the Northwest (Fig. 3). The south-western median-joining network displayed a ‘star-like’ topology with one central and common/ancestral haplotype surrounded by several rare, derived haplotypes. Two 28S haplotypes, separated by one substitution, were obtained from 34 specimens. The first haplotype was represented by 25 specimens from the south-western area (lineage A’), two from Japan (one specimen from lineage A’ and one from lineage A’’) whereas the second haplotype was represented by seven specimens from the Philippines (lineage A’’). The Northwest (Japan and the Philippines) and the south-west areas (other localities) were significantly differentiated (FST = 0.61485, p-value <0.001). FST tests were not significant among localities within each of these two areas. The only significant exact tests (results not shown) were obtained when comparing the Philippines sample with the south-west localities. The non significance of the exact tests performed between Japan and any other locality should be interpreted with caution given the small sample size and the co-occurrence of the two lineages in Japan. No significant population structure was detected among south-western localities (AMOVA results - geography: FST = −0.00540, p-value = 0.7; bathymetry FST = −0.00398, p-value = 0.6; Table 3).
Tajima’s D and Fu’ FS statistics were negative for each of the south-west localities (except D for Papua New Guinea and Malekula), pointing to significant evidence of population expansion (Table 4). When grouping localities according to the genetic structure, both tests remained significantly negative for the south-west. Observed mismatch distributions were unimodal and not statistically different from the simulated distribution under an expansion model (Fig. 4).
COI haplotypes observed, simulated under a constant population size and a model of population expansion for the South-west Pacific populations of A. iwaotakii. Along x-axis are indicated the numbers of nucleotide differences between all pairs of sequences and on y-axis the frequencies of pairs. The table summarizes the parameters of demographic analyses under constant population size and demographic expansion. The confidence intervals at 99% of the parameters under a demographic expansion model are given in square brackets.
Larval Shell Morphology
Larval shells (prodissoconchs) were 544.33 µm (SD: ±37.58) in diameter, had a reddish colour and were easily distinguishable from the yellowish post-larval shell (dissoconch). The prodissoconchs II displayed numerous concentric lines (Fig. 5A); whereas the prodissoconchs I, situated close to the umbo, had a granulated texture and were 74.05 µm (SD: ±9.35) in diameter (Fig. 5B). The size of the prodissoconchs I, which corresponds to the early stages of veliger larvae, is directly related to that of the oocytes. The small size of the prodissoconchs I compared to the prodissoconchs II, suggested the absence of a yolky egg. Prodissoconch II records the duration of pelagic larval life. Thus, the well-developed prodissoconchs II observed here suggested that larvae spend a significant part of their life in the plankton. The few available data on related species suggested that these larvae could have dispersed over hundreds of kilometres .
Pictures: (A) Dorsal view showing prodissoconch I (PI) and prodissoconch II (PII); the white arrow indicates the boundary between the dissoconch and prodissoconch, (B) Detail of PI; the grey arrow indicated of the boundary between PI and PII.
Symbiont Diversity and Phylogeny Based on 16S rRNA Gene Sequence Analysis
The bacterial 16S rRNA alignment was 1459 bp long, and included 50 sequences corresponding to 9 phylotypes. A GenBank BLAST analysis revealed that phylotypes 1, 2, 3 and 4 were >97% similar to thiotrophic symbionts of bathymodioline mussels. Among those, phylotype 1 was dominant, represented by 35 clones from all analysed specimens (i.e. independently of locality and substrate). Phylotypes 2 and 3, each represented by 2 clones, were recovered from two specimens from the Philippines. Phylotype 4, including 6 clones, was recovered from only one specimen from the Solomon Islands and one from New Caledonia.
The five other phylotypes were singletons and bear no resemblance with mussel symbionts (results not shown). They most likely represent environmental bacteria, as they were >97% similar to Proteobacteria (epsilon- and gamma-Proteobacteria), Planctomycetes, and Bacteroidetes (Cytophaga Flavobacter Bacteroides, or CFB) that are also commonly found at/near vent communities.
Only thiotrophic symbiont sequences (corresponding to phylotypes 1 to 4) were included in the phylogenetic analyses. Trees were rooted on the methanotrophic symbiont of B. brooksi , . The topologies of the ML and BA reconstructions were identical, and confirmed that phylotypes 1 through 4 belonged to a single large clade which included all known thiotrophic symbionts of the Bathymodiolinae and other mussels from sunken organic substrates (Fig. 6). Moreover, these four phylotypes are resolved within a group of symbionts of organic falls mussels. The four phylotypes were closely related to symbionts of tiny mussels associated with sunken wood from the Philippines (AM503926, AM851093)  and to the symbionts of G. crypta and I. sp. C from Vanuatu .
Phylotypes associated with I. iwaotakii are shown in bold. Posterior probabilities (PP) and bootstrap values obtained from ML analysis are given above and below branches respectively. PP and bootstrap values lower than 0.90 and 50%, respectively, are not shown. The scale bar represents 0.5% estimated base substitution.
Localisation of Associated Bacteria
TEM observations of sections of gill filaments indicated the presence of extracellular, gram negative bacteria located between the microvilli of the host cells, throughout the lateral zone of each gill filament (Figs 7A–B).
(A) TEM view of gill filament of the lateral zone from a specimen of I. iwaotakii collected on wood off Vanuatu. Bacteria (black arrows) are located extracellularly in contact with microvilli. BL: blood lacuna; Lm: basal lamina. (B) Electron micrograph of the extracellular symbionts. Symbiotic bacteria possess a double membrane (white arrow) typical of Gram negative bacteria.
Digestive Tract Structure
LM observations of semi-thin sections of the digestive system revealed the presence of typical features of bivalve digestive tract consisting of an oesophagus, a stomach, an intestine and a well-differentiated digestive gland that surrounds the stomach and a part of the intestine. In all observed specimens: the unilaminar prismatic epithelium of the oesophagus had ciliated cells (Fig. 8B); the stomach epithelium had cubic cells (Fig. 8D) and a chitinous area corresponding to the gastric shield; the prismatic epithelium of the intestine (Fig. 8C) displayed a high density of microvilli. The digestive tract was curved and formed at least one loop (Fig. 8A). Both LM and TEM observations revealed the presence of digestive contents in the stomach and the intestine. The alimentary bolus was nevertheless difficult to identify. One rigid structure, about 296 µm wide and little damaged by digestion, could be identified as a foraminiferan test (Fig. 8E).
The specimen was collected on turtle bone off New Caledonia. (A) Overall view of the digestive tract (longitudinal sections). The black arrow indicates the location of microvilli in the intestine. (B) Cross section of the oesophagus lined by a stratified epithelium. (C) Cross section of the intestine. (D) Cross section of the stomach lined by a cuboidal epithelium. The white arrow indicates the gastric shield. (E) Longitudinal section of a detail of intestinal contents.
Genetic Divergence, Population Connectivity, and Demographic History
Our study confirms that Idas iwaotakii populations are divided into two distinct mitochondrial lineages, A’ and A’’, and confirmed their coexistence in Japan. But, although we confirm that specimens from the lineage A’’ from the Philippines have a distinct 28S rRNA haplotype, we show that in Japan, specimens from both A’ and A” lineages share the 28S rRNA haplotype typically associated with A’ in the south-western area. The combination of nuclear and mitochondrial data on a larger number of mussels thus suggests that the two mitochondrial lineages are not, as it has been hypothesised before , reproductively isolated.
At the regional scale (SW Pacific) the sampling of I. iwaotakii initiated by Lorion et al. (2009, 2010) ,  is improved here. Although the localities are separated by 500 km (New Caledonia/Vanuatu) to 2400 km (New Caledonia/Papua New Guinea), no genetic structure was detected. Moreover, our sampling effort covers a wide depth range, and the recruitment experiments deployed off New Caledonia allowed us to collect I. iwaotakii on bone, a substrate much more difficult to locate than sunken wood. Indeed, trees and other plant substrates can reliably be found in the vicinity of islands and continents skirted with well-developed coastal forests, whereas the distribution of skeletal remains has an unpredictable, idiosyncratic distribution. The New Caledonian specimens sampled from turtle bones show no genetic difference from other samples collected from sunken-wood at other localities. Similarly, no genetic structure is detected over a large bathymetric range (i.e. 460 m –2,307 m). Thus, I. iwaotakii is a widespread species that may colonise, over a wide depth range, organic substrates such as sunken-wood and bone . These results are congruent with those available for other species associated to organic remains (i.e. I. sp. C and G. crypta ).
The absence of genetic structure between south-western sampling localities suggests either high larval dispersal ability and an absence of barriers to dispersal or historical connectivity still detectable with COI and 28S. These results are consistent with the long larval stage here inferred from the size of prodissoconch II, and documented for close relatives from hydrothermal vent and cold seep environments. Indeed, larvae from B. azoricus could remain in the water column for 5 to 6 months , . Evidence of long-distance dispersal has also been found for I. modiolaeformis, I. argenteus and other Bathymodiolinae , , , –. Notably, Lutz et al. (1980)  revealed that B. thermophilus produces large numbers of small eggs that develop into planktotrophic larvae and potentially disperse over long distances. The assumption of large-scale dispersal ability is supported by the high gene flow documented among B. thermophilus populations from 13°N to 11°S latitude on the East Pacific Rise (∼ 2,500 km) , . Vents, seeps and organic remains, are patchy and often ephemeral habitats. In such highly fragmented habitats, establishment and maintenance of populations probably relies on the long, free-swimming, larval stage that in turn might also explain the wide geographical distribution of most species.
Based on our genetic data, we hypothesise that a small number of migrants from the northwest area have recently founded new successful populations in the south-western area. The association of a demographic expansion signal and a reduction of the genetic diversity in the southern populations support this hypothesis. However, this pattern is also consistent with allopatric divergence followed by secondary contact. The complex history of the Western Pacific, marked by tectonic plate movement (e.g. , ), volcanism and periodic sea level changes (e.g. ), might have impeded larval dispersal, during some periods, and thus favoured the emergence of new lineages through founder events but also the secondary contacts among isolated populations.
Geographic breaks between pairs of closely related species have been repeatedly documented in both Bathymodiolus s.s and Idas lineages. In Idas, the cold seep species I. modiolaeformis and I. macdonaldi (3.3% divergent at COI), were proposed as a potential amphi-Atlantic species-complex . In the Bathymodiolus lineage, the same was proposed for the seep complex of species B. boomerang and B. aff boomerang (2% divergent at COI, , ). Two pairs of vent species have a geographic structure along a mid-oceanic ridge system. The two sister-species B. thermophilus and B. antarcticus are respectively distributed in the Galapagos rift to the North and not to the South of the East Pacific Rise , , . Similarly the sister-species B. azoricus and B. puteoserpentis are respectively distributed in the North and in the South part of the Mid Atlantic Ridge , . However, in the Indo-West Pacific, the populations attributed to B. septemdierum, B. brevior and B. marisindicus, are not reproductively isolated and display no genetic structure over a very wide geographical area (see ).
Symbiotic Association and Insights into Nutritional Features of I. iwaotakii
In previous studies , , , thioautotrophic symbionts have predictably been found in each newly examined deep-sea mussel associated with organic remains. This new dataset supports this predictability and moreover shows that, within a species, the same dominant bacterial phylotype is found, independent of geographic location (the Philippines, Vanuatu and New Caledonia), substrate type (wood versus bone) or depth (441 m to 1767 m). This dominant phylotype is closely related to a symbiont detected in another species within the Idas lineage (I. sp. C) and also in another species from a distinct lineage (G. crypta) . These two species were also collected both on wood and bone. Phylogenetic relationships among sulphur-oxidizing symbionts are however poorly resolved. This lack of resolution is probably due to the relatively slow evolution rate of the 16S rRNA. More variable genetic markers have to be developed to better resolve symbiont phylogeny.
Electron microscopic analyses confirm the presence and abundance of bacteria in association with gill filaments. The bacteria are extracellular and are thus directly exposed to the reduced compounds from decaying organic remains. The extracellular localisation of symbionts has already been documented for other mussels associated with wood falls, notably for the Idas lineage in I. sp. C and I. sp. D , , , . By contrast, the symbionts of bathymodioline mussels from hydrothermal vents and cold seeps are mostly intracellular. Likewise, I. washingtonius, which is associated with whale bone, possesses intracellular bacteria located within gill bacteriocytes , . Thus, by contrast with the species included in Bathymodiolus s.s. lineage, the species included in the Idas lineage harbour either intracellular symbionts (I. macdonaldi or I. washingtonius)  or extracellular symbionts (I. iwaotakii, I. sp. C and I. sp. D) , . As I. washingtonius is sampled on organic remains, we suggest that the extra- or intra-cellular location of the bacteria is not strictly related to the environments as was previously suggested , .
Bathymodioline mussels possess a functional but considerably reduced digestive tract –. Some Bathymodiolus species (B. boomerang, B. heckerae, B. brooksi, B. thermophilus and B. aff. thermophilus) have a simple digestive tract with a small stomach and a straight midgut without any coiling or loop , , . Others such as B. azoricus and B. puteoserpentis have a coiled intestine and well-developed labial palps , . Intestines with recurrent loops have been observed in seeps specimens of I. macdonaldi . Based on stable isotope measurements, Deming et al.  suggested that I. washingtonius, may have a mixotrophic nutritional strategy involving both filter feeding and supply from symbionts. I. iwaotakii has a coiled intestine. Digestive contents were relatively abundant and varied. For example a rigid structure found in the intestine could be a foraminiferan test resembling Spiroplectammina taiwanica (Chang, 1956) (; see figures 29 A and B). Le Pennec and Prieur (1984)  also identified the tests of benthic Foraminifera and diatom frustules in the stomach contents of vent mytilids.
Overall, sulphur-oxidizing symbionts closely related to those previously identified in Bathymodiolinae are present in the gills of I. iwaotakii and the digestive tract is non-reduced and functional. These mussels associated with organic falls are thus potentially able to obtain carbon and other nutrients either from their autotrophic symbionts and/or by filter feeding. A longer intestine with recurrent loops suggests a significant contribution of filter feeding to the mussels’ diet, likely supplemented by nutrition derived from symbiont chemoautotrophy (e.g. ). The relative contribution of each pathway remains to be quantified. The concentration of hydrogen sulphide (H2S) available in the environment determines the ability of bacterial symbionts to provide food supply. Concentrations of reduced compounds probably vary depending on quantity, nature and state of degradation of the available organic substrates (e.g. ). A mixed diet might allow individuals to adapt to high variability in the availability of reduced compounds.
Evolutionary Significance of Biological Features Related to Environments
Although living on organic remains, Idas iwaotakii shares many biological similarities with the large mussels of Bathymodiolus s.s living in either vents or seeps: (i) association with chemoautotrophic symbionts, (ii) high larval dispersal and (iii) lack of geographical genetic structure. However, I. iwaotakii apparently accommodates to a wider range of ecological conditions than Bathymodiolus s.s. species (Fig. 9). Indeed, I. iwaotakii displays a very wide geographical distribution and a large bathymetrical range, has probably a mixed diet and is able to colonise various organic substrates (i.e. bone and vegetal remains). By contrast, Bathymodiolus s.s. species are restricted either to vents or seeps but are never found in both habitats nor on organic remains. This contrasts with giant mussels belonging to the “childressi” group that, like Bathymodiolus (sensus lato) platifrons or B. (s.l.) japonicus are found both at vent and seep sites . The straight intestine evidenced for most Bathymodiolus s.s. species suggests a greater dependency on the food supply provided by their autotrophic symbionts. This dependency may explain why they are restricted to habitat in which the reduced compounds remain available regularly, even if at variable concentrations.
The “thermophilus” lineage is represented by the dark grey rectangle and its sister lineage, corresponding to the genus Idas, by the light grey rectangle. Phylogenetic relationships correspond to a part of the combined COI mtDNA and 28S RNA phylogenetic tree from . T: thiotrophic symbiont; M: methanotrophic symbiont. In geographical patterns section, the ovals correspond to pairs of sister-species with an allopatric distribution and location maps illustrate the allopatric distribution of these sister pairs. References: –, , , , , –, , , –, , , , –.
New material was collected on board of M/VDA-BFAR (PANGLAO 2005, Co-PI P. Bouchet and L. Labe and Aurora 2007, Co-PI M. Manuel, and P. Bouchet) and on board of R/V Alis (BOA1, Co-PI B. Richer de Forges and S. Samadi; SANTO2006, Co-PI P. Bouchet, O. Pascal and H. Le Guyader; Salomon2, Co-PI B. Richer de Forges and P. Bouchet, Biopapua, Co-PI S. Samadi and L. Corbari). Sincere thanks to J. Lorion for his keen insight and his support, C. Djediat for his assistance with microscopic experiments and analysis, B. Buge for curation of specimens and the staff of the “Service de Systématique Moléculaire” (UMS2700 CNRS-MNHN). It is part of the agreement no.2005/67 between the Genoscope and the Museum National d’Histoire Naturelle on the project ‘Macrophylogeny of life’ directed by G. Lecointre. Special thanks to E. Pante for constructive comments and English improvement of the manuscript.
Conceived and designed the experiments: JT SS. Performed the experiments: JT LC OG SD AC SS. Analyzed the data: JT LC OG SD SS. Contributed reagents/materials/analysis tools: JT LC OG SD SS. Wrote the paper: JT SS.
- 1. McClain CR, Hardy SM (2010) The dynamics of biogeographic ranges in the deep sea. Proc R Soc B 277: 3533–3546
- 2. Tanguy A, Bierne N, Saavedra C, Pina B, Bachcre E, et al. (2008) Increasing genomic information in bivalves through new EST collections in four species: Development of new genetic markers for environmental studies and genome evolution. Gene 408: 27–36
- 3. Bettencourt R, Costa V, Laranjo M, Rosa D, Pires L, et al. (2011) Out of the deep sea into a land-based aquarium environment: investigating physiological adaptations in the hydrothermal vent mussel Bathymodiolus azoricus. ICES J Mar Sci 68: 357–364
- 4. Distel DL, Baco AR, Chuang E, Morrill W, Cavanaugh C, et al. (2000) Do mussels take wooden steps to deep-sea vents? Nature 403: 725–726
- 5. Miyazaki JI, Martins LdO, Fujita Y, Matsumoto H, Fujiwara Y (2010) Evolutionary process of deep-sea Bathymodiolus mussels. PLoS ONE 5(4): e10363
- 6. Fujiwara Y, Kawato M, Noda C, Kinoshita G, Yamanaka T, et al. (2010) Extracellular and mixotrophic symbiosis in the whale-fall mussel Adipicola pacifica: a trend in evolution from extra- to intracellular symbiosis. PLoS ONE 5(7): e11808
- 7. Lorion J, Buge B, Cruaud C, Samadi S (2010) New insights into diversity and evolution of deep-sea Mytilidae (Mollusca: Bivalvia). Mol Phylogenet Evol 57: 71–83
- 8. Duperron S, Lorion J, Samadi S, Gros O, Gaill F (2009) Symbioses between deep-sea mussels (Mytilidae: Bathymodiolinae) and chemosynthetic bacteria: diversity, function and evolution. C R Biol 332: 298–310
- 9. Won YJ, Jones WJ, Vrijenhoek RC (2008) Absence of cospeciation between deep-sea Mytilids and their thiotrophic endosymbionts. J Shellfish Res 27: 129–138.
- 10. Petersen JM, Zielinski FU, Pape T, Seifert R, Moraru C, et al. (2011) Hydrogen is an energy source for hydrothermal vent symbioses. Nature 476: 176–180
- 11. Le Pennec M, Prieur D (1984) Observations sur la nutrition d'un mytilidae d'un site hydrothermal actif de la dorsale du Pacifique oriental. C R Acad Sci Ser III Sci Vie 298: 493–498.
- 12. Hily A, Le Pennec M, Prieur D, Fiala-Medioni A (1986) Anatomie et structure du tractus digestif d'un Mytilidae des sources hydrothermales profondes de la ride du Pacifique oriental. Cah Biol Mar 27: 235–241.
- 13. Page HM, Fisher CR, Childress JJ (1990) Role of filter-feeding in the nutritional biology of a deep-sea mussel with methanotrophic symbionts. Mar Biol 104: 251–257.
- 14. Gustafson RG, Turner RD, Lutz RA, Vrijenhoek RC (1998) A new genus and five new species of mussels (Bivalvia, Mytilidae) from deep-sea sulfide/hydrocarbon seeps in the Gulf of Mexico. Malacologia 40: 63–112.
- 15. Pile AJ, Young CM (1999) Plankton availability and retention efficiencies of cold-seep symbiotic mussels. Limnol Oceanogr: 1833–1839.
- 16. Duperron S, Halary S, Lorion J, Sibuet M, Gaill F (2008) Unexpected co-occurrence of six bacterial symbionts in the gills of the cold seep mussel Idas sp. (Bivalvia: Mytilidae). Environ Microbiol 10: 433–445
- 17. Lorion J, Halary S, do Nascimento J, Samadi S, Couloux A, et al. (2012) Evolutionary history of Idas sp. Med, (Bivalvia: Mytilidae), a cold seep bearing multiple symbiont. Cah Biol Mar 53: 77–87.
- 18. Deming JW, Reysenbach AL, Macko SA, Smith CR (1997) Evidence for the microbial basis of a chemoautotrophic invertebrate community at a whale fall on the deep seafloor: bone-colonizing bacteria and invertebrate endosymbionts. Microsc Res Techniq 37: 162–170.
- 19. Baco-Taylor AR (2002) Food-web structure, succession, and phylogenetics on deep-sea whale skeletons. PhD Thesis, the University of Hawaii.
- 20. Baco AR, Smith CR (2003) High species richness in deep-sea chemoautotrophic whale skeleton communities. Mar Ecol Prog Ser 260: 109–114.
- 21. Duperron S, Laurent MCZ, Gaill F, Gros O (2008) Sulphur-oxidizing extracellular bacteria in the gills of Mytilidae associated with wood falls. FEMS Microbiol Ecol 63: 338–349
- 22. Vrijenhoek RC (2010) Genetic diversity and connectivity of deep-sea hydrothermal vent metapopulations. Mol Ecol 19: 4391–4411
- 23. Lutz RA, Jablonski D, Rhoads DC, Turner RD (1980) Larval dispersal of a deep-sea hydrothermal vent bivalve from the Galápagos Rift. Mar Biol 57: 127–133.
- 24. Craddock C, Hoeh WR, Lutz RA, Vrijenhoek RC (1995) Extensive gene flow among mytilid (Bathymodiolus thermophilus) populations from hydrothermal vents of the eastern Pacific. Mar Biol 124: 137–146.
- 25. Vrijenhoek RC (1997) Gene flow and genetic diversity in naturally fragmented metapopulations of deep-sea hydrothermal vent animals. J Hered 88: 285.
- 26. Won Y, Young CR, Lutz RA, Vrijenhoek RC (2003) Dispersal barriers and isolation among deep-sea mussel populations (Mytilidae: Bathymodiolus) from eastern Pacific hydrothermal vents. Mol Ecol 12: 169–184.
- 27. Plouviez S, Shank TM, Faure B, Daguin-Thiebaut C, Viard F, et al. (2009) Comparative phylogeography among hydrothermal vent species along the East Pacific Rise reveals vicariant processes and population expansion in the South. Mol Ecol 18: 3903–3917
- 28. Samadi S, Corbari L, Lorion J, Hourdez S, Haga T, et al. (2010) Biodiversity of deep-sea organisms associated with sunken-wood or other organic remains sampled in the tropical Indo-Pacific. Cah Biol Mar 51: 459–466.
- 29. Smith CR, Baco AR (2003) Ecology of whale falls at the deep-sea floor. Annu Rev Mar Sci 41: 311–354.
- 30. Lorion J, Duperron S, Gros O, Cruaud C, Samadi S (2009) Several deep-sea mussels and their associated symbionts are able to live both on wood and on whale falls. Proc R Soc B 276: 177–185
- 31. Bouchet P, Heros V, Lozouet P, Maestrati P (2008) A quarter-century of deep-sea malacological exploration in the South and West Pacific: Where do we stand? How far to go? Mem Mus Natl Hist Nat 196: 9–40.
- 32. Glauert AM (1975) Fixation, dehydration and embedding of biological specimens: New York.: American Elsevier Publ. Co.
- 33. Spurr A (1969) A low-viscosity epoxy resin embedding medium for electron microscopy. J Ultrastruct Res 26: 1–43.
- 34. Folmer O, Black M, Hoeh W, Lutz R, Vrijenhoek R (1994) DNA primers for amplification of mitochondrial cytochrome c oxidase subunit I from diverse metazoan invertebrates. Mol Mar Biol Biotech 3: 294–299.
- 35. Duperron S, Nadalig T, Caprais J-C, Sibuet M, Fiala-Medioni A, et al. (2005) Dual symbiosis in a Bathymodiolus sp. mussel from a methane seep on the Gabon continental margin (Southeast Atlantic): 16S rRNA phylogeny and distribution of the symbionts in gills. Appl Environ Microbiol 71: 1694–1700
- 36. Tamura K, Dudley J, Nei M, Kumar S (2007) MEGA4: molecular evolutionary genetics analysis (MEGA) software version 4.0. Mol Biol Evol 24: 1596
- 37. Excoffier LG, Laval G, Schneider S (2005) Arlequin ver. 3.0: An integrated software package for population genetics data analysis. Evol Bioinform Online 1: 47–50.
- 38. Bandelt HJ, Forster P, Röhl A (1999) Median-joining networks for inferring intraspecific phylogenies. Mol Biol Evol 16: 37.
- 39. Polzin T, Daneshmand SV (2003) On Steiner trees and minimum spanning trees in hypergraphs. Oper Res Lett 31: 12–20
- 40. Weir BS, Cockerham CC (1984) Estimating F-statistics for the analysis of population structure. Evolution 38: 1358–1370.
- 41. Excoffier L, Smouse PE, Quattro JM (1992) Analysis of molecular variance inferred from metric distances among DNA haplotypes: application to human mitochondrial DNA restriction data. Genetics 131: 479.
- 42. Tajima F (1989) Statistical method for testing the neutral mutation hypothesis by DNA polymorphism. Genetics 123: 585.
- 43. Fu YX, Li WH (1993) Statistical tests of neutrality of mutations. Genetics 133: 693.
- 44. Slatkin M, Hudson RR (1991) Pairwise comparisons of mitochondrial DNA sequences in stable and exponentially growing populations. Genetics 129: 555.
- 45. Hudson RR (1990) Gene genealogies and the coalescent process. Oxf Surv Evol Biol 7: 44.
- 46. Altschul SF, Gish W, Miller W, Myers EW, Lipman DJ (1990) Basic local alignment search tool. J Mol Biol 215: 403–410.
- 47. Jobb G, von Haeseler A, Strimmer K (2004) TREEFINDER: a powerful graphical analysis environment for molecular phylogenetics. BMC Evol Biol 4: 18
- 48. Felsenstein J (1985) Confidence limits on phylogenies: an approach using the bootstrap. Evolution: 783–791.
- 49. Ronquist F, Huelsenbeck JP (2003) MrBayes 3: Bayesian phylogenetic inference under mixed models. Bioinformatics 19: 1572
- 50. Gelman A, Rubin DB (1992) Inference from iterative simulation using multiple sequences. Stat Sci 7: 457–472.
- 51. Fujita Y, Matsumoto H, Fujiwara Y, Hashimoto J, Galkin SV, et al. (2009) Phylogenetic relationships of deep-sea Bathymodiolus mussels to their mytilid relatives from sunken whale carcasses and wood. Venus 67: 123–134.
- 52. Duperron S, Sibuet M, MacGregor BJ, Kuypers MMM, Fisher CR, et al. (2007) Diversity, relative abundance and metabolic potential of bacterial endosymbionts in three Bathymodiolus mussel species from cold seeps in the Gulf of Mexico. Environ Microbiol 9: 1423
- 53. Berger MS, Young CM (2006) Physiological response of the cold-seep mussel Bathymodiolus childressi to acutely elevated temperature. Mar Biol 149: 1397–1402
- 54. Dixon DR, Lowe DM, Miller PI, Villemin GR, Colaço A, et al. (2006) Evidence of seasonal reproduction in the Atlantic vent mussel Bathymodiolus azoricus, and an apparent link with the timing of photosynthetic primary production. J Mar Biol Assoc U K 86: 1363–1371
- 55. Lutz RA, Jablonski D, Turner RD (1984) Larval development and dispersal at deep-sea hydrothermal vents. Science 226: 1451–1454.
- 56. Dean HK (1993) A population study of the bivalve Idas argenteus Jeffreys, 1876, (Bivalvia: Mytilidae) recovered from a submerged wood block in the deep North Atlantic Ocean. Malacologia 35: 21–41.
- 57. Salerno JL, Macko SA, Hallam SJ, Bright M, Won YJ, et al.. (2005) Characterization of symbiont populations in life-history stages of mussels from chemosynthetic environments. Biol Bull: 145–155.
- 58. Arellano SM, Young CM (2009) Spawning, development, and the duration of larval life in a deep-sea cold-seep mussel. Biol Bull 216: 149.
- 59. Tregoning P (2002) Plate kinematics in the western Pacific derived from geodetic observations. J Geophys Res 107: 2020
- 60. Hall R (2002) Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animations. J Asian Earth Sci 20: 353–431.
- 61. Siddall M, Rohling EJ, Almogi-Labin A, Hemleben C, Meischner D, et al. (2003) Sea-level fluctuations during the last glacial cycle. Nature 423: 853–858
- 62. Génio L, Johnson SB, Vrijenhoek RC, Cunha MR, Tyler PA, et al. (2008) New record of “Bathymodiolus” mauritanicus Cosel 2002 from the Gulf of Cadiz (NE Atlantic) mud volcanoes. J Shellfish Res 27: 53–61.
- 63. Olu-Le Roy K, von Cosel R, Hourdez S, Carney SL, Jollivet D (2007) Amphi-Atlantic cold-seep Bathymodiolus species complexes across the equatorial belt. Deep-Sea Res I 54: 1890–1911
- 64. Johnson S, Won Y-J, Harvey J, Vrijenhoek R (2013) A hybrid zone between Bathymodiolus mussel lineages from eastern Pacific hydrothermal vents. BMC Evol Biol 13: 21
- 65. O’Mullan GD, Maas PAY, Lutz RA, Vrijenhoek RC (2001) A hybrid zone between hydrothermal vent mussels (Bivalvia: Mytilidae) from the Mid-Atlantic Ridge. Mol Ecol 10: 2819–2831.
- 66. Faure B, Jollivet D, Tanguy A, Bonhomme F, Bierne N (2009) Speciation in the deep sea: multi-locus analysis of divergence and gene flow between two hybridizing species of hydrothermal vent mussels. PLoS ONE 4(8): e6485
- 67. Gros O, Guibert J, Gaill F (2007) Gill-symbiosis in mytilidae associated with wood fall environments. Zoomorphology 126: 163–172
- 68. Gros O, Gaill F (2007) Extracellular bacterial association in gills of «wood mussels». Cah Biol Mar 48: 103–109.
- 69. von Cosel R (2002) A new species of bathymodioline mussel (Mollusca, Bivalvia, Mytilidae) from Mauritania (West Africa), with comments on the genus Bathymodiolus Kenk & Wilson, 1985. Zoosystema 24: 259–272.
- 70. von Cosel R, Olu K (1998) Gigantism in Mytilidae. A new Bathymodiolus from cold seep areas on the Barbados accretionary prism. C R Acad Sci Ser III Sci Vie 321: 655–663.
- 71. von Cosel R, Comtet T, Krylova EM (1999) Bathymodiolus (Bivalvia: Mytilidae) from hydrothermal vents on the Azores triple junction and the Logatchev hydrothermal field, mid-Atlantic ridge. The Veliger 42: 218–248.
- 72. von Cosel R, Metivier B, Hashimoto J (1994) Three new species of Bathymodiolus (Bivalvia: Mytilidae) from hydrothermal vents in the Lau basin and the North Fiji basin, Western Pacific, and the Snake Pit area, Mid-Atlantic Ridge. The Veliger 37: 374–374.
- 73. Hottinger L (2006) Illustrated glossary of terms used in foraminiferal research. Carnets de Géologie/notebooks on Geology, Brest, Mémoire 2006/02 (CG2006_M02): 126 p.
- 74. Pailleret M, Haga T, Petit P, Prive-Gill C, Saedlou N, et al. (2007) Sunken wood from the Vanuatu Islands: identification of wood substrates and preliminary description of associated fauna. Mar Ecol 28: 233–241
- 75. Hashimoto J, Okutani T (1994) Four new mytilid mussels associated with deepsea chemosynthetic communities around Japan. Venus 53: 61–83.
- 76. Fiala-Medioni A, McKiness Z, Dando P, Boulegue J, Mariotti A, et al. (2002) Ultrastructural, biochemical, and immunological characterization of two populations of the mytilid mussel Bathymodiolus azoricus from the Mid-Atlantic Ridge: evidence for a dual symbiosis. Mar Biol 141: 1035–1043.
- 77. Duperron S, Bergin C, Zielinski F, Blazejak A, Pernthaler A, et al. (2006) A dual symbiosis shared by two mussel species, Bathymodiolus azoricus and Bathymodiolus puteoserpentis (Bivalvia: Mytilidae), from hydrothermal vents along the northern Mid-Atlantic Ridge. Environ Microbiol 8: 1441–1447
- 78. Cavanaugh CM, Wirsen CO, Jannasch HW (1992) Evidence for methylotrophic symbionts in a hydrothermal vent mussel (Bivalvia: Mytilidae) from the Mid-Atlantic Ridge. Appl Environ Microbiol 58: 3799–3803.
- 79. Distel DL, Lee HK, Cavanaugh CM (1995) Intracellular coexistence of methano-and thioautotrophic bacteria in a hydrothermal vent mussel. Proc Natl Acad Sci USA 92: 9598–9602.
- 80. Dubilier N, Windoffer R, Giere O (1998) Ultrastructure and stable carbon isotope composition of the hydrothermal vent mussels Bathymodiolus brevior and B. sp. affinis brevior from the North Fiji Basin, western Pacific. Mar Ecol Prog Ser 165: 187–193.
- 81. Kenk VC, Wilson BR (1985) A new mussel (Bivalvia, Mytilidae) from hydrothermal vents in the Galapagos Rift zone. Malacologia 26: 253–271.
- 82. Fisher CR, Childress JJ, Oremland RS, Bidigare RR (1987) The importance of methane and thiosulfate in the metabolism of the bacterial symbionts of two deep-sea mussels. Mar Biol 96: 59–71.
- 83. Olu-Le Roy K, Sibuet M, Fiala-Médioni A, Gofas S, Salas C, et al. (2004) Cold seep communities in the deep eastern Mediterranean Sea: composition, symbiosis and spatial distribution on mud volcanoes. Deep-Sea Res I 51: 1915–1936