- Research article
- Open Access
A remarkable diversity of bone-eating worms (Osedax; Siboglinidae; Annelida)
BMC Biology volume 7, Article number: 74 (2009)
Bone-eating Osedax worms have proved to be surprisingly diverse and widespread. Including the initial description of this genus in 2004, five species that live at depths between 25 and 3,000 m in the eastern and western Pacific and in the north Atlantic have been named to date. Here, we provide molecular and morphological evidence for 12 additional evolutionary lineages from Monterey Bay, California. To assess their phylogenetic relationships and possible status as new undescribed species, we examined DNA sequences from two mitochondrial (COI and 16S rRNA) and three nuclear genes (H3, 18S and 28S rRNA).
Phylogenetic analyses identified 17 distinct evolutionary lineages. Levels of sequence divergence among the undescribed lineages were similar to those found among the named species. The 17 lineages clustered into five well-supported clades that also differed for a number of key morphological traits. Attempts to determine the evolutionary age of Osedax depended on prior assumptions about nucleotide substitution rates. According to one scenario involving a molecular clock calibrated for shallow marine invertebrates, Osedax split from its siboglinid relatives about 45 million years ago when archeocete cetaceans first appeared and then diversified during the late Oligocene and early Miocene when toothed and baleen whales appeared. Alternatively, the use of a slower clock calibrated for deep-sea annelids suggested that Osedax split from its siboglinid relatives during the Cretaceous and began to diversify during the Early Paleocene, at least 20 million years before the origin of large marine mammals.
To help resolve uncertainties about the evolutionary age of Osedax, we suggest that the fossilized bones from Cretaceous marine reptiles and late Oligocene cetaceans be examined for possible trace fossils left by Osedax roots. Regardless of the outcome, the present molecular evidence for strong phylogenetic concordance across five separate genes suggests that the undescribed Osedax lineages comprise evolutionarily significant units that have been separate from one another for many millions of years. These data coupled with ongoing morphological analyses provide a solid foundation for their future descriptions as new species.
Osedax, a recently discovered genus of bone-eating marine worms, are proving to be far more diverse and geographically widespread than initially realized. The genus was described from two newly discovered species found on whalebones recovered from 2,893 m depth in Monterey Bay, California . Subsequently, three additional species were described from depths between 30 and 3,000 m in the Atlantic and Pacific oceans [2–4]. Now, five additional distinct evolutionary lineages are recognized from Monterey Bay, but these putative species remain to be formally described [5–8]. Here we report genetic evidence for seven additional putative species. Given this unexpected diversity of Osedax worms with distinct morphologies, depth ranges and ecological characteristics, a detailed examination of their evolutionary history is warranted.
The initial description of Osedax  included a phylogenetic analysis that placed the new genus in the polychaete annelid family Siboglinidae, which also includes the now obsolete tubeworm phyla Vestimentifera and Pogonophora [9, 10]. As adults, all siboglinids lack a functional digestive system and rely entirely on endosymbiotic bacteria for their nutrition. The other siboglinid taxa host chemosynthetic bacteria and live in reducing marine environments such as hydrothermal vents, hydrocarbon seeps and anoxic basins. Osedax, however, are unique because they penetrate and digest bones with the aid of heterotrophic bacteriathat are housed in a complex branching root system [6, 11]. Osedax also differ because they exhibit extreme sexual dimorphism involving dwarf (paedomorphic) males that live as harems within a female's tube [1, 4, 12].
Considering DNA sequence divergence between the only two species known at the time, Rouse et al.  suggested that Osedax may have begun to diversify during the late Eocene, around 42 million years ago (MYA), perhaps coinciding with the origin of large oceanic cetaceans. Yet, this hypothesis must be reexamined in view of our current discoveries of far greater morphological and molecular diversity in the genus (Fig. 1). Our present goals were to better characterize the genetic differences among the five named species and to use this information as a foundation for clarifying evolutionary relationships among the 12 undescribed operational taxonomic units, OTUs (Table 1). We examined DNA sequences from five genes. Mitochondrial cytochrome-c-oxidase subunit 1 (COI) was used to assess levels of sequence diversity within and among all 17 OTUs and to provide DNA barcodes that would facilitate the identification of Osedax species in subsequent discoveries. Phylogenetic analyses were conducted independently with mitochondrial COI and 16S rRNA and with three nuclear genes, Histone-H3, 18S and 28S rRNA. A combined analysis involving all five genes provided a robust phylogeny for the genus and identified several well-supported species-groups that diversified over a relatively short time scale, though the timing of these events during either the Mesozoic or Cenozoic remains uncertain. Formal descriptions of the new species from Monterey Bay are currently underway (Rouse, in progress).
We examined DNA sequences from five genes (Table 2). Substitution models were estimated separately for each gene. The percentage GC content was lower in the mitochondrial genes (33.9 - 40.2%) than in the nuclear genes (47.8 - 50.2%). The two protein-coding genes, COI and H3, exhibited the highest sequence divergence. Ratios of transitions to transversions were nearly one, and ratios of synonymous to non-synonymous substitutions were comparable for COI and H3. For each gene, the sequences were partitioned by codon position, and substitution parameters were estimated separately for each position. Indels were found in all three of the rRNA genes. On average, the lengths of indels and numbers of distinct haplotypes were similar. Ratios of transitions to transversions were about one-half for the three ribosomal genes.
We initially conducted separate phylogenetic analyses for each gene. Altogether 83 COI sequences from Osedax clustered into 17 evolutionary lineages (Figure 2a). Multiple COI haplotypes were included, when possible, to represent the sequence divergence among (D) versus that found within (π) each lineage (Table 3). Only one O. japonicus sequence was available from GenBank, and to date we have collected only single individuals of O. nude-palp-F and O. nude-palp-B. The mean pairwise D values among the Osedax OTUs ranged from 8.4 to 24.3%. The smallest pairwise D value, obtained for O. yellow-collar versus O. orange-collar, was an order-of-magnitude greater than the largest π value observed within these OTUs (0.82%). COI transitions began to saturate after about 12% divergence, but transversions were not saturated and many of them resulted in amino acid substitutions (Table 2).
Four additional genes revealed concordant phylogenetic differences among the Osedax OTUs (Figures 2b-e). The 16S, 28S, and H3 sequences differed among the 15 Monterey Bay OTUs, but sequences were not available for O. japonicus and O. mucofloris. Although their 18S sequences were identical, O. yellow-collar and O. orange-collar differed from all the other Monterey OTUs and from O. mucofloris. The nodes leading to O. spiral and O. frankpressi were not stable, but all five gene-trees were broadly congruent in their topologies. Incongruence length difference (ILD) tests of homogeneity revealed that four of the five gene partitions were not significantly in conflict (P range: 0.119 - 1.00). Only the H3 tree was incongruent with respect to the 16S and 18S rRNA trees (P = 0.03 and 0.02, respectively). This problem resulted because H3 provided weak resolution among Osedax species that clustered together on a long branch relative to the outgroup S. brattstromi. ILD tests of homogeneity between H3 and the other partitions without the outgroup eliminated all remaining incongruence (P range: 0.125 - 1.00).
Both the individual gene trees and the combined analysis involving concatenated sequences from all five genes identified several well-supported Osedax clades (Roman numerals I - V, Figure 3). Although limited sequence information was available for O. mucofloris (COI and 18S) and O. japonicus (COI), they fell firmly within clade IV. O. frankpressi was also well supported as a member of clade IV in the combined analysis, but its position varied in the COI tree. Estimates of the age of Osedax depended on assumptions about rates of nucleotide substitution for mitochondrial COI. Mitochondrial COI divergence (D) between cognate species of shallow-water marine invertebrates isolated across the Isthmus of Panama grows at a rate of about 1.4% per MY ; so, the substitution rate (r 1) equals D/2 or 0.7% per lineage per My. Assuming r 1 = 0.7%, Osedax would have split from its monoliferan relatives about 45 MYA (95% HPD bounds: 31 - 47 Mya) (Figure 3). Time (T) to the most recent common ancestor for the Osedax would be 24 - 29 MY. Alternatively, assuming a slower substitution rate (r 2 = 0.21% per lineage per MY) estimated for deep-sea hydrothermal vent annelids , Osedax would have split from monoliferans about 130 MYA (95% HPD bounds: 104 - 160 Mya). T for Osedax would be 81 - 97 My.
Genetic and morphological differences among five previously named Osedax species provide a useful reference frame for assessing levels of divergence among the twelve undescribed OTUs considered in this study. Osedax rubiplumus, O. frankpressi and O. roseus live together on whale carcasses at depths greater than 1,000 m in Monterey Bay, CA (Figure 1; Table 1). To date, we have found no evidence for interbreeding among them. For example, an examination of 116 male Osedax sampled from the tubes of 77 O. rubiplumus females found no cases of foreign males in the female's tubes, despite the presence of O. roseus and O. frankpressi on the same carcass at 1820 m depth. Also including O. mucofloris from Sweden and O. japonicus from Japan, the mean sequence divergence (D) for mitochondrial COI between pairs of the named species was 19.6% (range: 15.7 to 23.4%; Table 2). Correspondingly, the mean pairwise D among the undescribed OTUs was 19.9% (range: 8.4 to 23.7%). The smallest value (8.4% between OTUs O. yellow-collar and O. orange-collar) was an order-of-magnitude greater than the largest divergence observed within any of these named or undescribed OTUs (π = 0.8% for O. nude-palp-A). These π values probably are underestimates, however, because each was obtained from a single locality. Isolation-by-distance and population subdivision across oceanic barriers are expected to increase π within broadly distributed species; however, π rarely exceeds 1 - 2%, unless other factors are involved. Global-scale phylogeographic surveys of COI sequence diversity have estimated π values less than 1% within named species of deep-sea hydrothermal vent annelids, mollusks and crustaceans, whereas D values typically are greater than 4% among species [14–22]. Nonetheless, odd cases of accelerated COI substitution rates have been reported. Sex-biased mitochondrial transmission and heteroplasmy are associated with accelerated divergence in some bivalve mollusks , but no evidence exists for this phenomenon in annelids, and we have found no differences in the distribution of mitochondrial haplotypes between males and females for O. rubiplumus . High mitochondrial divergence rates have been reported for some marine and freshwater animals [24–26], but for the vast majority of cases mitochondrial COI is relatively conservative in its mutation rate within and among species. It is precisely the tendency of COI to discriminate clearly among the named species in many invertebrate taxa that has made this gene a common reference tool for DNA barcoding and molecular taxonomy [27, 28].
Although numerous species concepts have been debated over the years [29, 30], genealogical concordance across molecular and morphological characters provides a reliable indicator of longstanding evolutionary independence and consequently provides an operational criterion for species recognition . Our confidence that the 12 presently unnamed OTUs from Monterey Bay represent distinct evolutionary lineages and warrant further consideration for naming as species is bolstered by morphological differences and concordant divergence observed across multiple gene loci. Only 18S rRNA failed to distinguish between members of the closest pair of OTUs, O. yellow-collar and O. orange-collar. This highly conservative gene barely varies across the bivalve genus Bathymodiolus, globally widespread and diverse deep-sea mussels , or across a diverse clade siboglinid annelids, the vestimentiferans . Consequently the 18S differences reported for these Osedax OTUs are substantive. All the Monterey Bay OTUs also differed in their 16S, 18S, 28S and H3 gene sequences. Phylogenetic trees generated independently from each of these genes clustered the OTUs in essentially similar ways (Figure 2). The combined analysis involving concatenated sequences from the five genes clearly reveals the evidence for long-standing evolutionary independence among these lineages. Only single individuals presently represent two of these lineages, O. nude-palp-D and -F. Nonetheless, these individuals differed from one another and clustered phylogenetically in a concordant fashion for all five genes. Formal descriptions of the new taxa shall be treated in forthcoming publications, as we obtain the additional samples needed for morphological studies and museum vouchers. Failure to formally recognize such highly divergent evolutionary lineages as distinct species creates a risk of significantly underestimating biological diversity . In the meantime, attempts to identify these and other boneworms will be aided by the present gene sequences, which have been deposited in public databases including GenBank (Table 4) and the Barcode of Life Data System .
Individual gene trees (Figure 2) and the combined phylogenetic analysis (Figure 3) identified several well-supported groupings within Osedax (clades I - V). Osedax spiral (clade III) stands alone as the most atypical of these worms. Its oviduct does not extend beyond the trunk, and it lacks the vascularized anterior palps that characterize all other Osedax (Figure 1g). Unlike all other Osedax, O. spiral is a late successional species which lives at the sediment interface and produces long fibrous roots that penetrate the anoxic (black and sulfidic) sediments to exploit buried fragments of bone . The lack of palps in O. spiral probably represents a character loss under a most parsimonious reconstruction, because all other siboglinids bear an anterior crown composed of one or more palps. The nude-palp OTUs (clade II) differ because their palps do not bear the lateral pinnules seen in the other Osedax clades (Figures 1i and 1j). Lack of pinnules may represent a character loss, but supporting evidence regarding the homology and distribution of pinnules in other siboglinids is uncertain. Monoliferans have two or more palps, with numerous pinnules in the case of Vestimentifera, but pinnules are absent in Sclerolinum and in some frenulates [10, 35].
The remaining Osedax clades (I, IV and V) bear four palps with numerous pinnules that give the crown a feathery appearance (e.g., Figure 1a). The two members of clade V have long branched roots that are green in color (Figures 1e-f) and palps that are bright red with outwardly facing pinnules. Clades II and V share robust lobate roots. The two members of clade (I) have relatively short trunks and palps (Figure 1h), but they have not been found in great numbers because they are small and may have been overlooked in earlier samples. Members of clade IV, which have red, pink or even white crowns (Figures 1a-d), were recovered from depths of 1,020 m or less, excepting O. frankpressi, which has not been found shallower than 1,800 m. Occupation of shallow habitats might be a derived condition for these members of clade IV, though support for a shallow clade was weak (Figure 3). Addition of comparative sequence data from the other shallowmembers of this clade, O. japonicus and O. mucofloris, might help to strengthen this relationship (only 18S and COI data are available on GenBank for O. mucofloris and only COI for O. japonicus). Otherwise, no clear evolutionary pattern of depth utilization is apparent among the major Osedax clades. Several of these OTUs were sampled from a single depth, others were sampled across relatively narrow depth ranges (300 - 600 m for O. yellow-patch and O. orange-collar), and some were sampled across broad depth ranges (1,000 m for O. frankpressi, and O. rubiplumus and 1,200 m for O. roseus).
Age of Osedax
For now, we are unable to confidently delineate a timeframe during which Osedax split from its monoliferan relatives or the age (T) of the most recent common ancestor for this unusual genus. Present evidence indicates that Osedax species live primarily on organic compounds extracted directly from sunken bones. Their Oceanospirillales symbionts are capable of growing on collagen and cholesterol as primary carbon sources . Video evidence suggests that O. japonicus also grows on spermaceti, a wax found in the head of sperm whales . There are arguments to suggest that Osedax may not be nutritionally restricted to living on whale-falls. Experimental deployments of cow bones and observations of sunken possible pig bones reveal that Osedax can grow and reproduce on a range of mammalian tissues including those from terrestrial quadrupeds [7, 36]. So, it may be unwarranted to associate the evolution of these bone-eating worms with the origin and spread of oceanic whales, as previously suggested by Rouse et al. . Nonetheless, one of the scenarios that we have considered here is consistent with that hypothesis. If we assumed a divergence rate (d = 1.4% per MY) calibrated for mitochondrial genes from shallow-water marine invertebrates , and applied this rate (r 1 = d/2 = 0.70%/lineage/My) to COI divergence, we estimated that Osedax split from its monoliferan relatives about 45 Mya, possibly coincident with the origins of large archeocete cetaceans during the Eocene . According to this scenario, the most recent common ancestor for the Osedax sampled to date would have lived about 26 MYA, during the Late Oligocene and roughly coincident with the diversification of modern cetaceans .
Alternatively, we can assume a slower substitution rate (r 1 = 0.21%/lineage/My) calibrated from COI divergence in deep-sea annelids, including Vestimentifera , as was used by Rouse et al.  for estimating the origin of Osedax when only O. rubiplumus and O. frankpressi were known. Under this rate then Osedax would appear to be much older than previously hypothesized . This result is not surprising given the larger diversity of Osedax shown here. Accordingly, Osedax split from its monoliferan relatives during the Cretaceous, and the most recent common ancestor for the genus would have lived during the Late Cretaceous. Perhaps the calcified cartilage and bones from a variety of large Cretaceous vertebrates supported these worms -- e.g., mosasaurs, plesiosaurs, turtles, and possibly chondrichthyans and teleosts [39–42]. Fossilized snails and bivalves were recently found with plesiosaur bones; so the sunken carcasses of these large marine reptiles appear to be capable of supporting communities much like those found on modern whale-falls . Nevertheless, this scenario is problematic, because the major Osedax clades would have diversified around the Cretaceous-Tertiary (K/T) boundary, after the extinction of most large-bodied reptilians . Although dyrosaurid crocodylomorphs survived the K/T event, they were confined to relatively shallow coastal environments  and probably would not have supported Osedax. Large turtles and chondrichthyans also survived the K/T boundary , and large teleosts appeared again during the early Paleocene . It is unknown whether Osedax can exploit these resources; so, arguably a 20 MY gap may have existed during the Paleocene when there would have been little in the way of large vertebrate remains for Osedax. Another problem with this scenario is the concern that nucleotide substitution rates may be slower in the deep-sea vent annelids used to obtain the r 2 = 0.21% calibration rate .
The present phylogenetic evidence based on DNA sequences from multiple independent genes provides a solid foundation for future discoveries and taxonomic descriptions of Osedax species. However, our efforts to estimate evolutionary ages for the diversification of this unusual group of worms only allowed the erection of new hypotheses that could be tested with independent evidence from the fossil record. Soft-bodied invertebrates like Osedax do not often leave convincing fossils, but these worms might leave traces of their activity by the distinctive holes they bore into bones. To date, we have found no other animals that create similar borings in bones. Consequently, we have distributed whalebones containing Osedax to several paleontologists who are also examining the taphonomy of fossilized bones from plesiosaurs and cetaceans. It is to be hoped that these efforts will help us to narrow the age of this remarkable genus of bone-eating worms.
Materials and methods
Locations of the Monterey Bay whale-falls, except whale-634, are provided elsewhere . Whale-634 is the carcass of a juvenile gray whale that was sunk on 5 October 2004 at a depth of 633 m at 36.802°N and 122.994°W. We used the remotely operated vehicles, ROV Tiburon and ROV Ventana, operated by the Monterey Bay Aquarium Research Institute (MBARI) to collect Osedax-inhabited bones from five whale-fall localities (Table 1). Bones were transported to the surface in closed insulated containers and stored temporarily in cold (4°C) filtered seawater. Worms were dissected from the bones and photographed. Then a palp tip was removed and stored in 95% ethanol or frozen immediately at -80°C. The remainder of each specimen was preserved for anatomical studies and taxonomic descriptions. Voucher specimens were lodged in Scripps Institution of Oceanography Benthic Invertebrate Collection (catalogue numbers in Table 1). Other specimens will be distributed to other Museums upon their formal description (Rouse, in progress). For the present purpose, we list the approximate sizes (trunk plus crown length) and several morphological characteristics of each OTU (Table 1).
Published DNA sequences from Osedax mucofloris (18S rRNA and COI) and O. japonicus (COI) were recovered from GenBank . A previous phylogenetic analyses  placed Osedax in a clade that also includes the Monolifera, which includes Sclerolinum and vestimentiferan tubeworms . The frenulates, a diverse group of slender chemosynthetic worms are basal to the monoliferans and Osedax [10, 47]. Ongoing studies of siboglinid phylogeny revealed that Sclerolinum is presently our best choice as outgroup for this study of Osedax phylogeny. The vestimentiferan Lamellibrachia columna was also examined, and its substitution as outgroup did not substantively alter the tree topologies for the ingroup. Other vestimentiferans were not considered, however, because incomplete sequence data are available and because independent evidence from several genes suggests that rates of nucleotide substitution may have slowed down in these deep-sea worms [9, 14, 48]. Consequently, we have used DNA sequences from the monoliferan Sclerolinum brattstromi, collected near Bergen, Norway. GenBank accession numbers for all the DNA sequences used in this study are listed in Table 4.
Total DNA was extracted using the DNeasy kit (Qiagen, Valencia, CA, USA) according to manufacturer's instructions. We used primers that amplified approximately 1200 bp of COI , approximately500 bp of 16S rRNA , approximately 1000 bp of 28S rRNA , approximately 1800 bp of 18S rRNA , and approximately 370 bp of H3 . Amplification reactions with AmpliTaq Gold (Applied Biosystems Inc., Foster City, CA, USA) were conducted in a GeneAmp 9700 thermal cycler (Applied Biosystems Inc., Carlsbad, CA, USA) with the following parameters: 95°C/10 min, 35× (94°C/1 min, 55°C/1 min, 72°C/1 min), and 72°C/7 min. If available, at least six individuals of each species were sequenced for each locus. PCR products were diluted in 50 μl sterile water and cleaned with Multiscreen HTS PCR 96 filter plates (Millipore Corp., Billerica, MA, USA). The products were sequenced bidirectionally with the same primers on an ABI 3100 sequencer using BigDye terminator v.3.1 chemistry (Applied Biosystems Inc., Foster City, CA, USA).
Sequences were assembled using CodonCode Aligner v. 2.06 (CodonCode Corporation, Dedham, MA, USA), aligned using Muscle  and edited by eye using Maclade v. 4.08 . We used MrModelTest  and the Akaike information criterion  to determine appropriate evolutionary models for each gene (Table 2). COI and H3 were partitioned by codon position, and parameters were estimated separately for each position. RNA secondary structures were predicted with GeneBee and used to partition stems and loops in 16S, 18S, and 28S sequences. The doublet model was used for RNA stems and a standard 4 × 4 nucleotide model was used for RNA loops. The number of indel haplotypes for rRNA sequences (total number of indels, number after excluding overlapping indels, and average length of indels) were estimated with DNAsp v. 4.90.1  using the diallelic model. Gaps in the RNA sequences were treated as a fifth character-state in subsequent Bayesian phylogenetic analyses and as missing data in parsimony and maximum likelihood (ML) analyses. The program DAMBE  was used to examine saturation of the mitochondrial COI sequences for the Osedax OTUs and outgroup taxa.
First, each gene was analyzed separately using MrBayes v. 3.1.2 [60, 61]. Bayesian analyses were run as six chains for 5·106 generations. Print and sample frequencies were 1,000 generations, and the burn-in was the first 100 samples. We used AWTY  to assess whether analyses reached convergence and FigTree v. 1.1.2  to display the resulting trees. We then used the incongruence length difference (ILD) function implemented in Paup* v. 4.0  to assess congruence of the tree topologies produced by the individual gene partitions. ILD tests were conducted both with and without the outgroup taxa. The ILD partition homogeneity test was run for 1,000 replicates with 10 random additions of gene sequences.
A combined analysis was conducted with concatenated sequences from the five genes. If available, multiple individuals of each OTU were sequenced for each gene; however, the concatenated multilocus sequences used in the phylogenetic analyses were obtained from a single representative individual for each OTU. The five gene regions were partitioned separately according to the previously determined model parameters. Bayesian phylogenetic analyses were then conducted with MrBayes v. 3.1.2. Maximum parsimony analysis of the combined data set was performed with Paup* v. 4.0  using an equally weighted character matrix, heuristic searches using the tree-bisection-reconnection branch-swapping algorithm, and 100 random addition replicates. The resulting shortest tree included 3481 steps. A parsimony jackknife analysis (with 37% deletion) was run for 100 iterations with the same settings as the parsimony search. ML analysis was conducted using RAxML 7.0.4 (with bootstrapping) using GTR+I+G as the model for each partition on combined data. RAxML analyses were performed with the CIPRES cluster at the San Diego Supercomputer Center.
Relaxed molecular clock
A Bayesian, MCMC method implemented in Beast v. 1.4.8  was used to estimate the evolutionary ages of internal nodes in the tree topology derived from the combined phylogenetic analysis. Estimates of the time to most recent common ancestor (T) were based on two calibrations nucleotide substitution rates for mitochondrial COI. Substitution rates (r) were estimated as percentage per lineage per million years (my) so they equal one-half the divergence per unit of time (T) between taxa (r = 100 × D/2T). First, we assumed a conventional substitution rate, r 1 = 0.7%, based on D = 1.4% per my pairwise divergence rate commonly cited for shallow water marine invertebrates that were isolated by the emergence of the Isthmus of Panama . Second, we used a slower rate, r 2 = 0.21%, previously calibrated from a vicariant event that split cognate-species of deep-sea hydrothermal vent annelids between the East Pacific Rise and the northeastern Pacific ridge system about 28.5 myA . Calibrations were not available for the other genes.
We used a relaxed, uncorrelated, lognormal molecular clock with a general time reversible (GTR) substitution model that was unlinked across codon positions. Initial MCMC test runs consisted of 10 million generations to optimize the scale factors of the prior function. Three independent MCMC chains were run for 100 million generations, sampled every 1000 generations. Results were visualized in and FigTree v. 1.1.2 and Tracer v. 1.4 .
mitochondrial large subunit ribosomal RNA
nuclear small subunit subunit ribosomal RNA
nuclear large subunit ribosomal RNA
cytochrome oxidase subunit I
general time reversible
Monte Carlo Markov chain
million (106) years ago
operational taxonomic units
remotely operated vehicle.
Rouse GW, Goffredi SK, Vrijenhoek RC: Osedax: Bone-eating marine worms with dwarf males. Science. 2004, 305: 668-671. 10.1126/science.1098650.
Glover AG, Käilström B, Smith CR, Dahlgren TG: World-wide whale worms? A new species of Osedax from the shallow north Atlantic. Proc R Soc Lond B. 2005, 272: 2587-2592. 10.1098/rspb.2005.3275.
Fujikura K, Fujiwara Y, Kawato M: A new species of Osedax (Annelida: Siboglinidae) associated with whale carcasses off Kyushu, Japan. Zoolog Sci. 2006, 23: 733-740. 10.2108/zsj.23.733.
Rouse GW, Worsaae K, Johnson SB, Jones WJ, Vrijenhoek RC: Acquisition of dwarf male 'harems' by recently settled females of Osedax roseus n. sp. (Siboglinidae; Annelida). Biol Bull. 2008, 214: 67-82. 10.2307/25066661.
Braby CE, Rouse GW, Johnson SB, Jones WJ, Vrijenhoek RC: Bathymetric and temporal variation among Osedax boneworms and associated megafauna on whale-falls in Monterey Bay, California. Deep Sea Res I. 2007, 54: 1773-1791. 10.1016/j.dsr.2007.05.014.
Goffredi SK, Johnson SB, Vrijenhoek RC: Genetic and potential function of microbial symbionts associated with newly discovered species of Osedax polychaete worms. Appl Environ Microbiol. 2007, 73: 2314-2323. 10.1128/AEM.01986-06.
Jones WJ, Johnson SB, Rouse GW, Vrijenhoek RC: Marine worms (genus Osedax) colonize cow bones. Proc R Soc Lond B. 2008, 275: 387-391. 10.1098/rspb.2007.1437.
Rouse GW, Wilson NG, Goffredi SK, Johnson SB, Smart T, Widmer C, Young CM, Vrijenhoek RC: Spawning and development in Osedax boneworms (Siboglinidae, Annelida). Mar Biol. 2009, 156: 395-405. 10.1007/s00227-008-1091-z.
Halanych KM, Feldman RA, Vrijenhoek RC: Molecular evidence that Sclerolinum brattstromi is closely related to vestimentiferans, not frenulate pogonophorans (Siboglinidae, Annelida). Biol Bull. 2001, 201: 65-75. 10.2307/1543527.
Rouse G: A cladistic analysis of Siboglinidae Caullery, 1914 (Polychaeta, Annelida): formerly the phyla Pogonophora and Vestimentifera. Zool J Linn Soc. 2001, 132: 55-80. 10.1111/j.1096-3642.2001.tb02271.x.
Goffredi SK, Orphan VJ, Rouse GW, Jahnke L, Embaye T, Turk K, Lee R, Vrijenhoek RC: Evolutionary innovation: a bone-eating marine symbiosis. Environ Micobiol. 2005, 7: 1369-1378. 10.1111/j.1462-2920.2005.00824.x.
Vrijenhoek RC, Johnson S, Rouse GW: Bone-eating Osedax females and their "harems" of dwarf males are recruited from a common larval pool. Mol Ecol. 2008, 17: 4535-4544. 10.1111/j.1365-294X.2008.03937.x.
Knowlton N, Weigt LA: New dates and new rates for divergence across the Isthmus of Panama. Proc R Soc Lond B. 1998, 265: 2257-2263. 10.1098/rspb.1998.0568.
Chevaldonné P, Jollivet D, Desbruyères D, Lutz RA, Vrijenhoek RC: Sister-species of eastern Pacific hydrothermal-vent worms (Ampharetidae, Alvinelidae, Vestimentifera) provide new mitochondrial clock calibration. Cah Biol Mar. 2002, 43: 367-370.
Maas PAY, O'Mullan GD, Lutz RA, Vrijenhoek RC: Genetic and morphometric characterization of mussels (Bivalvia: Mytilidae) from Mid-Atlantic hydrothermal vents. Biol Bull. 1999, 196: 265-272. 10.2307/1542951.
Johnson SB, Young CR, Jones WJ, Warén A, Vrijenhoek RC: Migration, isolation, and speciation of hydrothermal vent limpets (Gastropoda; Lepetodrilidae) across the Blanco Transform Fault. Biol Bull. 2006, 210: 140-157. 10.2307/4134603.
Peek A, Gustafson R, Lutz R, Vrijenhoek R: Evolutionary relationships of deep-sea hydrothermal vent and cold-water seep clams (Bivalvia: Vesicomyidae): Results from the mitochondrial cytochrome oxidase subunit I. Mar Biol. 1997, 130: 151-161. 10.1007/s002270050234.
Won Y-J, Young CR, Lutz RA, Vrijenhoek RC: Dispersal barriers and isolation among deep-sea mussel populations (Mytilidae: Bathymodiolus) from eastern Pacific hydrothermal vents. Mol Ecol. 2003, 12: 169-184. 10.1046/j.1365-294X.2003.01726.x.
Hurtado LA, Lutz RA, Vrijenhoek RC: Distinct patterns of genetic differentiation among annelids of eastern Pacific hydrothermal vents. Mol Ecol. 2004, 13: 2603-2615. 10.1111/j.1365-294X.2004.02287.x.
Young CR, Fujio S, Vrijenhoek RC: Directional dispersal between mid-ocean ridges: deep-ocean circulation and gene flow in Ridgeia piscesae. Mol Ecol. 2008, 17: 1718-1731. 10.1111/j.1365-294X.2008.03609.x.
Guinot D, Hurtado LA: Two new species of hydrothermal vent crabs of the genus Bythograea from the southern East Pacific Rise and from the Galapagos Rift (Crustacea Decapoda Brachyura Bythograeidae). C R Biol. 2003, 326: 423-439. 10.1016/S1631-0691(03)00126-4.
Guinot D, Hurtado LA, Vrijenhoek RC: New genus and species of brachyuran crab from the southern East Pacific Rise (Crustacea Decapoda Brachyura Bythograeidae). C R Biol. 2002, 325: 1119-1128. 10.1016/S1631-0691(02)01520-2.
Stewart DT, Kenchington ER, Singh RK, Zouros E: Degree of selective constraint as an explanation of the different rates of evolution of gender-specific mitochondrial DNA lineages in the mussel mytilus. Genetics. 1996, 143: 1349-1357.
Audzijonyte A, Väinölä R: Phylogeographic analyses of a circumarctic coastal and a boreal lacustrine mysid crustacean, and evidence of fast post-glacial mtDNA rates. Mol Ecol. 2006, 15: 3287-3301. 10.1111/j.1365-294X.2006.02998.x.
Waters JM, Rowe DL, Apte S, King TM, Wallis GP, Anderson L, Norris RJ, Craw D, Burridge CP: Geological dates and molecular rates: rapid divergence of rivers and their biotas. Sys Biol. 2007, 56: 271-282. 10.1080/10635150701313855.
Burton RS: Intraspecific phylogeography across the Point Conception biogeogrphic boundary. Evolution. 1998, 52: 734-745. 10.2307/2411268.
Hebert PDN, Cywinska A, Ball SL, deWaard JR: Biological identifications through DNA barcodes. Proc Biol Sci. 2003, 270: 313-321. 10.1098/rspb.2002.2218.
Vogler AP, Monaghan MT: Recent advances in DNA taxonomy. Journal of Zoological Systematics and Evolutionary Research. 2007, 45: 1-10. 10.1111/j.1439-0469.2006.00384.x.
Hey J: On the failure of modern species concepts. Trends Ecol Evol. 2006, 21: 447-450. 10.1016/j.tree.2006.05.011.
Mayden RL: A hierarchy of species concepts: the denouement in the saga of the species problem. Species: The Units of Biodiversity. Edited by: Claridge MF, Dawah AH, Wilson MR. 1997, Chapman & Hall, 381-424.
Avise JC, Wollenberg K: Phylogenies and the origin of species. Proc Natl Acad Sci USA. 1997, 94: 7748-7755. 10.1073/pnas.94.15.7748.
Jones WJ, Won YJ, Maas PAY, Smith PJ, Lutz RA, Vrijenhoek RC: Evolution of habitat use by deep-sea mussels. Mar Biol. 2006, 148: 841-851. 10.1007/s00227-005-0115-1.
Bickford D, Lohman DJ, Sohdi NS, Ng PKL, Meier R, Winker K, Ingram KK, Das I: Cryptic species as a window on diversity and conservation. Trends Ecol Evol. 2007, 22: 148-155. 10.1016/j.tree.2006.11.004.
Ratnasingham S, Hebert PDN: BOLD: the barcode of life data system. Mol Ecol Notes. 2007, 7: 355-364. 10.1111/j.1471-8286.2007.01678.x. [http://www.barcodinglife.org]
Ivanov AV: Pogonophora. 1963, London: Academic Press
Vrijenhoek RC, Collins PC, Van Dover CL: Bone-eating marine worms: habitat specialists or generalists?. Proc R Soc Lond B. 2008, 275: 1963-1964. 10.1098/rspb.2008.0350.
Thewissen JGM, Williams EM: The early radiations of Cetacea (Mammalia): Evolutionary pattern and developmental correlations. Annu Rev Ecol Syst. 2002, 33: 73-90. 10.1146/annurev.ecolsys.33.020602.095426.
Deméré TA, McGowen MR, Berta A, Gatesy J: Morphological and molecular evidence for a stepwise evolutionary transition from teeth to baleen in mysticete whales. Sys Biol. 2008, 57: 15-37. 10.1080/10635150701884632.
Lingham-Soliar T: Anatomy and functional morphology of the largest marine reptile known, Mosasaurus hoffmanni (Mosasauridae, Reptilia) from the Upper Cretaceous, Upper Maastrichtian of the Netherlands. Philos Trans Biol Sci. 1995, 155-180. 10.1098/rstb.1995.0019.
O'Keefe F, Carrano M: Correlated trends in the evolution of the plesiosaur locomotor system. Paleobiology. 2005, 31: 656-675.
Kear B, Lee M: A primitive protostegid from Australia and early sea turtle evolution. Biol Lett. 2006, 2: 116-119. 10.1098/rsbl.2005.0406.
Kriwet J, Benton M: Neoselachian (Chondrichthyes, Elasmobranchii) diversity across the Cretaceous-Tertiary boundary. Palaeogeogr Palaeoclimatol Palaeoecol. 2004, 214: 181-194.
Kaim A, Kobayashi Y, Echizenya H, Jenkins RG, Tanabe K: Chemosynthesis-based associations on Cretaceous plesiosaurid carcasses. Acta Palaeontol Pol. 2008, 53: 97-104. 10.4202/app.2008.0106.
Bardet N: Extinction events among Mesozoic marine reptiles. Histor Biol. 1994, 7: 313-324. 10.1080/10292389409380462.
Barbosa J, Kellner A, Viana M: New dyrosaurid crocodylomorph and evidences for faunal turnover at the K-P transition in Brazil. Proc R Soc Lond B. 2008, 275: 1385-10.1098/rspb.2008.0110.
Friedman M: Ecomorphological selectivity among marine teleost fishes during the end-Cretaceous extinction. Proc Natl Acad Sci USA. 2009, 106: 5218-10.1073/pnas.0808468106.
Halanych K: Molecular phylogeny of siboglinid annelids (a.k.a. pogonophorans): a review. Hydrobiologia. 2005, 535-536: 297-307. 10.1007/s10750-004-1437-6.
McMullin E, Hourdez S, Schaeffer SW, Fisher CR: Phylogeny and biogeography of deep sea vestimentiferans and their bacterial symbionts. Symbiosis. 2003, 34: 1-41.
Nelson K, Fisher C: Absence of cospeciation in deep-sea vestimentiferan tube worms and their bacterial endosymbionts. Symbiosis. 2000, 28: 1-15.
Palumbi SR: Nucleic acids II: The polymerase chain reaction. Molecular Systematics. Edited by: Hillis DM, Moritz C, Mable BK. 1996, Sunderland, Massachusetts: Sinauer Associates, 205-247. 2
Lenaers G, Maroteaux L, Michot B, Herzog M: Dinoflagellates in evolution. A molecular phylogenetic analysis of large subunit ribosomal RNA. J Mol Evol. 1989, 29: 40-51. 10.1007/BF02106180.
Hillis DM, Dixon MT: Ribosomal DNA: molecular evolution and phylogenetic inference. Quart Rev Biol. 1991, 66: 411-453. 10.1086/417338.
Colgan D, Ponder W, Eggler P: Gastropod evolutionary rates and phylogenetic relationships assessed using partial 28S rDNA and histone H3 sequences. Zool Scripta. 2000, 29: 29-63. 10.1046/j.1463-6409.2000.00021.x.
Edgar RC: MUSCLE: a multiple sequence alignment method with reduced time and space complexity. BMC Bioinform. 2004, 5: 113-10.1186/1471-2105-5-113.
Maddison WP, Maddison DR: MacClade (Ver. 4.0): Computer Program for Phylogenetic Analysis, version 4.08. 2005, Sinauer Associates, Inc
Nylander JAA: MrModeltest, version 2. 2004, Distributed by the author, Evolutionary Biology Centre, Uppsala University
Akaike H: A new look at the statistical model identification. IEEE Trans Autom Contr. 1974, 19: 716-723. 10.1109/TAC.1974.1100705.
Rozas J, Sánchez-DelBarrio JC, Messeguer X, Rozas R: DnaSP, DNA polymorphism analyses by the coalescent and other methods. Bioinformatics. 2003, 19: 2496-2497. 10.1093/bioinformatics/btg359.
Xia X, Xie Z: DAMBE: Software Package for Data Analysis in Molecular Biology and Evolution. J Hered. 2001, 92: 371-373. 10.1093/jhered/92.4.371.
Huelsenbeck JP, Ronquist F: MRBAYES: Bayesian inference of phylogenetic trees. Bioinformatics. 2001, 17: 754-755. 10.1093/bioinformatics/17.8.754.
Ronquist F, Huelsenbeck JP: MRBAYES 3: Bayesian phylogenetic inference under mixed models. Bioinformatics. 2003, 19: 1572-1574. 10.1093/bioinformatics/btg180.
Nylander JAA, Wilgenbusch JC, Warren DL, Swofford DL: AWTY (are we there yet?): a system for graphical exploration of MCMC convergence in Bayesian phylogenetics. Bioinformatics. 2008, 24: 581-583. 10.1093/bioinformatics/btm388.
Rambaut A, Drummond A: FigTree: Tree Figure Drawing Tool, version 1.1.2. 2003, Institute of Evolutionary Biology, University of Edinburgh
Swofford DL: PAUP*: Phylogenetic Analysis Using Parsimony (*and other methods), version 4.0, Sinauer. 2002
Drummond AJ, Rambaut A: BEAST, Bayesian evolutionary analysis by sampling trees. BMC Evol Biol. 2007, 7: 214-10.1186/1471-2148-7-214.
Rambaut A, Drummond AJ: Tracer, version 1.4. 2003, University of Oxford
We thank the captains and crews of the R/V Western Flyer and R/V Point Lobos and the pilots of ROV Tiburon and ROV Ventana for their technical support and patience. We gratefully appreciate the role that W. Joe Jones played in the early phases of this research. Thanks to Ken Halanych for providing a tissue sample from Sclerolinum brattstromi, and to Julio Harvey for his editorial help. Funding for this project was provided by the Monterey Bay Aquarium Research Institute (The David and Lucile Packard Foundation), NSF Award #0334932 (under the Assembling the Tree of Life program) to investigate the Tree of Life for Protostomes, and SIO for start up funds to GWR.
RCV conceived of the project, directed the research, and composed much of the manuscript. SBJ obtained the DNA sequences and conducted most of the phylogenetic analyses. GWR obtained the images of Osedax OTUs, conducted morphological examinations, and contributed to the phylogenetic analyses and writing of the manuscript.