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Description and relationships of Chaetopterus pugaporcinus, an unusual pelagic polychaete (Annelida, Chaetopteridae).


Chaetopterids are an unusual polychaete group. All previously described species are benthic and tubiculous as adults. They have a body divided into three distinct regions--anterior, middle, and posterior--hereafter referred to as A, B, and C (after Crossland, 1904; Bhaud et al., 1994; Fig. 1c). Their larvae have a unique barrel-like form with one or two ciliated bands at the midsection and a large buccal funnel (Fig. 1a, b). Chaetopterid larvae are some of the largest among polychaetes, typically ranging in size from 0.4 to 2.5 mm. The largest polychaete larvae reported, with a maximum length of 12 mm, are the late stage of an unknown phyllodocid species (Tzetlin, 1998). Those phyllocdocid larvae consisted of a trochophore body and rudimentary adult trunk comprising up to 120 chaetigerous segments. Nozais et al. (1997) reported Poecilochaetus larvae with up to 50 segments and reaching nearly 10 mm. Late-stage spionid and Magelona larvae have been reported to be nearly 5 mm. Most polychaete larvae, however, seldom exceed 1.3 mm (Bhaud and Cazaux, 1987).

The taxonomy and systematics of the Chaetopteridae have never been comprehensively revised, and there is continuing confusion over the number of accepted species. For instance, Hartman (1959), following a suggestion by Fauvel (1927), synonymized all 25 Chaetopterus species into the single highly variable species C. variopedatus, suggesting that the species were local populations and reliable specific distinctions had not yet been found. In part this view of Chaetopterus may be due to the extended plank-tonic larval periods of some species whose larvae may remain in the water column for several months to over a year. Scheltema (1974) determined that the length of time chaetopterid larvae spend in the water column would easily allow their dispersal across ocean basins. This speculation supported the hypothesis of widespread genetic mixing and consequent taxonomic "lumping" to form large, cosmopolitan species complexes such as Chaetopterus variopedatus (Renier, 1804) and Spiochaetopterus costarum (Claparede, 1868). C. variopedatus is now considered a species complex that contains at least 18 species (Petersen, 1984a, b, 1997; Bhaud, 1998), though the redescriptions are yet to be formalized. Similarly, S. costarum has been shown to be a species complex (Bhaud and Fernandez-Alamo, 2000; Bhaud and Petti, 2001; Bhaud, 2003; Bhaud et al., 2003). Careful examination of Spiochaetopterus showed that, despite widespread larval dispersal, adult distributions of given species are far more limited than previously expected (Bhaud, 2003).

We describe here a new species, Chaetopterus pugaporcinus (Fig. 2), based on specimens that may be larvae or adults. We also present a phylogenetic analysis based on molecular data for the Chaetopteridae and provide the first molecular evidence to refute Hartman's proposal (Hartman, 1959) that Chaetopterus variopedatus is a single cosmopolitan species.

Materials and Methods

Eight specimens of the new species were observed and collected from the midwaters of Monterey Bay, California (Table 1), from 2001 to 2006. All in situ observations were made with the remotely operated vehicles Ventana or Tiburon (Robison, 1993). The ROV Ventana video system consisted of a Sony high-definition HDC-750A camera; the ROV Tiburon system was a Panasonic high-resolution, three-chip video camera. Video was recorded on high-quality BetaCam or HDTV tapes for subsequent analysis, and these are housed in the video archive at the Monterey Bay Aquarium Research Institute. Specimens were captured in 7.5-1 detritus samplers, which preclude the crushing and abrasion typically inflicted on soft-bodied animals by nets (Robison, 1993). Specimens were transferred directly from the ROV to still-water aquaria at in situ temperatures, where they were observed and photographed. Live specimens were photographed with a Nikon Coolpix 5000 as macro shots in the aquaria, as well as through a Nikon BH-2 compound microscope. Line drawings were produced both from digital images and by using a camera lucida attached to the microscope.

Fecal pellets were collected from four specimens. Pellets were removed from the still-water aquaria in which the live specimens were held from time zero until 6 days after collection. Pellets were removed with a glass pipette and placed into 2% gluteraldehyde in filtered seawater with 0.1 mol [l.sup.-1] sodium cacodylate. Pellets were shredded with fine dissecting needles in the fixative to create a slurry, filtered onto 0.2-[micro]m-pore polycarbonate filters (Osmonics, Inc.), air-dried, and coated with gold-palladium. Stubs were viewed on an ISI WB6 scanning electron microscope and digital images were captured.


Two specimens (labeled 13 Dec. 2001 and 3 Dec. 2002 in Table 1) of the new species were destroyed for sequencing. Additional Chaetopterus were obtained from four locations (Table 2) to address the validity of the cosmopolitan species complex (Petersen, 1984a, b; Petersen and Britayev, 1997). Throughout this paper, we differentiate Chaetopterus specimens either as undescribed--when their morphology and locality do not match any previously published--or as sensu the original description name. Representatives of the remaining chaetopterid genera, Mesochaetopterus, Phyllochaetopterus, and Spiochaetopterus, were obtained to complete the ingroup sampling. There is no hypothesis for the sister group to the Chaetopteridae, thus nine taxa were selected as outgroup terminals (Table 2) spanning the large polychaete clade Canalipalpata that contains the Chaetopteridae. Terminals included examples from Sabellida, Cirratuliformia, Terebelliformia, and Spionida (sensu Rouse and Pleijel, 2001); unfortunately, specimens of Magelona and Apistobranchus, two candidate sister taxa, were unattainable for inclusion in this project. Specimens (Table 2) were collected intertidally, using scuba, or from deep water with the ROV Tiburon.

Genetic data collection

Worms used for genetic data collection were placed in 70% to 95% ethanol after collection. Voucher specimens were placed in the Los Angeles County Museum of Natural History (LACM) or the South Australian Museum (SAM) along with the types (see Table 2 for accession numbers). If a specimen was large enough (greater than 0.05 g), tissue was cut from the midsection of the worm for DNA extraction, and the remains were preserved in formalin as the voucher. Genomic DNA was extracted from specimens by using DNAzol genomic DNA isolation reagent (Molecular Research Center, Inc., Cincinnati, OH) with the following modifications to the manufacturer's instructions. A 1- to 2-[mm.sup.2] cube of tissue was homogenized in 500 [micro]l of DNAzol reagent and placed in a rotating incubator at room temperature for 24-72 h. For each 24-h period, 10 [micro]l of 10 mg/ml proteinase kinase was added. To help visualize the DNA, 2 [micro]l of polyacryl carrier was added to each extraction. DNA was extracted from specimens of Paralvinella grasslei Desbruyeres & Laubier, 1982; Gunnarea capensis Johansson, 1927; Terebellides stroemii Sars, 1835; Spirorbis spirorbis (Linnaeus, 1758); Manayunkia athallasia Hutchings et al., 1981; Dodecaceria concharum Oersted, 1843; and Pectinaria granulata (Linnaeus, 1767) by using the Qiagen DNeasy tissue kit (Valencia, CA) according to the manufacturer's instructions.

An approximately 1800-bp fragment of small subunit ribosomal (18S) DNA was amplified with universal primers mitchA (5'-CAACCTGGTTGATCCTGCCAGT-3') and mitchB (5'-TGATCCTTCCGCAGGTTCACCTAC-3') modified from Medlin et al. (1988). The amplification profile was optimized for each extraction: 35 ramping cycles of 94 [degrees]C for 60 s, 58-64 [degrees]C for 60 s, 72 [degrees]C for 90-120 s, with an initial single denaturation step at 94 [degrees]C for 3 min and a final single extension step at 72 [degrees]C for 4-7 min. An approximately 650-bp fragment of the mitochondrial COI gene was amplified using primers HCO2198 (5'-TAAACTTCAGGGTGACCAAAAAATCA-3') and LCO1490 (5'-TCAACAAATCATAAAGATATTGG-3') (Folmer et al., 1994). The amplification profile was optimized for each extraction, optionally with a touchdown of five cycles of 94 [degrees]C for 60 s, 45 [degrees]C for 90 s, 72 [degrees]C for 60 s, and then 35 cycles of 94 [degrees]C for 30-40 s, 51 [degrees]C for 30-90 s, 72 [degrees]C for 60 s, with an initial single denaturation step at 94 [degrees]C for 60-120 s and a final single extension step at 72 [degrees]C for 5-7 min. An approximately 1100-bp fragment of large subunit ribosomal (28S) DNA was amplified with modified universal primers (Lenaers et al., 1989) LSUD1F (5'-ACCCGCTGAATTTAAGCATA-3') and D3ar (5'-ACGAACGATTTGCACGTCAG-3'). The amplification profile was optimized for each extraction: 35 cycles of 94 [degrees]C for 40-60 s, 60 [degrees]C for 30-60 s, 72 [degrees]C for 70-120 s, with an initial single denaturation step at 94 [degrees]C for 5 min and a final single extension step at 72 [degrees]C for 5-7 min.

PCR products were either sequenced directly after spin column purification (Ultrafree-DA columns, Millipore, Billerica, MA), following the manufacturer's protocol or, in a few cases, cloned according to the manufacturer's protocol of the Invitrogen (Carlsbad, CA) TOPO cloning kit. In the latter case, three to six colonies were chosen for plasmid DNA purification using a QIAprep spin miniprep kit (Qiagen, Valencia, CA). Plasmid DNA was digested with EcoRI to check for correct-size inserts. Cloned DNA was sequenced in both directions using M13 primers. All direct sequencing was carried out using the same primers that were used in the amplification, with the addition of three internal primers for 18S (514F 5'-TCTGGTGCCAGCAGC-CGCGG-3'; 1055F 5'-GGTGGTGCATGGCCG-3'; 1055R 5'-CGGCCATGCACCACC-3'). All sequencing was carried out with the BigDye terminator ver. 3.1 sequencing kit and analyzed on an ABI 3100 capillary sequencer (Applied Biosystems, Foster City, CA). Sequences were deposited in GenBank (accession numbers are listed in Table 2).


At least two of the three gene sequences were obtained from most samples (Table 2), with the exception of one ingroup taxon, Mesochaetopterus japonicus. The topology of the trees did not change whether or not taxa with missing sequences were included. We used a criterion that sequences could only be concatenated for a combined analysis when sequenced from the same individual. None of the previous chaetopterid sequences available from GenBank met this criterion; thus no sequences from GenBank were used in the final analyses.

Sequences were aligned with T-coffee (Notredame et al., 2000) and proofread by eye in MacClade ver. 4.04 OS X (Maddison and Maddison, 2000). Four separate preliminary Bayesian analyses were run on the aligned sequences with differing amounts of the alignments excluded. The most conservative analysis excluded any base for which any sequence contained a gap; the most inclusive included all regions. Two other analyses contained intermediate amounts of ambiguously aligned bases: one more conservative, in which any base for which 8 or more taxa had a gap was removed; the other less conservative, in which any base for which 16 or more taxa had a gap was removed. All were run as described below for the final Bayesian analyses but with only 11 million generations. No differences in ingroup generic relationships or in the relative support for the clades of interest were found among the four analyses; thus arbitrary removal of data was avoided by retention of all bases in subsequent analyses (see supplementary material at No ambiguously aligned bases were removed from the final analyses (18S = 12.3% ambiguously aligned; 28S = 14.3% ambiguously aligned; COI = 0% ambiguously aligned). The alignments are deposited in GenBank and TreeBase, and are available from KJO.

Parsimony analyses were conducted with the PAUP 4.0b 10 software package (Swofford, 2002). Parsimony trees were reconstructed from an equally weighted character matrix and the heuristic search option, using the tree-bisection-reconnection branch-swapping algorithm and 1000 random addition replicates. Gaps were treated as missing data because of the four taxa with missing sequences. Bootstrap and jackknife (37% deletion) values were obtained with the same settings as the parsimony analysis.

Bayesian analyses of the data sets were conducted using MrBayes 3.0b4 (Huelsenbeck and Ronquist, 2001). Standard procedures based on Modeltest 3.5 (Posada and Crandall, 1998) were implemented in PAUP to select the most appropriate models for the analyses. The relative fit of models was assessed by the Akaike information criterion, AIC = -2 In L + 2n where L is the maximum likelihood score and n is the number of free parameters of the model. Smaller values of AIC are preferred (Akaike, 1974; Posada and Crandall, 2001), and the General Time Reversible + Proportion Invariant + Gamma (GTR + I + [GAMMA]) represents the optimal model with respect to the 18S and 28S data and General Time Reversible + Site Specific (GTR + SS) with respect to the COI data. Genes were unlinked in the concatenated analyses. Each markov chain, three heated and one cold, was started from a random tree and all four chains ran simultaneously for 3 to 52 million generations (see below), with trees being sampled so that the resulting data set from each run contained at least 10,000 data points after at least 1000 had been discarded as burnin. Tracer ver. 1.2 (Rambaut and Drummond, 2003) was used to check auto-correlation of individual parameters and to check that the 1000 generations discarded as burnin were sufficient to ensure that the chain had reached convergence before inference from the Markov chain Monte Carlo data set was made. Several repetitions of the analysis converged on similar parameter estimates (numerous runs of ca. 3 million, three runs of 11 million, one run of 31 million for individual genes and 52 million for the concatenated sequences).



CHAETOPTERIDAE Audouin & Milne-Edwards, 1833

Chaetopterus Cuvier, 1830

Chaetopterus pugaporcinus, new species

Type material

The holotype, collected from Monterey Bay, California, 36.32[degrees]N, 122.89[degrees]W, in December 2004 by KJO and BHR, is deposited at the Los Angeles County Museum of Natural History Allan Hancock Foundation Polychaete Collection (LACM-AHF POLY 2173). All specimens collected are of undetermined sex. Four paratypes exist and are deposited, two at LACM (LACM-AHF POLY 2174 and 2175) and two at the South Australian Museum, Adelaide (SAM E3508, E3509). One specimen is partially sectioned along the longitudinal axis of the body; the region-A chaetae are mounted on permanent slides; the remaining tissue, consisting of anteroventral body, is in 70% ethanol (SAM E3508). Tissue from an additional specimen, originally frozen and now in chilled 95% ethanol, and that of two additional specimens is retained by KJO at the Monterey Bay Aquarium Research Institute.


Small to medium-sized (10-21 mm in body length and width) Chaetopterus with peristomium and prostomium resembling larval preoral and postoral lobes (Fig. 1 and Fig. 3b). Peristomial palps short, rudimentary to as long as peristomium. Eyes absent. A middorsal ciliated groove running from posterior margin of segment A9 to at least posterior margin of region B. Body with two or three regions (regions A, B, and C, with segments of each region numbered separately as Al, A2, etc.; B1, B2, etc.). Region A with 9 chaetigers, parapodia uniramous except A9, with neuropodia as uncinal plates, notopodial lobes short and simple, lanceolate chaetae just projecting from dorsal to distal surface, lacking cutting spines. Region B composed of two greatly expanded, biramous segments (B1 and B2) and three additional uniramous segments, B1 much larger than B2, notopodia of B1-2 with up to 10 internal chaetae, neuropodia as uncinal plates in a single lobe. Region C consists of one segment at most and the pygidium, possibly with uncinal plates. Compressed nature of region C leaves room for further interpretation of segmentation there. Body formula = 9A, 5B, 1(+1)C = 15 segments.

Type locality

Monterey Bay, California, 36.32[degrees]N, 122.89[degrees]W, from 1029 m where the seafloor is 3500 m deep.


The species is named pugaporcinus (based on the following Latin roots and suffix respectively: puga = rump; porcus = pig; and inus = having the likeness of) for its resemblance to the "rump of a pig." Puga and porcus are nouns in opposition, resulting in a masculine specific epithet to agree in gender with Chaetopterus. For the sake of simplicity and euphony, an "a" was chosen as the connecting vowel instead of the usual "ato" or "i."


Holotype 17 mm long in life, paratypes 10-21 mm long in life. Region A with 9 segments, compressed so notopodia project anteriorly under prostomium, forming an arch running dorsoventrally (Figs. 3b and 4c). Each A-region notopodium with 6-10 lanceolate chaetae (Fig. 3d). Segment A9 with neuropodial uncini on either side of anteriormost portion of middorsal ciliated groove (Fig. 3b). Middorsal ciliated groove beginning at posterior margin of segment A9, continuing to at least posterior margin of region B. Prostomium large (to 20% of body length), bilobed, and folding towards the posterior (Figs. 3b and 4a). Peristomium broadly horseshoe-shaped, with short (no longer than length of peristomium) grooved palps; no eyes. Region B wth 5 segments. Segment B1 greatly enlarged, accounting for more than 80% of body length, and as broad as animal is long. Segment B2 nearly one-fourth as long as B1 at longest, B3-B5 compressed. Inflation of B1 and compression of anterior and posterior segments gives animal a nearly spherical appearance when undisturbed (Fig. 2). When disturbed, animal contracts, withdrawing region A, segments B3-5, region C, and the middorsal ciliated groove toward the body center (Fig. 4b). Neuropodial uncinal plates on posterior margin of segments in regions B and C, lateral to middorsal ciliated groove and with a single row of uncini. The sectioned specimen revealed notopodia in segments B1 and B2 with up to 10 internal, simple chaetae lateral to the uncinal plates. Region C difficult to discern from pygidium but seems to consists of 1 uniramous segment. The pygidium consists of a cylindrical appendage immediately dorsal to the anus.

Live animal semitransparent white to beige with dark brown to purple pigment lining interior of buccal region. Gut packed with dark material, making it easily distinguishable through body wall (Figs. 3c and 4b, d). No glandular plate, ventral shield, or plastron is found. Cilia present only in the middorsal, ciliated groove and lining interior of buccal region.


No stout, modified chaetae (cutting spines) on segment A4. Lanceolate chaetae in notopodia A1-A9 (Fig. 4e), measuring 1.14 to 2.34 mm long and up to 0.07 mm wide from an 18-mm-long specimen (SAM E3508), with longest chaetae found in chaetiger A5.

Uncini (Fig. 4f, g) present posteriorly in all chaetigers from A9. Ten to more than 40 uncini per uncinal plate, A9 consistently contained the most, with decreasing numbers found in posterior chaetigers. General uncinal shape is ellipsoid or rounded-rectangular, measuring 37 by 22 [micro]m in maximum dimensions; decreasing slightly in posteriormost segments. Teeth are prominent and few, 8-12. Tooth roots are slightly oblique relative to anterior-posterior direction of uncinal plate. Posterodorsal face with distinct shoulder overhanging a concavity leading to a sharp heel projecting slightly from flat or convex sole. Ventral insertion zone roughly convex, with posterior height less than the anterior height. Uncini of region B as above (Fig. 4g) to those with less pronounced shoulder and concavity above the projecting heel (Fig. 4f).


Dorsoventrally broadened S-shaped gut projects into cavity formed by segments B1 and B2, arching ventrally and then dorsally before decreasing abruptly and traveling along dorsal body wall directly to anus (Fig. 3c). Small orange, glandular organ attached to posterior portion of digestive tract within B3-5 segments, and numerous pouches of connective tissue attached to the gut and filled with fluid. Interior of B1 and B2 forming a well-developed coelomic cavity filled with the fluid-filled pouches. Septa are distinct between region A segments but incomplete between region B and C segments, which are indicated by the presence of uncinal plates and annulations on the external surface (Fig. 4b-d).

One half of one paratype (SAM E3508) was sectioned longitudinally to search for gametogenic tissue and to examine septation and internal chaetae. No decisive gametogenic tissue was found. No gametes were seen through the nearly transparent body walls of any of the individuals collected.


The unusual body form of C. pugaporcinus allows few direct morphological comparisons with described chaetopterids. This novel species is morphologically most similar to Chaetopterus and Mesochaetopterus on the basis of larval form, size, and uncinal form. Angle of the tooth roots, relative to the anterior-posterior direction of the uncinal plate, has been used (Bhaud, 2003) to distinguish Mesochaetopterus (perpendicular) from Chaetopterus (oblique). Chaetopterus pugaporcinus uncini are most similar to those of Chaetopterus, yet the morphology suggests that this feature may vary more than shown by Bhaud's (2003) examples. The new species also resembles Chaetopterus in having five region-B segments, although their form differs considerably from those previously described in Chaetopterus larvae or adults. The short palps are typical of Chaetopterus. These three features alone are insufficient to determine the taxonomic affinities of this unusual species.

This new species differs from all previously described Chaetopterus species in the general form of the body (spherical body consisting of segment B1 and B2, with remaining segments compressed to the anterior and posterior surfaces of the two enlarged segments); the shape of the uncini (overhang, concavity, and sharp heel on the posterior-dorsal face); the lack of cutting spines on segment A4; and the presence of internal notochaetae in B2. The molecular data further support the uniqueness of this species (total uncorrected divergence = 18S: 0.4%-1.6%, 28S: 1.7%-7%, COI: 18%-21%) when compared to other Chaetopterus. The novelty of this species extends beyond the differences mentioned above, to the combination of larval and adult features and extended use of the larval habitat. It is not yet possible to determine whether the specimens are the first pelagic member of Chaetopteridae to be described or gigantic larvae that have yet to metamorphose and settle, because no reproductive individuals have been found.

Chaetopterus pugaporcinus resembles L5 stage (competent to metamorphose) Chaetopterus larvae (Irvine et al., 1999) in many ways. Typical chaetopterid larvae are compact, barrel-shaped, and nearly as wide as long in earlier stages; they elongate as they age. They possess one or two ciliated mesotrochal rings (Blake, 1996, reports as many as three) and adult chaetae (Bhaud, 2003). The form of the prostomium and peristomium of C. pugaporcinus resembles enlarged larval preoral and postoral lobes, with the prostomium folding dorsally. The arrangement of region A segments after relaxation, the form of pygidial tissue ventral to the anus, the lack of dorsal-ventral flattening of region A, the lack of elongation of the entire body, and the pelagic habitat are additional similarities shared with larval chaetopterids. L6 stage Chaetopterus larvae (mid-metamorphosis) differ from C. pugaporcinus in the form of the prostomium and peristomium, the general shape of region A, the presence of aliform notopodia in segment B1, the development of an accessory feeding organ, and the relative size and shape of segments in region B and C (Irvine et al., 1999). Thus, the specimens described here have not yet developed the morphology of L6 stage larvae as described by Irvine et al. (1999).

Despite the similarities to L5 stage Chaetopterus larvae, there are also several notable differences. Chaetopterus pugaporcinus lacks ciliated trochal bands, a key larval characteristic. The trochal bands are present into L6 stage larvae, when they are incorporated into the aliform notopodia of segment B1 (Irvine et al., 1999). None of the elaborate notopodia often found in other chaetopterids have been observed in C. pugaporcinus. L5 stage Chaetopterus show no external evidence of segmentation surrounding the mesotrochs (the tissue that will become segments B1-2, Irvine et al., 1999), whereas C. pugaporcinus has well-developed B1 and B2 annulations and biramous parapodia on these segments. Also, just anterior to the pygidium, L5 larvae possess a pair of lateral outgrowths that will become notopodia of segment C1 (Irvine et al., 1999); C. pugaporcinus lacks these notopodia. Several nonlarval features are present in C. pugaporcinus, including well-developed septation of segments A1-9, infolding of the epidermis designating segments of regions B and C, uniramous parapodia in segments following B2, and an enlarged coelomic cavity within region B.

Mesochaetopterus larvae are the largest chaetopterid larvae reported to date, reaching as much as 2.5 mm in length, whereas most chaetopterid larvae range from 0.4 to 1 mm (Bhaud and Cazaux, 1987). The specimens described here were nearly an order of magnitude larger than any chaetopterid larvae reported previously. Despite the 11-mm range in total length observed, specimen morphology was consistent from one specimen to the next, differing only in the length of the peristomial palps and possibly the number of segments in region C (+1). Palp length appears correlated to the specimen size: rudimentary palps were found on the smallest specimens and longer palps on larger specimens. As is characteristic of Chaetopterus, even the longest palps were never longer than the peristomium. The specimen that may have an additional region C segment was not the largest specimen collected. Specimens shrank considerably when damaged and shriveled further when preserved, even when relaxed prior to preservation. Preserved specimens measure 4-11 mm. Shrinkage is commonly observed in pelagic polychaetes, especially tomopterids, alciopids, and typhloscolecids (KJO, pers. obs.). Sizes of larvae reported in the literature are likely a mixture of live and preserved measurements, with the largest measurements taken from fresh material. Thus our measurements (up to 21 mm) can be directly compared to Bhaud and Cazaux's (1987) greatest measurement of 2.5 mm.


Chaetopterus pugaporcinus has been found in the water column between 875 and 1221 m, in water 1600 to 3500 m deep. The animal is neutrally buoyant when uninjured and remained so in the laboratory for as long as 6 days. If an animal was injured, region B shriveled and the specimen sank to the bottom of the aquarium.

In situ specimens were observed attached to a cloud of mucus that was several times the size of the animal. Water disturbance generated by the ROVs caused separation of the animals from their mucous clouds. Specimens held in the laboratory were observed to produce mucus that formed unorganized clouds from the middorsal ciliated groove and from the cylindrical pygidial projection dorsal to the anus. The resulting mucous cloud was not released by the animal but remained in contact with the cylindrical pygidial projection (Figs. 3c and 4b). Fecal pellets were found in the mucous cloud after several hours.

It is assumed that feeding occurs by collection of sinking marine "snow" particles in the mucus produced from the middorsal ciliated groove. Periodically, the mucous cloud would have to be drawn into the mouth and the aggregate consumed. Feeding by collection of particles on mucus is common in pelagic larvae and other gelatinous zooplankton. For example, Poecilochaetus larvae are reported to produce a three-dimensional network of mucous strands that they then move along individually while feeding on small particles that adhere to the strands (Hamner et al., 1975), and larval pectinariids were recently shown to utilize a mucous filter while feeding in the water column (Pernet, 2004). Pseudothecosomatous pteropods use mucous webs manipulated by ciliary action to feed in the midwater (Gilmer, 1972), and larvaceans produce elaborate mucous feeding structures. Adult tubiculous chaetopterids feed by filtering through mucous bags manipulated by the aliform notopodia and cilia of the middorsal food groove (MacGinitie, 1939), and chaetopterid larvae are known to produce mucus (Nozais et al., 1997). It is likely that C. pugaporcinus feeds by the production of a mucous web that is manipulated by cilia of the middorsal groove and buccal area, although this was not observed directly.

Fecal pellets contained primarily skeletal remains of pelagic phytoplankton: coccolithophores, individual coccoliths, and diatom frustules (identified via scanning electron microscopy). They also contained pelagic foraminiferans, phaeodarians, silicoflagellates, dinoflagellates, as well as some unidentified soft material. Items in the fecal pellets were consistent with holopelagic suspension feeding on marine snow (KJO, unpubl. data).

Additionally, the mucous cloud may increase buoyancy, as also observed in Poecilochaetus larvae (Nozais et al., 1997). However, C. pugaporcinus specimens were able to maintain their positions in the aquaria for several hours without a mucous cloud.


Chaetopterus pugaporcinus is neutrally buoyant, and when encountered in situ, each specimen was fully inflated, floating in the lower mesopelagic portion of the water column. The oral surface is relatively dense and keeps the animal's anterior end oriented down at all times. There was no active response to light, water disturbance, or the sound of the ROV, other than a slight contraction of regions A and C and the middorsal ciliated groove. When physically disturbed in situ, specimens did not change their posture or the distended nature of region B. When undisturbed in the laboratory, the animal floated in the upper one-third of the tank, attached to a mucous cloud. When exposed to isotonic magnesium chloride, or when the health of the animal deteriorated, the inflation of region B relaxed and the animal stretched longitudinally. No settling behavior was observed in animals kept in the laboratory, nor was swimming observed. There was no apparent ability to interact with any surface or object other than the mucous cloud. Specimens did not display any locomotory abilities.

One specimen was held in a still-water aquarium for 26 h. The floor of the tank was furnished with deep-sea mud and sand more than three body lengths deep, with a cluster of rocks on one side. The specimen made no attempt to interact with the substrate during that period, nor was any sign of the onset of metamorphosis observed. Irvine et al. (1999) report that it takes as little as 6 h for an L5 stage Chaetopterus larva to reach late L7 stage and complete metamorphosis.


One specimen was examined for bioluminescence and was found to produce light in two forms. Only this single specimen was tested, due to the destructive nature of the physical stimulation. Bright blue light outlined the peristomium/prostomium after direct physical stimulation. The area glowed for 3-6 s, then abruptly extinguished. Additionally, minute green, bioluminescent particles were spewed from the middorsal ciliated groove or surrounding area, and the posterior end. These small glowing specks were dispersed throughout the mucous cloud produced at the same time, and glowed vividly for 1-2 s before fading slowly. The mucus and bioluminescent particles were apparently forced away from the body by as much as two body lengths.

Luminescence is common in Chaetopterus (Nicol, 1952; Martin and Anctil, 1984; Nishi, 2000). Transitory and undispersed light is produced when direct physical stimulation or freshwater are applied to the peristomial palps, feeding structures on the dorsal surface of region B, and notopodia of region C. Nicol (1952) also found that photogenic glands on the aliform notopodia give off a luminescent secretion suspended in mucus that is dispersed in the surrounding water. Our observations do not conflict with any of these findings, but few comparisons can be drawn between them because of the differences in the structures present on C. pugaporcinus.

Phylogenetic relationships

Alignment of the concatenated sequences resulted in 3666 aligned base pairs. Of those, 2677 were either invariable or parsimony uninformative, leaving 989 parsimony informative base pairs. The equally weighted data matrix recovered two most parsimonious trees of length 5058, with a consistency index of 0.545, a retention index of 0.449, and a rescaled consistency index of 0.245. The strict consensus of these trees is shown on the left side of Figure 5 with poorly supported nodes (having bootstrap and jackknife values below 70%) collapsed.

Individual genes were also analyzed separately; informative sites included 513/1791 bp for the 18S gene; 687/1151 for the 28S gene, and 513/720 for the COI gene (162 first position, 112 second position, 239 third position). Individual gene trees are shown in Figure 6.

Chaetopteridae are consistently shown to be a monophyletic group containing two well-supported clades: clade 1 containing Mesochaetopterus and Chaetopterus and clade 2 containing Phyllochaetopterus and Spiochaetopterus (Figs. 5 and 6). Spiochaetopterus bergensis Gitay, 1969, is found nested among the Phyllochaetopterus terminals used here, suggesting that the latter may be paraphyletic, though further sampling of Spiochaetopterus is clearly needed.

Mesochaetopterus is found to be sister to Chaetopterus according to the 18S sequence data (Fig. 6), as well as in the combined analysis (Fig. 5). However, the 28S data show Mesochaetopterus nested among the Chaetopterus clade as sister group to C. pugaporcinus, and the COI data poorly supports the position of Mesochaetopterus in relation to Chaetopterus sp. 1.

Chaetopterus pugaporcinus falls as part of a Chaetopterus clade in the combined analysis, as well as with the 18S and COI sequences alone. Thus this novel pelagic chaetopterid is designated here as a species of Chaetopterus despite its extreme morphological modifications.

The two specimens of C. pugaporcinus sequenced were found to have identical sequences for all genes, with the exception of one ambiguous base in the 28S sequences. Total sequence differences between Chaetopterus specimens (total uncorrected divergence = 18S: 0.4% to 1.6%; 28S: 1.7% to 7.0%; COI: 18% to 21%) further support the idea that C. variopedatus sensu Hartman (1959) is actually a species complex and that the author unnecessarily synonymized a number of valid species. Chaetopterus pugaporcinus is considered a valid species owing to the sequence differences from Chaetopterus specimens collected from nearby localities for all three genes analyzed, as well as to their novel morphology.


Phylogenetic relationships

All of our analyses place Chaetopterus pugaporcinus within clade 1 (Mesochaetopterus and Chaetopterus), suggesting that the novel species described here belongs to Chaetopterus. The combined data set shows that it is most reasonable to place the new species as part of Chaetopterus, as do the 18S and COI data. The 28S data would place both Mesochaetopterus and C. pugaporcinus within Chaetopterus. Thus we have conservatively named the new species as a Chaetopterus, coinciding with the morphological findings.

Relationships in and around the Chaetopteridae are not well known, yet the monophyly of the group has never been questioned owing to the uniqueness of the chaetopterid body form. All genes examined provided further strong support for the monophyly of the group.

Relationships within the Chaetopteridae have been proposed as far back as Potts (1914), and of the four genera, Chaetopterus and Mesochaetopterus are most similar to each other. They are distinguishable by a feature of the uncini (Bhaud et al., 2002), as well as by the number and arrangement of region B and C segments and parapodial form. Phyllochaetopterus and Spiochaetopterus are also similar to each other with respect to their modified chaetae and their uncini (Bhaud, 2003) and are separated by the presence (Phyllochaetopterus) or absence (Spiochaetopterus) of "tentacular cirri" on chaetiger 1. Note that these tentacular cirri are in fact lobes containing chaetae (Rouse and Pleijel, 2001). Bhaud (2003) pointed out the difficulty of using hard parts (modified chaetae and uncini) to distinguish between Phyllochaetopterus and Spiochaetopterus, whereas these characters typically work well to distinguish these genera from Mesochaetopterus and Chaetopterus.

Our present data indicate that Mesochaetopterus is the sister group to Chaetopterus (Figs. 5 and 6), though this result is not apparent in the 28S data. Great difficulties were encountered when amplifying DNA from Mesochaetopterus specimens (three M. taylori and one M. japonicus) for large subunit ribosomal (28S) and COI genes, suggesting that mutations have taken place in the primer regions used. This difficulty was not encountered consistently within any other taxa during this project, or with amplification of the 18S ribosomal gene from Mesochaetopterus specimens. These mutations could be a synapomorphy for the group. Further taxon sampling, additional primer design/sequencing, and careful morphological work are necessary to fully determine the nature of the relationship between Mesochaetopterus and Chaetopterus.

Suspended larvae or holopelagic paedomorphic species?

There is no set number of days that chaetopterid larvae spend in the plankton; thus the larval period can be extended when appropriate habitat is not found (Bhaud et al., 1990; Hadfield and Strathmann, 1996). Whether the specimens described here are simply wayward larvae, swept off the continental shelf and unable to settle, thus growing to unusual size and developing adult features, or are the first known representatives of a holopelagic chaetopterid species, is yet to be resolved. However, we suggest that C. pugaporcinus is not a suspended larva waiting to metamorphose, despite the larval features present. Larval features of C. pugaporcinus include prostomial and peristomial form, lack of dorsoventral flattening of region A, lack of elongation of the body, form of pygidial tissue, and pelagic habitat. The principal evidence in favor of a holopelagic chaetopterid species is the lack of all ciliated mesotrochal rings and the presence of adult features. The latter include well-developed septation of segments A1-9, infolding of the epidermis designating segments of regions B and C, presence of parapodia on segments of regions B and C, and an enlarged coelomic cavity within region B. The same combination of larval, adult, and missing characters was found in each specimen, regardless of their broad size range (10-21 mm). If these were larvae waiting to settle, one would expect more adult features in the larger, older individuals and more larval features in the smaller, younger individuals, as found by Tzetlin (1998). However, the only differences we found were the relative lengths of the peristomial palps and possibly an additional region C segment in one medium-sized specimen. Palp length did not vary widely when considered relative to peristomium length, and palps are usually present in stage L5 Chaetopterus larvae. Palps no longer than the peristomium are a generic character of Chaetopterus.

Chaetopterus pugaporcinus was a particularly distinctive chaetopterid because, among other characters, it lacks modified A4 chaetae. If these specimens are larvae, they are nearly 10 times larger than any reported chaetopterid larva, and the largest is nearly twice the size of the largest larval polychaete reported (Tzetlin, 1998). A large larva would most likely metamorphose into a relatively large species, and it seems unlikely that such a distinctive macrofaunal species would have been unobserved with the extensive benthic sampling carried out off California (Blake, 1996), unless it is utilizing a poorly studied (midwater) or rare habitat. A large undescribed chaetopterid has indeed been found in large numbers around a whale fall in Monterey Bay (G.W. Rouse and C. E. Brady, unpubl. data), but it differs dramatically from C. pugaporcinus (Phyllochaetopterus sp. 1: tentacular cirri, uncini, glandular crescent, modified chaetae, and significant total uncorrected sequence divergence, 18S: 3%, 28S: 13%, COI: 26%).

Chaetopterus pugaporcinus is found within a narrow depth range regardless of distance from shore or bottom depth, possibly suggesting adaptation to a specific habitat. In Monterey Bay, this depth range coincides with the bottom of the oxygen minimum zone. The lower interface of the oxygen minimum zone is often the site of concentrated marine snow and other debris that has fallen, essentially unchanged, through the above layer of low oxygen, and represents a relatively rich food source (Wishner et al., 1995). The ecological flexibility of chaetopterid larvae is well established (Bhaud and Duchene, 1996; Irvine et al., 1999), so it is reasonable to consider that a holopelagic form has arisen within the Chaetopteridae and that it resembles their pelagic larvae. Holopelagic polychaetes have evolved independently several times among annelids (Rouse and Pleijel, 2001).

Paedomorphosis (juvenile features retained in adults) is a mechanism of evolutionary change sometimes seen as simplification of the body, a feature common in mesopelagic animals (Herring, 2002) and may be the case with C. pugaporcinus. Chaetopterus pugaporcinus lacks the modified chaetae (cutting spines) used to cut the tube to allow for growth, a feature directly related to tubiculous living and one that may "weigh heavily" on a neutrally buoyant animal. It seems reasonable that these would be lost after adoption of a holopelagic lifestyle and therefore would be autapomorphic losses for C. pugaporcinus.


Chaetopterus pugaporcinus exhibits a combination of larval and adult features, and the habitat in which the specimens were found is typical only of chaetopterid larval stages. The question of adult status is not resolved because none of the eight specimens collected had recognizable reproductive products. This question would be fully resolved if a reproductive individual were collected in midwater or if a benthic adult were found that genetically and to some extent morphologically matched that described here. Regardless, the species introduced here is particularly interesting because of its great size and its continued survival deep in the water column with a consistent combination of larval and adult features. This prolonged survival is accomplished by retention of larval features already adapted to a pelagic life and loss of features necessary for a tubiculous life.


We are indebted to Fredrik Pleijel, Eijiroh Nishi, Robert Vrijenhoek, Shane Anderson, and Megan Dethier for providing specimens. Steve Haddock, Christy Schnitzler, W. Joseph Jones, C. Robert Young, and Lynne Christianson were extremely helpful with the molecular portion of the project. Jonathon Krupp and Kurt Buck were very helpful with the SEM work. Thanks also to the pilots of the ROVs Ventana and Tiburon, and the crews of the RVs Point Lobos and Western Flyer for their expertise and dedication to the exploration of the deep sea. Thanks to two reviewers for suggestions that improved the manuscript. A particular thanks is due Mary Petersen for advice and suggestions that greatly improved the manuscript. The David and Lucile Packard Foundation provided support for this project through the MBARI Midwater Ecology Group.

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(1) Monterey Bay Aquarium Research Institute, 7700 Sandholdt Rd., Moss Landing, California 95039; (2) South Australian Museum, Nth Terrace, Adelaide, SA 5000, Australia; and (3) California Institute of Technology, Dept. Environmental Science and Engineering, MC 138-78, 1200 East California Blvd., Pasadena, California 91125

Received 14 November 2005; accepted 24 October 2006.

* To whom correspondence should be addressed. E-mail:

[dagger] Current address: Marine Biological Research Division, Scripps Institution of Oceanography, La Jolla, CA 92093-0202.
Table 1 Chaetopterus pugaporcinus collection information

              Location near
Date          Monterey Bay, CA                   Accession no.

 1 Oct. 2001  36.57[degrees]N, 122.52[degrees]W  SAM E3509
13 Dec. 2001  36.69[degrees]N, 122.05[degrees]W  n/a
 3 Dec. 2002  36.69[degrees]N, 122.05[degrees]W  SAM E3508
16 Dec. 2004  36.32[degrees]N, 122.89[degrees]W  Holotype LACM-AHF POLY
25 Mar. 2005  36.34[degrees]N, 122.29[degrees]W  Paratype LACM-AHF POLY
 9 Aug. 2005  36.71[degrees]N, 122.06[degrees]W  Paratype LACM-AHF POLY
10 May. 2006  36.60[degrees]N, 122,38[degrees]W  n/a
24 Jun. 2006  36.65[degrees]N, 122.12[degrees]W  n/a

                                             Depth (m;
              Fixative (fixative,            collection,  Temp.
Date          preservative)                  seafloor)    ([degrees]C)

 1 Oct. 2001  Formalin                       1221, 3500   3.4
13 Dec. 2001  Frozen, ethanol                 990, 1600   4.0
 3 Dec. 2002  Formalin, ethanol & sectioned  1121, 1600   3.6
16 Dec. 2004  Formalin, ethanol              1029, 3500   3.8
25 Mar. 2005  Gluteraldehyde, formalin        965, 3000   3.9
 9 Aug. 2005  Gluteraldehyde, formalin        875, 1600   4.3
10 May. 2006  Formalin                       1098, 1600   3.69
24 Jun. 2006  Gluteraldehyde                 1203, 2100   3.48

              Salinity  Oxygen
Date          (PSU)     (ml/l)

 1 Oct. 2001  34.5      0.56
13 Dec. 2001  34.5      0.39
 3 Dec. 2002  34.5      0.52
16 Dec. 2004  34.4      0.41
25 Mar. 2005  34.4      0.34
 9 Aug. 2005  34.5      0.24
10 May. 2006  34.4      0.50
24 Jun. 2006  34.4      0.56

Table 2 Collection data and sequence information for outgroup and
chaetopterid specimens

                                   18S GenBank  28S GenBank  COI GenBank
Taxon                              Acc. #       Acc. #       Acc. #

Dodecaceria concharum              AY577891     DQ209242     DQ209262
  Oersted, 1843 Cirratulidae
Paralvinella grasslei              AY577886     N/A          DQ209259
  Desbruyeres & Laubier,
  1982 Alvinellidae
Glyphanostomum sp. Ampharetidae    DQ209225     DQ209240     DQ209260
Pectinaria granulata (Linnaeus,    AY577890     DQ209239     DQ209258
  1767) Terebelliformia
Terebellides stroemii Sars,        AY577893     DQ209241     DQ209261
  1835 Terebelliformia
Prionospio Spionidae               DQ209226     DQ209246     DQ209266
Manayunkia athallasia Hutchings    N/A          DQ209245     DQ209265
  et al., 1981 Sabellidae
Spirorbis spirorbis (Linnaeus,     AY577887     DQ209244     DQ209264
  1758) Serpulidae
Gunnarea capensis Johansson,       AY577892     DQ209243     DQ209263
  1927 Sabellariidae

Ingroup Chaetopteridae
Spiochaetopterus bergensis         DQ209214     DQ209229     N/A
  (Gitay, 1969)
Phyllochaetopterus sp. 3           DQ209215     DQ209230     DQ209249
Phyllochaetopterus sp. 1           DQ209213     DQ209228     DQ209248
Phyllochaetopterus sp. 2           DQ209216     DQ209231     DQ209250
Phyllochaetopterus socialis        DQ209212     DQ209227     DQ209247
  Claparede, 1868
Mesochaetopterus taylori Monro,    DQ209217     DQ209232     DQ209251
Mesochaetopterus japonicus         DQ209218     N/A          N/A
  Fujiwara, 1934
Chaetopterus sarsii Boeck, 1861    DQ209221     DQ209235     DQ209254
Chaetopterus sp. 1                 DQ209219     DQ209233     DQ209252
Chaetopterus sp. 2                 DQ209222     DQ209236     DQ209255
Chaetopterus cf. luteus Stimpson,  DQ209220     DQ209234     DQ209253
C. pugaporcinus (2 specimens)      DQ209224,    DQ209238,    DQ209257,
                                   DQ209223     DQ209237     DQ209256

                                   Museum Acc.
Taxon                              # (voucher)  Collection Locality

Dodecaceria concharum              SAM E3355    Iceland
  Oersted, 1843 Cirratulidae
Paralvinella grasslei              SAM E3388    Pacific
  Desbruyeres & Laubier,
  1982 Alvinellidae
Glyphanostomum sp. Ampharetidae    SAM E3517    Monterey Bay, CA
Pectinaria granulata (Linnaeus,    SAM E3358    Iceland
  1767) Terebelliformia
Terebellides stroemii Sars,        SAM E3359    Iceland
  1835 Terebelliformia
Prionospio Spionidae               SAM E3516    Monterey Bay, CA
Manayunkia athallasia Hutchings    SAM E3518    South Australia
  et al., 1981 Sabellidae
Spirorbis spirorbis (Linnaeus,     SAM E3357    Iceland
  1758) Serpulidae
Gunnarea capensis Johansson,       SAM E3360    South Africa
  1927 Sabellariidae

Ingroup Chaetopteridae
Spiochaetopterus bergensis         SAM E3558    Spitsbergen, Norway
  (Gitay, 1969)
Phyllochaetopterus sp. 3           SAM E3512    Sydney, Australia
Phyllochaetopterus sp. 1           SAM E3514    Monterey Bay, CA
Phyllochaetopterus sp. 2           SAM E3513    Sydney, Australia
Phyllochaetopterus socialis        N/A          Roscoff, France
  Claparede, 1868
Mesochaetopterus taylori Monro,    SAM E3570    Friday Harbor, WA
Mesochaetopterus japonicus         SAM E3571    Kyushu, Japan
  Fujiwara, 1934
Chaetopterus sarsii Boeck, 1861    SAM E3557    Trondheimsfjord, Norway
Chaetopterus sp. 1                 SAM E3511    Santa Barbara, CA
Chaetopterus sp. 2                 N/A          Banyuls, France
Chaetopterus cf. luteus Stimpson,  SAM E3510    South Australia
C. pugaporcinus (2 specimens)      LACM POLY    Monterey Bay, CA
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Author:Osborn, Karen J.; Rouse, Greg W.; Goffredi, Shana K.; Robison, Bruce H.
Publication:The Biological Bulletin
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Geographic Code:1U9CA
Date:Feb 1, 2007
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