Review Article |
Corresponding author: Céline Labrune ( celine.labrune@obs-banyuls.fr ) Academic editor: Christopher Glasby
© 2019 Céline Labrune, Nicolas Lavesque, Paulo Bonifácio, Pat Hutchings.
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
Labrune C, Lavesque N, Bonifácio P, Hutchings P (2019) A new species of Pista Malmgren, 1866 (Polychaeta, Terebellidae) from the north-western Mediterranean Sea. ZooKeys 838: 71-83. https://doi.org/10.3897/zookeys.838.28634
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A new species of Terebellidae, Pista colini sp. n., has been identified from the harbour of Banyuls-sur-Mer, north-western Mediterranean Sea. This new species was found in very high densities, exclusively in gravelly sand deposited manually, and was not found in the original source habitat of the gravel. This species is characterized by the colour of the ventral shields with pinkish anterior part and a blood red posterior part in live specimens, a pair of unequal-sized plumose branchiae inserted on segment II and anterior thoracic neuropodia with long-handled uncini. The presence of long-handled uncini even in the smallest specimens constitutes the major difference between Pista colini sp. n. and other Pista species with a single pair of branchiae such as P. lornensis and P. bansei.
Annelida, gravel deposits, harbour, Pista colini sp. n., taxonomy, Terebellida
Terebellids belong to a very species-rich group of sedentary polychaetes, widely distributed in most marine benthic substrates, from shallow waters to deep-sea environments (
Currently, morphological-based studies on Pista-like genera (
The present study provides the description of a new species of Pista from the north-western Mediterranean Sea, based on morphological characters. Molecular data (COI gene) are provided for further investigations.
The first specimens of the new Pista species were sampled in 2012 in the harbour of Banyuls-sur-Mer (French Mediterranean Sea; WGS84: 42°28.87'N, 3°08.15'E; 3 m depth; Fig.
Holotype and most paratypes were deposited at the Museum national d’Histoire naturelle, Paris (MNHN), other paratypes were deposited in the Australian Museum, Sydney (AM). Non-type additional material was lodged in collections of Banyuls-sur-Mer and Arcachon Marine Stations in France.
Samples for DNA analysis were removed from a live specimen (paratype MNHN-IA-TYPE 1853) placed in ethanol 96% and frozen at -20 °C. Extraction of DNA was done with QIAamp DNA Micro Kit (QIAGEN) following protocol supplied by the manufacturers. Approximately 650 bp of COI (cytochrome c oxidase subunit I) genes were amplified using primers polyLCO and polyHCO (Carr et al. 2011). The PCR (Polymerase Chain Reaction) was carried out with Gotaq G2 Flexi DNA Polymerase (PROMEGA), with 50 µL mixtures contained: 10µL of 5X Colorless GoTaq Reaction Buffer (final concentration of 1X), 1.5 µL of MgCl2 solution (final concentration of 1.5mM), 1 µL of PCR nucleotide mix (final concentration of 0.2 mM each dNTP), 0.5 μl of each primer (final concentration of 1µM), 0.2 µl of GoTaq G2 Flexi DNA Polymerase (5U/µl), 1 μl template DNA and 33.8 µL of nuclease-free water. The temperature profile was as follows: 94 °C/600s – (94 °C/40s-44 °C/40s-72 °C/60s) *5 cycles -(94 °C/40s-51 °C/40s-72 °C/60s) *35 cycles -72 °C/300s -4 °C. Amplified PCR products were analysed by electrophoresis in a 1 % p/v agarose gel stained with ethidium bromide and were sent to GATC Biotech Company to complete double strain sequencing, using same set of primers as used for PCR. Overlapping sequence (forward and reverse) fragments were merged into consensus sequences and aligned using Clustal Omega. Sequences were translated into amino acid alignment and checked for stop codons to avoid pseudogenes. The minimum length coverage was around 660 bp. Sequence obtained in this study has been deposited in GenBank (http://www.ncbi.nlm.nih.gov/genbank/). The accession number is given in the section Genetic data.
Amphitrite cristata Müller, 1776, by original designation.
Transverse prostomium attached to dorsal surface of upper lip; basal part as thick crest, eye spots sometimes present; distal part shelf-like. Buccal tentacles all uniformly cylindrical. Peristomium restricted to lips; relatively short upper lip, hood-like; swollen, cushion-like and mid-ventral lower lip. Segment I reduced dorsally, with pair of lobes of variable size and position; segments II–IV also with pairs of lobes of variable size and position, sometimes extending for a few more segments. Anterior segments highly glandular ventrally, with discrete, smooth to slightly corrugated, rectangular to trapezoidal mid-ventral shields. Paired arborescent, pectinate or plumose branchiae present from segment II, typically two pairs, on segments II and III, rarely a single pair or three pairs. Conical to rectangular notopodia beginning on segment IV, all aligned, typically extending for 17 segments, until segment XX; notochaetae all distally winged, frequently broadly winged. Neuropodia beginning on segment V, as low ridges in conjunction with notopodia and short pinnules posteriorly; neurochaetae as long-handled avicular uncini, at least on anterior neuropodia, frequently until segment X or termination of notopodia, then short-handled; uncini in partial to completely intercalated double rows on segments XI–XX. Nephridial papillae present on segment III, genital papillae on variable number of segments, usually on segments VI–VII, posterior and dorsal to notopodia. Pygidium smooth to slightly crenulated (after
Type material. Banyuls-sur-Mer harbour, Gulf of Lion, Mediterranean Sea, France (42°28.867'N, 3°08.154'E, 3 m depth), subtidal in gravely sands, all collected 16 July 2012 except MNHN-IA-TYPE 1853 collected 12 July 2017. Holotype: MNHN-IA-TYPE 1850, complete, 70 segments, total length 17.6 mm, thoracic length 4.8 mm, anterior width 0.6 mm, Paratypes: AM W.50625, 1 specimen, posteriorly incomplete, total length 11 mm, thoracic length 7 mm, anterior width 1.0 mm; AM W.50626, 3 specimens plus 1 posterior fragment 5 mm with pygidium, 1 complete, total length 11 mm, thoracic length 5 mm, anterior width 0.5 mm, 1 complete, total length 12 mm, thoracic length 5 mm, anterior width 0.5 mm, 1 posteriorly incomplete, length 16 mm, thoracic length 8 mm, anterior width 0.8 mm, 2 specimens mounted for SEM. MNHN-IA-TYPE 1851, 1 specimen, posteriorly incomplete, total length 14.3 mm, thoracic length 3.7 mm, anterior width 0.7 mm; MNHN-IA-TYPE 1852, complete specimen, total length 9.70 mm, thoracic length 4.6 mm, anterior width 0.9 mm; MNHN-IA-TYPE 1853, complete collected 12 July 2017, thoracic length 4.4 mm, anterior width 1.1 mm, posterior part cut for molecular analysis; MNHN-IA-TYPE 1854, complete length 18.2 mm, anterior width 0.7 mm, mounted for SEM; MNHN-IA-TYPE 1855, complete, 1 specimen, total length 9.0 mm, thoracic length 3.1 mm, anterior width 0.7 mm.
Additional material. Banyuls-sur-Mer harbour, Gulf of Lion, Mediterranean Sea, France (42°28.867'N, 3°08.154'E, 3 m depth), subtidal in gravely sands, all collected 16 July 2012. BAN.Pista.08, 1 specimen, complete, total length 10.0 mm, thoracic length 3.7 mm, anterior width 0.8 mm; BAN.Pista.09, 1 specimen gravid, posteriorly incomplete, thoracic length 5.1 mm, anterior width 0.7 mm; BAN.Pista.10, complete, 1 specimen, total length 22.7 mm, thoracic length 7.8 mm, anterior width 0.9 mm; BAN.Pista.12, complete, 1 specimen, total length 12.4 mm, thoracic length 4.6 mm, anterior width 0.6 mm.
Comparative material.
Pista bansei Saphronova, 1988 Holotype reg. # 47667, 47°41'N, 139°34.1'E, Sea of Japan, Tartary Strait, off Nelma, 105 m; 4 paratypes reg. # 47668 according to
Additional material from R/V “Vityaz” stations 59, 119, 1587a, 3350, 3569, 1086. (For locality details see
(based on holotype). Holotype is a complete specimen, 17.5 mm in length, 0.6 mm in width at segment X and with 70 segments (Fig.
Transverse prostomium attached to dorsal surface of upper lip. Buccal tentacles all of similar width inserted ventrally on prostomium, shorter than smallest branchia; long tentacles situated centrally in dorsal region, longer than largest branchia (Fig.
Pista colini sp. n., SEM images: A Anterior part, dorso-lateral view B Anterior part, lateral view C Anterior part, ventral view D Branchial filaments A from paratype MNHN-IA-TYPE 1854 B–D from paratype AM W.50626. Key: LL: lateral lobes, bs: branchial stalks, ll: lower lip, SI, SII, and SIII: Segments I, II, and III.
Notochaetae, broad-winged capillaries, with fine tips (Fig.
Pista colini sp. n.: A Thoracic notochaeta of segment VI B Thoracic uncini of segment V C Abdominal uncini D Thoracic uncini in single row E Thoracic uncini in double row F Abdominal uncini A from paratype MNHN-IA-TYPE 1853 B, C from additional material BAN.Pista.12 D from paratype AM W.50626 (SEM image) E, F from paratype MNHN-IA-TYPE 1854 (SEM images). Key: Lh: long-handled uncinus, bh: broken-handled uncinus.
Pygidium with slightly crenulated margins (hardly visible even under stereomicroscope but clearly visible under SEM).
Branchiae, lips and base of tentacles not stained. Extremity of tentacles staining and retained as blue/brown even after being washed in ethanol for some days (Fig.
Complete individuals ranging from 9.0 to 22.7 mm in length, 0.5 to 1.1 mm in width at segment X and between 59 to 72 segments. Thoracic lengths vary between 3.1 and 7.8 mm. One gravid specimen was found (BAN.Pista.09). It was incomplete, but thoracic length was 5.1 mm and anterior width 0.7 mm. These measurements correspond to a small size species. Live specimens pinkish with translucent buccal tentacles; ventral shields divided in two parts, anterior part pinkish, posterior part blood red (Fig.
The name of species is dedicated to the nephew of the first author Colin Labrune who is already a little budding naturalist.
Only known from Banyuls-sur-Mer harbour, France (Mediterranean Sea).
Pista colini sp. n. was sampled at 3 m depth on gravelly sand recently deposited manually in Banyuls-sur-Mer harbour. It was found in very high densities (446 ind. m-2 in April 2012 and 1176 ind. m-2 in July 2012) a few weeks after the sediments had been deposited. We sampled again in November 2012 but there was no more gravel and Pista colini sp. n. was absent. The species is not found in the harbour if no gravel deposits are present. In the undisturbed part of the harbour, median granulometry was ca. 50 µm while the median granulometry of the gravelly sand in which this species is found was ca. 800 µm. In July 2017, we sampled a week after another fresh load of sediment with gravel had been deposited and we found high densities of Pista colini sp. n. living in tubes made from heterogeneous sediment agglomerated with mucus.
The COI gene was successfully sequenced and published at NCBI GenBank for paratype MNHN-IA-TYPE 1853 with accession number MK584933.
The presence of a single pair of branchiae is a stable character in Pista colini sp. n. More than 100 specimens were observed, of different sizes and all of them had a single pair of branchiae, some were also observed alive. Our observations support
Although
According to
All the specimens of P. colini sp. n. examined here, even the smallest (59 chaetigers, thoracic width at segment X: 0.5 mm), which are comparable in size with the individuals that
Based on examination of the type material of
We thank the captains and crew of RV “Nereis II” for technical assistance during sampling. The authors are grateful to Lyvia Lescure for sorting the macrofauna, Jean-Michel Amouroux for help in identification, and Guillemine Daffe (OASU, EPOC) for molecular analysis. Many thanks to the Laboratoire de Biologie Intégrative des Organismes Marins (BIOM, UMR 7232) who let CL use their wonderful Zeiss stereomicroscope equipped with camera. The authors also sincerely thank Elena Kupriyanova and Mayya Gogina for the translation of the Russian literature of Saphronova. Elena was very helpful in interpreting the data and resolving the discrepancies between the published paper and the material examined by us in Russia. We should also like to thank Sue Lindsay at Macquarie University, Sydney for taking the SEM images for us. We would like to thank the reviewers for their detailed comments and insightful suggestions which led to a significant improvement of the paper.