Laminatubus alvini ten Hove & Zibrowius, 1986
publication ID |
https://doi.org/ 10.11646/zootaxa.4915.1.1 |
publication LSID |
lsid:zoobank.org:pub:CF63FF06-0FDF-49FF-8914-2BD5C1EA80CF |
DOI |
https://doi.org/10.5281/zenodo.4457969 |
persistent identifier |
https://treatment.plazi.org/id/193D87F9-4307-2124-FF31-FB8AF6C33547 |
treatment provided by |
Plazi |
scientific name |
Laminatubus alvini ten Hove & Zibrowius, 1986 |
status |
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Laminatubus alvini ten Hove & Zibrowius, 1986 View in CoL
Figures 6–8 View FIGURE 6 View FIGURE 7 View FIGURE 8
Laminatubus alvini ten Hove & Zibrowius, 1986 View in CoL (description, line drawings, photo of tube, SEM of tube ultrastructure).
Laminatubus alvini View in CoL .— Tunnicliffe (1992) (distribution Galapagos; East Pacific Rise: 13°N to 21°N); Desbruyères & Segonzac (1997) (diagnosis, figures, distribution Galapagos; East Pacific Rise: 21°N to 23°S); Mullineaux & Manahan (1998) (photo of colony in situ); Mullineaux et al. (1998) (recruitment at 9°50′N vent localities); Tunnicliffe et al. (1998) (biogeography: Guaymas vents 27°N, EPR at 21°N, Galapagos); Michelli et al. (2002) (9°50′N vent localities, ecology); Mullineaux et al. 2003 (9°50′N vent localities, succession); Desbruyères et al. (2006) (diagnosis, figures, distribution Galapagos; East Pacific Rise: 21°N to 23°S); Hey et al. (2006) (name and photo, 31°S and 32°S vent localities); Kupriyanova et al. (2006) (phylogeny, morphology and DNA; specimen from 31°S); Vinn et al. (2008) (tube ultrastructure and mineral composition; specimen from 9°N); ten Hove & Kupriyanova (2009) (diagnosis, SEM of chaetae from Galapagos Rift specimen); Mullineaux et al. (2009) (9°50′N vent localities, ecology; Goffredi et al. (2017) (DNA; two specimens from 23°N vent).
Material examined. AM: W.38421, 12°50’N, 103°57’W, Jeanie Site, 2010 Mescal cruise; W.49888, W.49956– 499562; W.49961 and W.38421 prepared for GoogleMaps SEM; SAM: E5851 View Materials – E5879 View Materials ; SIO-BIC: A8568–8579 (see Table 1 View TABLE 1 for localities and measurement) . FMNH: 7045; SAM: 1717, E3531; SIO-BIC: A1654, A1658, A1660, A1662, A1668, A1670, A6158, A6327 (see Tables 1 View TABLE 1 and 2 for localities and GenBank accession numbers).
Description. TUBE: white opaque, semi-circular to circular in cross-section, without wide flaring peristomes, growth rings indistinct, attached to the substrate throughout its length. High, sharp, undulating longitudinal keel and distinct solid flattened attachment flange lacking alveoli present ( Fig. 6A, B View FIGURE 6 , 7A View FIGURE 7 ). External hyaline layer present.
RADIOLAR CROWN: Radioles not connected by inter-radiolar membrane ( Fig. 7C, D, E View FIGURE 7 ), arranged into slightly ascending spiral of up to two whorls. Stylodes and radiolar eyes absent.
PEDUNCLE: smooth cylindrical (circular in cross-section), at least twice as thick as normal radioles ( Fig. 7 View FIGURE 7 C–E), gradually merging into opercular ampulla, constriction absent ( Fig. 7B, C View FIGURE 7 ). Small distal latero-dorsal “winglets” (flattened distal parts of the peduncle) or pair of lateral wings proximal to opercular ampulla absent. Peduncle inserted on left side of radiolar crown, below line of radioles ( Fig. 7C, D, E View FIGURE 7 ).
OPERCULUM: bulbous to inverted conical proximal semi-transparent ampulla with distinct distal flattened to convex or pointed yellowish-brownish endplate covered with thickened cuticle ( Fig. 7 View FIGURE 7 A–C).
COLLAR AND THORACIC MEMBRANES: collar high, covering bases of radiolar lobes, clearly trilobed, with longer and wider ventral lobe and smaller lateral ones ( Fig. 8A View FIGURE 8 ) and entire edge ( Fig. 7D, E View FIGURE 7 , 8A View FIGURE 8 ), continuous with thoracic membranes as wide as thoracic tori, forming apron across anterior abdominal chaetigers ( Figs 7E View FIGURE 7 , 8A View FIGURE 8 ). Pairs of small, wart-like protuberances of collar chaetiger or elongated tonguelets between ventral and lateral collar parts absent.
THORAX: with collar chaetiger and five uncinigerous chaetigers ( Fig. 7E View FIGURE 7 ), fascicle of collar chaetae separated from first uncinigerous chaetiger by a wide gap ( Fig. 8A View FIGURE 8 ). Thoracic tori of approximately same length, gradually converging posteriorly, forming distinct triangular depression ( Fig. 8A, C View FIGURE 8 ), but not touching each other medio-ventrally ( Fig. 8C View FIGURE 8 ). Collar chaetae fascicle with limbate and poorly developed Spirobranchus - type chaetae or special chaetae absent altogether ( Fig. 8B View FIGURE 8 ). Subsequent thoracic chaetae simple limbate, of two sizes, Apomatus chaetae absent ( Fig. 8D View FIGURE 8 ). Uncini along entire thorax saw-shaped with 5–6 teeth, anterior fang simple pointed ( Fig. 8F View FIGURE 8 ). Pair of prostomial eyes absent.
ABDOMEN: with up to 120 abdominal chaetigers. Achaetous anterior abdominal zone absent, distinct chaetae with long shaft (length similar to that of thoracic tori) starting from first abdominal segment. Tips of chaetae slightly bent and hollow, made of two rows of pointed teeth, thus true trumpet-shaped chaetae ( Fig. 8E View FIGURE 8 ). Posterior capillary chaetae absent. Uncini saw-shaped anteriorly, with pointed fangs and 5–7 teeth, similar to thoracic ones; posterior-most uncini rasp-shaped with 3–4 rows of teeth, bluntly pointed fang and 7–8 teeth in profile view ( Fig. 8G View FIGURE 8 ). Posterior glandular pad absent ( Fig. 7C View FIGURE 7 ).
SIZE: length up to 29 mm (5.2–29 mm, Table 1 View TABLE 1 ). Radioles and operculum accounting for 2/5 of entire animal length.
COLOUR: white radiolar crown, white to yellowish body ( Fig. 7 View FIGURE 7 B–E)
Distribution. Hydrothermal vents fields of East Pacific Rise, from 23°N to 38°S.
Reproduction. Two specimens from Alvin Dive 4091 released eggs 150 µm in diameter.
Remarks. Ten Hove and Zibrowius (1986) reported the distribution of L. alvini as “four areas with hydrothermal activity on the Galapagos Ridge and on the East Pacific Rise (approx. 1°N, 10°N, 13°N and 21°N), at depths of about 2500–2600 m ”, with the type locality being the Galapagos vents. Desbruyères & Segonzac (1997) and Desbruyères et al. (2006) reported distribution on the Galapagos vents and the East Pacific Rise from 21°N to 23°S. In their review Tunnicliffe et al. (1998) extended the distribution with their reporting of L. alvini from the sedimented Guaymas Basin vents at 27° N and Hey et al. (2006) reported the species further south on the East Pacific Rise from 31°– 32°S vent localities. We did not sequence L. alvini from the type locality, but did demonstrate that a single Laminatubus species, with very little genetic variability extends along the East Pacific Rise from 38°S to 23°N. We lacked specimens from the sedimented Guaymas Basin vents at 27°N, but samples from the nearby seeps in the Guaymas Basin turned out to be one of the new species described below.
Catalogue number | Length, mm | Alvin Dive | Coordinates | Depth, meters |
---|---|---|---|---|
AM W.49888 | P7, Th2, A4 | A4091 | 37°40.351S,110°52.617W | 2236 |
AM W.49956 | P5.5, Th1.5, A3 | A4091 | 37°40.351S, 110°52.617W | 2236 |
AM W.49957 | P11, Th3.5, A- | A4091 | 37°40.351S, 110°52.617W | 2236 |
AM W.49958 | P12, Th2, A- | A4094 | 31°0939S, 111°55.919W | 2237 |
AM W.49959 | P11, Th3.5, A9.5 | A4094 | 31°0939S, 111°55.919W | 2237 |
AM W.49960 | P11, Th2.5, A- | A4096 | 23°32.780S, 115°34.179W | 2595 |
AM W.49961 | P11, TH3.5, A8.5 | A4096 | 23°32.780S, 115°34.179W | 2595 |
AM W.49962 | P11, Th2.5, A9 | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5851 | P8, Th2.5, A- | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5852 | P8, Th3, A6 | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5853 | P11, Th2, A- | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5854 | P7, Th2, A3 | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5855 | P6.5, Th1.5, A3 | A4091 | 37°40.351S, 110°52.617W | 2236 |
SAM E5856 | P-, Th2, A6.5 | A4091 | 37°40.351S, 110°52.617W | 2236 |
SAM E5857 | P3, Th1, A2 | A4091 | 37°40.351S, 110°52.617W | 2236 |
SAM E5858 | P3, Th0.7, A1.5 | A4091 | 37°40.351S, 110°52.617W | 2236 |
SAM E5859 | P3, Th1.5, A- | A4091 | 37°40.351S, 110°52.617W | 2236 |
SAM E5860 | P6, Th1, A- | A4091 | 37°40.351S, 110°52.617W | 2236 |
SAM E5861 | P3, Th0.6, A- | A4091 | 37°40.351S, 110°52.617W | 2236 |
SAM E5862 | P6, Th-, A- | A4091 | 37°40.351S, 110°52.617W | 2236 |
SAM E5863 | P4, Th1, A2.5 | A4091 | 37°40.351S, 110°52.617W | 2236 |
SAM E5864 | P6, Th1, A4 | A4094 | 31°0939S, 111°55.919W | 2237 |
SAM E5865 | P6, Th2, A- | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5866 | P4, Th1.5, A2.5 | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5867 | P9 | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5868 | P -, Th1.5, A2.5 | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5869 | P4.5, Th1, A3 | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5870 | P11, Th3, A- | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5871 | R6, Th3, A- | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5872 | P6, Th1.5, A3 | A4091 | 37°40.351S, 110°52.617W | 2236 |
SAM E5873 | P9, Th4, A- | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5874 | P9, Th2, A7 | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5875 | P6.5, Th1.5, A4.5 | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5876 | P6, Th1, A3 | A4096 | 23°32.780S, 115°34.179W | 2595 |
SAM E5877 | P6.5, Th1, A3 | A4096 | 23°32.780S, 115°34.179W | 2595 |
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Laminatubus alvini ten Hove & Zibrowius, 1986
Rouse, Greg W. & Kupriyanova, Elena K. 2021 |
Laminatubus alvini
ten Hove & Zibrowius 1986 |
Laminatubus alvini
ten Hove & Zibrowius 1986 |