Synallactes virgulasolida, Massin & Hendrickx, 2010

Luna-Cruz, Ana K. & Hendrickx, Michel E., 2018, New records of Synallactes virgulasolida Massin & Hendrickx, 2010 (Echinodermata: Holothuroidea) from the eastern Pacific, Zootaxa 4444 (4), pp. 491-500: 492-498

publication ID

https://doi.org/10.11646/zootaxa.4444.4.9

publication LSID

lsid:zoobank.org:pub:2BB0031E-B4F0-47C6-8D45-3E4FB37D6744

persistent identifier

http://treatment.plazi.org/id/0380186C-CB57-FFEC-F0A8-2D73BF3CD19E

treatment provided by

Plazi

scientific name

Synallactes virgulasolida
status

 

SynallactES virgulaSOlida Massin & Hendrickx, 2010 

( Figs. 2 View Figure , 3 View Figure )

Synallactes virgulasolida Massin & Hendrickx, 2010: 600  , figs. 1‒3.

Material examined. TALUD III, St. 14-A (24°38'48"N, 108°26'54"W), Aug 19, 1991, 69 specimens (TL 123‒234 mm), AD, 1016‒1020 m depth (ICML-EMU-12094).

TALUD XVI-B. St. 5 (28°48'N, 115°24'06"W), May 24, 2014, 37 specimens, (TL 39‒112 mm), BS, 772‒776 m depth (ICML-EMU-12095). St. 6, 29°08'09"N, 115°33'26"W, May 24, 2014, 59 specimens, (TL 155‒285 mm), BS, 1004‒1102 m depth (ICML-EMU-12096). St. 7 (29°21'12"N, 115°39'08"W), May 31, 2014, 1 specimen, (TL 155 mm), BS, 710‒750 m depth (ICML-EMU-12097). St. 17 (29°54'18"N, 116°01'30"W), May 29, 2014, 12 specimens, (TL 28‒162 mm), BS, 734‒774 m depth (ICML-EMU-12098). St. 18, 30°39'18"N, 116°25'54"W, May 25, 2014, 1 specimen, (TL 187 mm), BS, 740‒785 m depth (ICML-EMU-12099). St. 26, 31°46'06"N; 116°58'21"W, May 26, 2014, 11 specimens, (TL 165‒290 mm), BS, 982‒989 m depth (ICML-EMU-12100).

Characteristics. The examined material fits well with the original description provided by Massin & Hendrickx (2010) in the following aspects: cylindrical body almost uniform in width throughout ( Figure 2A, I View Figure , II). Body length from 28 to 290 mm, body wall thickening in organisms larger than 100 mm. Mouth ventral and anus terminal. Up to 20 shield-shaped tentacles arranged in a unique circle, each with 6‒9 distal digitation ( Figure 2A View Figure , III). Four groups of long papillae towards anterior end and above crown of tentacles, arranged as follow: two superior groups, with a variable number of papillae (2‒4 in each group, more frequently 3), and 2 lateral groups, usually with 2 papillae each ( Figure 2A View Figure , III). Dorsally papillae thin, hook-shaped, with pointed end covering entire dorsal surface; in large organisms they follow an arrangement approximately of 6 rows along the body. Ventral ambulacral feet wide, rounded towards posterior end, covering entire ventral region, generally shorter and less prominent towards posterior end of body. Distal end of feet with supporting sucking disk. Anus surrounded by 5 groups of small and tapering papillae, frequently 3 per group ( Figure 2A View Figure , IV).

Two sacciform Polian vesicles toward right dorsal interradial. Up to three tin stone canals toward right dorsal radial, terminating in a semi-spherical madreporite with oval plate. Gonad in one tuft, with several tubules not branched toward left dorsal radial, extending below half the length of the animal. Bifid longitudinal muscles.

Calcareous ring of five radial and five interradials plates, lacking posterior processes ( Figure 2A, V View Figure ). Plates vary in robustness depending on their position in the calcareous ring, but are similar in shape between dorsal and ventral plates. Two radial and three interradial dorsal plates, taller and wider than their complementary ventral plates that are low and outstretched. Radial plates slightly wider in middle region than towards ends, at anterior and posterior margins with a center short slit pointing towards the center of the piece and this generates two short divisions in each of the margins. Interradial dorsal plates semi-square, at anterior parts gently curved and posterior margins with a marked slit pointing towards the center of the piece; in ventral region elongated and at posterior margins lightly concave.

Ossicles in body wall tables of two kinds: small tables (60‒120 µm across) formed by a base of four short and thin arms generally with or without perforated ends, arms sometimes connected through a circular margin, central pillar long (50‒230 µm high), smooth and widened at the base, ending in a crown-like projection formed by 3‒4 short branches joined together ( Figure 3A, I, 3B, I View Figure ). Very large tables (100‒950 µm across) formed by a base of long widening arms, perforated and branched towards the outer end, similar to a racket, 3‒5 arms and 4‒11 holes per arm, central pillar (up to 170 µm high), almost as long as each of the arms ( Figure 3A View Figure , II, 3B, II). Two forms of tables present in dorsal and ventral regions, less frequently in ambulacral feet. Huge, massive and smooth rods (90‒700 µm long), more slender and slightly curved rods (100‒750 µm long) and club shaped ossicles (100‒600 µm long) present in ventral and lateral ambulacral feet ( Figure 3C, I View Figure ). Perforated end plate of the ventral and lateral tube feet with holes and margin irregular (up to 450 µm across) ( Figure 3C View Figure , II). Dorsal and tentacular papillae with cross-shaped ossicles, similar to tables of the body wall, and huge and smooth rods (130‒1050 µm long) ( Figure 3A View Figure , III). Tentacles with long, smooth or spiny curved rods, with or without perforated ends (130‒880 µm long) ( Figure 2B View Figure ).

Color. In alcohol, body wall light brown or gray, tube feet and tentacles light yellow, beige or white.

Remarks. In all specimens of TALUD XVI-B were observed huge, massive and smooth rods and club shaped ossicles in the ventral and lateral ambulacral feet. According to Massin & Hendrickx (2010) this is a feature that separates to S. virgulasolida  from other species of Synallactes  . In the original description of the species, the authors have also mentioned “this is a good discriminant character which has not be observed in other Synallactes  ".

Variation was observed in cross-shaped ossicles protruding outside in the dorsal and tentacular papillae, mentioned by Massin & Hendrickx (2010), these were presented in smaller quantity with increasing size of the animals. These forms are arranged along the entire papilla above a mesh made of rod-shaped spicules. In addition, we observed a reduction in number of tables of the body wall and of dorsal papillae with animals growth. All types of spicules, of different sizes, were present in almost all specimens of different sizes. Consequently, there seems to be no relationship between size of the ossicles and size of the animals ( Table 2). In one case, however, very large spicules were present in three organisms of an intermediate size ( TALUD XVI-B, St. 5, body length 52, 55 and 62 mm); these corresponded to body wall tables of four arms, for which some ossicles had an approximate width of 950 µm. Although these forms clearly stood out in their dimensions, we are sure that the specimens belong to S. virgulasolida  due to their external characteristics and the presence of massive, smooth rods and club-shaped ossicles in the ventral and lateral ambulacral feet just like mentions in the original description. Changes in the ossicles during holothurians growth have been reported in very few species, mostly from shallow waters (Solís- Marín, 2003). These changes include modification in the forms and amount of the spicules ( Mitsukuri, 1897; Thandar, 1987; Massin, 1994; Cutress, 1996).

On the other hand, the calcareous ring did not present a transformation that could be related to the growth of the animal. In at least five specimens of different sizes ( TALUD XVI-B, St. 6, body length 270, 245, 175, 165 and 68 mm) in which this structure was observed, there was no reduction or reabsorption of its pieces. Therefore, it is likely that the ring does not disappear in the final growing stages. Differences in the forms of the dorsal and ventral ring pieces were observed. Variation in shape between the pieces of the calcareous ring has been noted in some Synallactidae  species ( Solís-Marín, 2003, 2009).

Compared with the original description, the specimens that were examined herein exhibited almost exactly the characteristics observed by Massin & Hendrickx (2010) in the original material (three specimens of 50, 60 and 85 mm), although the new material is of larger size (i.e., 165‒290 mm). The line of ambulacral feet between the bivium and the trivium was not constantly observed in the examined material. However, we believe that this variation does not depend on the age of the organisms, but is rather related to ease with which the ambulacral feet contract. Accordingly, it is a characteristic that can be affected by the process of fixation, as reported for the arrangement of the crown tentacles.

Contrary to what the authors mentioned in the original description, i.e., that specimens of larger sizes may have lost their calcareous ring, we have observed this structure in specimens with body length between 163 and 270 mm. The shape of the radial and interradial pieces was conserved and there was no changes due to a reduction processes. In the same way, the reduction in numbers of spicules with advancing the age (or increasing the size) was limited to body wall tables and tentacular papillae tables.

In the specimens of TALUD III, ossicles could not be observed due to the preservation process (concentrated formaldehyde). These specimens were identified based on the external characteristics in the original description, including: arrangement of the papillae on entire dorsal surface, distribution of ventral ambulacral feet, very long papillae over the crown of tentacles, form and arrangement of tentacles, presence of small and tapering anal papillae, and shape of the calcareous ring.

Ecology. Environmental data available in the original description of S. virgulasolida  included (one sample only): 1300 m depth, 5 °C, 0.20 ml O2/l, and sediments made of fine black mud ( Massin & Hendrickx, 2010). The specimens reported herein were collected in a much wider bathymetric range (710‒1102 m), in 4.17‒5.81 °C, 0.15‒0.48 ml O2/l, and in 34.40‒34.48 ups. The species occurs in a wide variety of sediments made of 3.65‒12.08 % clays, 40.93‒84.46 % silt, and 5.34‒55.43 % sands, with an organic carbon content of 17.93‒52.02 mg /g (1.79‒5.20 % of organic matter) ( Table 1). Mexican records correspond to a bathymetric fringe located below the Oxygen Minimum Zone (OMZ) where a diverse community composed of mollusks, crustaceans, and other groups of echinoderms is known to occur (see Hendrickx et al., 2011, 2016; Hendrickx & Serrano, 2010; Papiol et al., 2016). Dissolved oxygen values measured close to the seafloor indicate that S. virgulasolida  is able to tolerate mild (<0.5 ml O2/l) to severe (<0.2 ml O2/l) hypoxic conditions. The bathymetric range where it occurs is also favorable to species well adapted to oxygen deficiency due to reduced competition for food which, in the case of many sea cucumbers, consists mostly of organic particles (deposit or suspension feeding) ( Graham & Thompson, 2009). OMZ areas are known to be rich in organic deposits ( Papiol et al., 2016).

Density of organisms. Density estimated for S. virgulasolida  in the seven sampling stations varied considerably, from a minimum of 2.63 orgs/ha (TALUDXVI-B, St. 18) to a maximum of 170.32 orgs/ha ( TALUD III, St. 14-A). The highest density values were found in the 1004‒1020 m depth range, while the lowest values corresponded to a depth range of 710‒785 m ( Table 1).

Unpublished records. The Benthic Invertebrates Collection at Scripps Institute of Oceanography ( SIOAbout SIO) contains four lots of S. virgulasolida  , three from off Southern California, USA, and one from off Chile. St. M 6-T2, La Jolla Canyon (32°52'N, 117°32' W)GoogleMaps  , August 13, 1971, 1 unmeasured specimen, Otter trawl, 732‒860 m (SIO- E2751) (Coll. T. Matsui; Id. D. Pawson ). St. M15-OT22, off Del Mar (32°59'N, 117°38'W)GoogleMaps  , April 4, 1974, 1 unmeasured specimen, Otter trawl, 920 m (SIO-E2746) (Coll. T. Matsui; Id. D. Pawson ). St. M1-2, San Diego Through (32°57'N, 117°32'W)GoogleMaps  , February 3, 1971, 1 unmeasured specimen, Otter trawl, 768 m (SIO-E2768) (Coll. T. Matsui; Id. D. Pawson ). St. MV 72-II-27, off Arica , Chile (18°40'30"S, 70°36'W)GoogleMaps  , May 7, 1972, 3 unmeasured specimens, R/V T. Washington, Otter trawl, 768‒968 m (Coll. S. Luke; Id. D. Pawson ). 

Distribution. Previous to this study, S. virgulasolida  was known only from the type locality, off SE Baja California (25°24'26"N, 110°37'36"W), in the Gulf of California ( Figure 1 View Figure ) ( Massin & Hendrickx, 2010). The material examined herein includes an additional record within the Gulf of California, off the east coast of the peninsula, and a large series of records off the west coast of the Baja California Peninsula where it had not been reported previously. The data obtained from the Benthic Invertebrates Collection at SIOAbout SIO further increase the distribution range of this species, from southern California (32°59'N) to off Chile (18°40'30"S), equivalent to a range of almost 52° of latitude. Including the data available in the SIOAbout SIO collection, the general bathymetric range of S. virgulasolida  is set at 710‒1300, with a large majority of records between ca 710 and 1102 m depth.

SIO

Scripps Institution of Oceanography

Kingdom

Animalia

Phylum

Echinodermata

Class

Holothuroidea

Order

Aspidochirotida

Family

Synallactidae

Genus

Synallactes

Loc

Synallactes virgulasolida

Luna-Cruz, Ana K. & Hendrickx, Michel E. 2018

2018
Loc

Synallactes virgulasolida

: 600