Crispatotrochus cornu (Moseley, 1881)
publication ID |
https://dx.doi.org/10.3897/zookeys.1066.69697 |
publication LSID |
lsid:zoobank.org:pub:133CE040-A5AF-44F1-BC9A-558C2F06A8AA |
persistent identifier |
https://treatment.plazi.org/id/992D51AB-7CFE-2521-E6A2-650D84D920E6 |
treatment provided by |
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scientific name |
Crispatotrochus cornu (Moseley, 1881) |
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Crispatotrochus cornu (Moseley, 1881)
Fig. 3E, F View Figure 3
Cyathoceras cornu Moseley, 1881: 156-157, pl. 4, fig. 7 (in part). - Cairns 1979: 67, pl. 12, figs 1, 3.
Crispatotrochus cornu . - Cairns 1991: 15. - Kitahara and Cairns 2008: 63. - Cairns and Polonio 2013: 70-71, figs 2L-M, 3A-B, 10.
Type locality.
Off Rio de la Plata, Uruguay (HMS ‘Challenger’ stn. 320: 37°17'00"S, 53°52'00"W); 1097 m ( Moseley 1881).
Type material.
Lectotype and paralectotype are deposited at the NMNH ( Cairns 1979).
Material examined.
None.
Imagery data.
UCTES_NAD 17 F (1 specimen): Eastern margin, off Isipingo; 49 m.
Description.
Corallum ceratoid, attached through a robust pedicel (PD:GCD = 0.4) that expands into an encrusting base. Calice elliptical (GCD:LCD = 1.2) with a serrated calicular margin. Only imaged specimen examined (NAD 17 1F) 5.9 × 5.0 mm in CD, 2.2 mm in PD, and 7.0 mm in H. Theca granulated. Costae prominent at calicular margin, with C1--2 more prominent and distinctive. No intercostal striae. Corallum white.
Septa hexamerally arranged in four complete cycles according to the formula: S1-2 > S3 > S4 (48 septa). S1-2 equal in size and exsertness, with slightly sinuous axial margins, and almost meet columella. Remaining septa (S3-4) becoming progressively less exsert. S3 ~ ¾ the width of S1-2, and have the most sinuous axial margins. S4 rudimentary, also with straight to slightly sinuous axial margins. Septal faces bear small and blunt granules. Fossa moderately deep, with a rudimentary fascicular columella composed of two twisted elements.
Distribution.
Regional: Eastern margin of South Africa, off Isipingo; 49 m. Elsewhere: Seamount or ridge on Heezen fracture zone, South Pacific; 549 m ( Cairns 1982).
Remarks.
The imaged specimen, that forms the basis of this species report, is consistent with the known description of Crispatotrochus cornu in having a robust pedicel and septa hexamerally arranged in four complete cycles (S1-2 > S3 > S4), but differs in having an exceptionally sinuous as opposed to a straight S3 as previously reported ( Cairns 1979, Kitahara and Cairns 2008). This species groups with the other Crispatotrochus that have septa hexamerally arranged in four cycles ( C. inornatus , C. galapagensis Cairns, 1991, C. rugosus Cairns, 1995, and C. irregularis Cairns, 1982), all previously reported from the Pacific Ocean. Crispatotrochus cornu appears to be a juvenile form and is similar to the specimens collected by RV Gerda and RV Pillsbury stations which display a pedicel measuring ½ of the calicular diameter ( Cairns 1979). However, Cairns (1979) highlights that these specimens were omitted from the description/account on the bases of immaturity and their small size. Species may have septa arranged in a decameral or hexameral fashion ( Cairns 1979, 1991), the latter being the pattern observed in the imaged specimen reported herein (UCTES_NAD17F). Nonetheless, the South African record (UCTES_NAD17F) was collected at a much shallower depth than the previously known. Despite this, specimen is added to the account and represents a new record for the Crispatotrochus in the southwest Indian Ocean.
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