Lithoglyptes, Aurivillius, 1892
publication ID |
https://doi.org/ 10.11646/zootaxa.1013.1.3 |
publication LSID |
lsid:zoobank.org:pub:09072535-2701-4A27-AA94-0159EBE871E9 |
DOI |
https://doi.org/10.5281/zenodo.5049266 |
persistent identifier |
https://treatment.plazi.org/id/03C987BB-FFA8-FFD2-FE8E-912697689C45 |
treatment provided by |
Felipe |
scientific name |
Lithoglyptes |
status |
s.s. |
Lithoglyptes View in CoL View at ENA s.s. Aurivillius, 1892
( Figs. 1 View FIGURE 1 , 2 View FIGURE 2 )
Diagnosis: Lithoglyptinae having twosegmented caudal appendages plus pedestals, an operculum with a pair of posterior lobes (inconspicuous in L. indicus and L. ivanovi ), opercular bars without long posterior projections or auricles, and a mantle without orificial knob or lateral bars.
Four of the 14 species attributed to Lithoglyptes s.l. are retained in Lithoglyptes s.s. They are the type, L. indicus Aurivillius, 1892 ; L. viatrix Grygier & Newman, 1985 ; L. tectoscrobis Grygier & Newman, 1985 ; and L. ivanovi Kolbasov, 1998 . They are united by a common morphology such as their opercular bars lacking the long projections ( Fig. 1 B, F, H, J View FIGURE 1 ). Such anteriorly or posteriorly hooked projections on the opercular bars are seen in species belonging to the new genera proposed herein ( Figs. 3 A View FIGURE 3 ; 4 A View FIGURE 4 ; 5 View FIGURE 5 AD, E; 6 A, B). The opercular bars of three of the four species are armed with small, simple teeth and denticles ( Figs. 1 B, H View FIGURE 1 ; 2 A, B View FIGURE 2 ), but in the fourth, L. ivanovi , they bear some bifid teeth ( Fig. 1 J View FIGURE 1 ), a feature seen in the two new genera. The presence of short posterior or "carinal" lobes on the opercular bars is characteristic of L. viatrix and L. tectoscrobis ( Fig. 1 B, F View FIGURE 1 ), the same area in L. indicus and L. ivanovi being marked by a patch of spines ( Fig. 1 H, J View FIGURE 1 ). Lateral bars and/or an orificial knob are completely absent in the armament of the mantle in these four species ( Figs. 1 A, F, H View FIGURE 1 ; 2 A View FIGURE 2 ).
A calcareous, “rostral” plate ( Fig. 1 A, C View FIGURE 1 ), associated with the attachment disk cementing it to the substratum, was described for L. viatrix and L. tectoscrobis ( Grygier & Newman 1985; Kolbasov 2000a). It is possible the other two species also have such a calcareous plate, but they would have to be removed mechanically from the substratum to find out. The caudal appendages of the species of this genus each consist of two segments supported by a pedestal on either side of the anus. The basal segment supports one or two setae and the terminal segment supports a tuft of four or more long, plumose setae at the distal end ( Figs. 1 G, I, K View FIGURE 1 ; 2 G View FIGURE 2 ).
The sac of mature dwarf males, known for some species, may possess lateral projections and a short, thick stalk between the body and the antennules ( Fig. 1 E View FIGURE 1 ).
Surficial ultrastucture of L. viatrix was studied in detail utilizing SEM ( Fig. 2 View FIGURE 2 ). Rows of large multifid scales, common to most Acrothoracica ( Smyth 1986; Kolbasov 1999 a, 2000b, 2000c, 2000d, 2000e; Kolbasov & Høeg 2000), occupy the lateral faces of the opercular area. Occasionally papillae and short setae ( Fig. 2 B, C View FIGURE 2 ) occur between the large multifid scales. The cuticle of the area occupied by an orificial knob, when present, lacks teeth, setae or multifid scales ( Fig. 2 A View FIGURE 2 ). Exposed cuticle of the attachment disk has rounded, transverse lines apparently corresponding to the growth lines of the calcareous plate ( Fig. 2 D View FIGURE 2 ).
In Lithoglyptes View in CoL s.s., as in all lithoglyptid species studied with SEM ( Kolbasov 1999 a, 2000 a, 2000c, 2000d, 2000e; Kolbasov & Høeg 2000; Kolbasov, unpublished data), the surface of the sheets of cuticle forming the attachment disk are covered with dense, filiform structures arranged in irregular, transverse rows ( Fig. 2 E, F View FIGURE 2 ) and it has been suggested they serve as passages for the secretion of cement ( Kolbasov 1999a; Kolbasov & Høeg 2000).
Distribution: Representatives of the genus are found in the Red Sea, Indian Ocean, Sumatra, Java, Java Sea, Coral Sea, and Hawaii. Depth: subtidal zone ( L. indicus and L. ivanovi ) or at approximately 500 m ( L. viatrix and L. tectoscrobis ).
Hosts: Mainly in scleractinians such as Enallopsammia ampheloides and some undetermined corals. Also in Thais sp. and some undetermined molluscs.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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Lithoglyptes
Kolbasov, Gregory A. & Newman, William A. 2005 |
Lithoglyptes
Aurivillius 1892 |