Euceramus transversilineatus ( Lockington, 1878 )
publication ID |
https://doi.org/ 10.11646/zootaxa.5045.1.1 |
publication LSID |
lsid:zoobank.org:pub:B12C62E3-70D0-4989-BB1A-F4A75C492D8F |
DOI |
https://doi.org/10.5281/zenodo.5532193 |
persistent identifier |
https://treatment.plazi.org/id/03D62C6B-7777-FFD0-4EF9-5803FDFFAEC2 |
treatment provided by |
Plazi |
scientific name |
Euceramus transversilineatus ( Lockington, 1878 ) |
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Euceramus transversilineatus ( Lockington, 1878) View in CoL
( Figs. 4 View FIGURE 4 , 5 View FIGURE 5 )
Porcellana transversilineata Lockington 1878: 396 View in CoL , 405.
Euceramus transversilineatus View in CoL .— Glassell 1938: 426, pl. 30; Haig 1960: 190, fig. 7(2), pl. 36, fig. 2; Abele & Kim 1989: 21.
Material examined. Panama [Pacific]: 1 ov. female, cl 8.4, cw 5.1 ( MZUSP 33494 View Materials ), Las Perlas Is., small rocky islet off north-eastern coast of Isla Saboga , depth at low tide 0.5 m, rock-sand bottom, strong current passage, deep under large rock on sand and small coral fragments, associated with holothurian, Holothuria sp. , leg. A. Anker, 21.04.2015 .
Previous records from Panama. Haig (1960); Abele & Kim (1989).
Distribution. East Pacific: Mexico and Panama (Taboga Is., Las Perlas Is., Panama Canal area) ( Glassell 1938; Haig 1960; Abele & Kim 1989; present study).
Ecology. Shallow subtidal, from just below the tide mark to 62 m. Glassell’s (1938) material came from “extreme low water, from the sand and shell material at the base of gorgonian corals”, as well as from “12 fathoms” (= 22 m). Haig (1960) reported E. transversilineatus from depths between 3.5 and 62 m, on sand, shell, sand and shell, sandy mud and sand with coralline algae bottoms. The single Las Perlas specimen was collected in slightly shallower conditions, about 0.5 m at spring low tide (> 3 m at high tide). It was found firmly clinging to a medim-sized sea cucumber, Holothuria sp. ( Fig. 5 View FIGURE 5 ). The association of E. transversilineatus with holothurians has never been reported before, although it is presently unknown whether this porcelain crab is an obligate (or at least frequent) symbiont of holothurians or whether this finding is merely incidental.
Remarks. According to Glassell (1938), E. transversilineatus is more closely related to the western Atlantic E. praelongus than to its eastern Pacific congener E. panatelus , differing from both species by the carapace much shorter and with more distinct striations; the antennae shorter and not setose; the P2–P4 dactyli more uniform and falcate; and the telson longer relative to its width. In addition to the shape of the carapace, the two eastern Pacific can be easily separated by their colourations, creamy beige in E. transversilineatus ( Fig. 4 View FIGURE 4 ) vs. white in E. panatelus ( Fig. 3 View FIGURE 3 ).
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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Euceramus transversilineatus ( Lockington, 1878 )
Ferreira, Luciane Augusto De Azevedo & Anker, Arthur 2021 |
Euceramus transversilineatus
Abele, L. G. & Kim, W. 1989: 21 |
Haig, J. 1960: 190 |
Glassell, S. A. 1938: 426 |
Porcellana transversilineata
Lockington, W. N. 1878: 396 |