Synalpheus brevidactylus Anker & Tóth, 2008
publication ID |
https://doi.org/10.11646/zootaxa.5666.1.1 |
publication LSID |
lsid:zoobank.org:pub:278A0EE3-FA26-430F-B32B-91507D3AB8F7 |
DOI |
https://doi.org/10.5281/zenodo.16610167 |
persistent identifier |
https://treatment.plazi.org/id/26013B60-426F-4F17-1FEC-FE024B4EF96F |
treatment provided by |
Plazi |
scientific name |
Synalpheus brevidactylus Anker & Tóth, 2008 |
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Synalpheus brevidactylus Anker & Tóth, 2008 View in CoL ( Figs. 9 View FIGURE 9 , 10 View FIGURE 10 )
Material examined: Pernambuco — Continental Shelf off Recife : 1 OV , 27.ii.2018, 8°13′52.1′′S 34°37′42.7′′W, 50.0 m depth, in sponge, DZ / UFRGS 7052 View Materials GoogleMaps ; 1 OV, same data as DZ/ UFRGS 7052 View Materials , MOUFPE 21815 View Materials GoogleMaps ; 1 M, 27.ii.2018, 8°13′36.8′′S 34°37′41.9′′W, 51.0 m depth, in sponge, MOUFPE 21813 View Materials GoogleMaps ; 1 M, 27.ii.2018, 8°13′52.1′′S 34°37′41.2′′W, 51.8 m depth, in sponge, DZ / UFRGS 7053 View Materials GoogleMaps .
Description: Anker & Tóth (2008).
Distribution: Panama and Brazil (Pernambuco) ( Anker & Tóth, 2008; this study).
Ecology: Associated with the sponges Neopetrosia subtriangularis ( Duchassaing, 1850) and Calyx podatypa ( Laubenfels, 1934) , growing on substrates such as coral rubble and seagrass; in heterosexual pairs; 1– 51.8 m ( Anker & Tóth, 2008; this study). Sampled at the continental shelf off Recife (all lots cited above) in association with sponges, on coral rubble and algae bottom, at depths from 50–51.8 m.
Remarks: Synalpheus brevidactylus is characterized by a rostrum distinctly longer than the orbital teeth, broad at the base and tapering to the tip; by the fixed and movable fingers of the minor chela excavated on the cutting edges, with the dactylus bearing scattered gambarelloid setae on dorsal surface; by the uropodal exopod armed with two to three lateral teeth ( Figs. 10B, C View FIGURE 10 ); and by the telson presenting a longitudinal median depression ( Fig. 10D View FIGURE 10 ) ( Anker & Tóth, 2008; Anker et al. 2012; this study). Additional diagnostic characters are: the carpus of the second pair of pereiopods divided into five articles, with the first four times as long as the second ( Fig. 9F View FIGURE 9 ), the third maxilliped ending in a set of six or seven spiniform setae ( Fig. 10E View FIGURE 10 ), and the palm of the major chela is approximately three times as long as the fingers ( Anker & Tóth, 2008). The material examined revealed morphological variations when compared to the original description of the species. For instance, a male specimen (MOUFPE 21813) exhibited a rostrum and orbital teeth that were subequal in length, with the rostrum being narrower (vs. rostrum longer and broader than the orbital teeth) (for comparison, see Fig. 9 A View FIGURE 9 and Anker & Tóth, 2008, Fig. 8A View FIGURE 8 ). The fingers of the major chela were strongly unequal in length, with the dactylus being square/rounded and longer than the fixed finger (vs. dactylus slightly longer and more bulging than the fixed finger) (see Figs. 9B, C View FIGURE 9 , and Anker & Tóth, 2008, Figs. 8C, E View FIGURE 8 ). Additionally, the distodorsal tooth of the basicerite is slightly more acute (vs. distodorsal margin of the basicerite with a subacute point). The blade of the scaphocerite is longer, extending beyond the ventrolateral tooth of the basicerite and reaching the end of the distolateral tooth of the scaphocerite (vs. blade of scaphocerite reaching the end of the ventrolateral tooth of the basicerite and halfway to the distolateral tooth of the scaphocerite) (for comparison, see Fig. 9 A View FIGURE 9 and Anker & Tóth, 2008, Fig. 8A View FIGURE 8 ). In another specimen (1 OV, MOUFPE 21815), the tooth of the right orbital hood is partially fused to the rostrum (vs. typical tridentate front) and the uropodal exopod had three fixed teeth on the right side and two on the left (vs. uropodal exopod with three or four fixed teeth in both sides) (see Anker & Tóth, 2008, Figs. 8I, K View FIGURE 8 ). This study provides the first record of S. brevidactylu s in the southwestern Atlantic and expands its known bathymetric distribution from 3 ( Anker & Tóth, 2008) to 51.8 m.
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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