Thesea pyrrha, Carpinelli & Cordeiro & Castro & Kitahara, 2022
publication ID |
https://doi.org/ 10.11646/zootaxa.5116.1.4 |
publication LSID |
lsid:zoobank.org:pub:B3470E9E-D0A6-4C30-8C00-BFD71AF4A668 |
DOI |
https://doi.org/10.5281/zenodo.6366433 |
persistent identifier |
https://treatment.plazi.org/id/F858DA32-C707-FFC1-ADE8-F95188E10800 |
treatment provided by |
Plazi |
scientific name |
Thesea pyrrha |
status |
sp. nov. |
Thesea pyrrha View in CoL sp. nov.
Thesea sp. : Tixier-Durivault, 1970, p. 152 –153, fig. 3 (MNHN paratype).— Castro et al., 2006, p. 175 (station list).
Holotype. USNM 73349 About USNM , 23°12'21"S, 44°31'36"W, Ilha Grande Bay , Rio de Janeiro, Brazil, collected by Clarisse Rohlfs, 04/29/1980. GoogleMaps
Paratypes. MNHN (accession number unavailable), Calypso st. 100, 22°12,5'S, 40°59'W, off Cape São Tomé, Rio de Janeiro, 39 m (fragment) GoogleMaps ; MNRJ 5078 View Materials , 22°19’07” S, 40°49’34” W, off Macaé , Rio de Janeiro, 57–60 m GoogleMaps ; MNRJ 2641 View Materials , 22°25'S, 41°05'W, off Macaé, Campos Basin , 51 m (one colony) GoogleMaps ; MNRJ 1377 View Materials , Laje de Santo Antônio, off Ipanema Beach , Rio de Janeiro, 10 m (4 colonies) ; MNRJ 1979 View Materials , Laje de Santo Antônio, off Ipanema Beach , Rio de Janeiro, 10 m (6 colonies) ; MNRJ 333 View Materials (between 23°11,5'S, 44°28,3'W and 23°13,2'S, 44°34,9'W), Ilha Grande Bay , Rio de Janeiro, 30 m (two colonies) GoogleMaps ; USNM 1659638 About USNM , 23°12'21"S, 44°31'36"W, Ilha Grande Bay , Rio de Janeiro, Brazil (same collection data of the holotype) GoogleMaps ; MNRJ 1859 View Materials , Xavier Island, Florianópolis , Santa Catarina, 19 m (one colony) ; MNRJ 2474 View Materials , Arvoredo Island, Florianópolis , Santa Catarina, 3 m (two colonies) ; MNRJ 4876 View Materials , 23°03’S, 43°92’W Cagarras Archipelago, Rio de Janeiro, shallow-water (fragment) ; USNM 51601 About USNM , between Rio Grande and Chuí , Rio Grande do Sul, Pascal II R/V; MZUSP 8699 View Materials , 27°16’S, 48°22’W, Arvoredo Island , Florianópolis, Santa Catarina, shallow-water (fragment) GoogleMaps ; MZUSP 8700 View Materials , 28°45’S, 48°71’W, Lobos Island , Santa Catarina, shallow-water (one colony) ; MZUSP 8701,28°45’S, 48°71’W, Lobos Island , Santa Catarina, shallow-water (four colonies) ; MZUSP 8702 View Materials , 28°45’S, 48°71’W, Lobos Island , Santa Catarina, shallow-water (two colonies) ; MZUSP 8703 View Materials , 28°45’S, 48°71’W, Lobos Island , Santa Catarina, shallow-water (two colonies) ; MZUSP 8704 View Materials , 28°45’S, 48°71’W, Lobos Island , Santa Catarina, shallow-water (one colony) ; MZUSP 8705 View Materials , 28°45’S, 48°71’W, Lobos Island , Santa Catarina, shallow-water (one colony) ; MZUSP 8706 View Materials , 28°73’S, 49°02’W, Laje da Jaguaruna , Santa Catarina, shallow-water (three colonies) .
Description. Colonies white, yellow, orange or red, 3 to 10 cm tall and 3 to 9 cm in width, planar to sparsely bushy ( Figs. 1A View FIGURE 1 , 3 View FIGURE 3 ). Branches oriented upwards up to the 6 th order, terminal branchlets between 0.5–6.7 cm long. Main branch from 2.5 to 18 cm long and from 5 to 15 mm in width. Proximal diameter of branches of 1.6–2.8 mm, and 1.2–2.1 mm distally. Branch thickness varying from slender proximally to thicker in the median portion; tips rounded and slightly slender. Polyps only on branches, disposed in four main alternate rows, sometimes irregular. Calyces ( Fig. 1 View FIGURE 1 C-D) usually low and sometimes absent, with eight marginal teeth, formed by convergent spindles. Sometimes calyces may have up to 0.9 mm in height and 1 mm in diameter. Coenenchymal surface with two-faced sclerites, externally corrugated and internally densely filled with tubercles ( Figs. 1B View FIGURE 1 , 2A View FIGURE 2 ), 0.34–0.6 mm long and 0.03–0.25 wide, disposed side by side, creating a surface with granulose appearance ( Fig. 1C View FIGURE 1 ). Two-faced sclerites of the outer layer interleaved by uniformly tuberculated spindles 0.23–0.26 mm long ( Fig. 2B, D View FIGURE 2 ). Calyces with smaller sclerites, often slender than those from coenenchyme, mostly tuberculated spindles and clubs ( Fig. 1C View FIGURE 1 ) up to 0.24 mm in length. Inner coenenchymal layer with tuberculated spindles ( Fig. 2E View FIGURE 2 ) 0.12–0.23 mm long and 0.02–0.11 wide. Polyp sclerites are spindles and rods straight or curved ( Fig. 2F View FIGURE 2 ), 0.06–0.28 long and 0.001–0.01 mm wide.
Habitat and distribution. Brazil, off Rio de Janeiro, Santa Catarina and Rio Grande do Sul (22° to 33°S) on shallow to mesophotic hard substrates (3 to 60 m).
Etymology. The species epithet pyrrha (Gr. pyrrhos, flame-colored, red, yellowish-red), alludes to the flamecolored color of live specimens that range from vivid-red to yellowish-red.
Comparative materials. Thesea gracilis (MCZ 4160, holotype); T. bicolor ( MCZ 4626 About MCZ , holotype) ; T. granulosa ( MCZ 4624 About MCZ , holotype) ; T.rubra ( MCZ 4627 About MCZ , holotype) ; T. citrina Deichmann, 1936 ( MCZ 4632 About MCZ , holotype) ; T.rugosa Deichmann, 1936 ( MCZ 4633 About MCZ , syntype) ; T. parviflora Deichmann, 1936 ( MCZ 4635 About MCZ , holotype) ; T. grandiflora Deichmann, 1936 ( MCZ 4641 About MCZ , syntype) ; T. hebes Deichmann, 1936 ( MCZ 4642 About MCZ , syntype) ; T. antiope ( USNM 50848 About USNM , holotype) .
Remarks. Thesea pyrrha sp. nov. differs from Thesea antiope by not having the doublehead sclerites in the surface of the coenenchyme. Thesea gracilis ( Gray, 1868) , T. guadalupensis ( Duchassaing & Michelotti, 1860) and T. bicolor have more or less regular elongate sclerites in the coenenchyme, in which the outer face is sparsely granular. Thesea citrina , T. rugosa, T. grandiflora and T. parviflora have a similar granular sculpture pattern on their large plate-like coenenchymal sclerites. In Thesea hebes , its outer surface corresponds to the smaller portion of the sclerite, with a smooth surface as well. Thesea rubra has a nearly smooth outer surface. On the other hand, T. granulosa has stout sclerites in the outer coenenchyme, with tubercles fused in groups, but rarely forming projecting ridges. Interestingly, specimens obtained from greater depths (e.g. MNHN, 39 m; MNRJ 2641, 51 m) tend to have more prominent calyces than those from shallower waters (<20 m), in accordance with previous findings for other octocoral taxa (Grigg, 1970; West et al., 1993; Kim et al., 2004; Joseph et al., 2015).
In this manuscript, we prioritize the description of T. pyrrha and discussions are limited to the systematics of the genus Thesea . For that reason, we choose to keep it in the formal family Plexauridae , rather than describing a new family, for which purpose a morphological assessment of the genera Adelogorgia, Psammogorgia, and Swiftia would be necessary.
Molecular analyses
The sequencing of the samples of Thesea pyrrha sp. nov. resulted in partial fragments of the mitochondrial genes mtMutS (~590 bp) and COI+igr (~600 bp) and of the nuclear 28S rDNA (~560 bp). Most samples had only mtMutS and COI+igr successfully sequenced, but the samples 8699, 8700 and 8702 had all three regions determined. The concatenated alignment totaled 2.055bp, which were partitioned according to the best nucleotide evolutionary model as: HKY+G (mtMutS), HKY+I+G (COI), and GTR+G
(28S).
The species traditionally included in the family Gorgoniidae were recovered in different arrangements in each phylogenetic reconstruction. The ML topology recovered a large gorgoniid clade with low statistical support ( Fig. 4 View FIGURE 4 ). On the other hand, the BI recovered four main clades containing gorgoniids, all with Leptogorgia representatives (mostly not identified to species level). The clade named “ Gorgoniidae ” ( Fig. 4 View FIGURE 4 ) is the only monophyletic clade of the family recovered by ML. This clade is composed by Leptogorgia, Antillogorgia, Eugorgia, Gorgonia, Pacifigorgia, Phyllogorgia, and Pseudopterogorgia.
Morphologically identified plexaurids grouped into a large clade with high statistical support ( Fig. 4 View FIGURE 4 ), being composed by Alertigorgia, Iciligorgia, Menella, Muricea, Muriceopsis, Paraplexaura, Pinnigorgia, Plexaura, Plexaurella Pseudoplexaura, Pterogorgia, and Siphonogorgia. The clade Bebryce-Lytreia-Heterogorgia was strongly supported and recovered in all reconstructions. Eunicella (traditionally Gorgoniidae ) was also recovered in all analyzes closer to Plexauridae .
Adelogorgia, Psammogorgia, and Thesea
Swiftia simplex falls into a sister clade of Psammogorgia spp. and Adelogorgia, which was monophyletic in all systematic reconstructions. These genera are also closely related to Swiftia and a namely Thesea sp. from Honduras ( AY683089 View Materials ). Adelogorgia, Psammogorgia, and Swiftia were related to Thesea pyrrha sp. nov. in all analyzes.
Specimens of Thesea sp. ( AY683083 View Materials – Galapagos, and KP324345 View Materials – New Caledonia) fall in clades distant from all Eastern Pacific and Atlantic congeners in all analyzes and need to be re-examined taxonomically. Sequences of the specimen from Galapagos AY683083 View Materials are identical to that from Euplexaura sp. ( GQ342518 View Materials ), whereas that from the New Caledonian specimen was also somewhat similar and, thus, recovered as closely related. Specimens of Thesea from Brazil were recovered as a monophyletic group with high-statistical support in all analyzes. They had in Thesea sp. ( MF319967 View Materials – Eastern Pacific) their sister clade. Results from the p- distance analyzes indicate that Psammogorgia is the genus closest to Thesea (0.096). Interspecific distances between sequences of Thesea sp. nov. vary from 0 to 0.360 ( Table 1 View TABLE 1 - Sup. Material).
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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Thesea pyrrha
Carpinelli, Ágatha Nascimento, Cordeiro, Ralf Tarciso Silva, Castro, Clovis Barreira & Kitahara, Marcelo Visentini 2022 |
Thesea sp.
Castro, C. B. & Pires, D. O. & Medeiros, M. S. & Loiola, L. L. & Arantes, R. C. M. & Thiago, C. M. & Berman, E. 2006: 175 |
Tixier-Durivault, A. 1970: 152 |