Myrmekioderma rea (de Laubenfels 1934 )
publication ID |
https://doi.org/ 10.11646/zootaxa.5031.1.1 |
publication LSID |
lsid:zoobank.org:pub:CC3A59D1-E09E-407E-93F4-4796FD3D7C19 |
DOI |
https://doi.org/10.5281/zenodo.5495432 |
persistent identifier |
https://treatment.plazi.org/id/110587B3-4D19-4802-FF53-FD9D496D333B |
treatment provided by |
Plazi |
scientific name |
Myrmekioderma rea (de Laubenfels 1934 ) |
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Myrmekioderma rea (de Laubenfels 1934) View in CoL
Tables 6, 7; Figs. 12A–G View FIGURE 12 , 16L View FIGURE 16
Synonymy and references: Anacanthaea rea de Laubenfels (1934: 11) ; Epipolasis rea , Epipolasis reiswigi and Myrmekioderma styx : see references compiled in Muricy et al. (2011: 96); Myrmekioderma rea: Muricy et al. (2011: 96) , Rützler et al. (2014: 72), Pérez et al. (2017: 11), and van Soest (2017: 56).
Type locality. Puerto Rico .
Material examined. CNPGG-2261, Triangulo Oeste reef (20.95629°N, - 92.308609°W), 8 m depth, coll. Oscar Bocardo, 10 September 2017 GoogleMaps ; CNPGG-2433, Cabezo reef (19.05086°N, - 95.82388°W), 8.3 m depth, coll. Diana Ugalde, 30 August 2018 GoogleMaps .
Description. Massive habit; larger specimen size 7.5 × 5 × 3 cm ( Fig. 16L View FIGURE 16 ). Surface slightly irregular, covered by sand and calcareous debris. Pores are not visible. Oscules scattered up to 2 mm diameter. Color in vivo orangishyellow, pinkish beige preserved in ethanol. Consistency firm and slightly resilient.
Skeleton. The ectosomal region is constituted by acanthoxeas perpendicular to the surface in a palisade-like structure ( Fig. 12A View FIGURE 12 ). Some acanthoxeas in a paratangential and criss-cross arrangement ( Fig. 12B View FIGURE 12 ). It is covered by a crust of sand grains and calcareous debris, up to 200 µm thick. Choanosomal region with longitudinal tracts (up to 120 µm thick) of large oxeas towards the surface. The large oxeas are also scattered in between. Raphides scattered throughout the skeleton; in trichodragmas. Rounded channels, up to 100 µm diameter, are horizontally aligned beneath the palisade of acanthoxeas. Channels scattered in the choanosome, up to 130 µm in diameter. Scattered debris was also found in the choanosomal region ( Fig. 12B View FIGURE 12 ).
Spicules. Megascleres: Large oxeas with styloid and strongylote modifications, stout, slightly curved to sinuous, some forms double bent, and smooth ( Fig. 12C View FIGURE 12 ). The tips are conical, stepped, or blunt; 535– 807 (161.3)– 1110/8– 11.5 (1.5)–14 µm ( Figs. 12D–E View FIGURE 12 ). Acanthoxeas are slightly curved to sinuous; some are double bent, covered irregularly with minute spines, sometimes smoother at the middle region ( Figs. 12F–G View FIGURE 12 ). With sharp and acerate tips; 235– 362 (48.9)–420/7.2– 10.7 (2)–14 µm. Microscleres: raphides very thin; 120– 150.3 (20.7)–180 µm in length.
Distribution. Mexico (current records), US (Florida), Barbados, Bahamas, Cuba, other countries in the Caribbean Sea ( Diaz et al. 1993); Guyana ( van Soest 2017).
Remarks. Van Soest (2017) believed the observed variability in Guyana’s specimens obtained from the same trawl (98 m and 65 m depth) was intraspecific. He observed variation in the habit (i.e., broad knoll, club-shaped body or finger-shaped body) and spiculation (i.e., the shape of oxeas and number of categories of oxeas and raphides). We extend this intraspecific variation of M. rea by considering specimens from Belize ( Rützler et al. 2014) and the GoM (present study), both no deeper than 20 m. These specimens have massive cushion shape habits. In adition, spicule measurements of the Mexican specimens analyzed in our study (particularly of oxeas) are thinner than those in specimens from Belize and Guyana. However, in general, our material’s spicule measurements are more similar to specimens from Belize than the ones from Guyana ( Table 1).
Intraspecific variation of Myrmekioderma rea can be observed in Brazilian specimens too ( Rosa-Barbosa 1995, Mothes et al. 2004, 2006). They were all reported with a massive habit, similar to our material’s and Belize’s ( Rützler et al. 2014), but devoid of raphides in northern Brazil ( Mothes et al. 2004), and possessing styles (744.2– 1497/10–23.9 µm) and small trichodragmas (23–92/4.6–13 µm) in materials reported by Mothes et al. (2006), from southern Brazil. These variations deviate from typical spiculation of M. rea in specimens from Guyana, the Caribbean region, and the GoM (our material) ( Table 1). Previous and the present records of M. rea are from shallow to mesophotic depths on coral reefs (de Laubenfels 1953; van Soest & Stentoft 1988; Díaz et al. 1993; Rützler et al. 2014), and from muddy sand bottoms down to 100 m depth ( van Soest 2017).
Order Biemnida Morrow, 2013
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