Astropecten polyacanthus ( Müller & Troschel, 1842 )

Pourvali, Naser, Aliabadi, Mohammad-Ali Salari, Salamat, Negin, Hesni, Majid Askari, Ranjbar, Mohammad Sharif, Carter, Hugh & Price, Andrew. R. G., 2025, Systematics, distribution and ecology of sea stars (Echinodermata: Asteroidea) from Iranian waters of the Persian Gulf and a revised identification key, Zootaxa 5647 (3), pp. 201-234 : 212-214

publication ID

https://doi.org/10.11646/zootaxa.5647.3.1

publication LSID

lsid:zoobank.org:pub:82D8AE6A-998E-4577-9919-29F470D6DA40

DOI

https://doi.org/10.5281/zenodo.15819749

persistent identifier

https://treatment.plazi.org/id/6233CD02-6124-3F7E-FF24-82963A5BA9F3

treatment provided by

Plazi

scientific name

Astropecten polyacanthus ( Müller & Troschel, 1842 )
status

 

Astropecten polyacanthus ( Müller & Troschel, 1842) View in CoL : 68

Material examined: 1 specimen (ZMSBUK-1642)

R: 74mm, r: 18mm

Description: ( Figs. 15–17 View FIGURE 15 View FIGURE 16 View FIGURE 17 )

Five long arms, rectangular in cross section, with a relatively small disc ( R /r:>4:1). Actinal and abactinal surface very flattened. Abactinal paxillae relatively large, particularly so toward the axis of the arms and centre of the disc where they bear up to 18 granules; peripheral paxillae somewhat smaller with up to 8 central granules; madreporite clearly visible but not large; body margin defined by supero-marginal plates each with a large vertically erect, sharp spine, except on the second and occasionally third most proximal plates were this is absent. Most proximal supero-marginal spine very prominent. Infero-marginal plates each with a prominent spine and 4–5 smaller spines arranged in a fine row along the distal plate edge. Remainder of infero-marginal plate covered in smaller spinelets. Actinal surface largely covered by an extension of the infero-marginal plates; adambulacral plates with three furrow row spines; terminal disc in tube feet absent, feet instead tapering to distinctive point.

Observations:

Mainly found in sandy and/or sandy-rock shores from the intertidal to 5 m. Live specimens have a tendency to almost disappear into sandy bottoms by sifting themselves into the substrate. Recorded in the present study at Nayband Bay , Bostaneh in main land and, Qeshm, Hengam , Larak , Hormuz, Lavan and Kish Islands .

Previously reported from the Persian Gulf: ( Mortensen 1940; Clark & Bowen 1949; Clark & Rowe 1971; Basson et al. 1977; Price 1982a; Price 1982b; Price 1983; Khayat 2005; George 2012; Pourvali et al. 2014; Pourvali 2015; Adeli et al. 2022); present study.

R

Departamento de Geologia, Universidad de Chile

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