Pilumnus cursor A. Milne-Edwards, 1873
publication ID |
https://doi.org/10.6620/ZS.2024.63-38 |
persistent identifier |
https://treatment.plazi.org/id/5C3287DF-FF9E-8E68-13C6-F90AFD8C0CB4 |
treatment provided by |
Felipe |
scientific name |
Pilumnus cursor A. Milne-Edwards, 1873 |
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Pilumnus cursor A. Milne-Edwards, 1873 View in CoL
? Pilumnus cursoni — J Jiang and Zhou 1982: 681.
Taxonomy: Ng (1988a).
Type: Syntype ñ in MNHN ( Ng 1988a).
Type locality: New Caledonia.
Distribution: Indo-West Pacific: so far confirmed from Phuket, Thailand and New Caledonia only (see Remarks below).
Habitat: Subtidal; in coral rock ( Ng and Davie 2002).
Remarks: Records elsewhere previously recognized as “ P. cursor ” comprises a species complex, and various of these in the region had been referred to other species ( Ng 1988a). This local record is thus very likely “either incorrect or suspicious” ( Ng and Davie 2002: p. 382) and needs to be verified. Until then, we retain this record for the time being.
Pilumnus longicornis Hilgendorf, 1878 #
? Pilumnus andersoni View in CoL — Shen 1940a: 228.
? Pilumnus cf. andersoni View in CoL — Horikoshi and Takeda 1982: tab. 1.
Pilumnus longicornis View in CoL — Horikoshi and Takeda 1982: tab. 1; Morton and Morton 1983: 273.
Taxonomy: Balss (1933), Sakai (1939), Takeda and Miyake (1968).
Type: Holotype ò in ZMB ( Balss 1933).
Type locality: Inhambane, Mozambique.
Distribution: Western Indian Ocean to Central Pacific: from South Africa, Madagascar, Persian Gulf, Arabian Sea and Bay of Bengal, to Southeast and East Asia reaching Japan, and Indonesia, Australia, New Zealand towards Hawaii ( Takeda and Miyake 1968; Garth and Kim 1983; Yang et al. 2008).
Habitat: Intertidal and subtidal; rocky shores down depths of 10 to 20 m, also on sandy substrates down to depths of 85 m ( Sakai 1976).
Remarks: Balss (1933) synonymized P. andersoni De Man, 1887 (type locality Mergui Archipelago) under P. longicornis Hilgendorf, 1878 , arguing that the morphological variations between the two (whether frontal and supraorbital margin denticulate) were age-dependent. Shen (1940a), however, cited Alcock (1898: p. 191) who interpreted the two as distinct, listing the Hong Kong material as P. andersoni . Following Balss (1933) for the moment, we list the Hong Kong records under P. longicornis .
Pilumnus minutus De Haan, 1835 #
? Pilumnus cf. minutus View in CoL — Horikoshi and Takeda 1982: tab. 1; Wong et al. 2021: 36, fig. 56, pl. 11D.
Pilumnus minutus View in CoL — Ong Che and Morton 1992: tab. 1.
Taxonomy: Sakai (1939), Takeda and Miyake (1968).
Type: Status unknown ( Davie 2002; not reported by Yamaguchi and Baba 1993).
Type locality: Japan, locality unspecified.
Distribution: Western Indian Ocean to West Pacific: from South Africa, Maldives, Red Sea, Persian/ Arabian Gulf, Bay of Bengal, Southeast and East Asia to Japan, Indonesia, Australia and New Caledonia ( Takeda and Miyake 1968; Yang et al. 2008).
Habitat: Intertidal to subtidal; along crevices of rocks, or on sandy or muddy substrates, or in sponges; depth up to 50 m ( Dai and Yang 1991).
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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Pilumnus cursor A. Milne-Edwards, 1873
Wong, Kingsley J. H., Ng, Peter K. L., Shih, Hsi-Te & Chan, Benny K. K. 2024 |
Pilumnus cf. minutus
Wong KJH & Tao S-r & Leung KMY 2021: 36 |
Pilumnus longicornis
Morton B & Morton J. 1983: 273 |
Pilumnus cursoni
Jiang J & Zhou Q. 1982: 681 |
Pilumnus andersoni
Shen C-J. 1940: 228 |