Loricella profundior ( Dell, 1956 )
publication ID |
https://doi.org/ 10.11646/zootaxa.4981.2.4 |
publication LSID |
lsid:zoobank.org:pub:F3FD1EFA-2058-44B5-88EE-A82CCB968D21 |
DOI |
https://doi.org/10.5281/zenodo.4923614 |
persistent identifier |
https://treatment.plazi.org/id/82770F72-FF96-287D-2BE1-FF6975368D34 |
treatment provided by |
Plazi |
scientific name |
Loricella profundior ( Dell, 1956 ) |
status |
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Loricella profundior ( Dell, 1956) View in CoL
( Figs. 1 View FIGURE 1 , C, D, 2–7 View FIGURE 2 View FIGURE 3 View FIGURE 4 View FIGURE 5 View FIGURE 6 View FIGURE 7 )
Paricoplax profundior Dell 1956: 157 View in CoL , figs. 213–219; O’Neill 1987: 134; Xu 1990: 377.
Loricella profundior, Beu 1967: 478 View in CoL ; Fitzgerald 1969: 23; Beu 1977: 42; Powell 1979: 25; Kaas 1990: 178 (in part); 1991: 22 (in part); Kaas et al. 2006: 67 (in part); Spencer et al. 2009: 197.
Loricella oviformis, Kaas 1985: 310 View in CoL (in part, not Squamophora oviformis Nierstrasz, 1905 ).
Sinolorica profundior, Xu 1990: 377 .
Type material. Holotype ( NMNZ M972 ), not seen.
Type locality. New Zealand, Chatham Islands, off the Forty Fours , 238 m.
Material examined. Tonga Islands, Tongatapu, N/O “Alis”, BORDAU 2 stn CP1510, 21°05.5’S, 175°23’W, 461–497 m, 1 spm (MNHN-IM-2013-59980), BL 11.5 mm, 31.05.2000 GoogleMaps ; stn CP1545, 21°17’S, 175°17’W, 444–447 m, 1 spm (MNHN-IM-2013-59981), BL 9.0 mm, 05.06.2000 GoogleMaps ; stn DW1628, 23°22’S, 176°18’W, 400–416 m, 2 spms (MNHN-IM-2013-59982, MNHN-IM-2013-59983), BL 8.0–11.0 mm, 19.06.2000 GoogleMaps ; New Zealand, southern Kermadec Ridge , Rumble V volcano, RVTangaroa, 36°8.80’S, 178°12.20’E, 772–951 m, 1 spm ( NMNZ M.319774), BL 18.0 mm, 23.05.2001 GoogleMaps ; Chatham Rise, RVTangaroa, 42°35.15’S, 179°10.57’E, 602 m, 1 spm ( NMNZ M.183839), BL 11.5 mm, 29.12.2003 GoogleMaps .
Distribution. New Zealand (238–772 m: Dell 1956 and this study), Tonga (416–461: this study).
Remarks. Specimens from Tonga and New Zealand are very similar to the holotype (NMNZ M972) in shape and structure of the shell. Dorsal scales have grooves near the edge of the distal part. Aspecimen (NMNZ M.319774) from New Zealand (BL 18 mm) has a dorsal elevation of 0.27, slit formula 12/1/sinus + 8 obsolete, 18 gills on each side, and the nephridiopore and gonopore arranged between 4–5 and 5–6 gills accordingly counted from the last one. Aspecimen (MNHN-IM-2013-59983) from Tonga (BL 11 mm) has dorsal elevation of 0.31, slit formula 14/1 (rare 2)/sinus + 5 obsolete (valve II has two slits in one side), 16 gills in each side extending from valve IV to valve VII, nephridiopore and gonopore arranged between 4–5 and 5–6 gills accordingly counted from the last one, and a radula 1.6 mm long with 38 transverse rows of mature teeth.
L. profundior is very similar to L. scissurata , but differs from the latter in having grooves on the dorsal scales near the edge of the distal part (vs pits on the dorsal scales in L. scissurata ) and a shorter postmucronal area.
L. profundior differs from L. eernissei in having grooves on the dorsal scales near the edge of the distal part (vs smooth dorsal scales in L. eernissei )
NMNZ |
Museum of New Zealand Te Papa Tongarewa |
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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SubClass |
Neoloricata |
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Genus |
Loricella profundior ( Dell, 1956 )
Sirenko, Boris 2021 |
Loricella oviformis, Kaas 1985: 310
Kaas, P. 1985: 310 |
Loricella profundior, Beu 1967: 478
Spencer, H. G. & Marshall, B. A. & Willan, R. C. 2009: 197 |
Kaas, P. & Van Belle, R. A. & Strack, H. L. 2006: 67 |
Kaas, P. 1990: 178 |
Powell, A. W. B. 1979: 25 |
Beu, A. G. 1977: 42 |
Fitzgerald, M. L. 1969: 23 |
Beu, A. G. 1967: 478 |
Paricoplax profundior
O'Neill, M. H. B. 1987: 134 |
Dell, R. K. 1956: 157 |