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A taxonomic review of the Norwegian species of Raphitoma (Gastropoda: Conoidea: Raphitomidae)

Høisaeter, Tore

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Høisaeter, Tore (2016): A taxonomic review of the Norwegian species of Raphitoma (Gastropoda: Conoidea: Raphitomidae). Fauna norvegica 36: 9-32, DOI: 10.5324/fn.v36i0.1839, URL: https://doi.org/10.5324/fn.v36i0.1839

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9 Fauna norvegica 2016 Vol. 36: 9-32. A taxonomic review of the Norwegian species of Raphitoma (Gastropoda: Conoidea: Raphitomidae) Tore Høisæter1 Høisæter T. 2016. A taxonomic review of the Norwegian species of Raphitoma (Gastropoda: Conoidea: Raphitomidae). Fauna norvegica 36: 9-32. The problematic conoidean genus Raphitoma s.l. in inshore Norwegian waters is revised based on fresh material from all along the coast of Norway. This largely shallow water group is represented by at least six species in Norwegian waters of which two, Raphitoma obesa n.sp. and R. maculosa n.sp. are described as new, and another Raphitoma aequalis (Jeffreys, 1867) is reported from Norway for the first time. The taxonomic and nomenclatural status of R. reticulata (sensu Jeffreys 1867) and R. asperrima (sensu Forbes & Hanley 1853) are discussed. Empty shells of several additional species indicate that the number of Raphitoma-species living in the North East Atlantic will be further increased in the future. The morphological variability of each species is described if possible. Shell morphology, including microsculpture and protoconch details as deduced from LM photographs, are used for distinguishing the species. Some easily observable behaviour and soft part morphology features were found to be promising areas for further studies. doi: 10.5324/fn.v36i0.1839. Received: 2015-02-19. Accepted: 2015-12-22. Published online: 2016-02-24. ISSN: 1502-4873 (printed), 1891-5396 (electronic). http://zoobank.org/8520BB86-9308-4775-A570-5F4FD64C68EB Keywords: distribution, Norwegian inshore waters, North Sea, morphology, taxonomic characters, new species 1. Department of Biology University of Bergen P.O. Box 7800 N-5020 Bergen Norway Corresponding author: Tore Høisæter http://www.zoobank.org/Authors/8701A4E7-5BD0-4E70-8F68-ED4E51936B2F E-mail: [email protected] INTRODUCTION Recently the troublesome taxonomy of Conoidea has been put on a firmer basis based mainly on extensive new material from the tropical western Pacific. This has led to both a detailed molecular phylogeny of the entire superfamily (Puillandre et al. 2008, 2011, Bouchet et al. 2011) and to several generic revisions (e.g. Olivera et al. 2008, Puillandre et al. 2009, 2010, Morassi & Bonfitto 2010, Fedosov 2011). One of the outcomes of this work has been that the artificial ‘family’ Turridae (sensu Powell 1966) is split into 13 monophyletic families of which the Raphitomidae is the largest and most diverse. Species from the North-East Atlantic have only sporadically been included in these revisions, regrettably, as some of the name bearing types within this megadiverse group are from this region. The North-East Atlantic deep-water conoidean species were revised by Bouchet & Warén (1980) but no corresponding revision of the inshore species in Norwegian waters has been done. The numerous Mediterranean species are under revision by Pusateri et al. (2012, 2013), and so far four species of Raphitoma have been described. The present review is an attempt at a morphologically based description of the known Norwegian species of Raphitoma as traditionally understood. With the exception of two species, Raphitoma reported from Norwegian coastal waters are rare, and little material is available for a critical review. Thirty two species of Raphitoma are listed as European in CLEMAM (2015). Two recent check lists from the Mediterranean mention 14 species from Malta (Cachia et al. 2001) and 14 from Italian waters (Spada 2008). Ten of the species are common to the two lists. Some of the species Høisæter: Revision of Raphitoma in Norwegian waters 10 MATERIAL AND METHODS This revision covers roughly the same region as defined in Høisæter (2009), i.e. the Norwegian inshore waters and shelf, but excluding the North Sea and the western ‘slope’ of the Norwegian Trench. A total of some 210 specimens and c. 220 empty shells of Raphitoma collected by the author around the Norwegian coast from 60° to 71°N between 1967 and 2008 (see Høisæter 2009) and c. 140 specimens from Nordland (67° to 68°N) and 145 from Skagerrak (58° to 59°N) collected and sorted by Per Bie Wikander, were available for study of morphological characters. A few valuable specimens donated by David Osca and Per Johannessen from the Norwegian west coast and the North Sea are included as well. In addition 35 lots of older material from the University Museum of Bergen Natural History Collections (ZMBN) have been studied. A photograph of the holotype of Defrancia purpurea var. oblonga Jeffreys, 1867 has been provided by USNM (United States National Museum Washington DC). Other abbreviations used in the text: BMNH (Museum of Natural History London); S.D. (Subsequent Designation); W/L (width to length ratio). The characters found to be most useful are: Macrosculpture (Figure 1) microsculpture (Figure 2) protoconch (Figure 3) colour pattern and sometimes, relative length of the siphonal canal. The study of conchological characters was supplemented by a few observations of crawling animals. Descriptions of shell morphology and living animals are based on photographs taken under a stereo microscope with an Olympus 4.1 Mpix. digital camera and processed in Adobe Photoshop™. All photographs (except those copied from published articles as specified in the figure captions) were taken and processed by the author. All material is deposited at ZMBN. considered valid in CLEMAM or Spada (2008) are regarded as synonyms in Cachia et al. (2001) and vice versa. The recently started revision of the Mediterranean species of the group by Pusateri et al. (2012, 2013) indicates that at least 21 species, of which four are undescribed, are living in the Mediterranean. The check list by Cachia et al. (2001) contains brief descriptions and sketchy drawings of each species and seems at present, together with the so far incomplete revision of Pusateri et al. (2012, 2013), to be the best guide to the Mediterranean members of the group. Four of the North-European species are treated in the well-known series by Fretter & Graham (1985) and Graham (1988), while useful drawings of the same four species are presented in Hubendick & Warén (1976). During a comprehensive survey of the distribution of shell bearing gastropods along the Norwegian coast (Høisæter 2009), several difficulties were encountered in identifying specimens of Raphitoma s.l. by use of standard identification guides (e.g. Graham 1988). These problems were mainly due to large variability in shell characters and apparent overlap in morphology between closely related species. Since then, more material has become available, permitting a detailed description of several Norwegian species from both living specimens and shells with intact colour pattern and protoconchs. By combining behaviour with macro-morphological and micro-morphological shell characters, I conclude that at least six species, of which two are described as new, are found in Norwegian waters. The Norwegian species of the group are compared with the British species, especially as described in Jeffreys (1867). To my knowledge this work by Jeffreys is the most recent revision of the group from the North-Eastern Atlantic. Some of my results have been suggested before but not based on such diverse material and never properly discussed in the scientific literature. Figure 1. Raphitoma spp., sculptural details. A. R. linearis (4.9 mm); B. R. cf. echinata (11.1 mm); C. R. maculosa n.sp. (7.2 mm). Scale bars = 500 µm. 11 Fauna norvegica 36: 9-32. 2016 Figure 2. Details of microsculpture of six specimens of Raphitoma. A. R. linearis; B and C. R. aequalis; D. R. obesa n.sp.; E. R. maculosa n.sp.; and F. R. concinna. Scale bars = 200 µm, except F = 500 µm. Figure 3. Raphitoma spp, protoconchs. A. R. linearis; B. R. aequalis; C. R. maculosa n.sp. D. R. concinna. Scale bar = 200 µm. RESULTS Conchological characters The macrosculpture consists of strong axial ribs crossed by spiral cords. Where these two structural elements cross each other, nodes of varying strength are created. The extremes are drawn out into pointed spikes (Figure 1B) and, at the other extreme, in modest swellings on the ribs (Figure 2F). Most species have nodes of intermediate strength (Figures 1A and C). I did not find it worth while to measure the relative length of the siphonal canal as it is usually both variable and hard to measure, e.g. Figures 11 and 23 (although rather constant for some taxa, see Figure 6). The microsculpture turned out to be rather specific for each taxon varying from a smooth silky surface (Figure 1B), a surface densely covered with tiny pustules (Figures 2B - D) to a rough, slightly wrinkled surface (Figure 2F). Shell colour pattern may be a useful character in some species, but in other species it is variable, and is anyway fading fast when the snail dies or is stored in ethanol. All Norwegian species of the genus have protoconchs with an apical whorl with ten to twelve dense spirals followed by two to three whorls with the characteristic ‘raphitomine’ decussate sculpture. The number of protoconch whorls ranges from four (Figure 3A) to a little more than three (Figure 3C, D). In some species the protoconch ends in a keel (Figures 3A, B). The apical angle varies from c. 42° (Raphitoma linearis, Figure 3A) to c. 54° (R. aequalis and R. concinna, Figures 3B, D). The diameter of the apical whorl is sometimes a useful taxonomic character (cf. Figure 3B with 3D) as is the W/L ratio of the protoconch (Figure 3D shows a protoconch wider than high, as opposed to the three others in Figure 3). TAXONOMY Conoidea Fleming, 1822 Raphitomidae Bellardi, 1875 (Type genus Raphitoma Bellardi, 1847) Daphnellinae Casey, 1904 Pleurotomellinae F. Nordsieck, 1968 Taraninae Casey, 1904 Tatcheriidae Powell, 1942 In reviewing a taxon of organisms, two types of problems must be confronted, the identification and descriptions of the boundaries between different members of the taxon, and determination of the correct names of these members, on every taxonomic level. Both of these are highly relevant for the group under study here. The intraspecific variability within many of the species makes it hard to definitely delimit the species (identify species boundaries). Neither the names Høisæter: Revision of Raphitoma in Norwegian waters 12 mainly on protoconch morphology, although a few divergent genera (i.e. Hemilienardia, Veprecula and ‘Raphitoma’ rubroapicata) included in the clade named Raphitomidae in their analysis, have multispiral protoconchs lacking the characteristic diagonally cancellated sculpture. In Bouchet et al. (2011) some 60 genera are listed as valid, including both Philbertia (with Leufroyia as a synonym) and Cenodagreutes, in addition to Raphitoma. This list has been brought up to date in Bouchet (2015), in which 67 genera are accepted, and both Philbertia and Cenodagreutes are listed as synonyms of Raphitoma. In Bouchet et al. (2011) the Raphitomidae is cited as the largest and most variable taxon in the Conoidea, and is documented by 21 shell photos, eight radula photos and five protoconchs. None of these are of the name-bearing genus, Raphitoma. In Puillandre et al. (2008, 2011), two specimens purported to belong to Raphitoma are included, none of them belong to Raphitoma s.s. Genus Raphitoma Bellardi, 1847 Type species - Raphitoma histrix Bellardi, 1847 (S.D. Monterosato 1872); Mediterranean Pliocene fossil. (See below and discussion in van Aartsen et al. 1984:88). Cordieria Monterosato, 1884, non Roualt, 1848. Cirillia Monterosato, 1884, non Rondani, 1856. Cenodagreutes E.H. Smith, 1967. Leufroyia Monterosato, 1884. Lineotoma Nordsieck, 1977, nomen novum pro Cirillia Monterosato, 1884, non Rondani, 1856. Philbertia Monterosato, 1884. Members of Raphitoma are distinguished from other genera in the family by having a small to medium sized, elongated, turreted shell with uniformly convex whorls. Pronounced reticulate sculpture of strong axial ribs and strong spiral cords. A characteristic multispiral, cancellated, ‘raphitomine’ protoconch of 3 to 4 whorls (or similar species with paucispiral protoconchs). Remarks. Northeast Atlantic species of this group have been shuttled between a host of different ‘genera’ during the last two centuries. Pleurotoma, Mangelia, Defrancia, Clathurella, Raphitoma have, at various times since the 1820ies been used for members of the group. Raphitoma was used in a wide sense by Bellardi (1847), but this usage was apparently not adopted by any of his contemporaries. Marshall (1912) settled for Clathurella, as Defrancia, preferred by Jeffreys (1867) was preoccupied. Philbertia Monterosato, 1884 (introduced by Monterosato in 1884 as a section within his new, but preoccupied, genus Cordieria) was adopted by Thiele (1929) as the most comprehensive genus-name for these species, with four subgenera and a number of sections. Raphitoma was regarded as a synonym of Mangelia Risso, 1826 by Thiele. (Curiously of the family, names of the genus or genera included, nor the names of individual species found in Norwegian waters, are satisfactorily resolved. I follow Bouchet et al. (2011) in elevating ‘Raphitominae’ to full family status, and also largely accept their scope of the group. According to the diagnosis of Bouchet et al. (2011) members of this family are variable both in shape and size, sculpture variously developed, but most typically with well-developed spiral and axial elements. Anal sinus either subsutural, shaped as a ‘reversed L’, or on subsutural ramp, very shallow to rather deep. The protoconch either multispiral planktotrophic (the majority), or paucispiral. The multispiral protoconch with spirally striated protoconch I and protoconch II with diagonally cancellated sculpture. No operculum. Radula of hypodermic marginal teeth of very variable size and morphology. Radula apparatus sometimes reduced or lacking completely. Remarks. Until recently this taxon has been known as Daphnellinae, attributed by Powell (1966) to Hedley, 1922, but by Kantor & Sysoev (1986) to Casey, 1904. Taylor et al. (1993), following Ponder & Warén (1988) attributed it to Deshayes, 1863. Bouchet & Rocroi (2005) could not find this name in any of the publications of Deshayes, and argue that the name was first used by Casey (1904), as ‘tribe’ Daphnellini. For reasons of priority, the taxon should thus be named Raphitominae, as this name was introduced by Bellardi in 1875. Bouchet et al. (2011) seem to have overlooked the fact that Raphitomidae is based on a genus with a fossil type species (see discussion below), which conflicts with their ambitions to exclude all family names that cannot be applied to a molecular clade. This complicates their classification based on molecular data, as the relationship between the fossil type of Raphitoma and the Recent species of the ‘genus’ they included in the molecular analysis has not been resolved. Thus the member of ‘Raphitoma’ (‘Raphitoma’ rubroapicata (E.A. Smith, 1871)) included in the molecular analysis on which the family concept is based, is definitely not a Raphitoma as defined by the type species, or of the clade of Recent species from the North East Atlantic recognized as Raphitoma since 1984. More recently (WoRMS 2015) this species has been assigned to Etrema Hedley, 1918, which according to Bouchet et al. (2011) is a genus in Clathurellidae. As is apparent from the abbreviated diagnosis above, the assignment of a genus to this family is anything but straightforward, and this impression is strengthened when looking at figures 7 (shells) and 8 (radula teeth) in Bouchet et al. (2011). However, as suggested by several authors (e.g. Powell 1966, Oliverio 1995, Kilburn 2009) the diagonally cancellated multispiral (‘raphitomine’) protoconch is (almost) diagnostic for the family. Inclusion of species with paucispiral protoconch is usually based on shell morphological similarity to species having multispiral protoconchs with the characteristic diagonally cancellated sculpture. The assignment should ideally be supported by other characters, e.g. type of radula or foregut anatomy or lack of operculum. The molecular phylogeny of Puillandre et al. (2011) largely support a classification based 13 Fauna norvegica 36: 9-32. 2016 included in the key and illustrated, but not treated in detail, as it is not yet verified from the region defined as ‘Norwegian’ in this work (see Material and Methods above.). Key to Norwegian members of Raphitoma. 1a. Protoconch with four whorls, microsculpture small granules or pustules or smooth ...................................... 2 2a. Microsculpture of isolated small pustules ............... 3 3a. Shell with white ground colour and purplish spiral cords. Narrow shells ..................... R. aequalis 3b. Shell completely white (or colourless). Wide shells .................................................... R. obesa n.sp. 2b. Microsculpture of small granules more or less merging together ............................................. R. linearis 2c. Shell surface smooth and glossy, macrosculpture ‘spiky’ ....................................................... R. cf. echinata 1b. Protoconch with max. 3.5 whorls, microsculpture different .......................................................................... 4 4a. Apex wide, axial ribs if present, wavy, fading away near aperture ........................................ R. concinna 4b. Axial ribs strong and regular, detectable on siphonal canal ................................................................. 5 5a. Shell with elongated siphonal canal ....................... R. maculosa n.sp. 5b. Solid shells with thickened outer lip with internal teeth .......................................... R. purpurea Raphitoma maculosa n.sp. Figures 1C, 2E, 3C and 4 - 6 http://zoobank.org/1A0C5382-5BC7-4EDE-880699054F8A5071 Murex reticulatus Renier, 1804 (Suppressed by ICZN) Defrancia reticulata, Renier - Jeffreys 1867; Friele 1874 Clathurella reticulata, Ren. - G.O. Sars 1878 Clathurella reticulata, Brocc. - Marshall 1912 Raphitoma echinata - sensuSmith & Heppell 1991; Heppell et al. 1997; Høisæter 2009, non Brocchi, 1814. Raphitoma asperrima (Brown, 1827) - Fretter & Graham 1985 [in part]; Graham 1988 [in part]; Philbertia asperrima (Brown, 1827) - Hubendick & Warén 1976 [in part]; Høisæter 1986 Type material. Holotype ZMBN 107134. Type locality. Liholmsrennen, Raunefjorden, Hordaland county, 60°18’N, 05°09’E; 70–90 m. G.O. Sars 1878 had ‘reintroduced’ Raphitoma as a name for Teretia spp). Powell (1966) interpreted Philbertia more or less in the same way as Thiele. He used Raphitoma, for only two species, the Fossil Pleurotoma hystrix de Cristofori & Jan, 1832 (cited as type species) and the Recent Clathurella pseudohystrix Sykes, 1906. Powell compared Raphitoma with the Indo-Pacific Veprecula Melvill, 1917 whose teleoconch sculpture is similar but with a different (non-raphitomine) protoconch sculpture. Powell did not directly compare his two Raphitoma species with the numerous North East Atlantic and Mediterranean species he included in Philbertia. Based on the authority of Thiele and Powell, Philbertia has been universally accepted as the common name for all European species of Raphitoma sensu Bouchet & Gofas 2015, until van Aartsen et al. (1984) decided that species with a planktotrophic protoconch needed a separate name. As Pleurotoma philberti (Michaud, 1829), the type species of Philbertia has a paucispiral protoconch, species with a multispiral protoconch should in their opinion be renamed. Van Aartsen et al. (1984) thus resurrected Raphitoma with Raphitoma histrix Bellardi, 1847, as type species. Bouchet (1990) presented convincing arguments against placing species with planktotrophic protoconchs in different genera from similar-looking species with paucispiral protoconchs. This opinion has won almost universal approval (e.g. Oliverio 1996, Rolán et al. 1998, Pusateri et al. 2012). The reasoning used by van Aartsen et al. (1984) for introducing Raphitoma as a substitute for Philbertia for the species with a multispiral protoconch is thus unnecessary. However, as Raphitoma has priority it was reintroduced as the common name for this group, almost by default (it was not mentioned in Bouchet 1990). The type species, Raphitoma histrix is a Mediterranean Pliocene fossil, originally known by a nomen nudum: Pleurotoma hystrix de Cristofori & Jan, 1832 which was the name used for the type species by Monterosato (1872). Van Aartsen et al. (1984:89) point out that this nomen nudum was validated, in a slightly different spelling, as Raphitoma histrix, by Bellardi (1847:85). However, the correct identification of R. histrix has proved to be difficult, as the several specimens figured under this name apparently represent a number of different species. The specimen figured as Raphitoma histrix by Bellardi (1847) must be considered lost (van Aartsen et al. 1984). Van Aartsen et al. proposed to accept a specimen of Pleurotoma hystrix De Cristofori & Jan, 1832, photographed by Pinna (1971) and later by Pinna & Spezia (1978) as a ‘syntype’, as lectotype for the species. This solution to the problem is based on a number of unprovable assumptions, and will have to be discussed in a wider context by Mediterranean authors. Probably the matter is best served by designating a neotype. Species descriptions Below follows a description of each of the species found in inshore Norwegian waters. One species, R. cf. echinata is Høisæter: Revision of Raphitoma in Norwegian waters 14 Figure 4. Raphitoma maculosa n.sp. Holotype, 7.2 mm long. From Liholmsrennen, Raunefjorden, 60°18’N, 05°09’E, 70–90 m. (ZMBN 107134). Microsculpture from a specimen from Bodø (Figure 6C). Scale bar = 200 µm. Figure 5. Raphitoma maculosa n.sp. Holotype 7.2 mm, photographed alive in a petri-dish. Figure 6. Five shells of Raphitoma maculosa n.sp. Shells to scale, the largest 11.8 mm. A. ZMBN 15527 (Jondal, 50–120 m); B. East of Andøya 69°17’N, 60–80 m; C. North of Store Hjartøy, Bodø 67°18.5’N, 70 m; D. Liholmsrennen, Raunefjorden, 60°18’N, 05°09’E, 70–90 m; E. Kinnarosen 60°14’N, 120–100 m. 15 Fauna norvegica 36: 9-32. 2016 present in northern Norway. The distribution outside Norway is unknown because of possible confusion with R. cf. echinata (see below). Remarks. This species was called Raphitoma echinata (Brocchi, 1814) in Høisæter (2009), based on the assumption that it was conspecific with the species given this name in several fairly recent check-lists from the British Isles (e.g. Smith & Heppell 1991, Heppell et al. 1997). The species is called Raphitoma asperrima (Brown, 1827) in other North European identification guides (Hubendick & Warén 1976, Fretter & Graham 1985, Graham 1988). The name ‘asperrima’ was first used for a ‘variety’ of R. purpurea (Montagu, 1803) by Forbes & Hanley (1853), but according to Jeffreys (1867:318), the type of Brown’s Fusus asperrimus was a shell of Trophonopsis muricatus (Montagu, 1803). This synonymy I find reasonable, based on the drawing in Brown (1827). This synonymy is also accepted in WoRMS (Gofas 2015a). The name R. echinata (Brocchi, 1814) for a British species was introduced indirectly by Jeffreys (1867), as he picked the oldest (Murex reticulatus) of several names for a complex of Mediterranean shells that he regarded as synonyms (“It is…M. echinatus of Brocchi, Pleurotoma Cordieri of Payraudeau, P. rude of Scacchi =[Raphitoma pupoides (Monterosato, 1884)]”). Murex reticulatus Renieri, 1804, was suppressed by ICZN (Opinion 316 Dec. 17, 1954) and Murex echinatus Brocchi, 1814, based on a fossil, was (on the authority of Brocchi 1814 and Monterosato 1884) introduced as a subjective synonym of the unavailable M. reticulatus. Whether the Mediterranean R. echinata is really conspecific with the British species discussed by Jeffreys, is impossible to verify until the Mediterranean species complex to which R. echinata belongs is properly revised. Jeffreys had, however, described the British species already in 1847 under the name Pleurotoma scabrum (“I described the present species (D. reticulata Renier) as P. scabrum under the impression that it was distinct from the Mediterranean shell and not merely a variety”). A photograph of a syntype of this species is presented in Warén (1980, Pl. 6, Fig. 12). Unfortunately this photograph is too small to reveal any details of the sculpture of the shell. One important detail visible is the short siphonal canal, shorter than in my specimens of R. maculosa. Combined with the description in Jeffreys (1847) and the more detailed one (for D. reticulata) in Jeffreys (1867) it is anyway possible to compare the British species with my Norwegian specimens. In 1847, Jeffreys compared his P. scabrum with R. linearis: “It differs from Pl. lineare in the volutions being more tapering, and generally in its more slender form, and in the ribs and transverse striæ being sharper and more elevated, giving the shell a scabrous appearance.” Although it cannot be completely excluded that Jeffreys’ P. scabrum is conspecific with R. maculosa n.sp., the fact that scabrum has not been used since Jeffreys listed it as a synonym of R. reticulata in 1867, argues for rejecting the name as a nomen oblitum according to the rules in ICZN. Etymology. From Latin macula, spot, stain, mark. Referring to the white spots sprinkled all over the head-foot complex. Material examined. One specimen (holotype) (70-90 m) and one shell (120-100 m) from Raunefjorden, western Norway, and one specimen (70 m) and one shell (80-60 m) from northern Norway. A shell from Bergen (ZMBN 16639) and one from Jondal, Hardanger, 50-120 m (ZMBN 15527). Description. (Based mainly on the holotype, the specimen studied alive, from Liholmsrennen, Raunefjorden, Figures 4 and 5). Max size 10.8 mm (Figure 6A). Shell fairly thick and opaque; height 2.27 to 2.47 times the diameter; apical angle 48°. Body whorl 65–69 % of total shell height. Shell colour, judging from the specimen in Figure 5 (photographed alive), with ground colour light yellowish white, with most spiral cords reddish brown on the nodules, much lighter brown on the cords between ribs. Spiral cords no. 5 and 6 from the top on the body whorl much lighter coloured than the rest. The shell has a more ‘spotted’ appearance than the other species in the genus. Protoconch (Figures 3C and 4) with 3 to 3 ½ whorls, with a coarse decussate grid and ending in a weak spiral keel. Protoconch W/L: 0.96. Protoconch colour milk chocolate brown. The 7.2 mm long specimen has four and a half teleoconch, convex whorls, with a deep and distinct suture. Sculpture consisting of numerous, slightly prosocline axial ribs crossed by spiral cords. Five or six narrow cords on penultimate whorl. The narrow axial ribs create, together with the strong spiral cords, a pattern of deep trapezoid pits wider than high (Figure 1C). Aperture narrow with a long and narrow siphonal canal, with eight spiral cords below ‘bend’ in siphonal canal (counted on dorsal side of the shell). Microsculpture not very distinct but apparently somewhat diffuse, small irregular oblong granules (Figure 4). Foot with numerous bright white spots on a more diffuse gray-white background (Figure 5). The siphon extends a long distance in front of the siphonal canal, and appears somewhat bulb-shaped in front with 30 to 40 opaque white spots on the slightly grayish background. Variability. The variability of the sculpture is well illustrated in Figure 6B and C, depicting two shells from northern Norway. The empty shell from Andfjorden (Figure 6B) has a more coarse sculpture with fewer axial ribs and fewer and stronger spiral cords than the specimen from Hjartøy just west of Bodø (Figure 6C). The available material (five shells, of which three are rather worn) does not permit a more detailed description of the shell variability. Distribution. In Norway reported (as R. reticulata) as rare from narrow inlets in the archipelago north of Bergen (around 60°35’N) (Friele 1874). Not found by Norman (1879). In my large material of shells of Raphitoma s.l. from most of the Norwegian coast, only two specimens and two shells may reasonably be referred to this species. It is thus presumably distributed from Hardangerfjorden south of Bergen to Andfjorden (69°17’N, 60-80 m; only empty shell found). The specimen from Hjartøy in Nordland (67°18’N, 60 m) indicates that it is still (1976) Høisæter: Revision of Raphitoma in Norwegian waters 16 A complicating factor is the presence in British waters of another species belonging to the same species complex, but never having been formally accepted as a separate species. This species is represented in my material by a single 11.1 mm long shell from 138 m, near Gullfaks oil field 61°05’N, on the western slope of the Norwegian Trench (Figure 7). Its main difference from R. maculosa, in addition to the very spiky ‘nodules’ is the smooth, almost satiny surface between the spiral cords, only interrupted by lines of growth. A similar looking shell from Shetland is illustrated in Fretter & Graham (1985) under the name R. asperrima (Brown). I suspect, based on the drawing in combination with their detailed description that Fretter & Graham actually used both specimens of R. maculosa n.sp. and the species illustrated in Figure 7 as basis for their R. asperrima. As Fusus asperrima Brown is accepted as a synonym of Trophonopsis muricatus (see above), the shell shown in Figure 7, needs another name. It might be a British form of R. echinata, but as this subgroup of Mediterranean Raphitoma [R. echinata, R. cordieri and R. horrida (Monterosato, 1884)] are yet to be properly revised, and their shell surface judging from available illustrations on the internet, is more porcellaneous than satiny, it might be better to choose a name based on British material. R. formosa (Jeffreys, 1867) is a candidate, but I feel it prudent to rather emphasize its similarity to one of several recent species of the Mediterranean R. echinata group (e.g. Gofas et al. 2011) as R. cf. echinata. Raphitoma aequalis (Jeffreys, 1867) Figures 2B, C, 3B and 8 - 11 Defrancia linearis var. aequalis Jeffreys, 1867:369 Cordieria (Cirillia) aequalis, Jeffr. - Monterosato 1884 Clathurella æqualis, de Monterosato - Locard 1892 Mangelia linearis var. intermedia Forbes & Hanley, 1853:472 Clathurella linearis var. intermedia F. and H. - Marshall 1912 Pleurotoma (Pleurotomoides) æqualis (Jeffreys) Monterosato - Dautzenberg & Fischer 1925 Cenodagreutes aethus E.H. Smith, 1967a:1 Philbertia linearis aequalis (Jeffreys) - Rodriguez Babio & Thiriot-Quiévreux 1974 Raphitoma aequalis (Jeffreys, 1867) - Sabelli et al. 1990; Cachia et al. 2001; Høisæter 2009 Defrancia linearis (Montagu, 1803) [in part] - Friele 1874 Clathurella linearis - G.O. Sars 1878 Philbertia linearis (Montagu, 1803) [in part] - Hubendick & Warén 1976; Høisæter 1986 Raphitoma linearis (Montagu, 1803) [in part] - van Aartsen et al. 1984 (?); Fretter & Graham 1985; Graham 1988; Smith & Heppell 1991; Olsen 1994 (?); Heppell et al. 1997 Type material. Types could not be found (Warén 1980). Holotype and one paratype of Cenodagreutes aethus E.H. Smith, 1967, in California Academy of Sciences, Department of Invertebrate Zoology, Type number 320 (holotype) and 321, see Figure 10 below. Type locality. Great Britain. Type locality for Cenodagreutes aethus E.H. Smith, 1967, off Farland Point, Isle of Cumbrae, Firth of Clyde, Scotland (55°44’N, 04°57’W) on a bottom of stones and mud in 20 m. Material examined. Around 245 specimens from 85 stations between 58° and 69°N on the coast of Norway. Description. (Based mainly on specimens illustrated in Figures 8 and 11A). The size of the specimen in Figure 8, 10.1 mm, is the maximum recorded for the species. Shell moderately narrow (height rarely more than 2.25 times the diameter). Body whorl 53 to 70 % of total shell height. Shell subfusiform with convex whorls and with deeply incised sutures. Sculpture of moderately pronounced axial ribs (costae) crossed by narrow spiral cords, six cords on penultimate whorl. The space between spiral cords two to three times wider than the spiral cords. Where the cords cross the ribs, rather low, smooth and glossy tubercles are produced. Axial ribs disappear gradually towards the base. Yellowish white to golden yellow ground colour with reddish brown spiral cords. On penultimate whorl, the sixth (or seventh) spiral cord from top often white or much lighter than remaining cords. Every second or third rib pure white in some specimens. In specimens from deeper water, ground colour usually almost white and spiral cords with much less pigment than in those from shallower water (Figures 11F and H). Aperture an elongated oval drawn out into a siphonal canal of varying length, longer in juveniles than in adults, but never as long as in equally long R. maculosa n.sp. Shallow anal sinus in outer lip near suture. Spiral cords on the siphonal canal smooth, wider and closer together than on the whorls above the aperture. Teleoconch microsculpture of fine, well separated microscopic pustules (Figures 2B, C and 8), best visible between spiral cords in upper parts or in juvenile shells. Protoconch of 3.5 to 4 (varies) light brown, convex whorls (Figures 3B and 8). Protoconch W/L: 0.97. Apical angle 50° to 54°. Apical whorl from 180 to 220 µm in diameter. Protoconch ending in a weak spiral keel. A specimen observed alive in a petri-dish (Figure 9) turned out to be rather sedate. It crawled slowly along in its preferred direction, with the siphon extending only a fraction of a mm in front of the siphonal canal. The foot is wide, tapering to a narrow point posteriorly and has distinctly recurved anterolateral corners. The foot and siphon is uniformly white. Variability. This is a variable species, both as regards colour and shape (Figure 11). The Height to width ratio varies a lot as does the length and width of the siphonal canal. The colour may be light yellowish white with scattered light brown spiral cords, or darker yellow with reddish brown cords. However the colour is fading fast in preserved specimens and thus the colours in the descriptions may not be completely reliable. The colour pattern appears to vary geographically as 17 Fauna norvegica 36: 9-32. 2016 Figure 7. A shell of Raphitoma cf. echinata 11.1 mm, from 138 m, near Gullfaks oil field 61°05’N. Figure 8. Raphitoma aequalis. 10.1 mm. From Kvæfjord in Troms county, 68°50’N, 30 m. The protoconch from a juvenile from 67°15’N and microsculpture from a juvenile from Bukkasundet, 60°15’N (Figure 11G). Scale bars = 200 µm. Figure 9. Raphitoma aequalis. A specimen photographed crawling in a petri-dish. Specimen from Hillersholmen (Figure 11D), 5.2 mm. Figure 10. Cenodagreutes aethus. Holotype, (from E.H. Smith 1967a) right, together with a specimen of R. aequalis from Grovfjord (Figure 11A). Høisæter: Revision of Raphitoma in Norwegian waters 24 Figure 18. Raphitoma purpurea. 7.1 mm long. From Hjartøysundet, 67°17.5’N, 75-64 m. Figure 19. Five shells of Raphitoma purpurea. Shells to scale, the largest 11.25 mm. A. Bergen (ZMBN 28685); B. Foldafjorden, between Gauvene and Tårnfallene, 64°40’N, 11°07.5’E, 60-20 m, shell gravel (1969); C. West of Svinøy, 64°55’N, 11°22’E, 175-20 m, shell sand; D. Lamholmen, North of Gjerdingen 64°57.5’N, 11°25’E, 30 m (1969); E. Kallnes, Lillesand, 58°15’N, 08°26’E, 8 m (1988). Figure 20. Raphitoma purpurea. A. Specimen from Pointe d’Arcouest, Bretagne, France, low tide, 11.8 mm; B. Defrancia purpurea var. oblonga Jeffreys, 1867, holotype, Jersey (original photo of holotype USNM 190029), 10.6 mm; C. Murex purpureus, lectotype, Salcombe Bay, Devon (BMNH 1995089), 15.1 mm (from Rolán et al. 1998, size corrected by Giannuzzi Savelli pers. comm.). 25 Fauna norvegica 36: 9-32. 2016 coast of France. Diagnosis. Raphitomids with broad, wavy axial ribs; dense and numerous, low spiral cords (three to four on adapical teleoconch whorl). Microsculpture of dense, rather conspicuous growth lines, or rugae, no granules or pustules. Protoconch with three or four whorls, the apical one wider (at c. 220 to 250 µm diameter) and lower than in the ‘multispiral’ species in the Raphitoma group, and with a weak, incipient rounded keel for a quarter of a whorl at the transition to the teleoconch. The characteristic cancellated sculpture covers 1½ of these whorls, while the apical 1½ whorls are covered by eight to nine punctuated spiral striae. Remarks. Leufroyia was introduced by Monterosato (1884) as one of two genera, the other being Cordieria (Monterosato, 1884), encompassing Raphitoma sensu Bouchet & Gofas 2015.The diagnosis was brief (“Gruppo ben distinto ad anfratti rigonfi, costati, spiralmente striati; bocca ingrossata internamente, levigata, senza denti nè solchi”) [“Distinct group with convex whorls, with costae, spirally striated; aperture inflated, internally smooth, without teeth or grooves”]. Most of these descriptive terms could be applied to many other species of Raphitoma s.l. However the group was well distinguished by the three species included, R. leufroyi, R. concinna (Scacchi, 1836) and R. erronea (Monterosato, 1884). Later authors have used Leufroyia both as a genus and a subgenus, but have apparently had difficulties in specifying the morphological characters distinguishing the taxon. Defined by van Aartsen et al. (1984:91) as: “...species with noncarinate, but still diagonally cancellate protoconch whorls,...”; by Campani (1999): “Protoconch multispiral of four whorls, with diagonally cancellated sculpture on at least the two lower whorls, not carinate but regularly rounded.” [translated from Italian]; and by Cachia et al. (2001:63): “Protoconch consisting of three rounded whorls, first blunt, last two cancellated, rather oblique ribs on body whorl”. In my opinion (based on the Norwegian material), the main diagnostic morphological characters are the details of the (micro)sculpture as specified above. The protoconch is certainly different from other Raphitoma species, but the number of whorls and the presence or absence of a terminal keel might be of specific rather than generic value, as evidenced by the SEM-photo in Campani (1999) of a protoconch belonging to R. leufroyi which is very similar to my R. concinna, but with four rather than three whorls, and no visible keel. A single Norwegian species is referable to the subgenus. Raphitoma (Leufroyia) concinna (Scacchi, 1836) Figures 2F, 3D and 21 - 23 Pleurotoma concinna Scacchi, 1836:12, Figure 18 (fide Cretella et al. 2005) Raphitoma concinna (Scacchi, 1836) - Rolán 1983; Sabelli et al. 1990; Öztürk et al. 2004; Høisæter 2009; CLEMAM % of total height. Siphonal canal short and wide. Sculpture on siphonal canal of thickened spirals sectioned into numerous nodules by the axial ribs. Outer lip thickened and (usually) with eleven coarse denticles on the inside. Fairly deep and narrow anal sinus. Protoconch (only conserved in the specimen from Hjartøysundet, Figure 18) short and narrow, with three whorls and apical angle 40° to 45°. Protoconch W/L: 0.97. The protoconch is smaller than in any of the other species found in Norwegian waters. Microsculpture hard to tell from old, worn shells, but appear to consist of rather coarse granulation (Figure 18). Variability. The six shells seen (Figure 19) have a fairly constant morphology. The denticulation inside the thickened outer lip is present only in mature shells, as is the secondary spiral cords on body whorl. Distribution. In older Norwegian literature reported as rare around Bergen (M. Sars according to Jeffreys 1867, Friele 1874, Norman 1879, Hubendick & Warén 1976), and from Kristiansund (Danielssen according to Jeffreys 1867). In my material three empty (old) shells from 65°N, and one fresh shell from around 67°N, in addition to a single shell from the Skagerrak coast. Also reported from Bohuslän in Sweden (Malm according to Jeffreys 1867). Around the British Isles, it occurs everywhere except on the North Sea coast. Most common in the southern part, but also found occasionally around Shetland (Seaward 1990). Elsewhere found from the Atlantic coast of France and southwards to the Strait of Gibraltar. According to Cachia et al. (2001) also in the Mediterranean at least as far east as Malta, although Monterosato (1884) and van Aartsen et al. (1984) claim that it does not occur in the Mediterranean. Not included in newer check-lists of Mollusca from the Mediterranean. Remarks. Characterized by thickened outer lip with heavy denticulation, short and narrow protoconch and very prominent tubercles where axial ribs are crossed by spiral costae. The species is reported to reach 23 mm in length (Rolán 1983), so the shells in my material are small, although the heavy teeth on the inner lip on all but one of the shells seen, indicate that they are mature. Jeffreys (1867:374) described a ‘variety’, Defrancia purpurea var. oblonga from the Channel Islands (Figure 20B above) which is distributed along the southern and western coast of the British Isles as well as the Atlantic coast of France. The ‘variety’ is accepted as a valid species, Raphitoma oblonga (Jeffreys, 1867) by Pusateri et al. 2012. Compared with the sympatric form of R. purpurea (Figure 20A) it is less solid and turreted and with significantly more ribs and cords. According to Jeffreys (1867:374) the colour and other characteristics of the soft parts are different for the two species. R. oblonga has not been recorded from Norwegian waters. Subgenus Leufroyia Monterosato, 1884 Type species. Pleurotoma leufroyi Michaud, 1828, S.D. Crosse (1885) (fide Pusateri et al. 2012). Recent, Mediterranean Høisæter: Revision of Raphitoma in Norwegian waters 26 brown cords on light background (e.g. Figure 23G). Wide variation in the H/D ratio and the relative length of the siphonal canal. A specimen studied alive (Figure 22) was, as opposed to the other three species observed alive, reluctant to extend its foot much out of the aperture. The colour appears to be clear, translucent white. Distribution. In Norway known from near Bodø, 67°11’N, 14°20’E, and southwards. Rare north of Hordaland county, but fairly common in shallow water on the western coast and apparently also on the Skagerrak coast. The northern distributional limit is based on a single juvenile in the material of Per Wikander from 1976, the former northern limit was Trondheimsfjorden (around 64°N). Seven specimens from the Skagerrak coast (1972 to 1989) in the material of Per Wikander. According to Olsen (1994) seven records from Oslofjorden in 2014; Gofas 2015bDefrancia Leufroyi Michaud - Jeffreys 1867; Friele 1874; Norman 1879 non Pleurotoma leufroyi Michaud, 1828:121 Clathurella Leufroyi, Mich. - G.O. Sars 1878 Philbertia leufroyi (Michaud) - Hubendick & Warén 1976; Høisæter 1986 Raphitoma leufroyi (Michaud, 1828) - Fretter & Graham 1985; Graham 1988; Cachia et al. 2001 Fusus Boothi Brown in J. Smith, 1839:98 Leufroyia Boothii, Brown - Monterosato 1884 Raphitoma boothii (Brown in Smith, 1839) - Olsen 1994 Raphitoma (Leufroyia) boothii (Brown in Smith, 1839) - van Aartsen et al. 1984; Smith & Heppell 1991; Heppell et al. 1997 Type material. Presumed lost (Cretella et al. 2005) Type locality. “In sinu Neapolitano et Tarentino parum frequens” (Cretella et al. 2005). Material examined. Sixty-two specimens from 31 stations from c. 58°N to 61°N on the coast of Norway. A single juvenile from Hjartøysundet, Bodø, Nordland county, 67°10.7’N, 14°20.3’E, 35 m, coarse shell gravel. Description. Based mainly on a specimen from Hillersholmen (Figure 21), 10.5 x 5.2 mm) and one from O-sundet (Figure 23C), 11.2 x 4.6 mm. Maximum size of those measured, 12.1 mm (specimen from O-sundet, Figure 23A). Shell thick and opaque; height 2.04 to 2.45 times the diameter (for shells longer than 9.5 mm), thus extremely variable (compare Figure 21 with Figure 23C). Body whorl 64-72 % (usually between 70 and 72 %) of total shell height. Shell colour variable, from dark brown to bright yellow, usually with dark spiral cords on a light-coloured background. Teleoconch whorls five (for 11-12 mm long specimens), convex with deep and distinct suture. Adapical teleoconch whorl 775-873 µm. Sculpture of numerous wide and dense axial ribs crossed by wide and low spiral cords, 12 on penultimate whorl. Distance between cords almost twice the width of the cord. Tubercles where cords cross axial ribs, low transverse swellings on ribs. Axial ribs fading out towards base, not discernible on siphonal canal. In some large shells hardly any ribs on body whorl. Siphonal canal of varying length usually short (but compare Figure 23F with 26G). Shallow and wide anal sinus in outer lip near suture. Outer lip thickened but not denticulated. Microsculpture (Figures 2F and 21) of growth lines and irregular rugae, never isolated pustules or granules. Protoconch (Figures 3D and 21) of three whorls, nine spiral rows of isolated ‘points’ on the apical 1½ whorl, the rest with diagonal diamonds as in other ‘multispiral’ species of Raphitoma. Diameter of apical whorl 225–250 µm. Apical angle 48°–54.5° (usually more than 50°). Protoconch W/L: 1.1. Protoconch colour same as teleoconch colour, usually with white apical tip (Figure 21). Radula illustrated in G.O. Sars (1878:Tab. VIII, Figure 3). Variability. A most variable species (Figure 23). Colour from dark brown to yellow, younger shells usually with dark Figure 21. Raphitoma concinna. 10.5 mm long. Specimen from Hillersholmen, 60°18’N, 8 m (1969). Protoconch from specimen in Figure 23H. Microsculpture from specimen in Figure 23J. Scale bars = 200 µm. Figure 22. Raphitoma concinna. A specimen (same as in Figure 23G) photographed alive in a petri-dish. 27 Fauna norvegica 36: 9-32. 2016 Figure 23. Ten specimens of Raphitoma concinna. Specimens to scale, the largest 12.1 mm long. A, C and E. O-sundet 60°35’N, 15–20 m (1969); B. Hillersholmen, 60°18’N, 8 m (1967); D. Hillersholmen, 60°18’N, 8 m (1968); F. Svelgen, 60°27’N, 20-10 m (2010); G. Bukkasundet, 60° 14.23’N, 05°12.33’E, c. 12 m (2007); H. Bukken, 60°14.23’N, 05°12.33’E, 15 m (2007); I. Hillersholmen, 60°18’N, 8 m (1969); J. Bukkasundet, 60°14’N, 05°12’E, 12-15 m (2007). leufroyi - Jeffreys 1867, Fretter & Graham 1985, Seaward 1990), and has been reported from the Atlantic coast of France and Spain (Rolán 1983). The species is found in the Mediterranean (described from the Bay of Naples) but according to Cachia et al. (2001) it is rare in Maltese waters. Reported from Cyprus in the eastern Mediterranean (Öztürk et al. 2004). Not reported by van Aartsen et al. (1984) from the Bay of Algeciras outside 1991-1992. In Oslofjorden only known from Drøbak in earlier literature. Reported also from Bohuslän in western Sweden (Hubendick & Warén 1976), and from the Kola inlet on the Murman coast of Russia (Nekhaev 2014:102, Fig. 10A), (this latter record however, is based on an empty shell of what appears to be Raphitoma obesa n. sp., see above). Further south in Europe it is common in British waters (as Raphitoma Høisæter: Revision of Raphitoma in Norwegian waters 28 than suspected so far. In addition the species named R. cf. echinata above will most likely be included in future reviews of the Norwegian Raphitoma fauna. Part of the reason for not attempting to formally increase the number of species belonging to the Norwegian fauna is the lack of live caught specimens. Colour pattern is often the first character used in identifying a shell, but even with living specimens this might be misleading because of variability. In shells long dead or stored in ethanol, the colours are rapidly fading. While the living snails show a distinct colour pattern with brightly coloured spiral cords (see e.g. Figure 11D and G, and Figure 16C and E), the shells having been stored for several years before being photographed, are usually more or less homogeneous in colour, e.g. uniformly yellowish or whitish (e.g. Figures 11A and B, and 16D and F). In addition to the shell colour pattern, soft part morphology and behaviour (Figures 5, 9, 15, and 22) are promising areas for further study. So far a single specimen of each of four species have been studied. The striking contrast in behaviour between the specimens of R. linearis and R. aequalis strongly support that these are separate species. Thus the specimen of R. aequalis (Figure 9) turned out to be rather sedate, moving slowly in a preferred direction. The specimen of R. linearis (Figure 15) was more ‘vivacious’, frequently and swiftly changing directions while crawling. In addition the part of the siphon of R. linearis in front of the siphonal canal is long, tubular and slightly narrower in front, while that of of R. aequalis is apparently comparatively wider but extend only a fraction of a mm in front of the canal when the animal is crawling. The foot of R. linearis (and presumably also the other three species) is deeply embayed in the mid-line, and has recurved anterolateral corners. As seen in Figure 15, the foot of R. linearis is very flexible and helps the animal to rapidly turn around if placed upside down on the substrate. No similar flexibility was observed in any of the other specimens observed. The siphon of R. maculosaalso extends a long distance in front of the siphonal canal while the animal is crawling. It is somewhat bulb-shaped in front, and have 30 to 40 distinct white spots on a slightly grayish background colour. White spots were distributed liberally over all visible parts of the head-foot complex in this specimen, as have been observed in other species of the R. echinata species complex. Protoconchs, macrosculpture, microsculpture and relative length of the siphonal canal, are useful, but variable characters for distinguishing between species. However, all of these are hard to describe in a way that is helpful for species identification. The microsculpture (Figures 1 and 2) may be the most useful of these, but sometimes even that one is hard to interprete. The transition zone between protoconch and teleoconch is sometimes a useful morphological detail to confirm the determination of a doubtful specimen. This is especially useful for distinguishing between R. aequalis and R. linearis. The latter species has two whorls of a dark purplish-brown colour between whorls of a much lighter hue. This colour difference is visible even in specimens stored for a long time in ethanol the Strait of Gibraltar. Remarks. Which name to use for this common species in the North Atlantic has been highly disputed. The North Atlantic taxon was originally named R. boothi (J. Smith, 1839), presumably without any comparison with Mediterranean relatives. Jeffreys (1867) compared British specimens with Mediterranean specimens of R. leufroyi and R. concinna. He concluded that the two were synonyms and that neither could be distinguished from R. boothi. R. leufroyi being the oldest should thus be the name to use. This decision has been adopted by most North European authors, and the species is listed as R. leufroyi in most check-lists from the region (e.g. Høisæter 1986, Graham 1988, Seaward 1990). However, authors from the Mediterranean region have not necessarily agreed. Thus Monterosato (1884) explicitly considered R. boothi to be different from R. leufroyi, and R. concinna to be a species distinct from both. In his opinion the two latter are confined to the Mediterranean, whereas the former is found only in the North Atlantic, outside the Mediterranean. Both R. concinna and R. leufroyi were reported from Ria de Vigo on the northwestern coast of Spain by Rolán (1983), R. concinna being by far the most common of the two. Van Aartsen et al. (1984) also considered all three to be specifically distinct, separating R. boothi from R. leufroyi. They did not compare R. concinna with R. boothi. Cachia et al. (2001) do not mention R. boothi, but report both R. concinna and R. leufroyi from Maltese waters. Warén (pers. comm.) has not been able to find any morphological differences between the Mediterranean R. concinna and specimens from the North Atlantic. Recently Gofas (2015b) and CLEMAM (2015) have accepted R. boothi as a synonym of R. concinna, and the latter should thus be the valid name for the North Atlantic species. According to descriptions and available illustrations (e.g. van Aartsen et al. 1984; Cachia et al. 2001 and Rolán 2005) R. leufroyi has a characteristic colour pattern and very prominent axial ribs, not found in Norwegian material. I follow the recent consensus and regard all members of the subgenus Leufroyia from the North Atlantic outside the Mediterranean to belong to R. concinna (Scacchi, 1836), and R. boothi (J. Smith, 1839) to be a subjective synonym of R. concinna. DISCUSSION Of the six species of Raphitoma described in the review, only three are relatively common in Norwegian inshore waters, and only one is common in waters north of c. 64°N. This review does not, however, pretend to exhaust the diversity of Norwegian members of the genus. Several more or less well preserved shells from the Skagerrak coast (58°-59° N) indicate that the list of Norwegian species is longer than the six species named above. Most of the shells not included belong in the R. linearis/R. aequalis/R. obesa group, but also a shell with clear affinity to the R. purpurea group but in too bad condition to be properly described, points towards a larger species pool 29 Fauna norvegica 36: 9-32. 2016 he described as new, he surprisingly did not compare with members of the R. linearis/R. aequalis complex. However, as is apparent from his detailed descriptions of shell characters as well as his holotype photographs (see Figures 10 and 17 above), C. aethus is most likely a synonym of R. aequalis, and C. coccyginus of R. linearis. It is highly unlikely that two species not previously described should be found sympatrically with the common look-alikes in 1967. This synonymy has been accepted in several recent check-lists (e.g. CLEMAM 2015, WoRMS 2015). R. linearis (or R. aequalis) was already in the 1870-ties shown to lack a radula (G.O. Sars 1878:348). G.O. Sars regarded the lack of radula to be of generic value, and suggested that R. aequalis (as R. linearis) should be generically separated from R. concinna (as R. leufroyi). More recently it has been extensively documented that species in the R. linearis complex lack radula (e.g. Sheridan et al. 1973 and Fedosov 2008). Neither G.O. Sars (1878) nor Fedosov (2008) suggested an alternative genus name for this subgroup of Raphitoma. Monterosato (1884) suggested Cirillia as name for this group, but did not refer to the lack of radula as a diagnostic character. However, Cirillia is preoccupied, and if the R. linearis complex is accepted as a genus-group taxon, it needs another name. Lineotoma Nordsieck (1977) has been suggested as a replacement name, but Cenodagreutes is older and might thus be the valid name for this group if DNA-based phylogenetic analyses should confirm that they constitute a clade of generic rank. ACKNOWLEDGEMENTS I am grateful to Per Johannessen of SAM/UNIFOB and David Osca of Museo Nacional de Ciencias Naturales, Madrid, but especially Per Bie Wikander from Grimstad, for providing important material. Louise Lindblom, Kenneth Meland and Solveig Thorkildsen of the Biodiversity Group of the Department of Biology, University of Bergen, for trying to tease out some DNA secrets of part of the material for an earlier version of the ms. Jon Anders Kongsrud at the University Museum of Bergen Natural History Collections is thanked for loan of museum material. Jean-Paul Kreps from Royal Belgian Institute for Natural Sciences donated specimens of R. purpurea from Bretagne. The late Christoffer Schander kindly read an early version and offered helpful comments. Last but not least thanks to Anders Warén for helping with literature and good advice. Riccardo Giannuzzi-Savelli and an anonymous referee provided much needed resistance, and forced me to thoroughly reanalyze my conclusions. Giannuzzi-Savelli has given much helpful advice in addition to his review of the ms. REFERENCES Aartsen JJ van, Menkhorst HP, Gittenberger E. 1984. The marine Mollusca of the Bay of Algeciras Spain with general notes on (see e.g. Figure 16F). The protoconch and transition zone of R. aequalis on the other hand has an almost uniform milkchocolate colour. Ideally types, or at least topotypes, should be studied in order to verify the names of the species treated. No type material or other extralimital museum material has been studied for this review, but the fact that the species has been described from British material and are easily distinguished from sympatric congeners, is in my opinion sufficient reason for adopting the well-known and already accepted species names: R. linearis, R. aequalis and R. purpurea for the Norwegian species. This group is sorely in need of DNA-based phylogenies, and when DNA-based analyses are produced, it might very well turn out that some Scandinavian species are different from their British counterparts. Available evidence indicates that most Mediterranean species of the genus are confined to the Mediterranean, but species of the R. linearis/ aequalis group as well as the R. leufroyi-groups are exceptions being found along the East Atlantic coast both south of and north of the Mediterranean. The acceptance of R. concinna as the name for Norwegian member of the R. leufroyi-group is partly based on this hypothesis. The material studied for this review is practically all the material ever collected from inshore Norwegian waters. A limited amount of material from deeper waters on the shelf or outer coast are listed in the MOD database (Environmental Monitoring Database [MOD https://projects.dnvgl.com/MOD/ Default.aspx?TOOL=ArtUt]). Most of this material is sorted from grab-hauls from 100 to 165 m depth, in the North Sea or on the western slope of the Norwegian Trench and thus outside the geographic area here considered part of the Norwegian faunal realm. As hinted to above, strict enforcement of the priority rules concerning the family name Raphitomidae, is not optimal. The continued use of Daphnellidae would have led to fewer taxonomic problems, as Daphnella is based on a well-known Recent species. Ideally, genera should be based on a phylogenetic analysis. The genera in common use today are mostly from a prephylogenetic era, and need confirmation from DNA-based analyses. As it is rather impractical to discard all names not yet based on a sound phylogenetic analysis, I find it acceptable to use Leufroyia as the name of a subgenus, as this is well supported by shell morphology, and has been adopted by most Mediterranean authors of check-lists. Most likely the heterogeneous subgenus Raphitoma will be split into several genus group taxa in the future, one for the R. linearis-group, one for the R. purpurea-group and one for the R. echinatagroup. Both the microand the macro-sculpture are sufficiently distinct in each of these groups to support such a splitting. E.H. Smith (1967a) argues that the lack of radula (and other peculiarities in the foregut anatomy) in at least two species from the Northeast Atlantic, justifies the erection of a separate genus, Cenodagreutes. 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