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Phylogeny of the deep-sea cirripede family Scalpellidae (Crustacea, Thoracica) based on shell capitular plate morphology.

A cladistic analysis of 23 extant species of the deep‐sea pedunculate cirripede family Scalpellidae was undertaken, based on 61 shell plate characters, and taking the Jurassic–Cretaceous scalpellomorph genus C retiscalpellum as an out‐group. The consensus tree shows progressive morphological change from basal to more derived taxa, but a derived group is marked by major morphological innovation, including 27 character state changes that permit subdivision of the family into two sharply demarcated clades – the more basal group is here placed within a redefined Scalpellinae ( A rcoscalpellum, A rcuatoscalpellum gen. nov., D iotascalpellum gen. nov., G raviscalpellum, R egioscalpellum gen. nov., and S calpellum), and a more derived group named A migdoscalpellinae subfam. nov. that shows numerous progressive trends in morphology, permitting the recognition of three genera ( A migdoscalpellum, C atherinum, and W eltnerium). The phylogeny is independently supported by a recently published multiple DNA marker‐based molecular phylogeny. The more basal Scalpellinae appeared in the Aptian (Early Cretaceous, 120 Mya), and derived Amigdoscalpellinae were already present by the Campanian (Late Cretaceous, 78 Mya), represented by C atherinum anglicum sp. nov. and A migdoscalpellum bellulum from the UK Chalk. Specialized receptacles to accommodate dwarf males in the apical interior of the scutum evolved at least three times during the history of the scalpellids. © 2015 The Linnean Society of London


INTRODUCTION
The Scalpellidae is a family of predominantly deepsea pedunculate cirripedes including approximately 250 valid species, which are currently placed in 29 genera and eight subfamilies (Young, 2007). It is considered to represent a monophyletic entity, on the basis of both morphological and molecular studies (e.g. Young, 2007;Pérez-Losada et al., 2008). The family has an extensive fossil record extending back into the mid-Cretaceous (Aptian, 125 Mya; Withers, 1935;Buckeridge, 1983).
The genus Scalpellum Leach, 1817 was used in the 19th and early 20th centuries as a broad concept, and as defined by Darwin (1851a) included pedunculate taxa possessing a relatively small number of lateral plate pairs (between four and six), encompassing all Scalpellidae and Calanticidae of current classifications. In his description of the Challenger cirripedes, Hoek (1883) included 43 species in Scalpellum, and suggested the possibility of further subdivision.
Tentative attempts to subdivide Scalpellum into groups and subgenera were begun by Pilsbry (1907) and Hoek (1907), who both used the form of the carina and the morphology of the dwarf males to characterize a number of subgenera and groups (for an exhaustive review, see Young, 1999). The genera were discussed by Withers (1953), who synonymized extensively, and the Treatise on Invertebrate Paleontology (Newman, Zullo & Withers, 1969) included just three genera in the family, which would now be considered as scalpellids: Scalpellum, Mesoscalpellum Hoek, 1907, andArcoscalpellum Hoek, 1907. The next decade saw a great proliferation of scalpellid genera: in a taxonomic account of the Antarctic cirripedes, Newman & Ross (1971) created seven new genera, and Zevina (1978a,b) added a further 22 genera, classified into eight subfamilies. Subsequently, Newman (1996) elevated three of these subfamilies to family status (Calanticidae, Lithotryidae, and Pollicipedidae), leaving eight subfamilies and 29 genera for the scalpellids.
The proliferation of new genera was commented on by Foster (1980: 523), 'The Scalpellidae have recently been reclassified by Zevina (1978a,b), who built on an earlier proposal by Newman & Ross (1971), but the classification is still more convenient than natural'. Young (1999: 186) subsequently applied cladistic analysis to the genera in order to assess the monophyly of subfamilies. He commented that, 'The characters used for supra-specific taxonomy are homoplastic, therefore forming paraphyletic subfamilies'. He also noted that the basal group Arcoscalpellinae and its constituent genera were probably paraphyletic, citing Trianguloscalpellum as an example (Young, , 1999; however, Young's 2007 review of extant scalpellids followed Zevina's generic classification in detail, although he commented on the significance of growthdependent features in scalpellid classification, which had not been taken into account in previous studies. In his papers on scalpellids, Paulo Young seldom provided generic diagnoses, an exception being Amigdoscalpellum (Young, 2007: 59). A subsequent paper by Shalaeva & Boxshall (2014) refigured Hoek's Challenger scalpellids (Hoek, 1883), provided revised generic diagnoses based on the translation of Zevina's original descriptions, and summarized points of discussion made by Young (notably the 1998 and2007 papers). A paper on the molecular phylogeny of Antarctic scalpellomorph cirripedes (Linse et al., 2013) implied the paraphyly of species assigned to Arcoscalpellum.
The present study of scalpellid plate morphology was initially stimulated by Jens Høeg, whose detailed work on scalpellid reproductive systems (Buhl-Mortensen & Høeg, 2006Yusa et al., 2011) posed important questions concerning the phylogenetic relationships of species. Recently, Lin et al. (2015) have published a molecular phylogeny of pedunculate thoracicans using multiple DNA markers. Their scalpellid phylogeny (Lin et al., 2015: fig. 3) compares well with the results obtained here from morphological analysis. In particular, this work suggested extensive poly-and paraphyly of the genera. In this paper, I undertake a systematic investigation of scalpellid plate morphology, using both articulated individuals and isolated plates, and following the procedures adopted for verrucomorphs and basal balanomorphs by Gale (2014b) and Gale & Sørensen (2014), respectively. Polarity is identified from the use of the Cretaceous scalpellomorph genus Cretiscalpellum as an out-group (see discussion below).

SPECIMENS
Twenty extant scalpellid species were selected in order to represent a significant part of the diversity of the group (Table 1); only fully grown specimens were used. Specimens were cleaned with hypochlorite, and both entire specimens and isolated, cleaned plates were photographed with either a USB camera (Veho 100) or an margin of the rostrolatera. The aperture, which permits extension of the cirri and penis, extends from above the scutal adductor to the apex of the terga.
There is a marked difference between large scalpellids that possess a thick, pilose cuticle (Young, 2007) and the smaller group, which have a thinner cuticle.
Additionally, the smaller group have proportionately thinner, more delicate plates.
Growth in most thoracican plates extends outwards from the umbo in an arc determined by the angles of the sides of the plate; in the carina, this is usually a relatively low angle, but in the scuta of forms such as Zeugmatolepas (Zeugmatolepadidae) with central umbones it can approach 180°.
In many neobalanomorphs, wall plates grow both basally and apically, by the development of lateral extensions from the parietes called alae and radii (Darwin, 1854;Otway & Anderson, 1985;Anderson, 1994;Gale & Sørensen, 2014), which are sharply demarcated by an upward turn in the growth lines. This was called diametric growth by Anderson (1994), and it serves to permit expansion of the orifice with growth.
A similar plate-growth strategy is present in many scalpellomorphs (Calanticidae and Scalpellidae), in which outgrowths from the plate margins adjacent to the umbo develop, initially as a low shelf that may extend apically above the umbo, or laterally on one or both sides of the plate (Fig. 5). The growth strategy is well illustrated by the ontogeny of Scalpellum stearnsi Pilsbry, 1890 (Fig. 5A-G), in which apical extensions (green) appear initially on the inframedian latus and progressively enlarge (Fig. 5B-G); concomitantly, the intraparietes on the carina enlarge, and eventually displace the carinal umbo to a subapical position (Fig. 5F, G). Extensions on the upper latus form an inverted V-shaped structure (Fig. 5F, G); finally, a prong-like extension develops on the scutum in the fully grown form (Fig. 5G).
These structures were called 'subepidermal secondary flanges' by Foster (1978). The surface of this shelf is marked by stepped growth lines, different from those on the rest of the plate (e.g. green area in Fig. 5H), and the umbo becomes subapical in position as a result. This growth mode is here called polymetric growth, and it probably developed as an effective means of infilling spaces in the tessellation of plates that make up the flattened box-shaped capitulum of groups such as scalpellids. A change in shape of any one plate would necessitate concomitant change in other plates in order to infill the resulting spaces in the tessellation.
Polymetric growth also provides important phylogenetic information. The shelf-like outgrowths with well-demarcated growth lines were initially encased in epidermal tissue, but subsequently became part of the external surface of the plate, flush with the rest of the surface, and the two sets of growth lines became incorporated into a single pattern. This is exemplified by R. regium and related species, in which a short, well-demarcated polymetric shelf is developed on the upper latus margin of the carinal latus (Figs 6P, 10J). In Arcoscalpellum michelottianum, Arcoscalpellum sociabile (Figs 2C, D, 6F, K, P), and all more-derived scalpellids this has become a wing-like extension of the carinal latus, which contacts both the upper latus and carina. The degree of demarcation and sculpture of these polymetric structures thus provides some evidence of the level of derivation from an ancestral state, which can be illustrated with carinae of the Cretaceous genus Virgiscalpellum Withers, 1935. Lessderived taxa possess clearly demarcated intraparietes, on which closely spaced growth lines run parallel with the tergal margin (Virgiscalpellum sp. nov; Fig. 5J, K); in the derived Virgiscalpellum beisseli (Bosquet & Müller, 1857), a sculpture of radial ribs extends seamlessly across the entire carina (Fig. 5L, M). Similar progress can be seen on the upper latus of W. stroemii (Fig. 5I), in which the upper region represented by the shelf in Figure 5H has an identical growthline pattern and sculpture to the remainder of the plate.  Collins, 1974, pl. 11, fig. 10, NHMUK In. 61368). Q, tergum (original of Collins, 1965, pl. 90, fig. 12, NHMUK In. 64259 (NHMUK In. 3440). Note the difference in surface sculpture between the external surface and the outgrowth. C, inframedian latus, Weltnerium nymphocola (Hoek, 1883), in which the polymetric portion of the plate (green) is flush with the rest of the plate, and has an identical sculpture. D, E, carina of Virgiscalpellum sp. nov., upper Campanian, Keswick Pit, Norwich, Norfolk, UK (Wood, 1988), to show polymetric intraparietes (green), which differs in sculpture from the parietal and tectal surface. F, G, carina of Virgiscalpellum beisseli (Bosquet and Müller, in Bosquet, 1857), in which the tectum, parietes, and intraparietes all have an identical sculpture of coarse radial ribs. Same locality. Scale bars: A, 5 mm; B-G, 1 mm.  Table 1 for details of localities. Note the migration of the position of the carinolatus umbo from apical to nearly basal, the progressive incurvature of the umbo, and the development of an upper latus surface. The lower four species are assigned to the Scalpellinae, the uppermost one to the Amigdaloscalpellinae. Scale bars: A-E, J, K-T, Y, 1 mm; F-I, U-X, 0.5 mm.

Terga
The terga underwent significant change during the evolution of scalpellids.

Rostrum
An unpaired, symmetrical rostrum is present in all thoracicans crownward of the Carboniferous Praelepas (Newman et al., 1969), with the exception of the Lepadidae. Although it is absent in a few scalpellids (e.g. , all of the taxa in the present study possess a rostrum, albeit sometimes a tiny one. In the out-group Cretiscalpellum (Figs 4D, F, 10A) the rostrum is triangular, slightly broader than tall, possesses a triangular raised central ridge, and lateral triangular wing-like processes (ls), which are overlapped by the rostrolatera. In scalpellids rostra fall into three categories: (1) broad, trapezoidal-triangular forms, with a subumbonal surface, broadly similar to those in the out-group, and a large triangular external surface (Arcoscalpellum michelottianum, Fig. 11I; Arcoscalpellum sociabile, Fig. 11E; D. rubrum, Fig. 11Q; R. regium, Fig. 11M); (2) tiny, oval-rhomboidal rostra, in which the external surface is limited to a small apical region (Am. rigidum, Fig. 12Q; Am. truncatum, Fig. 11A; Ca. novaezelandiae, Fig. 12I; Ca. striolatum, Fig. 12M); (3) rectangular-trapezoidal forms with a flat external surface that extends over the height of the plate   Table 1 for details of localities. Note the overall progression of morphological change from left to right in the shape of the scutum, with the basal-occludent angle becoming more acute, and the basal-upper latus angle more obtuse, leading to a more trapezoidal outline. Additionally, a small tergal surface develops, and the umbo becomes incurved, and the dwarf male receptacles become larger and better defined. The terga change from an ovalrhombic outline (I) to a right triangular one (J-L), the ventral margin has developed a narrow supracarinal surface (scs), with an inflexion where the tip of the carina rests against the carinal margin. See Table 1

Rostrolatus
The rostrolatus imbricates the rostrum on its ventral margin, and its upper margin shallowly overlaps the base of the scutum (Fig. 1B, C); its median margin articulates with the inframedian latus, and the basal margin contacts peduncular scales. A transverse ridge runs from the umbo to the angle of the basal margin and inframedian latus margin (Fig. 10G, H). The rostrolatera in scalpellids fall into two well-demarcated morphological groups: (1) a basal group in which these are broad, low, and gently concavo-convex, and in which the concave facet for rostral articulation extends over the height of the plate ( Fig. 11E-T); (2) a more derived group in which the plates are subrectangular to subtriangular, only slightly broader than tall, in which the rostral articular surface forms a short triangular  (Aurivillius, 1898), with a shallow V-shaped depression. Catherinum novaezelandiae (Hoek, 1883) has a deep, sharply defined receptacle in an apical position. Position of dwarf male receptacles/attachment sites indicated. See Table 1 for localities for extant taxa. Scale bars: B, 5 mm; A, 1 mm; and C, D, 0.5 mm.
▶ Figure 10. Homologies of scalpellid plates: A, Cretiscalpellum striatum (Darwin, 1851b), rostrum; B, E-G, J, K, Regioscalpellum regium (Thomson, 1873); C, H, I, Amigdaloscalpellum rigidum (Aurivillius, 1898); N, O, R, Amigdaloscalpellum truncatum (Hoek, 1883); C, Weltnerium stroemii (M. Sars, 1859); P, Diotascalpellum rubrum (Hoek, 1883). Arcoscalpellum sociabile (Annandale, 1905), L, M. A-D, ventral view of rostrum, lateral process that articulates with interior of rostrolatus is coloured brown. Note shape changes, from triangular-trapezoidal (A, B), to oval-rhombic (C), to triangular with large flat exterior face (D). E-I, rostrolatera. E-G, plesiomorphic broad, low morphology, with tall concave articular facet for rostrum (brown). H, I, derived condition, in which the pair of triangular plates have a long ventral articulation, the small rostrum is largely internal, and the rostral articular surface extends over only half the height of the plate (brown in I, rs, see also Figs 1C, 11). J-P, carinolatera. P, plesiomorphic condition, in which a low flange (olive green) overlaps the upper latus. J, L, development of the upper latus surface (blue), from a polymetric flange in (J), which extends in all more-derived taxa to become a tall surface (e.g. K; see also Figs 6, 7). K, M-O, interior of carinolatus, with carinal surface coloured pink, and lateral surface coloured lime green. In the plesiomorphic condition, the lateral surface is external (J), but this becomes internal (M) and the paired carinolateral articulate at the base. In the derived condition (N, O), the lateral surface has developed three ribs with intervening grooves that interlock with those on the opposing plate (e.g. Fig. 6E). A flat articulation surface (mauve) has also developed. Q, R, interior of carinae, to show articular surfaces for carinolatus. Figure 11. Evolution of rostra and rostrolateral plate morphology, ventral side: A-D, Amigdoscalpellum truncatum (Hoek, 1883); H, Arcoscalpellum sociabile (Annandale, 1905); I-L, Arcoscalpellum michelottianum (Seguenza, 1876); M-P, Regioscalpellum regium (Thomson, 1873); Q-T, Diotascalpellum rubrum (Hoek, 1883). Rostrum in ventral (rostral) aspect (A, E, I, M, Q); rostrolatus in external (C, G, K, O, S) and internal (B, F, J, N, R) views. Basal capitulum in ventral (rostral) aspect (D, H, L, P, T). Note similarity of plesiomorphic taxa (E-T), in which the rostrolatus is broad and low, and the rostrum is trapezoidal to triangular and chunky. The rostrolatera do not contact over the midline in these taxa. Note striking morphological differences in the more derived Amigdoscalpellum truncatum (A-D), in which the rostrolatus is narrower and taller, the plates meet over the midline, and the rostrum is tiny, tall, rhomboidal, and almost completely covered by the rostrolatera. The rostral articulation only extends over half of the rostrolatus (see also Fig

Upper latus
The upper latus infills the space between the scutum and tergum in basal scalpellomorphs, and slightly overlaps both plates (e.g. zeugmatolepadids, see Gale, 2014a: fig. 9). In Cretiscalpellum (Fig. 4A) and basal scalpellids (Fig. 2), the plate is overlapped by the carinolatus, and in all scalpellids the upper latus has developed a margin in contact with the carina, which is of variable height. In Arcoscalpellum michelottianum (

Inframedian latus
The inframedian latus rests between the subcarinolatus and the rostrolatus in Cretiscalpellum (Fig. 4A), and is overlapped by the subcarinolatus but overlaps the rostrolatus. In scalpellids, the inframedian latus slightly overlaps both the rostrolatus and the carinolatus plesiomorphically ( Fig. 2), and has no specialized contact with the upper latus, although it abuts this plate in Arcoscalpellum michelottianum (Fig. 2C). The basal scalpellid inframedian latus is low, triangular, and the umbo is slightly inclined towards the rostrolatus (Figs 2, 6H, I, M, N, R, S, W, X). In a more derived group, including Am. mamillatum (Fig. 3G Fig. 7C, E). The inframedian latus has an hourglass shape, with an expanded base and minimum width at the level of the umbo in Ca. novaezelandiae and Ca. striolatum (Fig. 7R, M). The growth of a polymetric shelf adjacent to the umbo and contacting the rostrolatus (Fig. 6G, H) is seen in Arcoscalpellum sociabile, and is developed further in fossil Arcoscalpellum (Fig. 5B). The shape and umbonal position of the inframedian latus have been used extensively in the taxonomy of scalpellids by Zevina (1978aZevina ( ,b, 1981, as discussed below in the systematic section.

Carinolatus
The carinolatera of scalpellids are highly diverse in shape, umbonal position, and in the presence and nature of articulation between the paired plates, the carina, upper latus, and inframedian latus. These features have not been discussed in any detail in previous studies, but because they evidently afford important phylogenetic information they are described more comprehensively here. The out-group Cretiscalpellum possesses two pairs of plates in the position of the carinolatus: an upper pair, usually rhomboidal in outline (Fig. 4I), and a lower pair (subcarinolatus of Withers, 1935: fig. 29), which are nearly equilaterally triangular (Fig. 4J), and overlap the subcarina. It has been presumed that the subcarinolatera were subsequently lost in evolution, together with the subcarina (Withers, 1935), because lower latera, including the subrostrum, are widely developed in more basal scalpellomorphs and are not present in scalpellids; however, the close similarity in shape between the subcarinolatus of Cr. striatum (Fig. 13Q, R) and the carinolatus of the Cretaceous scalpellid species Arcuatoscalpellum arcuatum (Fig. 13O, P) raises the possibility that these are actually homologous plates. Because of this uncertainty, the carinolatus of the late Early Cretaceous Arcuatoscalpellum arcuatum is taken as representing the plesiomorphic condition for scalpellids. This provides an essential indication of polarity, and the succession of taxa illustrated in Figures 6, 7, and 13 (bottom to top) are interpreted as representing a phylogenetic trend towards a more derived carinolatus morphology.

Group 3
In Arcoscalpellum michelottianum (Figs 2C, 6K, L, 13D, E), Arcoscalpellum quadratum (Dixon, 1850) (Fig. 13F), and Arcoscalpellum sociabile (Figs 2D, 6F, G) the internal flange has become an external upper latus surface (uls, blue coloured in Fig. 10L), the upper margin of which contacts the upper latus. The internally directed part of the flange has become a carinal margin (cm), which contacts the sides of the carina. At the same time, the umbo has become more strongly enrolled (Fig. 6F) and the dorsal margin more convex. The lateral surface of the carinolatus (green in Fig. 10M) has become inturned onto the interior of the plate, and the base of this contacts the base of the opposing carinolatus of the pair.
The shape and relationships of the carinolatus present in group-3 species such as Arcoscalpellum sociabile are essentially similar to those of all more-derived scalpellids (Figs 6A-E, 7), all of which possess a carinal margin, a tall upper latus surface, an enrolled umbo, and articulation between the pair of carinolatera. The most important modifications involve the nature of this articulation. In Am. truncatum (Figs 6B, E, 10O) and Am. rigidum (Fig. 7V, X) there is a flat articular contact between the pair (purple in Fig. 10O), and the lateral surface is modified into three ridges and grooves that run from the umbo, and interdigitate (Figs 6E, 7X) over the plane of contact. In Ca. striolatum the ridges oppose (Fig. 7S), whereas in Ca. novaezelandiae (Fig. 7N), W. nymphocola (Fig. 7F, I), and W. stroemii (Fig. 7B, D) the articular facet has rotated to a vertical position, forming an inner, taller articulation (Fig. 7D, I, N), and the umbones form a separate, shorter articulation. In some taxa, a separate carinal surface forms on the carinolatus adjacent to the carinal margin (e.g. Ca. novaezelandiae, Fig. 7K).

Peduncle
The peduncle of extant scalpellomorph cirripedes is made up of columns of plates that form at the boundary between the peduncle and the capitulum, usually after the full compliment of capitular plates have been added (Newman & Ross, 1998;Young, 2001). This is true in all taxa that have been studied, with the exception of the scalpellid Scalpellopsis (Young, 2001), in which peduncular plates are added before the final laterals. Thus, the youngest plates are usually found at the contact with the capitulum. The plates in scalpellids are added alternately in two series, sc-l-sr and rl-cl, which correspond with the eponymous capitular plates. Plesiomorphically, eight columns of plates are present (Newman & Ross, 1998;Young, 2001), but some scalpellids have a reduced number, and calanticids and pollicipedids have generated a very large number of small plate rows (Young, 2001). In the taxa studied here, eight columns are present in all but Am. truncatum and Am. rigidum, in which seven columns are present.

CLADISTIC ANALYSIS
Extant calanticids are unsuitable as an out-group for the Scalpelllidae, because their capitular plate development is highly variable, with 15-60+ laterals developed in various taxa (Jones & Hosie, 2009). Additionally, although they have long been classified as falling within (Zevina, 1981) or close to the scalpellids, molecular analysis places the calanticids as sister group to all extant thoracicans except Ibla, thus rather far removed from the Scalpellidae (Pérez-Losada et al., 2008). The genus Cretiscalpellum Withers, 1922 is abundant in the later Cretaceous (Albian-Maastrichtian), and first appears in the Late Jurassic (Tithonian; Gale, 2014a). Although sometimes classified as a calanticid, the valve morphology is very similar to that of basal scalpellids in overall form and sculpture ( Fig. 4; Buckeridge, 1983). Cretiscalpellum differs from scalpellids in its possession of paired subcarinolatera and a subcarina (Withers, 1935), and probably gave rise to scalpellids by the loss of these plates. It is therefore used as an out-group to the Scalpellidae. The highly derived and autapomorphic genus Scalpellum was not included in the analysis (see below).
Heuristic analysis of 23 extant species using 61 characters in PAUP (Appendix S1; Table S1) yielded a consensus tree (Fig. 14) that provides a clear and wellsupported picture of scalpellid phylogeny, forming a ladder of nested groups leading crownwards from the out-group to the most derived forms (nodes numbered 1-15). Although the changes superficially appear to represent a continuous morphocline, the introduction of synapomorphies is actually concentrated at three nodes, which represent major evolutionary steps in plate morphology. The most basal of these, node 6, involves 27 character changes, and with 100% bootstrap support is positioned at the base of a derived group that includes Amigdaloscalpellum, Catherinum, and Weltnerium, included in Amigdoscalpellinae subfam. nov. (see below). Within this group, significant changes occur at the base of a clade including Catherinum and more derived taxa (node 9, nine changes, 97% bootstrap support), and at the base of Weltnerium (node 11, 11 changes, 99% bootstrap support). Weltnerium includes the morphologically most derived scalpellids, which also show highly specialized reproductive strategies (Buhl-Mortensen & Høeg, 2006. The morphological tree derived here (Fig. 14) shows numerous similarities with the molecular phylogeny of Lin et al. (2015: fig. 3), although many taxa are different to those used in the present study. Group A corresponds exactly with the Scalpellinae as defined here, and group B corresponds with the Amigdaloscalpellinae (see Systematic Account, below). Secondly, within group B species referred to Weltnerium are the most derived, and species referred to Amigdaloscalpellum are the most basal, exactly paralleling the morphological analysis (Fig. 14). Group C (subgroup of group A) of Lin et al. (2015: fig. 3) is divided into two groups, one including Arcoscalpellum hirsutum (Hoek, 1883) and Arcoscalpellum michelottianum, the other including R. regium, corresponding precisely with the generic classification proposed here. In the molecular tree, Scalpellum is positioned within the other (unlettered) subgroup of group A, together with species here assigned to Diotascalpellum gen. nov. and Graviscalpellum. In the present study, G. pedunculatum occupies a more derived position within the Scalpellinae (Fig. 14).
The major difference between the trees derived from morphological and molecular analysis lies in the topology of the trees; the morphological data generate a tree that is a 'ladder' in which taxa have a sequential nested arrangement, leading progressively from the most plesiomorphic to the most apomorphic species (Fig. 14). In contrast, molecular analysis provides a branching 'tree', in which subgroups are rather sharply defined (Lin et al., 2015: fig. 3). The potential significance of these differences must await further study.

EVIDENCE FROM THE FOSSIL RECORD
The foregoing account provides evidence to support a scalpellid phylogenetic tree that represents a morphocline leading from least-derived taxa (closest to the out-group) through to the most-derived forms, such as W. nymphocola, which is both morphologically and reproductively very highly modified. It is now also possible to place fossil scalpellid taxa in this tree, in order to provide a minimum date for individual nodes on the cladogram (Smith, 1994). The Scalpellidae have an abundant fossil record in the Cretaceous and Cenozoic (e.g. Withers, 1935Withers, , 1953Collins, 1973;Zullo, 1990;Harzhauser & Schlögl, 2012), but all taxa described have been referred to three genera: Scalpellum (Eocene-present day), Arcoscalpellum (Cretaceouspresent day), and Virgiscalpellum (Late Cretaceous). It is therefore important to reassess the affinities of fossil scalpellids in the light of both the classification of Zevina (1978aZevina ( ,b, 1981 and the modifications proposed in this paper. Fossil taxa assigned to Arcoscalpellum Hoek, 1907 In his monographic treatment of Cretaceous Cirripedia, Withers (1935) referred most fossil species that would now be considered as scalpellids to either the genus Arcoscalpellum or the very distinctive Cretaceous genus Virgiscalpellum Withers, 1935 (Aptian-Maastrichtian). He referred a single species, Scalpellum glauerti Withers, with a bifid tergum, to Scalpellum (Neoscalpellum), which was subsequently assigned to a new genus, Pachyscalpellum Buckeridge, 1991. Withers (1935 split Cretaceous Arcoscalpellum into three groups (A. arcuatum Gp, A. fossula Gp, and A. maximum Gp), based on numerous plate characters, most notably of the carina. Zullo (1990) supported this division, and identified Arcoscalpellum conradi (Gabb, 1876) from the eastern seaboard of the USA as a Palaeocene descendant of the Arcuatoscalpellum fossula group, thus extending Withers' classification into the Cenozoic.
It is now possible to integrate Withers' (1935) fossil 'Arcoscalpellum' groups into the classification proposed here for extant basal members of the Scalpellidae (see below), based largely on the detailed comparative morphology of the carinolatus and its articulation with the carina and upper latus.
1. Arcuatoscalpellum gen. nov., for the Arcoscalpellum arcuatum group of Withers (1935). Cretaceous, Albian-late Maastrichtian (Fig. 4N-S). This represents the plesiomorphic condition for scalpellids, and displays significant similarities with the outgroup, including the divergently striated sculpture, the overlap between the carinolatus and upper latus, and the median ridge on the carina (Fig. 4C). 2. Diotascalpellum gen. nov., based on the living Scalpellum diota Hoek, 1907 (for an extended redescription, see Chan, Prabowo & Kwen-Shen, 2009), and including the Arcuatoscalpellum fossula group of Withers (1935). These forms are distinguished by the presence of a well-defined inframedian latus surface on the carinolatus, and minor overlap of the carinolatus over the upper latus (Figs 13K-O, 18A-G). 3. Regioscalpellum gen. nov., based on the living cosmopolitan Scalpellum regium Thomson, 1873, and including the Arcuatoscalpellum maximum group of Withers (1935). These forms are characterized by the presence of a crescentic polymetric shelf on the carinolatus adjacent to the upper latus. The overall morphology is remarkably similar in Cretaceous and living forms (e.g. Fig. 13G, H, R. regium; Fig. 18N (Hoek, 1883) and Arcoscalpellum quadratum (Dixon, 1850) from the Eocene.
It is interesting to note that Withers (1928) identified the presence of an apical, internal pit for complemental (dwarf) males in a Cretaceous scutum, which he subsequently described as Arcoscalpellum bellulum Withers, 1935 from the upper Campanian chalk of Norwich, UK. The morphology of the pits and the shape of the two known scuta, and the distinctive, even striation of their exterior, justify referral to the living genus Amigdoscalpellum. Arcoscalpellum turinensis Withers, 1953, from the Miocene close to Turin, Italy (Withers, 1953), is also referred to Amigdaloscalpellum.
Processing large quantities of upper Campanian chalk from various localities close to Norwich, Norfolk, UK, has yielded a suite of small and fragile scalpellid valves (scuta, terga, carinae, and carinolatera; Fig. 19C-K, N-Q, T, V), which are closely comparable with those of extant species of Catherinum, and are described below as Catherinum anglicum sp. nov. Distinctive characters include the incurved, acuminate apex of the scutum, and the large dwarf male receptacle. Additionally, Arcoscalpellum singletoni Withers, 1953 from the Miocene of Australia can be referred to Catherinum.

Morphology and origin of Scalpellum
Morphologically, the genus Scalpellum Leach, 1817 is a very distinctive form, in which the capitulum is broad, the umbones of the carina and scutum are subapical, the umbo of the carinolatus is basal, and the carinolatus typically has the form of a laterally projecting horn, recurved in some species (Fig. 15). Additionally, the inframedian latus is broad with a basal umbo, and the upper latus has a subapical umbo. Material of the genus was not included in the cladistic analysis because the species are so strongly autapomorphic. Four extant species were placed in the genus by Zevina (1981), namely Scalpellum scalpellum (type species), Scalpellum typicum Broch, 1947, Scalpellum stearnsi Pilsbry, 1890, and Scalpellum gibbum Pilsbry, 1907. Two of these are considered here: the widespread Indo-Pacific S. stearnsi (Chan et al., 2009; Fig. 15A, E, H, L-P, herein) and the north-west European S. scalpellum (Southward, 2006; Fig. 15B-D, F-K, herein). It is noteworthy that Withers (1953) described numerous fossil Scalpellum from the Eocene to the present day (see also Harzhauser & Schlögl, 2012).
Scalpellum has been placed in the Scalpellinae Pilsbry, 1907 by Zevina (1981), together with Pteroscalpellum, Barbascalpellum, Compressoscalpellum, and Ornatoscalpellum. This group was defined principally by the presence of a strongly bowed carina with a subapical umbo and the low umbo on the inframedian latera. It is evident that the subfamily is paraphyletic, because W. stroemii is shown here to represent a parallel development (Fig. 14).
The ancestry of Scalpellum was traced by Withers (1953) to the genus Arcoscalpellum, in the Eocene, based partly on study of the ontogeny of S. stearnsii, and also on the distribution and morphology of fossils. Withers (1953: figs 13-18) illustrated the ontogeny of S. stearnsi: young S. stearnsi strongly resemble Arcoscalpellum, and up to a capitular height of 6.4 mm, the only plate with a subapical umbo is the inframedian latus. The bowed, subapical carinal umbo is present at a capitular height of 8.5 mm, but the subapical scutal umbo and the distinctive apical extension of the scutum developed last. Withers (1953: 15) remarked that, 'it is evident that species included in Scalpellum s. str. were derived late from the Arcoscalpellum stock . . .' The morphology of the rostrum and rostrolatus in Scalpellum certainly support a more basal position for the genus within the Scalpellidae. The rostrum is trapezoidal in outline, with a large subumbonal surface (Fig. 15E, F), and is similar in form to that in Arcoscalpellum michelottianum (Fig. 11E). The rostrolatera are broad, low, and gently concavoconvex in both Scalpellum and basal scalpellids (compare Figs 11F, G and 15L, M).
There is now additional morphological and fossil evidence to support Withers' claim, in the form of a stratigraphical succession of species leading from the early Eocene Arcoscalpellum quadratum (Dixon, 1850), through Arcoscalpellum venablesi Withers, 1953 [both from the Lower Eocene (Ypresian) London Clay of Bognor Regis, UK], on to Scalpellum fischeri Bertrand, 1891 from the Middle Eocene (Lutetian) Calcaire Grossier of the Paris Basin (Figs 16, 17). As Withers (1953) remarked, the latter species is close to the extant S. stearnsi.
There is progressive change in morphology between these three species. The scutum (Fig. 16A, B, G, H, M, N) becomes progressively more elongated and narrow apically, and gradually develops the pointed process apical to the umbo that is characteristic of Scalpellum. The tergum (Fig. 16C, I, O) changes from a rhombic to triangular form, and the carinal margin becomes more concave. The apical part of the carina develops a shelf beneath the umbo in Arcoscalpellum venablesi (Fig. 16J-L), which becomes more apically extended in S. fischeri, as the umbo adopts a subapical position ( Fig. 16D-F). The lateral plates also display significant changes (Fig. 17): the rostrolatera in Arcoscalpellum quadratum (Fig. 17M, N) are similar to those found in many basal scalpellids (see Fig. 11F, G, J, K, N, O, R, S), with a broad, low outline and a concave facet for articulation with the rostrum on the interior. In Arcoscalpellum venablesi (Fig. 17H, I), the plate has broadened, and the rostral surface has become elongated and flat, as in Scalpellum (Fig. 17B, C). The  umbo of the carinolatus progressively develops a recurved, horn-like process (Fig. 17E, K, P), and the inframedian latus becomes progressively more flattened, and the umbo positioned more basally (Fig. 17D, J, O).
The stratigraphical age of Arcoscalpellum venablesi, of approximately 50 Mya, pre-dates the oldest reliable record of Scalpellum, S. fischeri, from the Middle Eocene (Lutetian) Calcaire Grossier, of the Paris Basin, at 47 Mya ( Fig. 16A-F; Withers, 1953). There is therefore both morphological and stratigraphical support for the hypothesis that Arcoscalpellum venablesi represents the evolutionary origin of Scalpellum, and that the genus was derived from Arcoscalpellum; thus, it is a basal scalpellid. The subfamily Scalpellinae (sensu Zevina, 1981) is subsequently polyphyletic.

DISCUSSION
Cladistic analysis of shell plate morphology (61 characters used; Fig. 14) for 23 extant species of scalpellids, belonging to eight genera, used the Cretaceous genus Cretiscalpellum as an out-group. This has provided the first phylogeny of the family, which broadly supports the suggestion of  that large species assigned by Zevina (1981) to Trianguloscalpellum, in which all plates possess apical umbones, are likely to occupy a basal position. The tree (Fig. 14) demonstrates a clear morphological progression from basal forms, here assigned to the new genera Diotascalpellum gen. nov. and Regioscalpellum gen. nov., through Arcoscalpellum, to species of Amigdaloscalpellum, and on to Catherinum. The most derived clade includes forms assigned by Zevina to Weltnerium, Tarasovium, and Ornatoscalpellum. The morphological progression is shown pictorially in Figures 7-9 (carinal side) and 11-12 (rostral side), from the bottom to the top of the page. Although these illustrations should not be taken as a real phylogenetic succession, they serve to illustrate the progressive morphological modifications that took place during the evolution of the family. The most important of these are described below.
1. Migration of the umbo of the carinolatus from an apical to a nearly basal position (Figs 6, 7), associated with incurvature of the umbo and shortening of the lateral margin. This all occurred in the basal (pre-Amigdoscalpellum) part of the family. 2. Formation and progressive enlargement of an upper latus surface and elongated carinal margin on the carinolatus (Figs 6, 7), also during early evolution. 3. Development of an articulation between opposing carinolatera, which evolved interpenetrant ridges (e.g. Figs 6E, 7X), then later developed a double symmetrical articulation (Fig. 7D, I, N). 4. Change in shape of the inferior median latus from a triangular, through rectangular, to pentagonal outline (Figs 6, 7), accompanied by basal migration of the umbo and development of an articulation with the scutum. 5. Dramatic changes in the size and shape of the rostrum, from a basal subtrapezoidal-triangular form of equal height to the rostrolatera, to a small, oval elongate form half the height of the rostrolatera (Figs 11A, 12I, M, Q). In the most derived condition, the rostrum developed a triangular, smooth external face (Fig. 12A, E). 6. Accompanying (correlative changes) in the rostrolatera, which plesiomorphically are broad and low (Fig. 11F, G, N Withers, 1953, pl. 26, fig. 13), NHMUK In. 34504; Q, upper latus, NHMUK In. 34504. Note that the rostrum changes from a trapezoidal ventral outline in Arcoscalpellum quadratum (L) to a rectangular one in Arcoscalpellum venablesi and S. fischeri (G, A); the rostrolatus in Arcoscalpellum quadratum (M, N) is typical of basal scalpellines (e.g. Fig. 11F, G, J, K, N, O, R, S), which possess a rectangular plate with a rounded concave socket for articulation with the rostrum. In Arcoscalpellum venablesi (H, I) and Scalpellum (B, C) the rostrolatus tapers ventrally, and the socket becomes an elongated trapezoidal surface. Scale bars: A, 0.5 mm; B-P, 1 mm.

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These changes are not evenly distributed through the branches of the cladogram, but display a very specific pattern of distribution. In the basal group (D. rubrum-Arcoscalpellum sociabile) the features of the rostrum-rostrolatera are highly conservative, whereas the carinolatus, and its relationships with the upper latus and carina underwent considerable evolution (Fig. 11). The most dramatic modifications within the family took place immediately preceding the evolution of Am. truncatum, in which there were 27 changes in character state, involving fundamental shifts in rostral, rostrolateral, carinolateral, and inframedian latus morphology, accompanied by a reduction in size, cuticular thickness, and pilosity. The importance of this node is reflected in nomenclatorial changes, with both the admittedly paraphyletic basal group and the derived group recognized as subfamilies (below).
Further significant morphological changes occurred at the base of the group including species assigned to Catherinum (nine changes in character state), and again at the base of Weltnerium (11 changes). These major sets of character changes and synapomorphies are used to define genera (see below).
The extensive fossil record of the Scalpellidae (e.g. Withers, 1935Withers, , 1953 permits some calibration of the tree (Fig. 14). The oldest scalpellid, Arcuatoscalpellum gen. nov. appears in the early Aptian, at approximately 125 Ma (dates from Gradstein et al., 2012). Diotascalpellum gen. nov. (Diotascalpellum angustatum Darwin) first appears in the late Albian, at 106 Mya, and Regioscalpellum gen. nov. (R. maximum) in the Coniacian at 89 Mya. By the late Campanian, at 75 Mya, both Catherinum and Amigdoscalpellum are present (see below). These dates are significant because the appearances of successive taxa are congruent with the order of nodes on the cladogram; the only exception is the late first occurrence of Arcoscalpellum at 55 Mya. Secondly, they suggest that the bulk of evo-lution in the Scalpellidae took place over the 40-Myr interval between the Aptian and late Campanian. This indicates that many of the extant genera have a Cretaceous origin, and that the modern representatives of the family record a large part of its phylogenetic history. The only group for which there is no fossil record is the most derived clade (Weltnerium).
Fossil evidence indicates that Scalpellum evolved from Arcoscalpellum in the Early Eocene (Withers, 1953; see also above). A remarkable feature of scalpellid genera as used here (see below) is their striking morphological conservatism. Cretaceous species of Diotascalpellum gen. nov. and Regioscalpellum gen. nov. can only be separated from living species using minor criteria of shell plate morphology (e.g . Figs 18, 19).
Much recent interest in scalpellids has focused on their reproductive strategies (Buhl-Mortensen & Høeg, 2006Yusa et al., 2011). Plesiomorphically, scalpellids are thought to be hermaphroditic (Foster, 1980), and the most basal living scalpellids identified here are hermaphrodites (Diotascalpellum diota (Hoek) and D. rubrum). More derived scalpellids (many Amigdaloscalpellinae) are androdioecious, the hermaphrodites housing dwarf males inside the scuta above the adductor muscle (Darwin, 1851a;Yusa et al., 2011), and others are dioecious, with large females and dwarf males (Buhl-Mortensen & Høeg, 2006Yusa et al., 2011). The interior of the scutum (Figs 8, 9) thus provides evidence of the level of reproductive specialization that can be applied to the fossil record (Høeg et al., unpubl. data).
A further interesting question is whether the scalpellids: (1) were an originally shallow-water family that subsequently colonized the deep sea; (2) were always a deeper-water family that periodically spread onto the shelves; or (3) originally extended from deep to shallow habitats, but were virtually excluded from the shelves in the Cenozoic. The problem here is the apparent absence of cirripedes in deep-water fossiliferous facies, particularly of Late Mesozoic age, which may be a result simply of their being overlooked. The presence of the deep-water Catherinum and Amigdoscalpellum in upper Campanian chalks of the UK, at the height of the Cretaceous sea level high (200 m above present; Hancock, 1990), however, could be taken as evidence that they had a long history in the deep sea about which we know very little.

SYSTEMATIC ACCOUNT
This section sets out to place the extant scalpellid taxa studied here, for which a phylogeny is presented (Fig. 14), into a taxonomic framework that reflects the morphological evolution of the group, and additionally incorporates some important fossil material, in order to put minimum dates on the nodes of the cladogram. This is controversial because it cuts directly across the classifications proposed by Newman & Ross (1971) and Zevina (1978aZevina ( ,b, 1981, which were used in a slightly modified form in the most recent taxonomic revision of extant forms by Young (2007). The classification is clearly provisional, because extensive molecular and reproductive studies on scalpellids are currently underway (e.g. Lin et al., 2015), and it will be necessary to extend the study to incorporate many more taxa, particularly those in which there is a significant reduction of capitular plates. A future, holistic classification of the Scalpellidae will require the integration of further morphological (arthropodal), reproductive and molecular information; however, the present study stands alone as a morphological and phylogenetic exercise.

Remarks
This definition works effectively for all known living and fossil forms, with the exception of the highly derived Scalpellopsis striatociliata Broch, 1922. The record of a subcarina in the Cretaceous species Diotascalpellum fossula (Darwin, 1851b) by Hébert (1855) and Withers (1935) is not substantiated by a re-examination of the material. The family appears in the Aptian (Early Cretaceous, about 120 Mya), and is represented by abundant fossil and living forms. In the Cretaceous and the Palaeogene, species were common in shallow and deep marine environments, with palaeodepths of as little as 20-30 m. Neogene and present-day records are almost exclusively from the deep sea. The present study identifies two groups, which are taken as subfamilies.

Amended diagnosis
Scalpellids in which the rostrolatus is broad, low, straplike, and gently incurved. The rostrum is broader than high, rectangular, trapezoidal or triangular, and large triangular lateral surfaces contact the interior of the rostrolatus. The articulation surface between the rostrum and rostrolatus extends over the entire height of both plates. Arcoscalpellum Hoek, 1907, Arcuatoscalpellum gen. nov., Diotascalpellum gen. nov., Graviscalpellum Foster, 1980, Regioscalpellum gen. nov., and Scalpellum Leach, 1817.

Remarks
This definition of Scalpellinae differs in major respects from that of Zevina (1978a), for whom the family was characterized by the subapical carinal umbo, the inflexed carina, and the subapical umbones of the upper and inframedian latus; however, the group as thus defined is polyphyletic (see above), and these features evolved independently a number of times within the Scalpellidae. The subfamily is therefore rediagnosed to include the basal group of scalpellids shown in Figure 14, which are technically paraphyletic, but can be readily identified.

Remarks
Scalpellum evolved in the Eocene from Arcoscalpellum, and a transition series is presented here (Figs 16, 17; see above).

CLASSIFICATION OF THE NON-SCALPELLUM SCALPELLINAE
This group was identified originally by Pilsbry (1907) as the 'S. velutinum (= S. michelottianum Seguenza, 1876) group', and was revived by , who noted that one group of species assigned by Zevina (1981) to the genus Trianguloscalpellum was characterized by large size and the presence of a thick, pilose cuticle. He identified two morphological trends within the group: a tendency to plate reduction, and displacement of the umbo of the carinolatus to a subapical position. For material from the Cretaceous, Withers (1935) identified three groups of Arcoscalpellum (then used to cover most fossil scalpellids), the A. arcuatum Gp, the A. maximum Gp, and the A. fossula Gp, distinguished by numerous plate characters. Zullo (1990) was able to trace the persistence of the two last-named groups from the Cretaceous into the Palaeogene. The new classification presented here builds on the observations of Withers, Zullo, and Young, and identifies five genera, four of which are extant, which reflect the progressive evolution of scalpellines during and since the Cretaceous (see above). These are based largely on detailed characters of the carinolatus, and its articula-tion with the carina and upper latus. The reclassification permits fossil taxa all traditionally assigned to Arcoscalpellum (Withers, 1935(Withers, , 1953 to be placed in natural groupings with extant taxa. Two of the groups described here were referred to Trianguloscalpellum Zevina (1978a), by Zevina (1981) and Young ( , 2007; however, the type species of this genus, S. balanoides Hoek, 1883, is a highly derived form that has additional primordial valves on the inframedian latus and some peduncular plates (see Broch, 1922), and is a hermaphrodite (Yusa et al., 2011). It is possibly related to R. gigas, with which it shares a tall articulation between the paired carinolatera.

Diagnosis
Basal scalpellines in which the carinolatus is slightly taller than broad, umbo apical, carinal margin convex, carina with median ridge; upper latus margin gently concave; inframedian latus surface not differentiated; on the interior, the surfaces overlapping the carina and upper latus are similar; external sculpture with strong radial ridges, weak reticulation.

Derivation of name
In eponymous reference to the type species.

Remarks
Material of the type species is illustrated here (Fig. 4M-S). Arcuatoscalpellum gen. nov. is the most basal scalpellid known, and ranges from Aptian to latest Maastrichtian in age. It shares many characters with Cretiscalpellum, including the sculpture and simple triangular morphology of the carinolatus.

Diagnosis
Scalpellines in which there is no specialized contact between the carina and carinolatus, merely a cresentic concavity on the interior of the plate that forms a rim PHYLOGENY OF THE SCALPELLIDAE 297 slightly overlapping the upper latus; umbo of carinolatus upright, only slightly incurved, dorsal margin gently convex; inframedian surface of carinolatus well demarcated and slightly inset.

Derivation of name
In eponymous reference to the type species.

Remarks
Cretaceous and extant species of Diotascalpellum gen. nov. have a very similar carinolatus morphology (e.g. Fig. 18A-G). The prevalence and diversity of species of Diotascalpellum in the Cretaceous supports its basal phylogenetic position. The earliest records are from the upper Albian (D. angustatum; Withers, 1935).

Remarks
The distinctive R. maximum (Fig. 18N, O, P, S) is common in Cretaceous chalks and marginal marine deposits from the Coniacian to the Maastrichtian (Withers, 1935), and Regioscalpellum gen. nov. is represented in the Eocene of Cuba by Arcoscalpellum sanchezae Withers, 1953. GENUS GRAVISCALPELLUM FOSTER, 1980 FIGURES 2E-H, 13A-C Type species Scalpellum pedunculatum Hoek, 1883, by original designation.

Diagnosis
Scalpellinae in which the rostrolatera and inferomedian latera are very low in proportion to the height of the capitulum; carinolatera have an elongated rhomboidal outline, with a prominent ridge on the long axis; the umbonal region of the carinolatus is weakly involuted. Pilsbry, 1907;Arcoscalpellum ungulatum Withers, 1953;Graviscalpellum grantmackiei Buckeridge, 1983. Foster (1980: 526) established Graviscalpellum to include 'Arcoscalpellids that are hermaphroditic, attain relatively large size and have lower latera about one tenth the height of the capitulum'. Subsequently, the genus was treated as a junior synonym of Anguloscalpellum Zevina, 1978b, because Zevina (1981 had included S. pedunculatum in that genus (e.g. Young, 2007); however, the type species of Anguloscalpellum, Scalpellum angulare Nilsson-Cantell, 1930, falls within the genus Weltnerium as redefined in this paper (trapezoidal scutum; deep, transversely elongated receptacle for dwarf male; rostrum with broad triangular external surface), and is evidently not related closely to S. pedunculatum. Therefore, Graviscalpellum is resurrected from synonomy to include both the extant G. regina (Pilsbry, 1907) and a number of fossil species from the Oligocene-Miocene of New Zealand (Buckeridge, 1983

Remarks
The name Arcoscalpellum was formerly applied to most living and many fossil scalpellids (Withers, 1935(Withers, , 1953Newman et al., 1969). After the revisions of Zevina (1978aZevina ( ,b, 1981, the genus was used in a restricted sense and identified by the 'inframedian latus triangular, reaching upper latus, umbo apical' (Shalaeva & Boxshall, 2014: 21). This condition is shown here to be plesiomorphic for scalpellids, and the genus is therefore redefined with reference to the morphology of the type species, Arcoscalpellum michelottianum. It encompasses a small group of more derived Scalpellinae (e.g. Fig. 2C, D) in which the carinolatus is in possession of a carinal margin and an upper latus surface (Fig. 10L, M). It ranges from the Eocene to the present day.

Diagnosis
Small, rather delicately constructed scalpellids in which the tergum is triangular, with a notched upper carinal margin to accommodate the tip of the carina, apical to which is a short supracarinal surface; scutum with discrete low tergal surface; carinolatus tall, umbo subapical, with well-developed carinal and upper latus margins; carinolatera of pair articulate firmly beneath carinal base; rostrolatus as tall as broad, subrectangular to subtriangular.

Discussion
This group is essentially identical with group B of Lin et al.'s (2015: fig. 3) molecular analysis, which includes a number of species studied here. The subdivision of this derived clade of scalpellids is provisional. The group is sharply and precisely defined by morphological characters, and the cladistic analysis indicates the direction of evolution; however, characters within the group are partly gradational.
1. The shape and relationships of the inferior median latus, used extensively in taxonomy by Zevina (1978aZevina ( ,b, 1981; see also Young, 2007;Shalaeva & Boxshall, 2014). Plesiomorphically, by comparison with the out-group, this is (1) triangular, (2) its apical margin does not extend to the scutum and upper latus, and (3) its umbo is apical (Figs 3, 6, 7). Note that there is considerable change in the shape and position of the umbo during ontogeny (Young, 2007). The development of two discrete surfaces, contacting the scutum and upper latus, respectively, appears to be a good synapomorphy of a more derived group of amigdoscalpellines, which is closely, and concomitantly, paralleled by the basal migration of the umbo. There also appears to be a division between a group with an hourglass-shaped ('waisted') inferior median latus (more basal) and a derived group in which the pentagonal plate is relatively broad, the lateral surfaces are parallel, and the umbo has migrated to the rostral margin. 2. Contact between the carinolatera, beneath the carina.
The polarity can be determined by the fact that all taxa with a triangular inferior median latus (evidently plesiomorphic) also possess a highly modified contact that is marked by interdigitating, alternate ridges radiating down from the umbo of the plate (Figs 6E, 7X). The more derived character state is a symmetrical contact, in which either a few ridges oppose precisely (e.g. Ca. recurvitergum; Fig. 7S), or in which the articulation is divided into a more basal, flat, slightly protruding contact surface and and upper, depressed, and more horizontal contact, a lower extension of the carinal surface (e.g. Catherinum novaezelandiae; Fig. 7N). 3. The nature of the contact between the scutum and upper latus. Plesiomorphically (e.g. Fig. 2), this is a simple, straight contact with no overlap, but in more derived taxa the slightly recurved apex of the upper latus rests in a groove on the scutum (e.g. Fig. 3A, B, E-G). A notch is present in the upper latus margin of the scutum at the same level ( Fig. 8C-D). 4. A sharp, acuminate, incurved umbonal tip on the scutum, incorporating the primordial valve, is present in more derived forms ( Fig. 8C-D). 5. The shape of the scutum changes during the evolutionary history of the scalpellids, from a subtriangular plesiomorphic form, in which the basaloccludent and basal-upper latus margins are at nearly right angles (Fig. 8A, E), to become progressively more trapezoidal (Fig. 8C, D, G, H). This is brought about by the increasingly acute basaloccludent angle and the increasingly obtuse basalupper latus angle (Fig. 1F). 6. The shape of the rostrum, and the extent and geometry of its external and internal surfaces. In Amigdoscalpellum and Catherinum, the rostra are oval, elongate, and very small, less than half the height of the rostrolatera. In the derived Weltnerium, the rostrum has a trapezoidal external surface, and the rostrum has the same height as the rostrolatera. 7. The shape and proportional size of the internal depression, between the umbo and the scutal adductor, which serves to accommodate dwarf males. In basal amigdoscalpellines, this is a U-shaped notch, extending variably inwards from the occludent surface. 8. Surface sculpture. The basal amigdaloscalpelline Amigdoscalpellum possesses a ubiquitous radial sculpture of raised, rounded ridges on all plates except the carina (e.g. Am. truncatum and Am. rigidum). Species of Catherinum have variable sculpture, from entirely smooth to possessing variably developed radiating ridges, which increase during ontogeny (Young, 2007). Species of Weltnerium are smooth, except for a variable coarse sculpture in W. stroemii.
The cladistic analysis demonstrates that there is a clear morphological progression from plesiomorphic to derived states in these characters; however, subdivision into clearly defined groups, effectively diagnosing genera, is problematic, because although the trends are directional, there is significant overlap in the distribution of the character states. For example, there are taxa in which the inframedian latus is hourglass shaped and there is significant overlap between the upper latus and the scutum, but which retain an interdigitating contact between the carinolatera (e.g. Young, 2007). Thus, there appears to be a limit to the use of morphological characters for defining clades, and the ultimate resolution may only be achieved by molecular analysis. However, the present study, and the examination of available material and literature, supports subdivision into three genera, using characters of the inframedian latus (Zevina, 1978a(Zevina, ,b, 1981.

Diagnosis
Sculpture of strong, radially arranged, rounded raised ridges on all plates except carina; carinolatera articulate across midline by means of zig-zagging, alternating ridges that diverge from umbones. Umbones of carinolatera central to subcentral, close to base of carina, not prominent. Inframedian latus narrow, triangular, more rarely elongate, rectangular, umbo apical, often not extending to top of carinolatus and rostrolatus. Rostrum small, less than half the height of the rostrolatus, narrow, rounded oval rhombic outline.

Remarks
Thus defined, Amigdaloscalpellum appears to be a monophyletic entity. The distinctive radial sculpture is also present, albeit in a weaker and more restricted form, on some fully grown individuals of a few species of Catherinum (e.g. Ca. australicum, Ca. recurvitergum, and Ca. striolatum; see . These can, however, always be distinguished on the basis of the morphology of the inframedian latus and the overlap of the scutum by the upper latus. Note that the genus as here defined also includes some taxa traditionally referred to Arcoscalpellum (such as Arcoscalpellum truncatum), which fall naturally in Amigdoscalpellum.

Remarks
As redefined here, Catherinum includes many of the species included in Verum by Zevina (1981). As noted by Young (2007), Catherinum fall into several distinct morphological groups. Although not dealt with here, many of the taxa assigned to Annandaleum (e.g. with strikingly reduced plates, such as Annandaleum japonicum Hoek, 1883), have an hourglass-shaped inferior median latus, at least in the juvenile stages, and are likely to be derived from species of Catherinum by plate reduction. Planoscalpellum Zevina, 1978b is a Catherinum-like form in which the upper latus umbo is unusually low on the scutum.

Diagnosis
Catherinum in which the occludent margin of the tergum is straight, and the external surface adjacent to this carries three ribs that diverge from the umbo. The upper part of the upper latus margin of the scutum is embayed. The carinolatus has a very broad upper latus margin.

Derivation of name
After East Anglia, in which the type material was collected.

Material
Fifty valves, including carinae, scuta, terga, and carinolatera, from the upper Campanian, Belemnitella mucronata zone chalk of Keswick and Cringleford Newfound Farm pits, Norwich, Norfolk, UK. The scutum illustrated is the holotype (Figure 19O), and the other illustrated valves are paratypes.

Description
The carina (Fig. 19E, I, P, T, V) is gently incurved towards the tergum, and the parietes are of even width; intraparietes are not developed. The tectal ridges are robust and broad (Fig. 19E, T), and the tectal surface between these is slightly convex. The tergum (Fig. 19Q) is elongated and triangular, and the carinal margin is slightly convex. Three radial ridges run from the umbo, subparallel with the occludent margin. The scuta (Fig. 19J, K, N, O) are concavo-convex, trapezoidal, and the umbo is pointed and incurved; the upper latus margin has a distinctive concavity just beneath the tergal-upper latus angle. A narrow groove runs parallel with the occludent margin. On the interior of the valve, a deep, oval dwarf male receptacle lies between the apex and the scutal adductor scar. The carinolatus (Fig. 19C, D, F-H) has a low, incurved umbo, and a tall carinal margin. The long, straight upper latus and inframedian latus margins are set at right angles. The plate is very typical of Catherinum of the Ca. hispidum (Fig. 19A, B) and Ca. striolatum (Fig. 7P, Q) type.

Remarks
Catherinum anglicum sp. nov. is perhaps closest to the extant Ca. hispidum from the Norwegian Sea. The carinae are very similar indeed, both carrying very broad, robust tectal ridges (Fig. 19I, S, T), and with shallow short grooves for articulation with the carinolatus in the interior (Fig. 19U, V). The terga are similar in shape, but the scutal margin is convex in Ca. hispidum and straight in Ca. anglicum sp. nov. Three divergent ribs run from the umbo, adjacent to the occludent margin in Ca. anglicum sp. nov., but these are absent in the living species (Fig. 19Q, R). The scuta both possess an incurved umbo, and a large, deep pit for dwarf males (Fig. 19J-O), which is directed slightly more transversely in Ca. hispidum. The carinolatera are similar in shape ( Fig. 19A-D, F-H), but the tergal margin is longer in Ca. anglicum sp. nov. It can be distinguished from small carinae of Diotascalpellum fossula by the absence of intraparietes. A further undescribed species of Catherinum is present in the Norwich chalk assemblage; this will be named subsequently. This is a very small species: the scuta have a maximum height of 2 mm, and the total height of the individuals was probably not more than 5 mm. It was possibly attached to living crustaceans or pycnogonids, by analogy with the small extant species Weltnerium nymphocola (Hoek, 1883)

Remarks
Weltnerium, as diagnosed here, is a monophyletic derived group characterized by a pentagonal inferior median latus with a low umbo, a tall, narrow rostrum with a large external surface, a markedly trapezoidal scutum, and a large transverse receptacle for dwarf males. Forms with subapical carinal umbones ('Ornatoscalpellum') and projecting carinolatera (some 'Tarasovium') fall into this category. It is not known from the fossil record.