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Cascolus ravitis gen. et sp. nov. is a three-dimensionally preserved fossil crustacean with soft parts from the Herefordshire (Silurian) Lagerstätte, UK. It is characterized by a head with a head shield and five limb pairs, and a thorax (pereon) with nine appendage-bearing segments followed by an apodous abdomen (pleon). All the appendages except the first are biramous and have a gnathobase. The post-mandibular appendages are similar one to another, and bear petal-shaped epipods that probably functioned as a part of the respiratory–circulatory system. Cladistic analysis resolves the new taxon as a stem-group leptostracan (Malacostraca). This well-preserved arthropod provides novel insights into the evolution of appendage morphology, tagmosis and the possible respiratory–circulatory physiology of a basal malacostracan.
Arthropods are the most diverse group of organisms in both the fossil record and the modern biota. The group originated in the Ediacaran and crown-group representatives occur in the early Cambrian [1,2]. Although arthropod phylogeny has generated huge debate, a combination of morphological and molecular data and evidence from fossils has increased consensus regarding the interrelationships of the major groups within the phylum (e.g. [3–6]). Crustaceans are the most abundant fossil arthropods, and the major pancrustacean groups first occur, or are supposedly present, in the Cambrian [2,6,7]. Here, we describe a new Silurian crustacean with preserved soft parts, Cascolus ravitis gen. et sp. nov., from the Herefordshire (Silurian) Lagerstätte, UK. Cascolus is resolved as a member of the stem-group of Leptostraca. Leptostracans are known almost entirely from living representatives. Leptostraca and the fossil archaeostracans constitute the Phyllocarida, which is normally considered sister to Eumalacostraca [4,8], and together they constitute Malacostraca. Cascolus provides important clues into the morphological evolution of the sister taxon of Eumalacostraca and of the Malacostraca, one of the major groups of Crustacea.
The Herefordshire Konservat-Lagerstätte in the Welsh Borderland, UK, is globally important as a source of unparalleled palaeobiological and phylogenetic data on a diversity of Mid-Silurian (approx. 430 Myr BP) invertebrate animals [9,10]. These include a brachiopod, a polychaete worm, aplacophorans, a gastropod, a stem-group asteroid, and most abundantly a range of arthropods comprising a stem-group euarthropod, a pycnogonid and other chelicerates, a marrellomorph, stem-group mandibulates, four ostracod species, a barnacle, a phyllocarid and a pentastomid [10–20]. Many additional forms, including a wide variety of sponge species, brachiopods, molluscs, arthropods and echinoderms, await study.
The fossils of the Herefordshire Konservat-Lagerstätte occur in calcareous nodules in a volcaniclastic deposit . They are preserved as calcitic in-fills in three dimensions. Using the custom SPIERS software suite the specimens are reconstructed as ‘virtual fossils’ [22,23]. After grinding of the fossil and image capture at 20 µm intervals extraneous material was removed digitally and fossil-matrix ambiguities were resolved. ‘SPIERSview’ was used to generate colour-coded three-dimensional interactive visualizations and reconstructions (figure 1), including stereo-pairs and an animation. The Oxford University Museum of Natural History (OUMNH) houses the original datasets that resulted from serial grinding.
Cascolus ravitis was coded into the extensive phylogenetic dataset of Legg et al.  as modified and used by Briggs et al.  (see electronic supplementary material, tables S1 and S2). This dataset, now composed of 316 taxa and 754 characters, was analysed under general parsimony in TNT v. 1.1 . All characters were unordered and weighted using implied weighting with a concavity constant of three. Tree searches used 100 random addition sequences with parsimony ratchet , sectorial searches, tree drifting and tree fusing . Nodal support was measured using symmetric resampling (each search using new technology searches with a change probability of 33%) and is reported as group supported/contradicted (GC) values. A Bayesian analysis of the dataset (electronic supplementary material, figure S2) failed to reach convergence after 15 million generations. The results displayed extensive polytomies and produced many branches inconsistent with most modern phylogenetic analyses of arthropods.
Phylum Arthropoda 
Subphylum Crustacea 
Class Malacostraca 
Subclass Phyllocarida 
Order Leptostraca 
Genus Cascolus gen. nov.
Type species Cascolus ravitis sp. nov.
Other species None.
The new crustacean is named in honour of the naturalist and broadcaster Sir David Attenborough, who grew up on University College Leicester campus, in celebration of his 90th birthday. Latin castrum ‘stronghold’ and colus ‘dwelling in’; alluding to the Middle/Old English source for the surname ‘Attenborough, derived from atten ‘at the’ and burgh ‘a fortified place’. Latin Ratae, the Roman name for Leicester, vita ‘life’ and commeatis ‘a messenger’.
An elongate body comprising a head with a head shield, pedunculate eyes and five limb pairs; and a trunk consisting of a thorax (pereon) with nine limb-bearing segments and an apodous abdomen (pleon). The first appendage is uniramous and has three slender flagella longer than the body. All other appendages are biramous and have a gnathobase. The post-mandibular appendages are similar to one another, except that the fourth head appendage bears a single petal-shaped epipod, and the fifth head appendage and each trunk appendage bear two petal-shaped epipods.
Herefordshire, England, UK; Wenlock Series, Silurian.
The body consists of a head bearing five pairs of appendages covered dorsally by a head shield and a thorax with nine tergites and corresponding limb-bearing segments behind which there are possibly two apodous segments extending into a region that is masked by extraneous matter (figure 1a,b,d,e). Total preserved length of the specimen is 8.9 mm; maximum width (1.3 mm) occurs at the head shield. All appendages except the first one in the head are biramous. The head shield is elongate and smooth, with maximum length axially and maximum width (approx. 70% of length) at just over half the distance from its anterior margin (figure 1a,e,i,l). The anterior margin of the head shield is inclined straight postero-laterally on both sides from a tiny axial indentation (figure 1a–c,h,i). In dorsal view the lateral margin is gently sinuous, curving adaxially around the eye. A gently inflated ridge traverses the head shield parallel to its anterior margin forward of the eyes (= ‘eye ridge’; figure 1a,i). A wide axial bell-shaped inflation lying between and posterior of the eyes transitions posteriorly into a dome-shaped axial inflation that widens gradually posteriorly (figure 1a,i). A broad, low occipital ring traverses the posterior one-sixth of the head shield (figure 1a,i). The posterior margin of the head shield extends slightly over the anterior margin of the trunk. Trunk tergites 1–4 are of a similar size whereas trunk tergites 5–9 are successively smaller (figure 1a,e,g). The widest (approximately mid-length) region of each tergite bears a transverse row of at least four tubercles arranged in pairs with each pair atop a weak ridge and consisting of one tubercle laterally and one slightly smaller tubercle dorsolaterally (figure 1a,f,g); other minor tubercles are also present. Anterior of the paired tubercles each tergite also has a shallow furrow posterior to a weak transverse ridge (= ‘half-ring’) (figure 1a,f,g). The posterior margin of each tergite is slightly higher than the succeeding tergite, which it overlaps to an unknown degree (figure 1a,f,g).
A small cone-shaped structure with a rounded end, presumed to be a labrum, projects posteroventrally at a point about 25% of the head length from the anterior margin (figure 1b,c,h). Head appendage 1 (antennule; light green, figure 1b,e,h–j,l) is uniramous and originates adaxially in front of the labrum just below the anterior margin of the head shield. The limb base is small, elongate spherical and projects more or less ventrally. Three long, fine, closely set thread-like flagella originate lateroventrally one below the other from the limb base. These extend posteriorly beyond the extremity of the trunk (only a proximal stub of the distalmost of the three flagella on the left limb is preserved). No podomeres (sensu Boxshall ) are discernible in the flagella. A pair of ovoid pedunculate eyes originate immediately below the anterior margin of the head shield just in front of the first appendage; the eyes project approximately 50% beyond the lateral margin of the shield (figure 1a–e,h,i,l).
Head appendages 2 to 5 and all trunk appendages are biramous. Head appendage 2 (antenna/second antenna; pink, figure 1b,h,i,k,l) originates just posterior of the attachment of the labrum. The inner edge of the limb base (representing at least a basipod) bears a gnathobasic endite, with at least one stout projection, adaxially directed towards the tip of the labrum. Both endopod and exopod are elongate and slightly tapered but short, not extending beyond the head shield. Both are flexed; it is difficult to resolve podomere boundaries, but the flexures suggest that several podmeres are present in each. The exopod is wider and longer than the endopod. The endopod extends ventrally and adaxially over the labrum. It is flexed in two regions, at about one-third length and near its distal end, and bears at least three fine, short spines/setae distally. The exopod projects abaxially forwards below the basipod of the first appendage and curves adaxially distally below the anterior margin of the head shield. Three flexures are discernible in the exopod, at about one-fifth and three-quarters length and near the tip. The nature of the termination is unknown.
Head appendage 3 (mandible; blue, figure 1b,e,h,i,l–n) originates just behind the labrum. Its limb base (representing at least a basipod) is large with a blade-like gnathobase on its inner margin projecting adaxially towards the position of the supposed atrium oris and bearing a row of stout projections (evident in the left limb). Both rami are stoutly developed and taper gradually. The endopod is wider and longer than the exopod and is flattened ab-adaxially. It consists of four successively smaller podomeres (evident on the left limb; figure 1m): podomeres 1 and 2 each have a single spine/seta (only the base is preserved) at mid-length on their inner margin and podomere 3 has two spines/setae at mid-length on its inner margin and at least one on its outer margin. The terminal podomere 4 bears a splay of at least four stout spines/setae. The exopod consists of five podomeres (evident on the left limb; figure 1n). The base of a tiny spine/seta is present on the outer margin of podomeres 3, 4 and 5, and there are two tiny spines/setae on the exopod tip.
Head appendage 4 (maxillula/first maxilla; lime green, figure 1b,e,h,i,l,o) originates just behind the mandible. The rami project posteroventrally. The limb base is large and elongate triangular in lateral view. It consists of a distal part (presumed basipod) to which the endopod and exopod are attached and a central part with a serrated blade (a gnathobase; interpreted to be coxal) on its inner margin that is directed anteroventrally towards the site of the presumed atrium oris. Between the gnathobase and the junction between the limb base and the presumed body wall/arthrodial membrane there is a precoxal area whose inner margin is of similar length to the gnathobase. The endopod is long, narrow, gently curved and tapers gradually. Articulations indicating at least the proximal podomere are evident (figure 1o). The exopod originates in a wide triangular-shaped connection between the outer margins of the presumed basipod and the coxa. The connection has broad, stout lateral margins flanking a much thinner central area. The main part of the exopod is petal-shaped and lamella-like with a weakly convex inner edge and a more strongly convex outer edge. Most of the exopod is very thin and impersistently preserved; its outer and inner margins are thicker. An epipod (here termed epipod 1) originates in a narrow connection on the outer proximal margin of the limb base; it is similar in form to the exopod but about half the size in area.
Head appendage 5 (maxilla/second maxilla; green, figure 1b,e,h,i,l,q) is similar in morphology to head appendage 4, including a presumed coxal gnathobase, but with an additional, smaller epipod (herein termed epipod 2) attached immediately proximal to epipod 1 on the outer edge of the limb base. The epipods and exopod are thin and edged by thicker margins. The exopod slightly overlaps epipod 1, which in turn slightly overlaps epipod 2 (e.g. figure 1e,q). Bases of tiny spines/setae are evident along the endopod.
Posterior to head appendage 4 all appendages up to and including trunk appendage 7 are each in turn slightly larger and more posteriorly directed; trunk appendages 8 and 9 are in turn slightly smaller. The morphology of the nine trunk appendages is similar to that of the posteriormost (fifth) head appendage. Trunk appendages 2 and 5 were selected for manual reconstruction in enhanced detail (figures 1r–u and and3):3): these reveal that the endopod consists of many short podomeres (approx. 20 in trunk appendage 2 and approx. 22 in trunk appendage 5; figure 1s,u), which become progressively shorter distally. Tiny slender spines/setae (at least two in proximal podomeres and one in more distal podomeres) project from the inner face of each podomere aligned in rows along the ramus (figure 1t(arrowed),u). A few spines/setae are also evident at mid-length on the outer face of the endopod of trunk appendage 2 (figure 1s). The gnathobase bears at least 12 spines/setae of similar size and length to those on the endopod (figure 1r,s,u). A single spine occurs on the inner proximal-most margin of the precoxal area of the limb base (arrowed in figure 1s,u). Similar fine structures are probably present on the other trunk appendages and head appendages 4 and 5.
The mid-length axial part of each sternite is raised to form a low node (figure 1p); there is no evidence of a food groove. The posterior and especially the anterior limit of each sternite is marked by a transverse ridge (figure 1p). The abdomen is poorly preserved. There are possibly at least two additional (apodous) segments beyond which (figure 1a,b,d; dark brown) there appears to be mainly extraneous matter that masks the remainder of the trunk.
The combination of morphological characters in the new fossil is unknown in any other arthropod and it is assigned to a new genus. Phylogenetic analysis of a large database (see Material and methods) resolves C. ravitis as a stem-group leptostracan and sister to Cinerocaris+Leptostraca s.s. (figure 2; electronic supplementary material, figure S1). Phyllocarida (i.e. Archaeostraca + Leptostraca) is normally considered sister to Eumalacostraca [4,8], and together they constitute Malacostraca (figure 2) (see  for a review of alternative positions of Leptostraca). Cascolus ravitis, together with the associated Herefordshire Lagerstätte phyllocarid Cinerocaris magnifica [2,34], represent the oldest known members of crown-group Malacostraca. Only one purported fossil representative of Leptostraca, the Permian Rhabdouraea, has been reported .
Cascolus ravitis displays heteronomous post-antennulary appendages, which is a characteristic of mandibulates and evident in crustaceans [32,33,37–40]. The three long flagella of the antennule of C. ravitis resemble those in stomatopod malacostracans and also in the Cambrian stem mandibulate Oelandocaris , but the limb base of the C. ravitis antennule differs in lacking segmentation. The antennulary flagella also recall similar features in the first head appendage of the megacheirans Leanchoilia from the Cambrian [42–44] and Enalikter from the Silurian, but the C. ravitis antennule differs fundamentally from the first (‘great’) appendage of megacheirans in lacking a bipartite peduncle and ‘elbow joint’. Furthermore, the flagella of C. ravitis do not originate from individual spinose segments of a ramus as they do in Leanchoilia. More significantly, given where C. ravitis falls in the cladogram (figure 2), its antenna differs markedly from the antenna in Leptostraca in being biramous rather than uniramous (see ). The antenna in both the two well-preserved phyllocarids from the Devonian Hunsrück Slate, Nahecaris stuertzi  and Oryctocaris balssi , is also biramous. Thus, the evolution of the antenna in leptostracans is likely to have involved modification and reduction of the number of rami .
Epipods, such as those on the rear head appendages and trunk appendages of C. ravitis, are known only in Eucrustacea (sensu ), where they occur in a few entomostracans (sensu ) and in Malacostraca. Appendages bearing two epipods, as in C. ravitis, are also present in some branchiopods, syncarids and in leptostracans [33,35], and at least two occur on appendages in the fossil Cinerocaris (figure 3). They may also be present in the Herefordshire Lagerstätte Tanazios, a putative stem-lineage crustacean , regarded as a labrophoran by Boxshall [33,50]. Cephalic epipods are rare, but one is present on the maxillule in copepods, and one occurs on the maxilla in myodocope ostracodes, where it is the only known example in this position in a living crustacean [33,35]. Cascolus ravitis, unlike Cinerocaris, has epipods on its cephalic limbs as well as those of the trunk.
The position of C. ravitis on the stem of Leptostraca is supported by the nature of the appendages at the rear of the head and in the trunk, with a paddle-like epipod and a multisegmented endopod with two rows of setae. Cascolus ravitis differs from other phyllocarids, including the living Leptostraca, in lacking a true carapace (that is, a head shield with a post-cephalic extension). However, the overall appearance of the cephalic shield (including ridges) and the presence of three flagella in the antennule are reminiscent of those features in stomatopods, which fall out at the base of the Eumalacostraca [4,8].
Malacostracans are arguably the only crustaceans with a tagmatized trunk . Tagmosis in C. ravitis differs from that in other malacostracans, which have a thorax (pereon) of eight somites and an abdomen (pleon) of seven in phyllocarids, including leptostracans, and six in Eumalacostraca. Cascolus ravitis, by contrast, has nine appendage-bearing thorax somites, followed by an unknown number of apodous, presumably abdominal somites and perhaps a telson. The number of thoracic segments may be a late stage in the reduction towards the eight that are characteristic of Malacostraca from a plesiomorphic many-segmented trunk with serially similar limbs  as in basal Miracrustacea s.l. such as Tanazios and remipedes (in contrast, molecular analyses argue for a few-segmented ancestor state ). The presence of one fewer abdominal somites in Eumalacostraca than in Phyllocarida may be the result of a similar process. Such variation may reflect shifts in Hox gene expression along the trunk [51,54]. The phylogenetic position of C. ravitis implies that the eight-segmented thorax of Malacostraca may have been acquired convergently in Phyllocarida (including leptostracans) and in Eumalacostraca.
Cascolus ravitis demonstrates a number of plesiomorphic features similar to those in remipedes and cephalocarids, notably the similarity of the fourth and fifth head appendages to those of the trunk, and the lack of an articulated rostrum projecting anteriorly from the carapace. A movable rostrum is present in Leptostraca, some fossil phyllocarids and Stomatopoda, and its absence is potentially a plesiomorphic feature of Malacostraca. The presence of two epipods attached to the base of appendages in C. ravitis lends support to the presence of a multi-epipod condition (two in Malacostraca and possibly three in Entomostraca) in the pancrustacean ground plan , although Boxshall [32,33,50] pointed out the difficulty of establishing homologies between these structures, particularly in fossil taxa.
The Herefordshire biota lived within the Welsh depositional basin, probably in a slope setting at water depths of 100–200 m . The remarkably preserved nature of C. ravitis, with no sign of distortion even of the extremely fine flagella, suggests that, like other animals of the Lagerstätte, it was preserved rapidly in vivo. The large paddle-shaped epipods and exopods may have functioned in locomotion and as respiratory (see ) and/or osmoregulatory organs. These laterally extensive structures recall the foliaceous epipods and exopods involved in respiration in, for example, the Recent leptostracans Nebalia and Dahlella [35,55,56]. Their relatively large surface area would presumably facilitate efficient oxygen uptake. The thick outer and inner borders and the intervening delicate cuticle of the epipods and exopods of C. ravitis draw close structural parallels with the epibranchial (efferent) and hypobranchial (afferent) canals and intervening thin tissue of gill lamellae of the living myodocopid ostracod Leuroleberis, and also with similar structures in living leptostracans, in which the canals function in transporting hemolymph in the respiratory–circulatory system [35,55]. The stout lateral margins of the triangular basal connection of each exopod of C. ravitis may also have housed circulatory canals and/or musculature.
The large stalked eyes of C. ravitis indicate an almost all-round field of view. As in most mandibulates the first head appendage of C. ravitis probably functioned as a sensory receptor of environmental conditions . Extant Leptostraca comprises a few tens of mostly small marine species (5–15 mm long) found in intertidal settings and down to more than 2000 m depth. Most species occur in less than 200 m. The majority are epibenthic suspension feeders, but carnivorous scavengers and bathypelagic representatives are also known. The cephalized post-antennulary appendages of C. ravitis are clearly specialized for feeding and its gnathobases probably functioned to process and channel food to the mouth, although there is no obvious food groove. Like many of its arthropod faunal associates C. ravitis may have been nektobenthic.
We thank Geoff Boxshall for his insightful comments on an earlier version of the MS; Sarah Joomun, Carolyn Lewis and Sean McMahon for technical support; two reviewers for their helpful input; and David Edwards and the late Roy Fenn for general assistance.
The triangle-mesh model of holotype specimen OUMNH C.29698 is available in VAXML/STL format from the Dryad Digital Repository: http://dx.doi.org/10.5061/dryad.g1q8p . Cladistic character-matrix datasets supporting this article have been uploaded as part of the electronic supplementary material.
Da.J.S., De.J.S., D.E.G.B. and M.D.S. designed the research and carried out fieldwork. D.L. performed phylogenetic analyses. Da.J.S. wrote the paper with scientific and editorial input from the other authors.
We have no competing interests.
We thank the Natural Environment Research Council (Grant NE/F018037/1), the Leverhulme Trust (grant no. EM-2014-068), Oxford University Museum of Natural History, the Yale Peabody Museum of Natural History Invertebrate Paleontology Division and English Nature for support.