[Palaeontology, Vol. 53, Part 6, 2010, pp. 1393–1409] TAPHONOMY AND AFFINITY OF AN ENIGMATIC SILURIAN VERTEBRATE, JAMOYTIUS KERWOODI WHITE by ROBERT S. SANSOM*, KIM FREEDMAN* , SARAH E. GABBOTT*, RICHARD J. ALDRIDGE* and MARK A. PURNELL*à *Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK; e-mails [email protected], [email protected], [email protected], [email protected] 6 Wescott Road, Wokingham, Berkshire RG40 2ES, UK; e-mail [email protected] àAuthor for correspondence Typescript received 14 July 2009; accepted in revised form 23 April 2010 Abstract: The anatomy and affinities of Jamoytius kerwoodi White have long been controversial, because its complex taphonomy makes unequivocal interpretation impossible with the methodology used in previous studies. Topological analysis, model reconstruction and elemental analysis, followed by anatomical interpretation, allow features to be identified more rigorously and support the hypothesis that Jamoytius is a jawless vertebrate. The preserved features of Jamoytius include W-shaped phosphatic scales, 10 or more W hite (1946) first described Jamoytius kerwoodi on the basis of two specimens from a Lower Silurian (Llandovery) horizon of the Lesmahagow inlier of Lanarkshire, Scotland, and considered it to be the most primitive known vertebrate. Numerous subsequent authors have disputed this conclusion or have disagreed with aspects of White’s (1946) interpretation (see Supporting Information, Data S1). Evidence from additional specimens collected at Lesmahagow localities (see Ritchie 1968, 1985 for synopses of locality and stratigraphy details) prompted Ritchie (1960, 1963, 1968, 1984) to redescribe Jamoytius as an ‘unspecialized anaspid’, possibly related to the extant jawless vertebrates. As shown by Plate 1, most of Ritchie’s (1960, 1968) interpretations of the anatomical features of Jamoytius differ from those of White (1946). Despite Ritchie’s treatment, Jamoytius continued to generate debate. Various authors challenged Ritchie’s work (e.g. Janvier 1981; Forey and Gardiner 1981) or suggested affinities with a range of subsequently discovered fossils (e.g. Janvier and Busch 1984; Briggs and Clarkson 1987). Cladistic analyses of the jawless vertebrates (e.g. Janvier 1981, 1996a, b; Forey 1984, 1995; Forey and Janvier 1993) have also failed to clarify the affinities of Jamoytius; the lack of agreement regarding its anatomical homologies has meant that different analyses have used different character codings. In addition to coding, choice ª The Palaeontological Association pairs of branchial openings, optic capsules, a circular, subterminal mouth and a single terminal nasal opening. Interpretations of paired ‘appendages’ remain equivocal. Phylogenetic analysis places Jamoytius and Euphanerops together (Jamoytiiformes), as stem-gnathostomes rather than lamprey related or sister taxon to Anaspida. Key words: Jamoytius, Euphanerops, phylogeny, taphonomy, Vertebrata, Gnathostomata, Silurian. of the in-group taxa included in the phylogenetic investigation has affected the placement of Jamoytius (Donoghue et al. 2000; Donoghue and Smith 2001; Gess et al. 2006). The position of Jamoytius on cladograms has consequently not stabilized, though Jamoytius usually appears as a sister taxon to the lampreys, the anaspids, or Euphanerops longaevus Woodward, 1900. Janvier and Lund (1983, p. 412) wrote, ‘These various interpretations cause one to wonder about the degree of imagination involved in the study of Jamoytius and other fossils preserved as tarry impressions.’ So why has it proved so difficult to produce a definitive interpretation of Jamoytius and to determine its affinities? The principal problem is one that affects interpretation of many problematic fossils – disentangling the different aspects of the process of anatomical reconstruction. The selection of an appropriate anatomical comparator upon which to base hypotheses of homology (comparisons being drawn either directly to a specific extant organism or clade, or indirectly through a fossil intermediate) can be especially problematic (Donoghue and Purnell 2009); the choice of interpretative model needs careful justification on the basis of characters present, preferably unequivocally, in the fossils. In the case of Jamoytius, almost all workers have considered it as a jawless vertebrate without explicit justification, and consequently, anatomical interpretations, doi: 10.1111/j.1475-4983.2010.01019.x 1393 1394 PALAEONTOLOGY, VOLUME 53 homology statements and phylogenetic analyses are all at risk of circularity. Jamoytius is generally preserved in two dimensions, and investigations have often concentrated on relating the shape of its features to the three-dimensional anatomical parts of presumably related organisms. Different workers have alternatively described the same circular features in Jamoytius as mouth, eyes and nasal structures (Pl. 1 and Supporting Information, Data S1). These interpretations are thus inherently equivocal. Anatomical and phylogenetic claims, and counterclaims, will continue to be insecure without further information about the topology, composition and taphonomic history of anatomical features, combined with explicit articulation of the methodology used to reach anatomical interpretations. MATERIALS AND METHODS Topological reconstruction and comparative anatomy. In order to address the problems of circularity and equivocal interpretations, a stepwise methodology separating topological considerations from anatomical interpretation was applied as advocated by Donoghue and Purnell (2009). First, the features of the fossils were identified and described (i.e. number and shape of distinct body parts, and the topological relationship between those body parts). By comparing specimens preserved in different orientations, three-dimensional reconstruction was possible (cf. Briggs and Williams 1981; Purnell and Donoghue 1999). Throughout this process of interpretation and reconstruction, no assumptions were made about the affinities of the organism or the homology of its features. Following topological description, an explicitly justified interpretative model was selected upon which to base anatomical hypotheses. Putative homologies were identified through the consideration of topological relationships between body parts (Rieppel and Kearney 2002) and were informed by evolutionary and potential taphonomic transformational sequences (i.e. assessing whether the appearance of a feature, or its absence, represents the original anatomical condition, or the results of post-mortem processes of decay and preservation). The intrinsic properties and composition of the body parts provided additional constraints on interpretations. Following translation of topological structures into anatomical interpretations, taxonomic assessments and phylogenetic analyses were employed to investigate the placement of the organism in an evolutionary context. Elemental analysis. Topological data were complemented by determination of the chemistry and preservation of particular features to provide evidence of original histology and ⁄ or composition (e.g. Butterfield 2002; Gabbott et al. 2004). Elemental mapping of some features of Jamoytius was performed on a LEO 435 VP Scanning Electron Microscope with an Oxford Instruments ISIS 300 EDX spectrometer operating in variable pressure mode at 10 Pascals with an accelerating voltage of 10 kV and a beam current of 500 picoamps for 1000 frames (approximately 14 h of run time). The specimens analysed in this study have not been subjected to hydrofluoric acid treatment (Ritchie 1963, 1968); smaller specimens were selected because of SEM chamber size limits. Phylogenetic analysis. Data matrices were constructed in MacClade 4.06 (Maddison and Maddison 2003). Heuristic searches were performed using PAUP 4.0 (Swofford 2002) with 1000 random sequence addition replicates and TBR (Tree bisection and reconnection) branch swapping. Where appropriate, characters were reweighted according to their rescaled consistency indices. To investigate the alternative topologies that satisfy phylogenetic relationships proposed on the basis of molecular data, heuristic searches were conducted using backbone constraint trees constructed in MacClade 4.06 (see below). Institutional abbreviations and publicly held material. NHM, Natural History Museum, London, P11284 (holotype), P11285, P47784-7; AMS, Australian Museum, Sydney, F64401, F1028416; NMS National Museum of Scotland, Edinburgh, 1959.1, 1966.3.1-3; BGS, British Geological Survey, Keyworth, 11882-3; Hunterian Museum, Glasgow, V.7792, V.8036V.8141, V.8148, GLHAM101382; UOE, University of Edinburgh, FR1628, FR1476, 20129-32, 20145, 20159-62. BODY PARTS, TOPOLOGICAL ANALYSIS AND RECONSTRUCTION Body shape In general aspect, Jamoytius has an elongate lozengeshaped body exhibiting a size range of 140–180 by 30– EXPLANATION OF PLATE 1 Jamoytius kerwoodi White holotype (NHM P11284a) immersed in 90 per cent ethanol with incident polarized light and filter, illustrating the conflicting interpretations of White (1946), in bold, and Ritchie (1960, 1963, 1968, 1984) in plain text. Scale bar represents 10 mm. PLATE 1 eye mouth eye eye not interpreted eye lateral fin fold branchial basket bifurcation of notochord branchial basket muscle blocks (with muscle fibres) unmineralized scales (with ornamentation) rays of dorsal fin not interpreted intermuscle spaces (myocommata) interscale spaces intestine one margin of intestine notochord one margin of intestine lateral fin fold ventral termination of body scales displaced skin lateral fin fold basal supports of dorsal fin not interpreted basal supports of anal fin not interpreted SANSOM et al., Jamoytius kerwoodi 1396 PALAEONTOLOGY, VOLUME 53 40 mm. The body is preserved with a varying degree of curvature (range of 40–90 degrees through the long axis of the body). One end of the body of Jamoytius shows a greater degree of morphological differentiation, containing multiple different substructures. This is provisionally taken to be the head (see later discussion), thus indicating anterior. Through comparison of paired and symmetrical body parts, specimens are identified as collapsed remains of a bilaterally symmetrical organism preserved in different orientations (some are dorso-ventrally collapsed, some laterally and others intermediate). There is not enough evidence to determine the original shape of the posterior of the organism, as most slabs do not possess the most posterior portion. When present, the posterior is preserved much more faintly than the rest of the body, sometimes too faintly to be discerned clearly. NHM P47784a exhibits what could be interpreted as two posterior lobes, but the region is poorly preserved and heavily prepared, thus obscuring the original body outline. ferent orientations, it is apparent that they are coincident with the body margin. Two distinct types of subcircle occur. Two have broad, dark margins and form a lateral, symmetrical pair, close to either the dorsal or ventral body margin (Text-fig. 1). Comparison of the shapes of these structures in dorso-ventral and laterally collapsed specimens indicates that their original shape was either a laterally flattened spheroid, or an outwardly opening cuplike structure roughly equating to half or two-thirds of a sphere (e.g. Text-fig. 1A). The other two subcircles have narrower margins and lie along the sagittal plane, one terminal, one subterminal in position (Text-fig. 1C,D). Irrespective of the orientations of the body, these axially located rings are preserved as approximately circular outlines. This indicates either that they were originally spherical, or that they were discs with sufficient rigidity at the time of body collapse to reorient into a bedding parallel attitude. Elemental mapping analysis performed on the anterior region of NHM P47787a shows a clear correlation of carbon with one of the paired, broader margined, anterior subcircles (Text-fig. 2B). Body parts Serial subrectangles. Towards the anterior end, many specimens preserve a pair of linear features composed of serially repeated, contiguous, subrectangular shapes Anterior subcircles. Four subcircles occur in the anterior region. From comparison of specimens preserved in difA B C D A B C T E X T - F I G . 1 . Anterior subcircles of Jamoytius (A–D) with corresponding graphic interpretations (below), where darker grey represents laterally paired subcircles with broader margins, lighter grey represents subterminal ring and medium grey represents terminal ring. A, NHM P11284a. B, NMS 1966.3.2. C, NHM P11285. D, NMS 1966.3.1. Scale bars represent 5 mm. D SANSOM ET AL.: TAPHONOMY AND AFFINITY OF THE SILURIAN VERTEBRATE JAMOYTIUS A B C D E F T E X T - F I G . 2 . SEM back scatter and elemental maps. A–D, W-shaped structures of GLAM V8141c (A, back scatter; B, Carbon; C, Calcium; D, Phosphorous). E–F, Anterior subcircle NHM 47787A (E, back scatter; F, Carbon). (Text-fig. 3A,B). The central areas of the subrectangles have the same coloration as the body but their perimeters are darker. Like the anterior subcircles, the lines of subrectangles are coincident with the body margin. The subrectangles are arranged in a ladder-like line, which lies at a shallow angle to the antero-posterior axis of the body. The precise number of subrectangles is difficult to establish and possibly varies between individuals. Jamoytius has been reported to have had as many as 17 subrectangles in each series (Ritchie 1984) and as few as seven (Forey and Gardiner 1981). In the case of the specimen discussed by the latter, the body is incomplete and the posterior portion of the region with subrectangles may be missing. On all specimens for which the entire length of 1397 the line of subrectangle rows is present, at least 10 can be identified, and on several, at least 14 (e.g. Text-fig. 3). W-shaped structures. Although they are not preserved in all specimens, among the most conspicuous features of Jamoytius are W-shaped, serially repeated structures. Their disposition indicates that they were coincident with the body outline, or at least very nearly so (Pl. 1; Textfig. 4A). Each W extends around the majority of the lateral body margin, leaving a gap on one body surface, either dorsal or ventral (Pl. 1; Text-fig. 4D; Ritchie 1968, pl. 4, fig. 1). The series of Ws does not extend along the entire antero-posterior axis of the body; they are absent from the anterior (e.g. Pl. 1) and their posterior limit is uncertain. The Ws consist of alternating narrow and broad zones. The narrow zones are prominent and generally show relief. They normally have a central area (200–300 lm wide), the same colour as the matrix of the siltstone in which the fossils are preserved, with very dark borders (c. 50 lm wide) on either side (Text-fig. 4C). In some instances, the narrow zones also exhibit a tuberculate texture (Text-fig. 4E; Ritchie 1968, pl.4, fig. 3), which is best observed on fragmentary specimens. The broad zones (1–3 mm wide) lack relief, but are darker in colour than other parts of the body. Within the broad zones are linear features, lighter in colour; some of these lines form dendritic patterns (Text-fig. 4C). Elemental mapping of the W-shaped stripes of specimen GLAM V8141c shows that the borders of the narrow zones and the whole of the broad zones contain associations of Ca and P (Text-fig. 2A) but not the other elements making up the matrix. Carbon is also present, but appears to have an inverse distribution to that of Ca and P; the W-shaped features are, therefore, interpreted as being composed of calcium phosphate, possibly with an organic component. Axial lines and rounded structures. In the holotype (NHM P11284a, Pl. 1, Text-fig. 5) and FR 1601 (Ritchie 1968; pl. 4, fig. 2, pl. 6, fig. 1), a pair of parallel, axial lines are noted in the middle of the trunk (each approximately 2 mm wide). Upon closer inspection, the lines are composed of contiguous lozenge- or oval-shaped units, each slightly longer than wide (Text-fig. 6B). In FR 1601, the region between the axial lines preserves the W-shaped structures from both the near and far side of the body, whilst the region outside of the axial lines preserves the Ws from only one side of the body (Text-fig. 6A). In NHM P11284a, one of the axial lines bifurcates towards the anterior. Towards the posterior of NHMP 11284a, the lines become less clear. Aligned with the axial lines are a parallel and paired posterior series of dark, rounded structures, which exhibit positive relief (Text-fig. 6B). 1398 A PALAEONTOLOGY, VOLUME 53 A T E X T - F I G . 3 . Anterior subrectangles with corresponding graphic interpretations (A, B) and ventro-lateral ‘folds’ (C, D). A, NMS 1966.3.2. B, NMS 1965.59a. C, NMS 1966.3.2. D, NHM P11285. Scale bars represent 5 mm. B B C D Their periodicity is approximately the same as that of the W-shaped structures. The alignment of the axial rounded structures with the axial lines, combined with the lozenge-shaped units of the lines, suggests that the rounded structures and axial lines may comprise the same structure. tures (Pl. 1, Text-fig. 3). They originate posterior to the serial subrectangles and continue posteriorly until they become indistinct. They are generally straight and exhibit wrinkling in some instances. Reconstruction Paired longitudinal ‘folds’. A pair of parallel linear features resembling collapsed folds is observed on the same surface of the body as the gap between the W-shaped struc- The general two-dimensional form of fossils of Jamoytius is presumed to be a result of the collapse of a soft body SANSOM ET AL.: TAPHONOMY AND AFFINITY OF THE SILURIAN VERTEBRATE JAMOYTIUS A B C dendritic pattern 1399 D broad zone narrow zone displacement E gap fractures tubercles W-shaped serially repeating stripes on the trunk of Jamoytius. A, NHM P11284a illustrating coincidence of stripes with the left body margin. B, GLAM 101283 ⁄ 1. C, GLAM V8141. D, NHM P47784a. E, NHM P11284a. Scale bars represent 5 mm (A–D) or 1 mm (E). TEXT-FIG. 4. during decay rather than compaction, and body fossils in different orientations can thus be equated to two-dimensional views of a three-dimensional organism (Briggs and Williams 1981). Most of the preserved features are evident in almost all the dorso-ventrally and laterally collapsed specimens that retain the appropriate portion of the body, and the three-dimensional architecture and position of these features can therefore be confidently modelled. Whilst the model is a simplification of some features (e.g. anterior subcircles), it corresponds well with all known specimens of Jamoytius, including those that are obliquely collapsed (Text-fig. 7). The accuracy of the model can be tested by its ability to predict the position of features in any newly discovered specimens. The antero-posterior axis and dorso-ventral axis are identified on the basis of the anatomical differentiation in the ‘head’ and symmetrical disposition of surface structures (e.g. paired subcircles and W-shaped structures), respectively; distinguishing dorsal and ventral remains problematic in the absence of a phylogenetic context. The model indicates that the paired axial lines and allied rounded structures are likely to be interior structures. They are preserved in only two specimens (NHMP 11284, oblique; FR1601, lateral) but it seems that both lines occur in the sagittal plane. Towards the anterior, one of the axial lines is very close to the surface with no gap in Ws towards the anterior; towards the posterior, the axial lines approach the midline. ANATOMICAL INTERPRETATION AND CHARACTER HOMOLOGY Establishing a phylogenetic context Historically, Jamoytius has been interpreted as a jawless vertebrate, but it lacks any unequivocal vertebrate synapomorphies (e.g. sensory canals, brain, skull, muscular pharynx, multi-chambered heart, liver, kidney etc.) or, for that matter, any unequivocal chordate synapomorphies (e.g. dorsal nerve chord, notochord, myomeres, endostyle ⁄ thyroid, pharyngeal arches, postanal tail). Paired sense organs can be reasonably interpreted as present in Jamoytius, but these are not unique to chordates (although within chordates, they are a vertebrate synapomorphy). Previous interpretations of Jamoytius as a vertebrate or even chordate have, therefore, not been adequately justified: anterior anatomical differentiation, serial stripes, axial lines, and a fusiform and curved body shape are not sufficient in themselves to support a chordate model. Such general conditions could be noted in a broad range of metazoan taxa, for example, articulated 1400 PALAEONTOLOGY, VOLUME 53 terminal subcircle lateral subcircle (l) serial subrectangles (l) A A subterminal subcircle ventral axial line lateral subcircle (r) Ws on right (proximal) surface serial subrectangles (r) Ws on left (distal) surface dorsal axial line W-shaped structures B axial line (r/v) axial line (l/d) anterior bifurcation ventro-lateral folds dorsal axial line ventral axial line linear rounded structures Ws on dorsolateral surface Body parts and topological interpretation of the holotype (NHM P11284a) of Jamoytius. Scale bar represents 10 mm. TEXT-FIG. 5. soft-bodied fossils such as the purported polychaete Pieckonia (e.g. Fitzhugh et al. 1997, fig. 7A.18). We can, however, compare Jamoytius with fossil or extant taxa that possess the particular topological features outlined above. Following redescription of Euphanerops (Janvier and Arsenault 2007), it is clear that it shares with Jamoytius the following features: dark anterior subcircles (specifically, a lateral pair, one terminal ring and one subterminal ring) and ladder-like rows of contiguous serially repeating anterior subrectangles (Text-fig. 8). Two other structures are comparable between the two genera but are not present in exactly the same condition: serially repeating antero-posterior stripes and paired ventro-lateral ‘folds’. Unlike Jamoytius, Euphanerops also preserves some unequivocal chordate synapomorphies (postanal tail, B axial rounded structures Axial structures of Jamoytius. A, Trunk of FR 1601 with reconstruction illustrating paired axial lines. B, Trunk of NHM P12284a with reconstruction illustrating paired axial lines and axial rounded structures. A1 from Ritchie (1968, pl. 6, fig. 1). Scale bars represent 5 mm. TEXT-FIG. 6. SANSOM ET AL.: TAPHONOMY AND AFFINITY OF THE SILURIAN VERTEBRATE JAMOYTIUS A 1401 B C T E X T - F I G . 7 . Different perspectives of the three-dimensional model compared with two-dimensional fossil specimens of Jamoytius preserved in different orientations. A, Dorsal perspective with NHM P11284a. B, Ventral perspective with NMS 1966.3.2. C, Lateral perspective (anterior-posterior axis slightly oblique) with NHM P11285. Scale bar represents 5 mm. notochord) and vertebrate synapomorphies (mineralized endoskeleton, anal fin with fin supports) (Janvier and Arsenault 2007). Given the similarities between Jamoytius T E X T - F I G . 8 . Anatomy of Euphanerops and Jamoytius. A, MHNM 01-02 drawing illustrating some of the features shared with Jamoytius. B, Reconstruction of Euphanerops. C. Reconstruction of Jamoytius in light of new data. A from Janvier and Arsenault (2007, fig. 3B2), B adapted from Janvier and Arsenault (2002, fig. 1b). Scale bar represents 10 mm (A). and Euphanerops in body parts and their topological relations, it is reasonable to infer that Jamoytius also possessed a postanal tail and notochord, which are not A lateral subcircles B C median subterminal subcircle contiguous subrectangles 1402 PALAEONTOLOGY, VOLUME 53 T A B L E 1 . Topological features identified in Jamoytius and their anatomical interpretations based upon a chordate comparator. Topological feature Anatomical interpretation Anterior subcircles (paired, lateral) Anterior subcircle (terminal) Anterior subcircle (subterminal) Anterior subrectangles Optic capsules W-shaped structures Axial lines with subunits Ventro-lateral paired ‘folds’ Single, terminal, nasal opening Round ventral mouth Multiple external branchial openings Rigid (probably mineralized) scales Axial skeleton Lateral fin folds? preserved in known specimens. We reject the alternative hypothesis that the similarities between Jamoytius and Euphanerops are mere coincidences, on grounds of parsimony. A chordate context for the interpretation of the body parts of Jamoytius is thus justified, and topology can be translated into anatomy in the light of this comparative model (Table 1). Anterior subcircles and subrectangles Anatomical interpretation. Given a chordate model, the lateral paired anterior subcircles are best interpreted as optic capsules. The positions of the optic capsules of Jamoytius can be interpreted as dorso-lateral given that in all chordates with eyes they are located on either lateral or dorso-lateral surfaces (rare exceptions include the ventro-lateral eyes of the bighead carp, Hypophthalmichthys nobilis). The dorsal and ventral surfaces of Jamoytius are thereby identified – the optic capsules are dorsal, and the gap between the W-shaped structures is along the ventral surface. Of the median anterior subcircles, the large rounded subterminal ring, which is now clarified as being located on the ventral body surface, is best interpreted as the oral opening. Its position and architecture are consistent with its interpretation as an annular cartilage (e.g. Ritchie 1963, 1968), such as that found in the extant lampreys. There are, however, no associated structures preserved that might support that hypothesis (e.g. circum-oral teeth, copular cartilages, oral papillae). The smaller, terminal subcircle is comparable to the single nasal opening observed in a number of jawless vertebrates, both extant and extinct. Its terminal position indicates that it is unlikely to be a pineal organ. The paired, serially repeating subrectangles compare closely to the branchial openings observed in fossil jawless vertebrates such as Euphanerops, osteostracans, and, to a lesser extent, extant jawless vertebrates such as lampreys. These animals possess a series of external branchial openings, which originate in the head region and descend ventrally towards the posterior. In Jamoytius, the subrectangles have previously been interpreted as internal, akin to the branchial basket of lampreys (Ritchie 1963, 1968; Forey and Gardiner 1981; Janvier 1981) and as such would be lateral to the gills. The coincidence of the structures with the body margin makes them more comparable with cartilaginous trematic rings surrounding the external branchial openings. The Jamoytius subrectangles are, however, contiguous and numerous, unlike the trematic rings of lampreys. The apparent variability in the number of paired branchial openings (10 or more pairs) may be because of the nature of preservation of these features but could also reflect real differences in the number of branchial structures; intraspecific variation in the number of branchial units occurs in some jawless vertebrates (i.e. hagfishes). Taphonomy and composition. Since Ritchie’s (1963) description of Jamoytius, the features of the anterior have generally been accepted as components of a cartilaginous endoskeleton in part because of their inferred decay resistance and similarity to that of lampreys. Jawless vertebrate cartilages are quite varied in composition, both within and between clades (e.g. Wright et al. 1998; Zhang et al. 2006), and this variability affects their decay resistance (Sansom et al. 2010b). There are no definite fossil precedents for the preservation of cartilage as organic films (Euphanerops remains equivocal (Janvier and Arsenault 2002, 2007), whilst interpretations for conodonts (e.g. Aldridge and Theron 1993) have been made through comparison with Jamoytius). This does not in itself rule out Ritchie’s (1963, 1968) interpretation of a cartilaginous endoskeleton in Jamoytius, however. Without analytical determination of the biomolecular composition of these features (which may be impossible in these fossils), their interpretation must rely solely on comparative anatomy and comparative taphonomy. The uniform preservation of the anterior structures as dark, flat films, coupled with their carbonaceous composition, is consistent with organic preservation. Furthermore, their wrinkles and folds indicate flexibility at the time of collapse; the absence of evidence of brittle deformation indicates they were not rigid. Ductile deformation need not rule out their interpretation as cartilaginous supports for body openings (e.g. annular and trematic rings), because cartilage, including that of jawless vertebrates, can exist in both rigid and flexible forms, but it does prompt consideration of other potential body margin-related biomolecules. For example, high concentrations of melanin are found in association with SANSOM ET AL.: TAPHONOMY AND AFFINITY OF THE SILURIAN VERTEBRATE JAMOYTIUS photosensory structures of lampreys (e.g. optic capsules, pineal organ, lateral line system (Young 1981)) and other body openings (e.g. branchial (Bagenal 1973)). The distribution of melanin in lampreys is, therefore, consistent with the interpretation of the anterior structures of Jamoytius having originally had a high melanin content. Currently, we are unable to determine whether the anterior structures of Jamoytius were melanin or cartilage. Regardless of whether they represent cartilaginous supports for body openings or skin pigment surrounding the body openings, the anterior subcircles and subrectangles are still best interpreted as a mouth, nasal opening, eyes and external branchial openings. W-shaped structures Anatomical interpretations. A number of fossil jawless vertebrates exhibit serial V-, W- or Z-shaped bands along the body. These have been interpreted either as myomeres (e.g. Haikouichthys, conodonts) or external dermoskeletal scales (osteostracans, certain anaspids). Similarly, the Wshaped structures of Jamoytius have been interpreted as muscle blocks (Forey and Gardiner 1981; White 1946) and as scales, either mineralized (Ritchie 1960) or unmineralized, ‘horny’ and carbonized (Ritchie 1968, 1984). Others regard any interpretations of these structures as equivocal (Janvier 1981). The Ws of Jamoytius appear to be single units, rather than a series of subunits arranged in a W-shape, as is the case in the scales of most vertebrates. Euphanerops also shows long, undivided structures that run the height of its flank, yet it is uncertain whether they are scales or myomeres (Janvier and Arsenault 2007). Taphonomy and composition. The narrow zones of the Wshaped structures have undergone brittle deformation in the form of fracturing and displacement in several specimens (Text-fig. 4D), thus indicating that they were rigid prior to collapse or compaction. Interpretation of the Ws as scales is supported by their rigid nature, tubercular ornamentation, preservation in relief and coincidence with the body margin. The W-shaped structures are phosphatic and rigid, demonstrating a very different taphonomic history to the anterior features (carbonaceous composition and ductile deformation). It is important to consider whether the phosphate of the Ws is primary or secondary. Within the Jamoytius horizon, primary phosphate occurs, for example, in the dermal denticles of the thelodont Loganellia (Märss and Ritchie 1998) and secondary phosphate is known in the form of fibrous mineralized muscle in the arthropod Ainiktozoon (Van Der Brugghen et al. 1997). The texture and colour of the phosphate of Jamoytius 1403 does not directly compare to either of these phosphates, so its nature remains unclear. The fracturing of the scales does, however, support the hypothesis that the scales were biomineralized in vivo, prior to their deformation. No evidence is found for the muscle fibres identified by White (1946). It seems likely that this was a misinterpretation of the dendritic pattern of the broad zone (Ritchie 1968), which cannot be reconciled with any feature of a myomere (Text-fig. 4C). The dendritic pattern occurs on specimens that have not been treated with hydroflouric acid (contra Forey and Gardiner 1981), but not on any specimen that exhibits tubercles. The variation in the appearance of scales among specimens may, therefore, relate to the level of the splitting of the scale passing through different hard tissues. This is observed in some osteostracans (R. Sansom, pers. obs.), in which the middle layer of the dermoskeleton can be exposed revealing a dendritic pattern of ‘intra-areal’ canals (e.g. Denison 1947; Janvier 1996a; Sansom 2008). The relative thinness of the scales of Jamoytius, however, is difficult to reconcile with the hypothesis that the broad zone dendritic pattern represents a canal system. Alternatively, the pattern could be an artefact caused by taphonomic processes such as fracture because of post-mortem shrinkage of the broad zones. Axial lines with subunits Anatomical interpretation. The linear, dorsal and ventral axial lines and their continuation posteriorly as lines of rounded axial features should be assessed through comparison with antero-posterior axial structures known in vertebrates, i.e. notochord, dorsal nerve cord, gut and vertebral elements. The contiguous lozenge ⁄ oval subunits are not consistent with previous interpretations as a notochord and a gut (White 1946), or margins of a gut (Ritchie 1968). A further inconsistency is the anterior bifurcation of one of the lines (dorsal) that, contra to Ritchie (1968), is not part of the branchial basket (Textfig. 5). The internal pattern of subunits within the lines is more in keeping with interpretation as an axial skeleton. The contiguous nature of the subunits towards the anterior and increasing separation towards the posterior is comparable to the condition of the arcualia in lampreys (Marinelli and Strenger 1954). The rounded or lozenge shape of the elements in Jamoytius does not, however, match the irregularly shaped cartilaginous arcualia of either lampreys (a single series dorsal to notochord) or Euphanerops (dorsal and ventral series, Janvier and Arsenault 2007, fig. 16). Rather, they are more comparable to the ‘haemal series’ of Euphanerops, more specifically the lozenge-shaped subunits of the posterior haemal 1404 PALAEONTOLOGY, VOLUME 53 series. Although the notochord of modern jawless vertebrates (hagfish and lampreys) is wide, the gap between the dorsal and ventral axial lines of Jamoytius is proportionally far larger, potentially making interpretation as dorsal and ventral arcualia problematic. Furthermore, the anterior bifurcation of the dorsal line in NHM P12284 is inconsistent with interpretation as arcualia. Whilst it is not possible to determine precise homology of the dorsal and ventral axial lines because of their unusual shape and position, it is likely that they are formed by subunits of some form of axial skeleton, either arcualia in a previously unobserved condition or a ‘haemal series’ comparable to that of Euphanerops (Janvier and Arsenault 2007). Taphonomy and composition. If interpretation of the dorsal and ventral axial lines of Jamoytius as axial skeleton is accepted, then comparison with extant jawless vertebrates indicates the subunits were likely composed of cartilage. The seemingly different nature of the preservation of the axial lines from that of the anterior subcircles ⁄ subrectangles does not mean that they cannot both be composed of cartilage: lamprey branchial cartilages have a different composition from arcualial and neurocranial cartilages (Fernandes and Eyre 1999; Robson et al. 1997). Notochords interpreted in fossil jawless vertebrates such as Gilpichthys (Bardack and Richardson 1977) and conodonts (Aldridge et al. 1993) have a banded appearance, seemingly because of overprinting of the myomeres. In Jamoytius, evidence of myomeres is not preserved. Whilst the W-shaped scales have a periodicity similar to that of the axial line subunits, there are instances of the narrow zones overlying the subunits. The subunits of the axial lines of Jamoytius are, therefore, unlikely to be a taphonomic artefact because of scales or myomere overprinting. In FR 1601, the region between the dorsal and ventral axial lines is the only region of the body to preserve the W-shaped scales from both lateral sides of the body (Text-fig. 6A). A similar pattern is observed in latestage decay of larval lampreys (e.g. Sansom et al. 2010a), which, when viewed laterally, reveal myomeres from both lateral sides of the body within the region occupied by the wide notochord, but not the dorsal and ventral sections of the body (R. Sansom, pers. obs.). Long, thin, paired appendages (lateral fin folds) do not occur in any form in extant vertebrates (Bemis and Grande 1999), so we have compared the structures in Jamoytius to those known in fossil jawless vertebrates. Pharyngolepis (an anaspid) and Euphanerops possess long, thin, paired ‘appendages’, which extend along the ventrolateral surfaces from the head to the anal region (Janvier and Arsenault 2007; Ritchie 1964). In both of these taxa, there are mineralized components of the ventro-lateral appendages. Jamoytius lacks such mineralized structures, and the ventro-lateral ‘folds’ are probably simple folds of the skin. Taphonomy and composition. Interpretation of the dorsoventral ‘folds’ as folds of skin without any form of mineralized supports raises the question whether the paired features are true anatomical features or a taphonomic artefact. If the majority of the body surface was covered with rigid scales (W-shaped structures), the more flexible ventral surface in the gap between scales would be prone to deformation during collapse. This hypothetical taphonomic scenario is perhaps supported by the wrinkling that occurs within the ventro-lateral folds of some specimens, but their paired nature argues against it (Text-fig. 3). It is therefore unclear whether these folds are distinct anatomical structures or merely a consequence of body collapse; homologizing them with the ‘appendages’ of Pharyngolepis and Euphanerops is thus currently problematic. PHYLOGENETIC ANALYSIS The evidence presented above indicates that Jamoytius is a jawless vertebrate of uncertain affinities, so we have used the most recent and comprehensive analysis of early vertebrate interrelationships (Gess et al. 2006) as a basis to investigate its precise phylogenetic position. The matrix of Gess et al. (2006) is based upon earlier matrices (Janvier 1996b; Donoghue et al. 2000; Donoghue and Smith 2001), updated and expanded to include subsequently discovered soft-bodied vertebrates, namely Haikouichthys and Myllokunmingia (Shu et al. 1999; Donoghue et al. 2003; Hou et al. 2002), Mesomyzon (Chang et al. 2006) and Priscomyzon (Gess et al. 2006) as well as oral characters relating to cyclostome monophyly. Paired longitudinal ‘folds’ Anatomical interpretation. The paired parallel ‘folds’ on the ventro-lateral body margins (Text-fig. 3) have been the source of conflicting interpretations. Some authors regard them as ‘lateral fin folds’ (Janvier 1981; Ritchie 1968; White 1946), whilst others find no evidence to support that view (Forey and Gardiner 1981; Westoll 1958). Coding. The coding used for Jamoytius by Donoghue et al. (2000) and subsequently by Donoghue and Smith (2001) and Gess et al. (2006) was based upon an earlier unpublished version of the data presented here (Freedman 1999), not all of which has survived subsequent scrutiny. Thus, the coding has been modified to reflect the interpretations herein (e.g. Table 1; Appendix S1). SANSOM ET AL.: TAPHONOMY AND AFFINITY OF THE SILURIAN VERTEBRATE JAMOYTIUS The matrix has also been updated to include additional data for Euphanerops (Janvier and Arsenault 2007), Haikouichthys (Zhang and Hou 2004), Arandaspida (Sansom et al. 2005) and Galeaspida (Wang et al. 2005). Euphanerops is taken to include Legendrelepis and Endiolepis (Janvier 1996c; Janvier and Arsenault 2007). Two taxa from the Middle Devonian of Scotland that have been proposed to have affinities with Jamoytius have been added to the matrix: Cornovichthys (Newman and Trewin 2001) and Achanarella (Newman 2002). Gess et al. (2006) employed presence ⁄ absence coding. Such coding methodology violates the requirements of logical independence of characters and can lead to false support for a cladogram (Strong and Lipscomb 1999; Forey and Kitching 2000). For example, absence of a nasohypophyseal opening is counted twice in two different characters (15 ⁄ 16), as is absence of dentine (80 ⁄ 81). The matrix presented here therefore utilizes contingent coding, A Forey 1995 Janvier 1996b Myxinoidea Petromyzontida Jamoytius Anaspida Ostraco/Jawed B 1 2 1 1 1 1 1 1 1 1 2 2 2 which necessitates the erection of additional characters (Appendix S1: characters 100–109). Furthermore, revision of the coding and coding strategy for the characters relating to the relationships of extant cyclostomes reveals that many of the physiological and miscellaneous characters are uninformative (P. C. J. Donoghue, unpublished data). These characters are removed here, whilst some of the neurological characters are revised (e.g. cerebellar primordia, retina). Results. Heuristic searches, including all taxa, found two most parsimonious trees of branch length 185 (Textfig. 9B). Jamoytius is placed as sister taxon to Euphanerops, united by a ventral mouth and annular cartilage (both homoplastic characters). These taxa (which could together be termed Jamoytiiformes Tarlo, 1967) are resolved as stem-gnathostomes because of their trunk dermal skeleton, separate anal fin and paired fin folds. Donoghue et al. 2000 Donoghue et al. 2001 Shu et al. 2003 Myxinoidea Petromyzontida Euphanerops Jamoytius Anaspida Ostraco/Jawed 1 1 1 1 3 Myxinoidea Petromyzontida Euconodonta Pteraspidimorphi Euphanerops Jamoytius Anaspida Ostraco/Jawed Tunicata Cephalochordata Myxinoidea Myxinikela Haikouichthys Cornovichthys Petromyzontida Mesomyzon Priscomyzon Mayomyzon Euconodonta Achanarella Jamoytius Euphanerops Anaspida Loganellia Turinia Heterostraci Arandaspida Astraspis Galeaspida Osteostraci Jawed Vertebrates 1405 Myxinoidea Petromyzontida Euconodonta Euphanerops Jamoytius Anaspida Ostraco/Jawed Myxinoidea Petromyzontida Euconodonta Pteraspidimorphi Euphanerops Jamoytius Anaspida Ostraco/Jawed C 2 1 1 1 1 1 1 1 1 1 2 1 1 1 1 1 1 2 Gess et al. 2006 Myxinoidea Petromyzontida Euphanerops Euconodonta Jamoytius Anaspida Ostraco/Jawed Tunicata Cephalochordata Haikouichthys Cornovichthys Myxinoidea Myxinikela Petromyzontida Mesomyzon Priscomyzon Mayomyzon Euconodonta Achanarella Jamoytius Euphanerops Anaspida Loganellia Turinia Heterostraci Arandaspida Astraspis Galeaspida Osteostraci Jawed Vertebrates T E X T - F I G . 9 . Phylogenetic relationships of Jamoytius. A, simplified versions of previous cladistic analyses of Forey (1995), Janvier (1996b), Donoghue et al. (2000), Donoghue and Smith (2001), Shu et al. (2003), and Gess et al. (2006) where Ostraco ⁄ Jawed represents other ostracoderms and jawed vertebrates. B, single most parsimonious tree from the unconstrained phylogenetic analysis with decay support indices. C, Strict consensus of trees resulting from analysis constrained for cyclostome monophyly with decay indices. 1406 PALAEONTOLOGY, VOLUME 53 Whether Jamoytius preserves these latter two characters is uncertain, but the same topology results when the paired appendages of Jamoytius are coded as unknown. Jamoytiiformes are placed closer to the root of total-group gnathostomes than Anaspida because of an absence of dermal head covering, dentine and lamellar aspidin. Close relationships between Jamoytius and Euphanerops have been reconstructed in previous phylogenetic studies (Janvier 1996a–c; Donoghue et al. 2000; Donoghue and Smith 2001; Shu et al. 2003), but always as part of a clade with Anaspida (Text-fig. 9A). Of the other taxa proposed to have jamoytiiform affinities, Cornovichthys is placed as a stem-vertebrate (in the sense that Petromyzontida and Gnathostomata comprise Vertebrata, whilst vertebrates and Myxinoidea constitute Craniata (Janvier (1981)), whilst Achanarella is placed as a stem-gnathostome in a more basal position than (Jamoytius + Euphanerops). Neither taxon is, therefore, resolved as part of a monophyletic Jamoytiiformes. The revisions incorporated in the data matrix used here also led to other changes in relationships among jawless vertebrates. Changing the coding strategy for dentine and odontodes has led to the thelodonts (represented here by Loganellia and Turinia) being identified as closer to the root of total-group gnathostomes than the pteraspidimorphi (represented here by Heterostraci, Arandaspida and Astraspis) on the gnathostome stem lineage. Furthermore, eucondonts are placed as sister taxon to fossil and extant lampreys, making conodonts stem-petromyzontids. Lampreys and euconodonts are united by possession of transversely biting teeth. Morphological evidence, both neontological and palaeontological, consistently finds lampreys (Petromyzontida) as more closely related to jawed vertebrates than hagfishes (Myxinoidea), as is the case here (Løvtrup, 1977; Janvier, 1981; Forey, 1984; Khonsari et al. 2009). Molecular investigations, however, identify the lampreys as more closely related to the hagfishes and thus support cyclostome monophyly (e.g. Delarbre et al. 2002; Delsuc et al. 2006). Phylogenetic analysis of our data matrix constrained for cyclostome monophyly identifies a less parsimonious solution (branch length 191) with a topology very similar to that of the unconstrained analysis, differing only in placement of the myxinoids and resolution amongst petromyzontids (Text-fig. 9C). The Jamoytiiformes are still recovered as stem-gnathostomes, whilst the euconodonts are recovered as stem-cyclostomes. EVOLUTIONARY IMPLICATIONS Jamoytius is commonly considered to represent a primitive member of a fossil or extant vertebrate clade, either a primitive anaspid (e.g. Ritchie 1963) or an ancestral lam- prey (e.g. Mallat 1984). Despite the fact that a number of its characters are plesiomorphic for chordates or for vertebrates, analysis here establishes sister taxon relationship with Euphanerops. In our unconstrained analysis, Jamoytiiformes represent a new grade in the evolution of stem-gnathostomes, after the evolution of a trunk dermal skeleton but before the evolution of lamellar aspidin and dermal head skeleton. Given the preservation of trunk dermoskeleton of Jamoytius (W-shaped scales), it is reasonable to assume that any head dermoskeleton would also be preserved if it had existed. The coding for absence of head dermoskeleton in Jamoytius, and subsequent placement of Jamoytiiformes on the gnathostome stem, therefore reflects phylogenetic absence rather than taphonomic loss (see Donoghue and Purnell 2009 for a discussion of alternative meanings of stem assignments). The position of Cornovichthys as a stem-vertebrate is supported by only one character (anterior otic capsules), the interpretation of which is equivocal in some taxa. The stem placements of Cornovichthys and Achanarella are likely to reflect taphonomic bias resulting from loss of characters through post-mortem decay (Donoghue and Purnell 2009; Sansom et al. 2010a, b). To further resolve the relationships of the Jamoytiiformes and putatively related taxa, reinterpretation of the relevant fossils is required using the same principles as applied here for Jamoytius. The phylogenetic placement of conodonts as stem-lampreys or stem-cyclostomes is contrary to the hypotheses from previous analyses in which conodonts are placed as stem-gnathostomes (Donoghue et al. 2000; Donoghue and Smith 2001). The new placement is not robust, but it is the most parsimonious on the basis of the morphological data analysed here. The instability of this result suggests that addition of further soft-bodied taxa to phylogenetic matrices of early vertebrates will potentially affect hypotheses of euconodont affinity. Our phylogenetic analysis does not raise any doubts about the placement of euconodonts within the vertebrates. Other stem-gnathostome taxa such as Pteraspidomorphi, Galeaspida and Osteostraci are resolved to be closer to the gnathostome crown than thelodonts. This proposal differs from previous suggestions of thelodont sister relationships with gnathostomes (Märss et al. 2007), chondrichthyes (Turner 1991) or the group (Galeaspida + Osteostraci + jawed vertebrates) (Donoghue and Smith 2001). Given the limited number of thelodont taxa included here, however, questions of thelodont affinity remain open to further investigation. Jamoytius has often been cited in defence of the lateral fin fold theory (e.g. Jarvik 1980; Shubin et al. 1997), an evolutionary developmental scenario in which the paired appendages of jawed vertebrates derive from continuous ventro-lateral fin folds of jawless vertebrates by the loss of SANSOM ET AL.: TAPHONOMY AND AFFINITY OF THE SILURIAN VERTEBRATE JAMOYTIUS the intermediate portion of the fin fold (Balfour 1876; Thacher 1877; reviewed by Coates 1994; Bemis and Grande 1999). The present study found no evidence for any skeletal or muscular structures that would allow an assessment of potential homologies with the paired fins of jawed vertebrates. Furthermore, the antero-posterior skin folds may represent taphonomic artefacts. Our results indicate that the structures of anaspids, thelodonts and potentially Jamoytius were acquired independently of paired fins restricted to the pectoral region in Osteostraci and Gnathostomata (Sansom 2009). CONCLUSIONS The study of the anatomy of problematic organisms can be aided by the use of a methodology designed to separate topological and morphological reconstruction from anatomical interpretation and to gather as much information as possible about the preserved features through taphonomic analyses. The application to Jamoytius demonstrates that it is a vertebrate, with preserved W-shaped phosphatic scales, ten or more paired external branchial openings, dorso-lateral optic capsules, a round ventral mouth, a terminal nasal opening, and, potentially, dorsal and ventral axial skeleton. Interpretations of paired fins remain equivocal. Analyses of the phylogenetic affinity of Jamoytius identify a sister taxon relationship with Euphanerops. This clade, the Jamoytiiformes, is a primitive group of stem-gnathostomes and does not form a clade with the Anaspida. Acknowledgements. This work was funded in part by a Natural Environment Research Council grant (NE ⁄ E015336 ⁄ 1 to SEG and MAP). KF was supported by an Overseas Research Student award (ORS ⁄ 96014039) and by R. A. Freedman. Various people are thanked for their assistance in enabling the study and loan of material including Sir Frederick Stewart, Peder Aspen (University of Edinburgh), Neil Clark (Hunterian Museum), Bobbie Paton, Liz Hide and Mike Taylor (National Museum of Scotland), Sally Young, Peter Forey and Martha Ritcher (Natural History Museum, London), Robert Jones and Alex Ritchie (Australian Museum) and Steve Tunnicliff (British Geological Survey). Tony Milodowski and Paul Wetton (British Geological Survey) kindly assisted with SEM analysis. We also appreciate the constructive comments of three anonymous reviewers and Philip Donoghue, which have allowed us to improve the manuscript. Editor. Philip Donoghue SUPPORTING INFORMATION Additional Supporting Information may be found in the online version of this article: 1407 Data S1. Previous interpretations of the affinity of Jamoytius. Appendix S1. Character list and matrix used in phylogenetic analysis – an updated version of Gess et al. (2006) with neurological characters adapted according to P. Donoghue (unpublished data). Please note: Wiley-Blackwell are not responsible for the content or functionality of any supporting materials supplied by the authors. Any queries (other than missing material) should be directed to the corresponding author for the article. REFERENCES A L D R I D G E , R. J. and T H E R O N , J. N. 1993. Conodonts with preserved soft tissue from a new Ordovician KonservatLagerstätte. Journal of Micropalaeontology, 12, 113–117. —— B R I G G S , D. E. G., S M I T H , M. P., C L A R K S O N , E. K. and C L A R K , N. D. L. 1993. The anatomy of conodonts. Philosophical Transactions of the Royal Society of London, Series B, 340, 405–421. B A G E N A L , T. B. 1973. Identification of British fishes. Houlton Educational Publications, Amsterdam, 199 pp. B A L F O U R , F. M. 1876. Monograph on the development of elasmobranch fishes. Journal of Anatomy and Physiology, 10, 377–441. B A R D A C K , D. and R I C H A R D S O N , E. R. 1977. New agnathous fishes from the Pennsylvanian of Illinois. Fieldiana Geology, 33, 489–510. B E M I S , W. E. and G R A N D E , L. 1999. Development of the median fins of the North American paddlefish (Polyodon spathula), and a reevaluation of the lateral fin-fold hypothesis. 41–68. In A R R A T I A , G. and S C H U L T Z E , H. P. (eds). Mesozoic fishes 2 – systematics and fossil record. Verlag Dr. Friedrich Pfeil, München, 604 pp. B R I G G S , D. E. G. and C L A R K S O N , E. K. 1987. An enigmatic chordate from the Lower Carboniferous Granton ‘shrimp-bed’ of the Edinburgh district, Scotland. Lethaia, 20, 107–115. —— and W I L L I A M S , S. H. 1981. The restoration of flattened fossils. Lethaia, 14, 157–164. B U T T E R F I E L D , N. J. 2002. Leanchoilia guts and the interpretation of three-dimensional structures in Burgess Shale-type fossils. Paleobiology, 28, 155–171. C H A N G , M.-M., Z H A N G , J.-Y. and M I A O , D. 2006. A lamprey from the Cretaceous Jehol biota of China. Nature, 441, 972–974. C O A T E S , M. I. 1994. The origin of vertebrate limbs. Development, 120 (Suppl. 1), 169–180. D E L A R B R E , C., G A L L U T , C., B A R R I E L , V., J A N V I E R , P. and G A C H E L I N , G. 2002. Complete mitochondrial DNA of the hagfish, Eptatretus burgeri: the comparative analysis of mitochondrial DNA sequence strongly supports the cyclostome monophyly. Molecular Phylogenetics and Evolution, 22, 184–192. D E L S U C , F., B R I N K M A N N , H., C H O U R R O U T , D. and P H I L I P P E , H. 2006. Tunicates and not cephalochordates are the closest living relatives of vertebrates. Nature, 439, 965–968. 1408 PALAEONTOLOGY, VOLUME 53 D E N I S O N , R. H. 1947. The exoskeleton of Tremataspis. American Journal of Science, 245, 337–365. D O N O G H U E , P. C. J. and P U R N E L L , M. A. 2009. Distinguishing heat from light in debate over controversial fossils. BioEssays, 31, 178–189. —— and S M I T H , M. P. 2001. The anatomy of Turinia pagei (Powrie), and the phylogenetic status of the Thelodonti. Transactions of the Royal Society of Edinburgh: Earth Sciences, 92, 15–37. —— F O R E Y , P. L. and A L D R I D G E , R. J. 2000. Conodont affinity and chordate phylogeny. Biological Reviews, 75, 191– 251. —— S M I T H , M. P. and S A N S O M , I. J. 2003. The origin and early evolution of chordates: molecular clocks and the fossil record. 190–223. In D O N O G H U E , P. C. J. and S M I T H , M. P. (eds). Telling the evolutionary time: molecular clocks and the fossil record. CRC Press, London, 288 pp. F E R N A N D E S , R. J. and E Y R E , D. R. 1999. The elastin-like protein matrix of lamprey branchial cartilage is cross-linked by lysyl pyridinoline. Biochemical and Biophysical Research Communications, 261, 635–640. F I T Z H U G H , K., S R O K A , S. D., K R U T Y , S., H E N D E R S O N , M. B. and H A Y , A. A. 1997. Polychaete worms. 64–83. In S H A B I C A , C. W. and H A Y , A. A. (eds). Richardson’s guide to the fossil fauna of Mazon Creek. Northeastern Illinois University, Chicago, 308 pp. F O R E Y , P. L. 1984. Yet more reflections on agnathangnathostome relationships. Journal of Vertebrate Paleontology, 4, 330–343. —— 1995. Agnathans recent and fossil, and the origin of jawed vertebrates. Reviews in Fish Biology and Fisheries, 5, 267–303. —— and G A R D I N E R , B. G. 1981. J. A. Moy-Thomas and his association with the British Museum (Natural History). Bulletin of the British Museum (Natural History). Geology, 35, 131– 144. —— and J A N V I E R , P. 1993. Agnathans and the origin of jawed vertebrates. Nature, 361, 129–134. —— and K I T C H I N G , I. J. 2000. Experiments in coding multistate characters. 54–80. In S C O T L A N D , R. and P E N N I N G T O N , R. T. (eds). Homology and systematics: coding characters for phylogenetic analysis. Taylor and Francis ⁄ Systematics Association, London, 217 pp. F R E E D M A N , K. 1999. Aspects of the taphonomy of jawless vertebrates. Unpublished PhD thesis, University of Leicester, 166 pp. G A B B O T T , S. E., H O U , X.-G., N O R R Y , M. J. and S I V E T E R , D. J. 2004. Preservation of Early Cambrian animals of the Chengjiang biota. Geology, 32, 901–904. G E S S , R. W., C O A T E S , M. I. and R U B I D G E , B. S. 2006. A lamprey from the Devonian period of South Africa. Nature, 443, 981–984. H O U , X.-G., A L D R I D G E , R. J., S I V E T E R , D. J., S I V E T E R , D. J. and F E N G , X.-H. 2002. New evidence on the anatomy and phylogeny of the earliest vertebrates. Proceedings of the Royal Society of London. Series B, Biological Sciences, 269, 1865–1869. J A N V I E R , P. 1981. The phylogeny of the Craniata, with particular reference to the significance of fossil ‘agnathans’. Journal of Vertebrate Paleontology, 1, 121–159. —— 1996a. Early vertebrates. Clarendon Press, Oxford, 393 pp. —— 1996b. The dawn of the vertebrates: characters versus common ascent in the rise of current vertebrate phylogenies. Palaeontology, 39, 259–287. —— 1996c. The Miguasha ‘Anaspida’. 134–140. In S C H U L T Z E , H. P. (ed.). Devonian fishes and plants of Miguasha, Quebec, Canada. Verlag Dr. Friedrich Pfeil, Munich, 374 pp. —— and A R S E N A U L T , M. 2002. Calcification of early vertebrate cartilage. Nature, 417, 609. —— —— 2007. The anatomy of Euphanerops longaevus Woodward, 1900, an anaspid-like jawless vertebrate from the Upper Devonian of Miguasha, Quebec, Canada. Geodiversitas, 29, 143–216. —— and B U S C H , R. M. 1984. Jamoytius-like vertebrates from the Lower Devonian Manlius Formation of New York State. Journal of Vertebrate Paleontology, 4, 501–506. J A N V I E R , P. and L U N D , R. 1983. Hardistiella montanensis n.gen. et sp. (Petromyzontida) from the Lower Carboniferous of Montana, with remarks on the affinities of lampreys. Journal of Vertebrate Paleontology, 2, 407–413. J A R V I K , E. 1980. Basic structure and evolution of vertebrates, Vol. 2. Academic Press, London, 337 pp. K H O N S A R I , R. H., L I , B., V E R N I E R , P., N O R T H C U T T , R. G. and J A N V I E R , P. 2009. Agnathan brain anatomy and craniate phylogeny. Acta Zoologica, 90 (Suppl. 1), 52–68. L Ø V T R U P , S. 1977. The phylogeny of Vertebrata. Wiley and Sons, London, 330 pp. M A D D I S O N , D. R. and M A D D I S O N , W. P. 2003. MacClade 4.06. Sinauer Associates, Sunderland, MA. M A L L A T , J. 1984. Feeding ecology of the earliest vertebrates. Zoological Journal of the Linnean Society, 82, 261–272. M A R I N E L L I , W. and S T R E N G E R , A. 1954. Vergleichende Anatomie und Morphologie der Wirberltiere, Heft I. Lampetra fluviatilis. Franz Deuticke, Vienna, 78 pp. M Ä R S S , T. and R I T C H I E , A. 1998. Articulated thelodonts (Agnatha) of Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences, 88, 143–195. E - T A L I M A A , V. N. —— T U R N E R , S. and K A R A T A J UT 2007. ‘‘Agnatha’’ II: Thelodonti. Handbook of Paleoichthyology, Vol. 1B. Verlag Dr. Friedrich Pfeil, München, 143 pp. N E W M A N , M. J. 2002. A new naked jawless vertebrate from the Middle Devonian of Scotland. Palaeontology, 45, 933– 941. —— and T R E W I N , N. H. 2001. A new jawless vertebrate from the Middle Devonian of Scotland. Palaeontology, 44, 43–51. P U R N E L L , M. A. and D O N O G H U E , P. C. J. 1999. Flattened fossils, physical modelling and the restoration of collapsed skeletons. 91–99. In S A V A Z Z I , E. (ed.). Functional morphology of the invertebrate skeleton. John Wiley & Sons, Chichester, 706 pp. R I E P P E L , O. and K E A R N E Y , M. 2002. Similarity. Biological Journal of the Linnean Society, 75, 59–82. R I T C H I E , A. 1960. A new interpretation of Jamoytius kerwoodi White. Nature, 188, 647–649. SANSOM ET AL.: TAPHONOMY AND AFFINITY OF THE SILURIAN VERTEBRATE JAMOYTIUS —— 1963. Palaeontological studies on Scottish Silurian fish beds. Unpublished thesis, University of Edinburgh. —— 1964. New light on the morphology of the Norwegian Anaspida. Skrifter Utgitt Av Det Norske Videnskaps-Akademi I Oslo 1. Matematisk-Naturvidenskapelige Klasse, 14, 5–35. —— 1968. New evidence on Jamoytius kerwoodi White, an important ostracoderm from the Silurian of Lanarkshire, Scotland. Palaeontology, 11, 21–39. —— 1984. Conflicting interpretations of the Silurian agnathan, Jamoytius. Scottish Journal of Geology, 20, 249–256. —— 1985. Ainiktozoon loganese Scourfield, a protochordate from the Silurian of Scotland. Alcheringa, 9, 115–142. R O B S O N , P., W R I G H T , G. M., Y O U S O N , J. H. and K E E L E Y , F. W. 1997. A family of non-collagen-based cartilages in the skeleton of the sea lamprey, Petromyzon marinus. Comparative Biochemistry and Physiology Part B: Biochemistry and Molecular Biology, 118, 71–78. S A N S O M , I. J., D O N O G H U E , P. C. J. and A L B A N E S I , G. 2005. Histology and affinity of the earliest armoured vertebrate. Biology Letters, 1, 446–449. S A N S O M , R. S. 2008. The origin and early evolution of the Osteostraci (Vertebrata): a phylogeny for the Thyestiida. Journal of Systematic Palaeontology, 6, 317–332. —— 2009. Phylogeny, classification and character polarity of the Osteostraci (Vertebrata). Journal of Systematic Palaeontology, 7, 95–115. —— G A B B O T T , S. E. and P U R N E L L , M. A. 2010a. Nonrandom decay of characters causes bias in fossil interpretation. Nature, 463, 797–800. —— —— —— 2010b. Decay of vertebrate characters in hagfish and lamprey (Cyclostomata) and the implications for the vertebrate fossil record. Proceedings of the Royal Society B-Biological Sciences, doi: 10.1098/rspb.2010.1641. S H U , D.-G., C O N W A Y - M O R R I S , S., H A N , J., Z H A N G , Z.-F., Y A S U I , K., J A N V I E R , P., C H E N , L., Z H A N G , X.L., L I U , J.-N. and L I U , H.-Q. 2003. Head and backbone of the Early Cambrian vertebrate Haikouichthys. Nature, 421, 536–539. —— L U O , H.-L., C O N W A Y - M O R R I S , S., Z H A N G , X.-L., H U , S.-X., C H E N , L., H A N , J., Z H U , M. and C H E N , L.-Z. 1999. Lower Cambrian vertebrates from South China. Nature, 402, 42–46. S H U B I N , N., T A B I N , C. and C A R R O L L , S. 1997. Fossils, genes and the evolution of animal limbs. Nature, 388, 639– 648. S T R O N G , E. and L I P S C O M B , D. 1999. Character coding and inapplicable data. Cladistics, 15, 363–371. 1409 S W O F F O R D , D. L. 2002. PAUP*. Phylogenetic Analysis Using Parsimony (*and other methods) Version 4. Sinuaer Associates, Sunderland, MA. T A R L O , L. B. H. 1967. Agnatha. 629–636. In H A R L A N D , W. B. (ed.). The fossil record. London Geological Society, London, 827 pp. T H A C H E R , J. K. 1877. Median and paired fins, a contribution to the history of vertebrate limbs. Transactions of the Connecticut Academy of Arts and Science, 3, 281–310. T U R N E R , S. 1991. Monophyly and interrelationships of the Thelodonti. 87–119. In C H A N G , M.-M., L I U , Y.-H. and Z H A N G , G.-R. (eds). Early vertebrates and related problems of evolutionary biology. Science Press, Beijing, 514 pp. V A N D E R B R U G G H E N , W., S C H R A M , F. R. and M A R T I L L , D. M. 1997. The fossil Ainiktozoon is an arthropod. Nature, 385, 589–590. W A N G , N.-Z., D O N O G H U E , P. C. J., S M I T H , M. M. and S A N S O M , I. J. 2005. Histology of the galeaspid dermoskeleton and endoskeleton, and the origin and early evolution of the vertebrate cranial endoskeleton. Journal of Vertebrate Paleontology, 25, 745–756. W E S T O L L , T. S. 1958. The lateral fin-fold theory and the pectoral fins of ostracoderms and early fishes. 180–211. In W E S T O L L , T. S. (ed.) Studies on fossil vertebrates. The Athlone Press, London, 263 pp. W H I T E , E. I. 1946. Jamoytius kerwoodi, a new chordate from the Silurian of Lanarkshire. Geological Magazine, 83, 89– 97. W O O D W A R D , A. S. 1900. On a new ostracoderm (Euphanerops longaevus) from the Upper Devonian of Scaumenac Bay, Province of Quebec, Canada. Magazine of Natural Hitsory, ‘series 7, 5, 416–419. W R I G H T , G. M., K E E L E Y , F. W. and D E M O N T , M. E. 1998. Hagfish cartilage. 160–170. In J Ø R G E N S E N , J. M., L O M H O L T , J. P., W E B E R , R. E. and M A L T E , H. (eds). The biology of hagfishes. Chapman and Hall, London, 578 pp. Y O U N G , J. Z. 1981. The life of vertebrates. Clarendon Press, Oxford, 645 pp. Z H A N G , G.-J., M I Y A M O T O , M. M. and C O H N , M. J. 2006. Lamprey type II collagen and Sox9 reveal an ancient origin of the vertebrate collagenous skeleton. Proceedings of the National Academy of Sciences, 103, 3180–3185. Z H A N G , X.-G. and H O U , X.-G. 2004. Evidence for a single median fin-fold and tail in the Lower Cambrian vertebrate, Haikouichthys ercaicunensis. Journal of Evolutionary Biology, 17, 1162–1166. SUPPLEMENTARY INFORMATION This chronological list (compiled by K. Freedman, post 1997 updated by R. Sansom) includes the published diagnoses and amendments to diagnoses of Jamoytius, as well as other descriptive/interpretative comments and suggested affinities. When a particular author has referred to Jamoytius in a similar way in more than one work, these references are covered together at the earliest date. An attempt has been made to include all references that presented new information, interpretations, or suggestions of affinities of Jamoytius, including all cladistic analyses. Not all of the many references to Jamoytius in textbooks, however, are itemized below, although some examples from popular texts are given. Woodward (on specimen label) wrote ‘Allied to Lasanius’. White (1946, p. 96) gave the following diagnosis: ‘Fossil Agnatha without armour or endoskeletal calcification; notochord persistent; simple lateral fin folds present; median fin fold represented by elongated dorsal and anal fins. Eyes probably simple, very large and anteriorly placed. Muscle-segments simple and numerous with a single flexure and undivided by horizontal septum. Mouth ? terminal; intestine short and straight.…rounded, rather elongate bodied but somewhat flattened head region; anterior margin of head transverse and eyes marginal. Dorsal fin continuous over hinder two-thirds of body; anal fin one-quarter as long, remote.’ White (1946) considered Jamoytius as ‘a conservative element of the main stock from which the various groups of craniate chordates arose’ (p. 95). Gregory (1951, p. 105) stated, ‘[Jamoytius] had long horizontal lateral fin-folds, running from behind the very small head to the base of the tapering tail, which, however, was not turned downward as it was in Anaspids. There was a long spineless dorsal fin and a shorter anal fin. The skin was apparently very thin and without armour. The internal skeleton seems to have been cartilaginous.’ He followed White (1946) in favouring Jamoytius as an ancestor to amphioxus [=Branchiostoma] and added that amphioxus might be related to the anaspids. Wängsjö (1952, p. 566) questioned White’s (1946) interpretation of the notochord and suggested that Jamoytius could be a larval or naked thelodont. Robertson (1953, pp 730, 734) described Jamoytius as an unarmoured form with paired fin folds. Robertson (1953) also said that Wängsjö placed Jamoytius with the Euphaneropidae in the anaspids. Wängsjö (1952), however, had argued that the shape of the head, with anteriorly placed eyes, excluded Jamoytius from the anaspids. White (1958) and Ritchie (1968) later quoted Robertson (1953) as assigning Jamoytius to euphaneropsid anaspids. Berg (1955, p. 25) classified Jamoytius as an anaspid, sharing an order with Endeiolepis aneri Stensiö, 1939 (but not Euphanerops). Berrill (1955, pp 200-215) accepted White’s (1946) interpretation and agreed in regarding Jamoytius as a primitive chordate, but proposed that the mouth was ventral and ‘considerably subterminal’ (p. 204) and that Jamoytius had amphioxus-like mouth structures and atrial cavity. Berrill (1955) also held that Jamoytius would have had lens-less eyes. 1 Denison (1956, p. 424) was ‘inclined to interpret this form quite differently [from White (1946)], considering it to be for its time an advanced, though not necessarily highly specialized, vertebrate. The absence of dermal armor, the fusiform body, the presence of long lateral and dorsal fin folds (if they really do exist), the highly developed metamerism, and the large eyes are all characters of a very active, fastswimming vertebrate, functionally more progressive than most of its contemporaries.’ Lehman (1957, pp 175-176) reviewed White (1946) and Stensiö (1958), compared Jamoytius with Endeiolepis, and considered Jamoytius as a possible anaspid. Robertson (1957, p. 167) followed White’s (1946) interpretation. Stensiö (1958, pp 238-240) regarded Jamoytius as an anaspid and provided the following amended diagnosis, here translated from the French: (External branchial openings unknown.) Scales of the dorsal crest absent and dorsal swimming fold is probably differentiated in a long, dorsal fin. Dorsolateral ranges of scales of the flank are very thin, especially distinctive by their internal ribs and their ornamentation, of an ordinary type, with an angular flexure. Lateral swimming fold is probably without exoskeleton. Anal fin probably fairly long. (Ranges of dorsoventral pre-branchial scales unknown.). Stensiö 1964 (pp 171-172) repeated this diagnosis. Smith (1957, p. 394), referring to Stensiö’s (1958) paper while in the press, concurred with his interpretation of scales and assignment to the anaspids. Smith (1957) added that the structures interpreted by White (1946) as ‘myocommata are the thickened, basal, dorso-ventral ridges of the scales’. Westoll (1958, pp 196-197) considered Jamoytius as a chordate without an exoskeleton and with little or no endoskeleton. He discussed White’s (1946) interpretation and recommended that the features identified by White as lateral fin folds could be better interpreted as dorsal and anal fins. White (1958, p. 229) noted that his interpretations and suggested affinity for Jamoytius had not been widely accepted by palaeontologists and discussed the work of Gregory (1951), Wängsjö (1952), and Robertson (1953). White (1958), however, still argued that Jamoytius ‘was the conservative derivative of the ancestor of them all.’ Ritchie (1960, p. 649), based on newly discovered material and reexamination of the type specimens, judged Jamoytius to have ‘…exoskeletal ossification (scales); lateral eyes; terminal, subcircular mouth; branchial apparatus not unlike that in the Anaspida and the living cyclostomes; fin rays in the lateral fin-folds; a hypoceral (?) tail.’ Jamoytius ‘shows a close relationship with the Anaspida…but of all the known fossil Agnatha, Jamoytius would seem to be the closest to the living Cyclostomata.’ Tarlo (1960, p. 117) followed Stensiö’s (1958) attribution of Jamoytius to the anaspids and his consideration that White’s (1946) ‘muscles' were scales with anaspid-like ornamentation. Tarlo (1960) added that the structures described by White (1946) as dorsal fin rays were dorsal ridge scales, but he accepted White’s (1946) interpretation of the notochord and intestine. 2 Swinton (1961, p. 36) figured a reconstruction of Jaymoytius [sic], based on White (1946), as a possible ‘relation of the very early vertebrates’. Ritchie (1963, pp 50-65, figs 10.2-10.3, and pls 15-22) described an annular cartilage in a near terminal position, cartilaginous eye capsules, and a cartilaginous, horizontally-aligned, ventrolateral branchial basket lying just behind the eyes with up to 15 gill pouches. He identified a tentative nasal structure, scales with ‘posthumous cracking’ (p. 59) composed of a horny epidermal material and tubercles in the interscale spaces, a long and straight intestine, possible lateral fin folds, a possible dorsal fin, and a probably hypoceral tail. Jamoytius ‘resembles closely the known anaspids and the living cyclostomes’ (p. 64), so Ritchie (1963) regarded Jamoytius as an unusual and primitive member of the anaspids. Dechaseaux (1963, pp 325, 328-330) concluded that Jamoytius could definitely be attributed to the agnathan vertebrates and could not be an ancestor to amphioxus. Deschaseaux (1963) subscribed to Ritchie’s (1960) view that, of all known fossil aganthans, Jamoytius most closely compared to the extant agnathans, but could still relate to the anaspids. Lehman (1964, pp 83-85) reviewed White (1946), Stensiö (1958), Berrill (1955), and Ritchie (1960) and accepted Ritchie’s (1960) interpretation and suggestion of affinity. Romer (1966, pp 17, 347R; 1968, p. 25) and Romer and Parson (1986, pp 43, 231) classified Jamoytius as an anaspid. Romer (1966) noted the presence of bony scales. Romer and Parson (1986) recognized separate gill openings, a lamprey-like branchial basket, and a single median nostril. Carter (1967, pp 26, 38-39) regarded Jamoytius as an anaspid or their close relative and remarked that it had an anaspid-like ventrolateral fin. Ritchie (1968) diagnosed Jamoytius as having an annular cartilage, sclerotic cartilages, cyclostome-like branchial basket, lateral trunk scales of unusual structure and composition, continuous dorsal fin and lateral fin folds, and probable hypocercal caudal fin. He deemed Jamoytius a ‘…cephalaspidomorph agnathan closely related to the anaspids and the living cyclostomes’ (p. 21) Bardack and Zangerl (1968, p. 1267) reported that ‘Jaymoytius [sic] has cyclostome characters such as a sub-terminal mouth, circular mouth and a branchial basket that begins behind the orbit; but Jaymoytius [sic] retains lateral fin folds, body scales, lacks a piston, and has 15 or more gill slits.’ They considered Jamoytius a possible ancestor to the lampreys. Bardack and Zangerl 1971 (p. 82) also noted the possible presence of an annular cartilage and established Jamoytius ‘…closer to cyclostome ancestry than the more usual Devonian anaspids…’ Colbert (1969, p. 17) said that Jamoytius ‘appears to be a very primitive jawless vertebrate, perhaps, occupying a position close to the ancestry of the lamprey and its relatives. The few, rather enigmatic fossil remains of Jamoytius show that this animal was small, elongated and tubular shaped. It had a terminal suctorial mouth, and, on each side of the head region, there was a row of circular gill openings, behind the eye. 3 There was a propulsive tail fin with a long lower lobe and a shorter deeper lobe and possibly there were lateral fin folds and a long dorsal fin, for maintaining balance. Although Colbert (p. 25) discussed White’s (1946) suggested affinity, he concurred with Ritchie by placing Jamoytius with the anaspids (p. 18). Wickstead (1969) compared the branchial structures in Jamoytius with those of larval amphioxus and the tail of Jamoytius with that of Asymmetron. He thought Jamoytius might represent a larval or metamorphosing acraniate. Olson (1971, pp 6-7) described Jamoytius as ‘a soft-bodied, fish-like creature’. He noted that White (1946) had regarded it as a vertebrate ancestor, but that most workers agreed to associate it with the anaspids or thelodonts. Halstead and Turner (1973, p. 70) cited the presence of a cartilaginous branchial basket and a round mouth and classified Jamoytius as an anaspid. Norman and Greenwood (1975, pp 30, 348) thought that Jamoytius, probably an aberrant anaspid, provided the only direct fossil evidence for a continuous ventrolateral fin fold. Nelson (1976, pp 22-23) listed Jamoytius as a ‘virtually naked’ anaspid. Janvier and Blieck (1979, p. 293) wrote that ‘the status of Jamoytius kerwoodi White is unclear, but it is likely that it is more closely related to the Petromyzontida than to the typical Anaspidida’. Lehman (1980, pp 229-230) continued to follow Ritchie (1960) and reported Jamoytius to have two symmetrical eyes, a round mouth, 7 branchial openings, and a hypocercal tail. He mentioned Stensiö’s (1964) association of Jamoytius with the anaspids and Ritchie’s hestitation in such an assignment of affinity. Forey and Gardiner (1981, pp 139-140) produced an amended diagnosis, recognizing ‘A naked cyclostome with a diphypcercal tail and branchial basket.’ They found no trace of scales or lateral fin folds, but reported an annular cartilage, ‘a branchial basket…with horizontal struts and a diphypcercal tail. The branchial basket has no more than seven openings…’ They concluded that ‘In our estimation the fossil looks very similar to the present-day lamprey…’ Janvier (1981, p. 139) followed Ritchie’s (1960, 1968) interpretation, but held some reservations about the scales and questioned the number of branchial openings and as to whether the annular cartilage ‘might also be a large olfactory organ…’(p. 139). Janvier (1981) considered Jamoytius as a sister-taxon to either the lampreys or the anaspids, but excluded it (along with Endeiolepis) from the anaspids due to the presence of a dorsal fin. Young (1981, p. 111) depicted Jamoytius with a notochord, a hypocercal tail, scales, lateral fin folds, an annular cartilage, and up to 15 branchial pouches with a branchial basket. He thought it probably an anaspid, but also proposed that it might be an ammocoete larva of an ostracoderm. 4 Hardisty (1982, p. 234) recorded that Jamoytius, a possible ancestor to the lampreys, appeared to have traces of an annular cartilage and a branchial basket. Halstead (1982, pp 170-171, 190) supposed that Jamoytius had scales, well developed paired fins, and a lamprey-like branchial basket, for which ‘… the arrangement of the gill openings was not compressed as in the anaspids but more akin to the situation of the lampreys.’ (p. 170). Halstead’s (1982) ‘cladogram’ showed Jamoytius as a sistertaxon to the anaspids and, together, as a sister-group to the lampreys, though he discussed other possible affinities. Janvier and Lund (1983, p. 412) thought Jamoytius had only seven branchial openings, a branchial basket, probably (horny?) scales, and possibly an anaspid-like paired fin. They also remarked, ‘Even more problematical is the head of Jamoytius, which shows a very short preorbital region, much too short to be considered similar to lampreys. The anterior black mass regarded by Ritchie (1960, 1968) and Forey and Gardiner (1981) as an annular cartilage might also represent a large, subterminal olfactory organ’ (p.412). Their cladistic analysis resolved Jamoytius as a sister-taxon to the lampreys, and together as a sister-group to the anaspids. Janvier and Busch (1984, pp 503, 505) reported that Jamoytius had horny (or poorly mineralized) scales, a possible annular cartilage, an elongate body shape, and a reduced anal fin. They linked Jamoytius with un-named ‘Jamoytius-like vertebrates’ on the basis of chevron-shaped unmineralized scales and discussed possible affinities with the lampreys. They concluded, however, that its only similarities to anaspids were craniate or vertebrate plesiomorphies. Mallatt (1984, p. 267) considered Jamoytius as an ancestral lamprey. Ritchie (1984), responding to Forey and Gardiner (1981), supported his previous interpretations and figured a new specimen with 15-17 ‘branchial arches (or apertures)’ (p. 254). Ritchie (1984) still thought of Jamoytius as ‘probably a close relative, if not an ancestor, of the petromyzontids’ (p. 255), but he was not certain whether the presence of a dorsal fin warranted removal of Jamoytius from the Anaspida sensu stricto, as suggested by Janvier (1981). Forey 1984 (p. 336) did not regard Jamoytius as an anaspid. Maisey (1986, p. 207) considered Jamoytius as an anaspid with a dorsal fin and listed (p. 210) possible characters linking the anaspids and lampreys, including the following from Jamoytius: branchial basket, continuous dorsal fin, reduced ossification, and annular cartilage? (noting, on p. 211, Janvier’s (1981) uncertainity over the interpretation of this feature). Briggs and Clarkson (1987, p. 110-112, 114-115) referred to the presence of V-shape scales in Jamoytius, and, on that basis, submitted that Jamoytius could form a clade with the Jamoytius-like vertebrates and Conopiscius. Janvier (1987, p. 850) noted the presence of elongated lateral fin folds. 5 Carroll (1988, pp 39, 40 596L) catalogued Jamoytius as a questionable anaspid with reduced armour and lamprey-like circular gill pocuhes and annular cartilage. Smith and Hall (1990, pp 302-03) reviewed the scales versus muscles debate. Arsenault and Janvier (1991, pp 28-32) placed Jamoytius as a sister-taxon to the lampreys, as they considered that it had the following characters: paired fins, ‘horny’ scales, sinuous branchial arches bearing spiny processes and associated trematic rings, an annular cartilage, approximately 30 branchial openings, elongation of the body, a dorsal fin, and a possibly reduced anal fin. Aldridge et al. (1993, pp 409-410), Aldridge and Theron 1993 (p. 116), and Aldridge and Donoghue 1998 (p. 19) accepted the presence of sclerotic eye cartilages in Jamoytius and compared them with structures in the conodont animals. Aldridge et al. (1993) also likened features of the conodont animals to the branchial structures of Jamoytius. Briggs and Kear (1993, p. 285) found no evidence for biomineralized scales. ‘The clear lines delineating the segments are most likely to be cartilaginous connective tissues which make up the myosepta (myocommata of White 1946), the dark surface in between representing the skin.’ Forey and Janvier (1993, p. 132) figured a cladogram with Jamoytius as a sister-taxon to the lampreys, and both together as a sister-group to the anaspids. Forey and Janvier (1994, pp 556, 560) provided a cladistic analysis indicating Jamoytius as a sister-taxon to the lampreys. Forey (1995, pp 276, 284, 286-287, 289-291) considered Jamoytius to have an annular cartilage, large eyes, a branchial basket with sloping gill pouches, a hypocercal tail, and paired ventrolateral fin folds. His cladistic analysis showed Jamoytius as a sister-taxon to the lampreys. Northcutt (1996, p. 239) wrote, ‘There is a general consensus that the lampreys share a common ancestor with a small extinct fish, Jamoytius…, but it is presently unclear whether this radiation is closely related to a second group of jawless fish, the anaspids…’ Janvier (1996a, pp 265, 270, 273-274, 278) produced a cladistic analysis that fixed Jamoytius as a sister-taxon to Euphanerops, and the two together as a sister-group to the anaspids (Text-fig. 5B). Janvier (1996b, pp 101-104, 238, 241) described Jamoytius as an eel-shaped form with no mineralised skeleton, which may have possessed elongate paired fins. Some specimens show tarry imprints of the eyes….possibly the olfactory organ or an annular cartilage…and a branchial ‘basket’ with about 20 branchial units or openings….’(p. 101). His cladistic analysis placed Jamoytius as a sister-taxon to the lampreys, Jamoytius and the lampreys together as a sister-group to Euphanerops, and all three together as a sister-group to the anaspids. 6 Pough et al. (1996, pp 184, 194) described lateral fin fold theory as being based upon the presence of the structures in anaspids like Jamoytius. Shubin et al. (1997, figure 1) illustrate Jamoytius as a continuous fin fold stage in the evolution of vertebrate limbs. Janvier (1998, p. 944) mentioned Jamoytius as a form without a mineralized skeleton, considered by some as an ancestor to the lampreys. Dineley (1999, p.42-44) discusses the various conflicting interpretations of Jamoytius anatomy and affinity. Shu et al. (1999) undertake a phylogenetic analysis of Haikouichthys and relatives, identifying Jamoytius as related to lampreys rather than anaspids and construct the primitive vertebrate condition as possesing lateral fin folds. Bemis and Grande (1999, p.61) highlight interpretations of Jamoytius as an example of circularity involved in discussion of the lateral fin fold hypothesis. Donoghue et al. (2000) compare the anatomy of conodonts with Jamoytius and undertook a parsimony analysis based upon this comparison. Jamoytius is resolved in a clade with anaspids but sister to Euphanerops. Donoghue and Smith (2001) expanded the phylogenetic analysis of Donoghue et al. (2000), and resolved Jamoytius as belonging to a clade containing Euphanerops and Anaspida. Shu et al. (2003) amend their phylogenetic analysis and resolve Jamoytius as sister to Anaspida. Gess et al. (2006) undertake a phylogenetic investigation based upon their description of Priscomyzon and resolve Jamoytius as a stem-gnathostome, not belonging to a clade including Euphanerops or Anaspida. Janvier and Arsenault (2007, p. 204-5) compared Jamoytius to Euphanerops considering the nature of the scales and median stains. They consider interpretations equivocal and as such reach few conclusions regarding Jamoytius’ anatomy or affinity. REFERENCES FOR SUPPLEMENTARY INFORMATION ALDRIDGE, R. J. and THERON, J. N. 1993. Conodonts with preserved soft tissue from a new Upper Ordovician Konservat-Lagerstätte. Journal of Micropalaeontology, 12, 113-117. —— SMITH, M. P., CLARKSON, E. N. K. and CLARK, N. D. L. 1993. The anatomy of conodonts.Philosophical Transactions of the Royal Society of London, Series B, 340, 405-421. ARSENAULT, M. and JANVIER, P. 1991. The anaspid-like craniates of the Escuminac Formation (Upper Devonian) from Miguasha (Québec, Canada), with remarks on anaspid-petromyzontid relationships.19-40. In CHANG, M. 7 M., LIU, Y. H., and ZHANG, C. (eds). Early vertebrates and related problems of evolutionary biology, Sciences Press, Beijing, 514 pp. BARDACK, D. and ZANGERL, R. 1968. First fossil lamprey: a record from the Pennsylvanian of Illinois. Science, 162, 1265-1267. —— —— 1971. Lampreys in the fossil record. 67-84. In HARDISTY, M. W. and POTTER, I. C. (eds). The biology of lampreys. Volume 1. Academic Press, New York, 423 pp. BEMIS, W. E. and GRANDE, L. 1999. Development of the median fins of the North American paddlefish (Polyodon spathula), and a reevaluation of the lateral finfold hypothesis. In G. Arratia and H. P. Schultze (eds). Mesozoic Fishes 2 Systematics and Fossil Record. Verlag Dr. Friedrich Pfeil, München, 41-68 pp. BERG, L. 1955. Classification of fishes, both recent and fossil. Trudy Zoologicheskogo Instituta Akademiya Nauk, SSSR, 20, 1-286. [In Russian]. BERRILL, N. J. 1955. The origin of vertebrates. Clarendon Press, Oxford, 257 pp. BRIGGS, D. E. G. and CLARKSON, E. N. K. 1987. An enigmatic chordate from the Lower Carboniferous Granton Shrimp-Bed of the Edinburgh District, Scotland. Lethaia, 20, 107-115. —— and KEAR, A. 1994a. Decay of Branchiostoma: implications for soft-tissue preservation in conodonts and other primitive chordates. Lethaia, 26, 275-287. CARTER, G. S. 1967. Structure and habit in vertebrate evolution. Sidgwick and Jackson, London, 520 pp. CARROLL, R. L. 1988. Vertebrate paleontology and evolution. W. H. Freeman and Company, NewYork, 698 pp. COLBERT, E. H. 1969. Evolution of the vertebrates: a history of backboned animals through time. John Wiley and Sons, Inc., New York, 535 pp. DENISON, R. H. 1956. A review of the habitat of the earliest Vertebrates. Fieldiana, Geology, 11, 357-457. DECHASEAUX, C. 1963. Jamoytius, Amphioxus et le debut de l'histoire des Vertebres. Annales de Paleontologie, 49, 325-330. DINELEY, D. L. 1999. Silurian fossil fishes sites of Scotland. In D. L. Dineley and S. J. Metcalf (eds). Fossil Fishes of Great Britain. Joint Nature Conservation Committee, Peterborough, 31-62 pp. DONOGHUE, P. C. J. and SMITH, P. 2001. The anatomy of Turinia pagei (Powrie), and the phylogenetic status of the Thelodonti. Transactions of the Royal Society of Edinburgh: Earth Sciences, 92, 15-37. —— FOREY, P. L. and ALDRIDGE, R. J. 2000. Conodont affinity and chordate phylogeny. Biological Reviews, 75, 191-251. GESS, R. W., COATES, M. I. and RUBIDGE, B. S. 2006. A lamprey from the Devonian period of South Africa. Nature, 443, 981-984. FOREY, P. 1984. Yet more reflections on agnathan-gnathostome relationships. Journal of Vertebrate Paleontology, 4, 330-343. —— 1995. Agnathans recent and fossil, and the origin of jawed vertebrates. Reviews of Fish Biology, 5, 267-303. —— and JANVIER, P. 1993. Agnathans and the origin of jawed vertebrates. Nature, 361, 129-134. —— —— 1994. Evolution of the early vertebrates. American Scientist, 82, 554-565. —— and GARDINER, B. G. 1981. J. A. Moy-Thomas and his association with the British Museum (Natural History). Bulletin of the British Museum (Natural History), Geology Series, 35, 131-144. 8 GREGORY, W. K. 1951. Evolution emerging. The MacMillan Company, New York, 736 pp. —— and TURNER, S. 1973. Silurian and Devonian ostracoderms. 67-79. In HALLAM, A. (ed.). Atlas of palaeobiogeography, Elsevier Scientific Publishing, Amsterdam, 531 pp. HARDISTY, M. W. 1982. Lampreys and hagfishes: analysis of cyclostome relationships. 165-259. In HARDISTY, M. W. and POTTER, I. C. (eds). The biology of lampreys. Volume 4B. Academic Press, London, 466 pp. JANVIER, P. 1981. The phylogeny of the Craniata, with particular reference to the significance of fossil ‘agnathans’. Journal of Vertebrate Paleontology, 1, 121159. —— 1987. The paired fins of anaspids - one more hypothesis about their function. Journal of Paleontology, 61, 850-853. —— 1996a. The dawn of the vertebrates: characters versus common ascent in the rise of current vertebrate phylogenies. Palaeontology, 39, 259-287. —— 1996b. Early vertebrates. Oxford Monographs on Geology and Geophysics No. 33. Clarendon Press, Oxford, 393 pp. —— 1998. Les vertébrés avant le Silurien. Geobios, 30, 931-950. —— and ARSENAULT, M. 2007. The anatomy of Euphanerops longaevus Woodward, 1900, an anaspid-like jawless vertebrate from the Upper Devonian of Miguasha, Quebec, Canada. Geodiversitas, 29, 143-216. —— and BLIECK, A. 1979. New data on the internal anatomy of the Heterostraci (Agnatha), with general remarks on the phylogeny of the Craniota. Zoologica Scripta, 8, 287-296. —— and BUSCH, R. M. 1984. Jamoytius-like vertebrates from the Lower Devonian Manlius Formation of New York State. Journal of Vertebrate Paleontology, 4, 501-506. —— and LUND, R. 1983. Hardistiella montanensis n.gen. et sp. (Petromyzontidda) from the Lower Carboniferous of Montana, with remarks on the affinities of the lampreys. Journal of Vertebrate Paleontology, 2, 407-413. LEHMAN, J. P. 1957. Un probleme non resolu: L' origine des Vertebres. La Nature, (3265), 174-177. —— 1964. L'origine des Vertebres. Traite de Paleontologie, 4, 78-91. —— 1980. Les progres recents de la paleontologie des Vertebres. Livre jubilaire du cent cinquantenaire 1830-1980, Memoire Hors Serie- Societe Geologique de France, 10, 227-244. MAISEY, J. G. 1986. Head and tails: a chordate phylogeny. Cladistics, 2, 201-256. MALLAT, J. 1984. Feeding ecology of the earliest vertebrates. Zoological Journal of the Linnean Society, 82, 261-272. NORMAN, J. R. and GREENWOOD, P. H. 1975. A history of fishes. Ernest Benn, Limited, London, 467 pp. NORTHCUTT, R. G. 1996. The agnathan ark - the origin of craniate brains. Brain Behavior and Evolution, 48, 237-247. OLSON, E. 1971. Vertebrate paleozoology. Wiley-Interscience, New York, 839 pp. POUGH, F. H., HEISER, J. B. and MCFARLAND, W. N. 1996. Vertebrate life. Prentice Hall International, New Jersey, 798pp. RITCHIE, A. 1960. A new interpretation of Jamoytius kerwoodi White. Nature, 188, 647-649. —— 1963. Palaeontological Studies on Scottish Silurian Fish Beds. Unpublished Ph.D. Thesis, 9 University of Edinburgh, Edinburgh. —— 1968. New evidence on Jamoytius kerwoodi White, an important ostracoderm from the Silurian of Lanarkshire, Scotland. Palaeontology, 11, 21-39. —— 1984. Conflicting interpretations of the Silurian agnathan, Jamoytius. Scottish Journal of Geology, 20, 249-256. —— 1985. Ainiktozoon loganense Scourfield, a protochordate from the Silurian of Scotland. Alcheringa, 9, 115-142. ROBERTSON, G. M. 1953. Some attempts at phylogeny of early vertebrates. Iowa Academy of Science, 60, 725-737. ROBERTSON, J. D. 1957. The habitat of the early vertebrates. Biological Reviews, 32, 156-187. ROMER, A. S. 1966. Vertebrate paleontology. University of Chicago Press, Chicago, 468 pp. —— and PARSON, T. S. 1986. The vertebrate body. Saunders College Publishing, Philadelphia, 679 pp. SHU, D.-G., CONWAY-MORRIS, S., HAN, J., ZHANG, Z.-F., YASUI, K., JANVIER, P., CHEN, L., ZHANG, X.-L., LIU, J.-N. and LIU, H.-Q. 2003. Head and backbone of the Early Cambrian vertebrate Haikouichthys. Nature, 431, 536-539. —— LUO, H.-L., CONWAY-MORRIS, S., ZHANG, X.-L., HU, S.-X., CHEN, L., HAN, J., ZHU, M. and CHEN, L.-Z. 1999. Lower Cambrian vertebrates from South China. Nature, 402, 42-46. SHUBIN, N., TABIN, C. and CARROLL, S. 1997. Fossils, genes and the evolution of animal limbs. Nature, 388, 639-648. SMITH, I. C. 1957. New restorations of the heads of Pharyngolepis oblongus Kiaer and Pharyngolepis kiaeri sp. nov., with a note on their lateral line systems. Norsk Geologisk Tidsskrift, 37, 373-402. SMITH, M. M. and HALL, B. K. 1990. Development and evolutionary origins of vertebrate skeletogenic and odontogenic tissues. Biological Reviews, 65, 277373. STENSIÖ, E. 1958. Les cyclostomes fossiles ou ostracoderms. 173-425. In GRASSÉ, P. (ed.). Traité de Zoologie, 13. Masson et Cie, Paris, 924 pp. —— 1964. Les Cyclostomes fossiles ou ostracodermes. 96-382. In PIVETEAU, J. (ed.). Traite de Paleontologie, 4. Masson et Cie, Paris, 387 pp. SWINTON, W. E. 1961. The story of prehistoric animals. Rathbone Books, London, 93 pp. TARLO, L. B. 1960. The invertebrate origins of the vertebrates. Report of the 21st International Geological Congreess, Copenhagen, 22, 113-123. WÄNGSJÖ, G. 1952. The Downtownian and Devonian vertebrates of Spitsbergen. IX Morphologic and systematic studies of the Spitsbergen Cephalaspids. Norsk Polarinstitutt Skrifter, 97, 1-611+addendum. WESTOLL, T. S. 1958. The lateral fin-fold theory. 180-211. In WESTOLL, T. S. (ed.). Studies on fossil vertebrates. The Athelone Press, London, 263 pp. WHITE, E. I. 1946. Jamoytius kerwoodi, a new chordate from the Silurian of Lanarkshire. Geological Magazine, 83, 89-97. —— 1958. Original environment of the craniates. 212-234. In WESTOLL, T. S. (ed.). Studies on fossil vertebrates. The Athelone Press, London, 263 pp. WICKSTEAD, J. M. 1969. Some further comments on Jamoytius kerwoodi White. Zoological Journal of the Linnean Society, 48, 421-479. YOUNG, J. Z. 1981. The life of vertebrates. Clarendon Press, Oxford, 645 pp. 10 APPENDIX Character list and matrix used in phylogenetic analysis – an updated version of Gess et al. (2006) with neurological characters adapted according to P. Donoghue (unpublished data). Changes to the matrix reflect changes due to 1) corrections of coding strategy, 2) correcting coding to reflect new or updated character observations and 3) new taxa and characters. (a) Brain, sensory and nervous system 1. Neural crest absent = 0, present = 1 2. Olfactory peduncles absent = 0, present = 1 3. Pineal organ (extra-ocular photoreceptor region expressing pineal opsins) absent = 0, present = 1 4. Adenohypophysis absent = 0, present = 1 5. Adenohypophysis simple = 0, compartmentalized = 1 6. Optic tectum absent = 0, present = 1 7. Cerebellar primordia absent = 0, present = 1 8. Pretrematic branches in branchial nerves absent = 0, present = 1 9. Flattened spinal chord absent = 0, present = 1 10. Ventral and dorsal spinal nerve roots united, absent = 0, present = 1 11. Mauthner fibres in central nervous system absent = 0, present = 1 12. Retina absent = 0, present = 1 13. Olfactory organ with external opening absent = 0, present = 1 14. Nasohypophyseal opening serving respiration (nasohypophyseal duct) absent = 0, present = 1 15. Single nasohypophyseal opening, absent = 0, present = 1 16. Position of nasohypophyseal opening: terminal = 0, dorsal = 1 1 17. Olfactory organ unpaired = 0, paired = 1 18. Extrinsic eye musculature absent = 0, present = 1 19. Otic capsule anterior to branchial series, absent = 0, present = 1 20. Semicircular canals in labyrinth absent = 0, present = 1 21. Vertical semicircular canals forming loops, absent = 0, present = 1 22. Externally open endolymphatic ducts absent = 0, present = 1 23. Electroreceptive cells absent = 0, present = 1 24. Sensory lines absent = 0, present = 1 25. Sensory-lines on head only = 0, on head plus body = 1 26. Sensory-line enclosed in grooves = 0, enclosed in canals = 1 (b) Mouth and branchial system 27. Pouch-shaped gills absent = 0, present = 1 28. Single confluent branchial opening, absent = 0, present = 1 29. Elongate branchial series: more than 10 gill pouches/slits = 0, fewer than 10 = 1 30. Gill openings lateral and arranged in slanting row, absent = 0, present = 1 31. Position of gill openings: laterally = 0, ventrally = 1 32. Opercular flaps associated with gill openings, absent = 0, present = 1 33. Endodermal gill lamellae, absent = 0, present = 1 34. Gill lamellae with filaments, absent = 0, present = 1 35. Mouth terminal = 0, ventral = 1 36. Oral hood absent = 0, present = 1 37. Velum absent = 0, present = 1 2 (c) Circulatory system 38. Multi-chamber heart absent = 0, present = 1 39. Closed pericardium absent = 0, present = 1 40. Open blood system absent = 0, present = 1 41. Paired dorsal aortae absent = 0, present = 1 42. Large lateral head vein absent = 0, present = 1 43. Lymphocytes absent = 0, present = 1 44. Subaponeurotic vascular plexus absent = 0, present = 1 (d) Fins and fin-folds 45. Dorsal fin: separate dorsal fin absent = 0, present = 1 46. Dorsal fin originates at posterior of branchial series = 0, restricted to posterior of trunk and/or caudal region = 1 47. Anal fin separate, absent = 0, present = 1 48. Fin ray supports, absent = 0, present = 1 49. Paired antero-posterior skin folds absent = 0, present = 1 50. Constricted pectoral fins with endoskeletal elements absent = 0, present = 1 51. Pelvic fins/flap, absent = 0, present = 1 52. Tail shape: no distinct lobes developed = 0, ventral lobe much larger than dorsal = 1, dorsal lobe much larger than ventral = 2, dorsal and ventral lobes almost equally developed = 3 53. Chordal disposition relative to tail development, isochordal = 0, hypochordal = 1, hyperchordal = 2 54. Preanal median fold absent = 0, present = 1 3 (e) Skeletal 55. Ability to synthesise creatine phosphatase absent = 0, present = 1 56. Visceral arches fused to the neurocranium absent = 0, present =1 57. Keratinous teeth absent = 0, present = 1 58. Circumoral teeth absent = 0, present = 1 59. Circumoral teeth arranged in radiating series, absent = 0, present = 1 60. Trematic rings absent = 0, present = 1 61. Arcualia absent = 0, present = 1 62. Piston cartilage and apical plate, absent = 0, present = 1 63. Midline retractor muscle and paired protractor muscles, absent = 0, present = 1 64. Transversely biting teeth (the wording of this character description has been modified in order reduce ambiguity; coding reflects Gess et al. 2006) , absent = 0, present 1 65. Jaws (dorsoventral bite), absent 0, present = 1 66. Chondroitin 6-sulphate in cartilage, absent = 0, present = 1 67. Braincase with lateral walls, absent = 0, present = 1 68. Neurocranium entirely closed dorsally and covering the brain, absent = 0, present = 1 69. Occiput enclosing vagus and glossopharyngeal nerves, absent = 0, present =1 70. Annular cartilage absent = 0, present = 1 71. Large oral disc absent = 0, present = 1 72. Tentacle cartilages; absent = 0, present = 1 4 73. Trunk dermal skeleton absent = 0, present = 1 74. Perichondral bone absent = 0, present = 1 75. Calcified cartilage absent = 0, present = 1 76. Cartilage composed of huge clumped chondrocytes, absent = 0, present = 1 77. Calcified dermal skeleton absent = 0, present = 1 78. Lamellar aspidin, absent = 0, present = 1 79. Cellular bone, absent = 0, present = 1 80. Dentine absent = 0, present = 1. Dentinous tissues are preserved in same deposits as Jamoytius in the thelodont Loganellia, but there is no evidence of dentine in any Jamoytius specimen. Jamoytius can therefore be reliably interpreted as lacking dentine. 81. Dentine present as mesodentine = 0, orthodentine = 1 82. Enamel/oid absent = 0, (monotypic) enamel = 1, enameloid (bitypic enamel) = 2 83. Three-layered exoskeleton consisting of a basal lamella, middle spongy (or cancellar) layer and a superficial (often ornamented) layer: absent = 0, present = 1 84. Cancellar layer in exoskeleton, with honeycomb-shaped cavities, absent = 0, present = 1 85. Scales/denticles/teeth composed of odontodes absent = 0, present = 1 86. Scale shape: diamond-shaped = 0, rod-shaped = 1 87. Oak-leaf-shaped tubercles, absent = 0, present = 1 88. Oral plates absent = 0, present = 1 89. Denticles in pharynx absent = 0, present = 1 5 90. Dermal head covering in adult state absent = 0, present = 1 91. Large unpaired ventral and dorsal dermal plates on head, absent = 0, present = 1 92. Massive endoskeletal head shield covering the gills dorsally, absent = 0, present = 1 93. Sclerotic ossicles absent = 0, present = 1 94. Ossified endoskeletal sclera encapsulating the eye, absent = 0, present = 1 (g) Miscellaneous 95. High blood pressure, absent = 0, present = 1 96. Hyperosmoregulation, absent = 0, present = 1 97. Male gametes shed directly through the coelom, absent = 0, present = 1 98. Forward migration of postotic myomeres, absent = 0, present = 1 99. Larval phase, absent = 0, present = 1 (h) Additional characters due to change in coding strategy and the previous characters upon which they are contingent 100. (3.) Pineal opening covered = 0, uncovered = 1 101. (13.) External nasal opening single = 0, paired = 1 102. (20.) Number of semicircular canals one = 0, two = 1, three = 2 103. (24.) Neuromasts in sensory liness absent = 0, present = 1 104. (38.) Relative position of atrium and ventricle of heart: well separated = 0, close to each other = 1 105. (43.) Lymphocytes antigen receptors VLR = 0, T and B = 1 6 106. (49.) Paired antero-posterior skin folds extend along the trunk = 0, anterior only =1 107. (61.) Ventral arcualia absent = 0, present = 1 108. (85.) Scales/denticles/teeth made up by single odontode = 0, made up by several odontodes = 1 109. (90.) Dermal head covering in adult state: micromeric = 0, large (macromeric) dermal plates or shield = 1 Tunicata 1-10-0000-000-0---?0--00--010??00000001000000?0000000?0000-00000-00000000000000--0-0-00-00000001011--------Cephalochordata 0-10-00000000-0---?0--00--000000100110-010000?000000010000-00000-00000000000000--0-0-00-00000000011--------Myxinoidea 100101001101111000110001001*0000100011001011010000001111101?1110000000100010000--0-0-00-0000000110-00000-?-Myxinikela ????????????1?10??1???????101?0???00????????010?0000?0???0?????0?????01000?0000--0-0-00-0-000??????0????-?-Petromyzontida 10111110101110111111001110101100110111110010110100011011111111110 110011000010000--0-0-00-0-00011111101111-0-Mesomyzon ??????????????????1???????101?0??101?????????10?000110???11?????0 ?????10000?0000--0-0-00-0-000???????????-?-Priscomyzon ??????????????????0???????101?0???011???????000?000?????1101????0 ????110000?0000--0-0-00-0-000???????????-?-Mayomyzon ?????????????0????0???????101?0???011???????010?000*0??????1?1??0 ????100000?0000--0-0-00-0-000???????????-?-Haikouichthys ??????????????????1????????01000??00????????00010000?1??00-?1000?????00000?0000--0-0-00-0-000???????????-0-Heterostraci ?11???1?????????1?0110?111111000?100???????101000003111??0?1??00?????00100?110110111001011000?????0?1???-?11 Astraspis ??1??????????????????0?100101100???????????1?1??000???1?????????0 ???????100?11011210101??11??0?????0?????-?10 Arandaspida ??1????????????????????110100100??00????????010?000??01??0?????0?????001???1101?2111111011?1??????0?????-?11 Anaspida ??1?????????1?11???????110100100??00????????01111001101??0?????0?????00100?1100--0-1101010000?????10????*?10 7 Jamoytius ????????????1?10???????????0010???10????????????100??01????????0????1001???1??0--0-?100-0-000??????0????0??Euphanerops ??????????????????????????10010??110?????????11110011?1?????1???0 ????100?0?10000--?-0?00-0-000???????????01-Osteostraci ?011?11?????1011?10111?111101-11?110?11?01?1110101022011?0?1??00?1110001110101100101001010111?????101?1?-?11 Galeaspida ?11??11?????11111?0111?111101-10?110?????1?1?1??000??011?0?1??00?11100010101100--0-1001010100?????101???-?01 Loganellia ???????????????????????111?01101??00????????11101003101??0????00?????00100?1101000-1000110000???????????1?00 Turinia ??????????????????????????1011?1??00?????????1?010??1?1?????????0 ?????0010??1101100-10001100?0???????????1?00 Jawedvertebrates 1111111101111-0-111111111100100101000111111011110112201000-010011111000111010111110100011001111000012111-110 Euconodonta ?????????????????1?????????????????0????????01010001101?00????10????00?000?1001?10-1?0010-000???????????-?1Cornovichthys ??????????????????1?????????010?????????????00??00111??????????0???????000-0?00--??0-0?-0-0?0?????????????-Achanarella ????????????????????????????0?0?????????????111??00?&???????????0 ???????000-0?00--??0-0?-0-0???????????????-- *=0/1 &=1/2 8
© Copyright 2026 Paperzz