Geological setting

The sampled sedimentary succession corresponds to Berriasian and Valanginian marine argillaceous limestones and marls, the remaining Early Cretaceous succession being lacking owing to a marked regression and corresponding erosion. The sampled site (Fig. 1) is situated 7 km east to the town of Ganges (North of Montpellier) close to a farm named ‘Mas d'Antrigoule’ (Gard County). In this area, the Early Valanginian sedimentary unit reaches a thickness of 150–200 m and corresponds to outer platform deposits (see ref. 3 for detailed invertebrate faunal list) marked by sedimentary perturbations (for example, sediment slumps) on the western side of the Vocontian Basin. This sedimentary unit is composed of finely stratified calcareous marls with intercalated decimetric argillaceous limestone beds. The sampled elasmobranch-rich horizon is an indurate hardground of about 20 cm thick including numerous bioclasts and worm tubes. The Valanginian age of this horizon is attested, among others, by the presence of Neocomites neocomiensis, whereas upper in the formation, the presence of Eristavites indicates the very base of the Late Valanginian3. Thus, the sampled horizon can be considered latest early Valanginian in age. Reworking of the fossils from Palaeozoic rocks is ruled out because teeth (especially the roots) are extremely fragile but well preserved and because no non-metamorphized (Hercynian episode) Palaeozoic marine strata crop out in the region.

Figure 1: Early Cretaceous palaeogeographic setting of Europe. Enclosed: close-up on the sampled site (red star) with surrounding geological units. Full size image

Systematic palaeontology

The systematic framework used here follows that of Ginter et al.4, whereas Cappetta5 is followed for terminology.

Class Chondrichthyes Huxley, 1880

Superorder Cladodontomorphii Ginter, Hampe and Duffin, 2010

Order Symmoriiformes Zangerl, 1981

Family Falcatidae Zangerl, 1990

Falcatidae indet.

(Fig. 2a–e)

Figure 2: Cladodontomorph shark teeth recovered from the Valanginian of southern France. (a–e) Falcatidae indet., VAL 36, tooth in (a) labial, (b) occlusal, (c) basal, (d) profile and (e) lingual views. Scale bar, 500 μm. (f–j) Ctenacanthiformes indet. VAL 54, tooth in (f) labial, (g) occlusal, (h) basal, (i) profile and (j) lingual views. Scale bar, 500 μm. (k–s) Cladodontomorphii indet. (k–o) VAL 55, tooth in (k) labial, (l) occlusal, (m) basal, (n) profile and (o) lingual views. (p) VAL 56, tooth in labial view. (q–s) VAL 57, tooth in (q) profile, (r) labial and (s) basal views. Scale bar, 500 μm. Full size image

Material. One tooth (specimen VAL 36).

Locality, horizon and age. Mas d’Antrigoule, (Gard County, Southern France); N. neocomiensis Zone, latest early Valanginian (Early Cretaceous).

Description

This unique tooth is composed of an elongate and slender main cusp strongly oriented lingually and sigmoid in profile view. This is flanked by two pairs of lateral cusplets also strongly lingually directed and well individualized. The main cusp and cusplets are united by fine but sharp and well-developed cutting edges running continuously. The outer pair of cusplets is about twice the size of the inner pair but all are equally slender. Crown ornament consists of rare vertical ridges on the labial face of the main cusp (two ridges) and outer cusplets (several ridges) that do not cover more than the lower third of the cusps. The lingual ornament consists of densely arranged and fine vertical ridges that are interrupted and slightly undulating. These are present on the main cusp and cusplets and do not reach the upper third of the cusps. The root is extremely thin and developed lingually (lingual torus). A medio-lingual bulge is present, devoid of foramina. Several foramina of variable sizes are present on both sides of the medio-lingual bulge, in the depressed marginal regions. The thin lingual root face is pierced by a wide median foramina and a pair of small foramina is present on the labial face below the contact between the inner and outer cusplet. The basal root face is fairly flat and pierced by various small foramina.

Remarks

The morphology presented by this tooth (sigmoid main cusp, two lateral cusplets with the outer pair being higher than the inner) is typical of cladodont sharks. Moreover, the small size of this tooth, slender main cusp, presence of a medio-lingual bulge and crown ornaments are combined characters that indicate affinities with Falcatidae (for example, Stethacanthulus, Denaea, Falcatus). Although most representatives of this family possess teeth with a baso-labial projection (absent in the tooth described here), some derived forms such as Stethacanthulus meccaensis lack this character4. The family Falcatidae and order Symmoriiformes were thought to have gone extinct after the Cisuralian (Permian), some 130 myrs before the Valanginian. Resemblances with chlamydoselachid neoselachians are only superficial. In chlamydoselachids, the root is holaulacorhize, although the main axial groove is secondarily closed lingually. Chlamydoselachid teeth have diverging outer pair of cusplets projecting lingually and nearly as developed as the main cusp. They show a very different root morphology with two lingual projections separated by a marked V-shaped notch and corresponding axial groove on the lingual protuberance, no occlusal median convexity and a basal face showing a median labio-lingual crest with depressed marginal areas.

Order Ctenacanthiformes Glikman, 1964

Ctenacanthiformes indet.

(Fig. 2f–j)

Material. One tooth (specimen VAL 54).

Locality, horizon and age. Mas d’Antrigoule, (Gard County, Southern France); N. neocomiensis Zone, latest early Valanginian (Early Cretaceous).

Description

This tooth is of minute size and wider (less than 1 mm wide) than high. The main cusp is slightly inclined lingually and flanked by a pair of lateral cusplets (one is broken) in more labial position. Both the main cusp and cusplet show a convex lingual face and fairly flat labial face. The cutting edges are fine and interrupted between the main cusp and cusplet by a narrow notch. The lingual face of the main cusp and cusplet bear a pair of oblique marginal folds that follow the outline of the cutting edges. The labial crown face shows a strong basal depression at the base of the main cusp, semi-circular in labial view. The root is fairly high but with a reduced labial face, depressed and overhung by the crown in its centre. The lingual face is dominated by a pair of wide and high root protuberances situated on each side of the base of the main cusp. The developed medio-lingual region of the root is pierced by a wide foramen that is flanked by two pairs of smaller foramina. Other smaller foramina are present on the margino-lingual root faces. The basal root face appears fairly concave. Two slight baso-labial protuberances are present as well as a thin baso-lingual bulge that is developed along the lingual root edge.

Remarks

By the presence of a pair of margino-lingual and baso-labial protuberances, the root morphology of this tooth is similar to that of some Ctenacanthidae (Glikmanius) and to other ctenacanthiforms of unknown affinities (Heslerodus, ‘Ctenacanthus’ costellatus). Likewise, the crown morphology (flat labial crown face, medio-labial depression at the base of the crown) is identical to the above-mentioned ctenacanthiform genera, although the size of the tooth described here is closer to that of Heslerodus. The combined dental characters present in this specimen allow its attribution to the ctenacanthiform sharks. More material would be needed to identify this probably new taxon at lower taxonomic ranks. Teeth of last representatives of the order Ctenacanthiformes (Heslerodus, Glikmanius) were known from the Guadalupian (Permian).

Cladodontomorphii indet.

(Fig. 2k–s)

Material. Four teeth (specimens VAL 55, 56, 57, 58).

Locality, horizon and age. Mas d’Antrigoule, (Gard County, Southern France); N. neocomiensis Zone, latest early Valanginian (Early Cretaceous).

Description

Teeth of this taxon are wider than high and under 2 mm wide. The main cusp is smooth, biconvex and slightly inclined lingually. This bears well marked and sharp cutting edges strongly oblique near the base of the cusp in labial view. A pair of converging and triangular lateral cusplets is present, well individualized from the main cusp by notches separating the cutting edges. The lateral heels are high, sharp and oblique. The mesial heel is not or poorly separated from the cusplets by a slight notch. Distally, however, a notch more deeply separates the mesial cusplet from the heel, which thus resembles an additional cusplet. The heels are oriented lingually and taper before reaching the marginal root angles. The root is thin, mesio-distally elongate and fairly labio-lingually compressed. The basal root face is flat with the exception of the branch extremities that are bent basally. A pair of baso-labial root protuberances is present, situated below the base of the main cusp. The labial root face is very low and slightly flared. The lingual root face is well-developed and strongly projects lingually. A wide bulge occupies the majority of the lingual face except the lingual edge. The bulge is pierced by a wide median foramen with corresponding notch that opens lingually. Numerous additional foramina are also present on the lingual root face. Lateral teeth differ from anteriors by the distal inclination of the main cusp, whereas latero-posterior teeth are smaller, less mesio-distally developed with a more robust main cusp.

Remarks

Teeth of this taxon show combined features of various cladodontomorph shark groups. The lingual root face is more reminiscent of that of some Symmoriidae (for example, Stethacanthulus), whereas the basal root face (pair of baso-labial protuberances) is more similar to that of some ctenacanthiform (for example, Glikmanius, Heslerodus) or cladoselachiform taxa (for example, Cladoselache). However, the peculiar crown morphology differs from that of representatives of cladodontomorphs and this taxon is thus left in open nomenclature within the Cladodontomorphii.

Complementary enameloid analyses

As a complement to the morphological identifications, we performed tooth enameloid microstructure analyses on two of the three Valanginian taxa described above as well as on a Permian cladodontomorph shark. Among the three enameloid layers (external shiny-layered enameloid (SLE); intermediate parallel-bundled enameloid (PBE); inner tangled-bundled enameloid), commonly present in teeth of neoselachian sharks (selachimorphs), only the PBE is considered the synapomorphy of this group6,7. This layer does not appear to be present in modern rays and skates (batoids) and in other stem chondrichthyan groups and hybodont sharks (which were claimed to have a single-layered enameloid in the vast majority of taxa studied, but see ref. 8). However, this assertion was based on extremely scarce data in comparison to the high stem chondrichthyan diversity and some of these rare analyses used section studies that do not allow clear identification of bundles9. We performed enameloid microstructure analyses on mid-Permian Ctenacanthiformes teeth of the species Neosaivodus flagstaffensis collected from the type locality in Arizona in order to test this hypothesis. Mid-Permian Ctenacanthiformes were chosen for this analysis because they are among the last representatives of the Palaeozoic Cladodontomorphii and their teeth did not suffer recrystallization as opposed to most Carboniferous stem Chondrichthyan fossil teeth.

Surface etching performed on the single tooth of Ctenacanthiformes indet. (Fig. 3a) shows the presence of bundles of crystallites below a well-developed outer layer composed of individualized and randomly oriented crystallites. Parallel bundles (PBE) run apico-basally and change orientation near the cutting edge where they are perpendicular to its axis. It should be noted that the change in orientation occurs relatively far from the cutting edge’s axis.

Figure 3: Enameloid microstructure of Valanginian and Permian cladodontomorphs. (a) Surface etching of Ctenacanthiformes indet. VAL 54, showing parallel bundles of enameloid crystallites running apico-basally and changing orientation near the cutting edge (left). Scale bar, 30 μm. (b,c) Enameloid microstructure of Cladodontomorphii indet. (b) VAL 58, surface etching of the broken apex showing parallel bundles of enameloid crystallites (in ‘cross section’) running apico-basally and changing orientation near the cutting edge (left). Scale bar, 15 μm. (c) VAL 57, surface etching of the distal cutting edge near the apex showing bundles of crystallites running apico-basally and changing orientation near the cutting edge (oriented perpendicular to the latter). Scale bar, 5 μm. (d–j) Neosaivodus flagstaffensis from the mid-Permian of Arizona. (d–g) MHNG GEPI V5619, lateral tooth in (d) lingual and (e) labial views. Scale bar, 5 mm. (f) Surface etching of the distal area of the labial face showing parallel bundles of enameloid crystallites. Scale bar, 60 μm. (g) Surface etching of the distal area of the labial face showing parallel bundles of enameloid crystallites oriented perpendicular to the cutting edge (bottom left) below a labial fold. Scale bar, 60 μm. (h–j) MHNG GEPI V5648, anterior tooth in (h) lingual and (i) labial views. Scale bar, 5 mm. (j) Surface etching of the broken apex showing parallel bundles of enameloid crystallites (in ‘cross section’) below the shiny layered enameloid layer composed of individualized crystallites. Scale bar, 8 μm. Full size image

Enameloid microstructure analyses made on two teeth of Cladodontomorphii indet. (Fig. 3b,c) show the presence of two distinct layers. The outer layer is composed of thin individualized crystallites randomly oriented. The inner layer is made of a typical PBE layer with apico-basally oriented bundles showing a low degree of compaction. Some superficial bundles of the PBE are oriented perpendicular to the cutting edge axis well away from the latter, and these superficial bundles make up the cutting edge’s thickness. No randomly oriented bundles were identified between the PBE and dentine.

Study of the enameloid microstructure of two N. flagstaffensis teeth (Fig. 3d–j) revealed the presence of two distinct enameloid layers. The outer layer is reminiscent of the SLE with thin, randomly oriented and individualized crystallites. This layer is well-developed and also makes up the vertical labial folds (Fig. 3g). On the labial crown face, near the distal cutting edge and below the SLE are bundles of crystallites showing a low degree of compaction (similar to the PBE of the Valanginian taxa studied here) and an orientation perpendicular to the cutting edge. Further from the cutting edges, bundles are oriented apico-basally (Fig. 3f) and are in direct contact with the underling dentine (Fig. 3j).