Systematic palaeontology

SAUROPODA Marsh 1878

DIPLODOCOIDEA Marsh 1884

FLAGELLICAUDATA Harris & Dodson 2004

DICRAEOSAURIDAE Huene 1927

Bajadasaurus pronuspinax gen. et sp. nov.

Etymology

Generic name from Bajada (Spanish for downhill, in reference to the locality Bajada Colorada) and saurus (Greek, lizard). Specific epithet from pronus (Latin, bent over forward) and spinax (Greek, spine), referring to the anteriorly pointed, curved, neural spines of the cervical vertebrae.

Holotype

Museo Municipal Ernesto Bachmann (Villa El Chocón, Neuquén) MMCh-PV 75; a nearly complete skull (including left maxilla, left lacrimal, both prefrontals, both frontals, both parietals, both postorbitals, both squamosals, left quadratojugal, both pterygoids, both quadrates, supraoccipital, exoccipital-opisthotic complex, basioccipital, basisphenoid, both prootics, both laterosphenoids, both orbitosphenoids, both dentaries, left surangular, both angulars, both splenials, left prearticular, left articular, isolated upper tooth row), both proatlases, atlantal neurapophyses, axis and the ?fifth cervical vertebra (Fig. 1A).

Figure 1 Skeletal reconstruction of Bajadasaurus pronuspinax gen. et sp. nov (MMCh-PV 75), location and quarry map. (A) The neck and skull reconstruction in left lateral view, showing preserved bones in white. The complete anterior cervical vertebra is located tentatively in the fifth position (see Description). The total count of cervical elements, as well as the relative extension of the neural spines, is based in the complete series of the related taxon Amargasaurus, the other dicraeosaurid with extremely elongated bifid neural spines along the neck. (B) A map of the surrounding area of the Ezequiel Ramos Mexía lake (Neuquén Province, Argentina) showing the type locality of Bajadasaurus (Bajada Colorada) indicated by a white star. (C) A quarry map showing the association and location of the remains in the field. at, atlas; ax, axis; cv, cervical vertebra; d, dentary; f, frontal; m, maxilla; po, postorbital; pt, pterygoid; qj, quadratojugal. Full size image

Locality and horizon

The remains were found in outcrops of the Lower Cretaceous (Late Berriasian–Valanginian14,15) Bajada Colorada Formation (Neuquén Basin, Patagonia, Argentina), at Bajada Colorada locality 40 km south of Picún Leufú town on the National Route 237 (Fig. 1B).

Diagnosis

Bajadasaurus pronuspinax can be diagnosed by the following autapomorphies (marked by an asterisk), as well as a unique combination of character states: post-temporal fenestra extended medially with a long parietal contribution (*); basipterygoid processes extremely slender and long, more than six times longer than lateromedially wide (*); elongate angular, longer than the anteroposterior surangular length; neural spine of the axis oriented vertically (*); paired, anteriorly curved, and extremely elongate bifid neural spines of anterior-mid cervical vertebrae (*).

Osteological description

Cranial bones and axial elements are preserved. The skull bones of Bajadasaurus include the dermal roof, braincase, palatal, and jaw elements. The axial remains consist of left and right proatlases, atlantal neurapophyses, axis and the ?fifth cervical vertebra (Figs 2 and S1–11).

Figure 2 Skeletal elements of Bajadasaurus pronuspinax gen. et sp. nov (MMCh-PV 75). (A–C) Skull roof and braincase in posterior (A), left lateral (B) and right lateral (C) views. (D,E) Left lower jaw in dorsal (D) and medial (E) views. F, Dentaries in anterior view. (G) Pterygoids in ventral view. (H) Left maxilla in medial view. (I) Left lacrimal in lateral view. (J) Left quadratojugal in lateral view. (K,L) Right quadrate in medial (K) and posterior (L) views. (M) Proatlases in dorsal view. (N) Atlantal neurapophyses in anterior view. (O,P), Axis in left lateral (O) and anterior (P) views. (Q,R) Fifth cervical vertebra in left lateral (Q) and anterior (R) views. an, angular; ar, articular; bo, basioccipital; bt, basal tubera; btp, basipterygoid process; ch, ‘chin’ of dentary; cn, cranial nerve; d, dentary; di, diapophysis; f, frontal; fm, foramen magnum; fo, fenestra ovalis; ls, laterosphenoid; met, metotic foramen; mp, medial process; nc, neural canal; ns, neural spine; os, orbitosphenoid; p, parietal; pfo, pneumatic fossa; po, postorbital; pocdf, postzygapophyseal centrodiapophyseal fossa; podl, postzygodiapophyseal lamina; popr, paraoccipital process; poz, postzygapophysis; pra, prearticular; pre, prezygapophysis; prsl, prespinal lamina; ptf, postemporal fenestra; qf, quadrate fossa; rm, replacement maxillary tooth; sa, surangular; sp, splenial; sq, squamosal; stf, supratemporal fenestra; vk, ventral keel; vp, ventral process. Full size image

The incomplete left maxilla is a flat and smooth bone that thickens in the dentigerous portion and thins toward the broken posterodorsal edge. The posterior ascending process is not preserved. However, the palatal shelf is visible in medial view as a thick horizontal lamina, as occurs in Dicraeosaurus16, Diplodocus17, and Rapetosaurus18. Eight alveoli are visible in medial view, with replacement teeth in most of them. This reduced count is only similar to Suuwassea8 (which possesses 7 alveoli, although the maxilla may be incompletely preserved) within diplodocoids which commonly bear more than 10–12 teeth in the maxilla (10–11 in Diplodocus19; 12 in Kaatedocus20; 12 in Dicraeosaurus16; 24 in Nigersaurus21).

The left lacrimal is nearly complete. The dorsal half is triangular in section with a straight lateral ridge as in Dicraeosaurus16, and unlike the projecting spur seen in Kaatedocus22. The ventral portion is anteroposteriorly broad and flat. A small foramen is present on the orbital face, unlike the broad foramen recognized in Dicraeosaurus16. The jugal contact seems to be stepped as in Diplodocus sp. (CM 11161).

Both prefrontals are wide-based triangular bones in dorsal view. A small participation of the prefrontal in the dorsal orbital rim is present, unlike the bigger contribution seen in Dicraeosaurus16 and Amargasaurus (MACN-N 15) in which the prefrontals are also proportionally larger and more robust.

The frontals are strongly fused to the parietals, which dorsally cover them in the mid-posterior region. In dorsal view, the frontals are broad posteriorly and narrow anteriorly, with a markedly sigmoidal lateral border, differing from the less pronounced border present in Diplodocus (CM 11161), Amargasaurus (MACN-N 15), and Dicraeosaurus16. As a result, the orbits are dorsally exposed. A similar condition is present in Lingwulong7. Both frontoparietal and postparietal foraminae are taphonomically joined along the skull midline, as a consequence of the broken bony bridge between them. The small frontoparietal foramen resembles the condition present in Suuwassea8, differing from the larger foramina seen in Amargasaurus (MACN-N 15) and Dicraeosaurus16. The frontals have a small contribution to the anterior margin of the supratemporal fenestra.

The parietals are anteroposteriorly extended over the skull roof. They are curved posteriorly with anterior crescent-shaped crests as in Amargasaurus (MACN-N 15). However, the muscular depressions anteriorly bounded by these crests are shallow as in Dicraeosaurus16 and Suuwassea8, differing from the deep depression seen in Amargasaurus (MACN-N 15). The postparietal foramen reaches the border of the supraoccipital crest. The supratemporal fenestra is roofed by the posterior segment of the parietal.

The postorbital has two main processes which contact the frontal dorsally and the jugal anteroventrally. While the orbital border is rounded, the posterior one is marked by a straight angle with a reduced indistinct posterior process, as in Amargasaurus (MACN-N 15) and Dicraeosaurus16.

The squamosal is massive posteriorly and becomes slender anteriorly, forming an enlarged anterior squamosal process, which strongly suggests a contact with the quadratojugal, differing from Diplodocidae. This contact ventrally frames a narrow lateral temporal fenestra that extends posterodorsally. Additionally, the medioventral surface of the squamosal is concave for the articulation with the quadrate head. In the posteroventral corner, a prominent, ventrally directed ‘prong’ is developed, as commonly occurs in dicraeosaurids23.

The left quadratojugal is a flat, transversely compressed bone, which ventrally borders a narrow lateral temporal fenestra. It is formed by two rami oriented at an obtuse angle, a situation only present in diplodocids (e.g., Diplodocus sp. CM 11161) and titanosaurs (e.g., Tapuiasaurus24). The maximum dorsoventral height of the anterior ramus is twice the minimum dorsoventral height.

Both pterygoids are partially preserved. They are complex, nearly planar, bow-like bones with four main processes. Two of them point posteriorly, enclosing an embayment that meets the pterygoid wing of the quadrate. The other two processes point anteriorly. The anterodorsal process is flat and short. The anteroventral process is long and narrow. A dorsoventral constriction occurs at one third of the total length, where a smooth crest develops to contact the long basipterygoid processes (Fig. S5).

Both quadrates are partially preserved. They are triradiate bones, with an elongate posterodorsal process, a short, rounded and low anterior pterygoid wing, and a ventral condyle. The shaft is posteriorly concave. A shallow fossa is present at mid-length on the medial surface, as occurs in Suuwassea8 and diplodocids22. In posterior view, a shallow longitudinal fossa is present. Ventrally, the articular condyle has a roughly triangular shape as in Suuwassea8 and diplodocids23.

The supraoccipital and exoccipital-opisthotic complex are completely fused. The supraoccipital is rhomboidal and bears a distinct and narrow sagittal nuchal crest as in other dicraeosaurids and Kaatedocus20. However the dorsal margins are nearly straight, unlike the stepped borders recognized in Dicraeosaurus16, Amargasaurus (MACN-N 15), and Suuwassea8. The post-temporal fenestra extends medially in Bajadasaurus, which represents an autapomorphy. The exit for cranial nerve XII in the dorsolateral corner of the occipital condyle is not discernable due to poor preservation. The anteroposteriorly flat paraoccipital processes project posteroventrally. The crista tuberalis is not robust but clearly delimits a shallow fossa in which the fenestra ovalis and the metotic foramen open posteriorly. A conspicuous crista prootica with a lateral expansion at its ventral end is present, as is common in dicraeosaurids22,25.

The basioccipital forms the main body of the occipital condyle and the paired basal tubera. Unlike Amargasaurus (MACN-N 15) and Dicraeosaurus16, the articular surface of the condyle does not exceed the width of the condylar neck. The condyle is dorsoventrally compressed.

The basal tubera hang from the base of the condylar neck and extend ventrally with a slightly convex posterior surface. A vertical sulcus extends along the midline of the tubercles. The basal tubera are slightly narrower than the occipital condyle as in rebbachisaurids and other dicraeosaurids23.

The basisphenoid forms the gracile and elongated basipterygoid processes, which extend anteroventrally. Unlike Dicraeosaurus16 and Amargasaurus (MACN-N 15), where these processes are robust structures and somewhat shorter, in Bajadasaurus they are longer and extremely slender (more than six times longer than lateromedially wide), thus representing a possible autapomorphy of the taxon. The diverging angle is narrow, less than 30 degrees, as in other Dicraeosauridae. The external foramen for the internal carotid artery opens on the lateral surface, where the basipterygoid processes and the basal tubera meet, as occurs in Amargasaurus26.

The prootic is a triangular and flat plate of bone with a reduced laterally exposed surface. Although no sutures are visible, the crista antotica and the opening for cranial nerve V may represent the limits with the laterosphenoid, as in other sauropods26. The opening for cranial nerve VII is located at the base of the crista prootica as in Amargasaurus (MACN-N 15), just above the external foramen for the internal carotid artery.

The laterosphenoid is completely fused with the prootic posteriorly and the orbitosphenoid anteriorly. The contact with the frontal is quite evident by the presence of an anteroposteriorly oriented suture, as occurs in Amargasaurus (MACN-N 15). The crista antotica is short, posterodorsally oriented, and disappears at the level of the opening for cranial nerve V, contrasting with the more conspicuous and extended crista antotica present in Amargasaurus (MACN-N 15) and Dicraeosaurus16. The foramina for cranial nerves II, III and V are horizontally aligned with respect to the skull roof.

Both subtriangular orbitosphenoids are plate-like bones that meet at the sagittal plane anteriorly. Paired optic foramina for cranial nerve II open at mid height, unlike Suuwassea8 and Kaatedocus20 in which the openings remain unpaired. Anterodorsally, the orbitosphenoids frame the exit of the cranial nerve I, which is partially compressed.

The dentary shows a symphyseal segment (oblique to the sagittal plane), a curved segment (corner), and the base of the posterior rami. Differing from the more squared jaws of diplodocids and rebbachisaurids17,21, it is a J-shaped element, as in other dicraeosaurids. It is a slender bone as in Suuwassea27, unlike the thick dentary of Dicraeosaurus16. Only the anterior region and the corner are dentigerous. It bears twelve full-grown teeth, some of which have unworn distal tips. The anteroventral margin of the dentary shows a dorsoventrally deep ‘chin’ as in flagellicaudatans28,29, and a labial prominence near the symphysis as in Dicraeosaurus16 and Suuwassea27. The subtriangular symphysis tapers ventrally as in Dicraeosaurus16 and Suuwassea27. The anterior external surface bears small, ovoid foramina. Medially, a posterior triangular embayment develops in which the surangular and the angular overlap. A shallow coronoid eminence is recognized behind the tooth row as is common in diplodocoids30.

The surangular is a transversely flat and elongated bone. It maintains constant depth and straightness until the articular region, where it curves ventrally and tapers. The retroarticular process is short relative to most diplodocids31. A small surangular foramen is anterodorsally located in the lateral surface. In medial view the surangular is partially covered by the articular and prearticular posteriorly, and the splenial anteriorly.

The angular is extremely elongated, and longer than the surangular, unlike the condition seen in diplodocids. The posterior region tapers dorsoventrally and curves slightly ventrally. Ventrally, the angular is straight except for the retroarticular segment, which curves medially.

The posterior half of the splenial is flat and covers the anterior portion of the surangular and a small portion of the angular medially. The posteroventral process is tongue-like, unlike Diplodocus17 where it tapers distally. This morphology is convergently present in titanosaurs such as Nemegtosaurus32 and Tapuiasaurus24.

The prearticular is a thin plate of bone, vertically located, that tapers posteriorly. Although incomplete, the anterior portion indicates the presence of a narrow adductor fossa unlike the conspicuous one seen in Diplodocus17. Posteriorly, an oblique flat process extends medially on the retroarticular region.

The wedge-shaped articular is tightly located between the surangular laterally, the prearticular medially and the angular ventrally. Dorsally, the articular shows a triangular perimeter with two main surfaces divided by a low ridge (perpendicular to the sagittal plane), located behind the glenoid region.

Twenty-four upper teeth in anatomical position were found in close association with the left maxilla. This count equals the tooth row of the dentary. Both upper and dentary teeth are narrow-crowned (Slenderness Index: 4.6), peg-like elements. They are nearly straight or slightly curved medially. Some of them show extremely reduced, low angled, single planar wear facets.

Left and right proatlases were preserved in articulation with the skull. They are fin-like triangular bones with an ovoid broad base, flat sides, and pointed distal ends as in Kaatedocus20 and Dicraeosaurus2.

The atlantal neurapophyses are triangular, wing-like thin bones, laterally convex and medially concave. The posterodorsal projection is rounded distally as in Amargasaurus26 and Galeamopus33, unlike the distally tapering ones present in Kaatedocus20. A medial rounded process projects anterodorsally at mid-length of the neurapophyses, as in Amargasaurus26 and Suuwassea34.

The axis is nearly complete, although the neural spine is broken and displaced laterally. The total height is twice the total length of the centrum, as in Dicraeosaurus2. The axial centrum is twice as long as posteriorly tall, as in other dicraeosaurids. The body is laterally constricted at mid-length. Large undivided pneumatic fossae are present as in Dicraeosaurus2, Suuwassea8 and Amargasaurus (MACN-N 15). The tall neural arch rests on the entire centrum. Deep triangular postzygapophyseal centrodiapophyseal fossae are present, as in Dicraeosaurus2 and Amargasaurus (MACN-N 15). The small diapophysis points backwards as in Suuwassea, unlike the ventrally pointed diapophyses of Dicraeosaurus2 and Amargasaurus (MACN-N 15). In anatomical position, the narrow vertical neural spine is non-bifurcated, triangular in cross-section and tapers distally, differing from other sauropods. The postzygapophyses and the spinopostzygapophyseal laminae embrace a deep triangular spinopostzygapophyseal fossa.

The ?fifth cervical vertebra is the most characteristic element of Bajadasaurus. With an extremely elongate, bifurcated neural spine, this vertebra is four times taller than long, only comparable with Amargasaurus (MACN-N 15). However, Bajadasaurus possesses anteriorly curved and slightly laterally pointed neural spines that differ from any other known sauropod. The centrum is two times longer than posteriorly tall and shallow undivided fossae are located along the lateral sides, as in Dicraeosaurus2, Amargasaurus (MACN-N 15), and Pilmatueia10 (MLL-Pv-004). However, Pilmatueia (MLL-Pv-004) differs from Bajadasaurus in having three small foramina and a deep centrodiapophyseal fossa associated to the lateral excavation of the centrum. The centrodiapophyseal fossa is absent in Bajadasaurus. Ventrally, the centrum of Bajadasaurus narrows in a longitudinal keel unlike other dicraeosaurids such as Pilmatueia10, Dicraeosaurus2 and Brachytrachelopan9, which develop a ventral keel in a transversely wide concave surface. These, plus other differences between Pilmatueia10 and Bajadasaurus such as the absence of median tubercle between the elongated neural spines in the latter and the phylogenetic position of both contemporaneous dicraeosaurid sauropods (see Phylogenetic analysis bellow) justify the taxonomic separation of both taxa. The neural arch is nearly as long as the centrum length with the neural spine base being located at the midpoint. This condition, along with the general proportions and laminar and/or apophyses (zygapophyses and diapophyses) arrangements are comparable with the fifth cervical of Dicraeosaurus2, the ?sixth of Brachytrachelopan9 and the seventh of Amargasaurus (MACN-N 15). In this context we tentatively assign this cervical vertebra to the fifth position. Stout epipophyses are located above the postzygapophyses. The rod-like, 58 cm long neural spines, maintain an ovoid section along their length except for the transversely compressed triangular base. A peculiar trait is that the tip of the spine is not acute as in Amargasaurus (MACN-N 15), but slightly expanded. The poor preservation of bone surfaces in the specimen precludes the recognition of longitudinal striations on the spine surface as those observed in Amargasaurus6, and inferred to support an external keratinized horn sheath. However, considering the extremely elongation of the neural spine (a condition very similar to that of Amargasaurus), external horn sheaths could be ascribed to Bajadasurus as well (see Discussion).

Phylogenetic analysis

The phylogenetic affinities of Bajadasaurus were evaluated in the context of a previous data set7 (see Methods and Supplementary Information for details). The analysis retrieved 820 most parsimonious trees of a length of 1114 steps. The strict consensus tree shows a large polytomy at the base of Neosauropoda, which can be resolved if two unstable taxa (Amargatitanis macni11,12 and Erketu ellisoni35) are pruned from the MPTs (see Supplementary Information). A reduced strict consensus tree recovered Bajadasaurus well nested within the family Dicraeosauridae (Fig. 3, Supplementary Fig. 12), sharing six synapomorphies with all dicraeosaurids, plus five synapomorphies shared with Lingwulong, Pilmatueia, Brachytrachelopan, Dicraeosaurus and Amargasaurus. Bajadasaurus is recovered as the sister taxon of a clade consisting of the lower Cretaceous Pilmatueia plus an unresolved derived group including the Cretaceous Amargasaurus, the Jurassic Brachytrachelopan, and Dicraeosaurus, supported by the presence of a supratemporal fenestra with a maximum diameter subequal to that of the foramen magnum (char. 47), and basipterygoid processes with an angle of divergence less than 30° (char. 69).