Dicraeosaurids are a group of sauropod dinosaurs characterized by a distinctive vertebral column with paired, long, neural spines, present in an extreme fashion in the South American form Amargasaurus cazaui. This distinctive morphology has been interpreted as a support structure for a thermoregulatory sail, a padded crest for display, a dorsal hump acting as fat reservoir, and even as inner cores for dorsal horns. Other inferred functions (if any) of this structure were related to sexual display and/or defense strategies. Here we describe a new dicraeosaurid sauropod, Bajadasaurus pronuspinax gen. et sp. nov., from Patagonia which preserves the most complete skull of the group and has extremely elongate bifid cervical neural spines that point permanently forward, irrespective of the neck position. Although much shorter versions of this neural spine configuration were already recorded for other dicraeosaurid taxa, the long, anteriorly bent spines of this new dinosaur support the hypothesis that these elongate spines of dicraeosaurid sauropods served as passive defense structures.
Since the finding of the nearly complete skeletons of Dicraeosaurus in the expeditions to the upper Jurassic “Saurian beds” of Tendaguru, Tanzania, led by Werner Janensch from the Geological-Paleontological Institute and Museum of the University of Berlin in the early 20th century (1909–1912), the presence of elongate bifid neural spines in the axial skeleton of this taxon was always a distinctive and iconic feature1,2. More than eighty years later, the discovery of a new, rather complete, dicraeosaurid skeleton from the Early Cretaceous of South America, Amargasaurus cazaui3, renewed discussions on the peculiar vertebral anatomy of these sauropod dinosaurs including interpretations as a support structure for a thermoregulatory sail, a padded crest as a display and/or clattering structure, a dorsal hump, or as internal cores of dorsal horns4,5,6.
At present, five other dicraeosaurid species are known from the Middle Jurassic of China (Lingwulong shenqui7), the Upper Jurassic of North America (Suuwassea emiliae8) and Central Patagonia (Brachytrachelopan mesai9), and the Early Cretaceous of North Patagonia (Pilmatueia faundezi10 and Amargatitanis macni11,12), but only Brachytrachelopan contributed to the knowledge of the entire cervical column, confirming the proposed shortening in the neck length within the group.
A new dicraeosaurid sauropod, Bajadasaurus pronuspinax gen. et sp. nov., from the Early Lower Cretaceous Bajada Colorada Formation (Northern Patagonia, Argentina), which includes dermal roof and palatal bones, a braincase, and a nearly complete lower jaw, expands the knowledge on the skull morphology of this group13. The preserved skull elements including the complete lower jaw allow the first reliable inference of the size and shape of a dicraeosaurid skull. Additionally, the skull was recovered in articulation with the anterior region of the neck and another cervical vertebra with exceptional development of anteriorly bent, bifid cervical neural spines, which informs hypotheses of defense behavior in sauropod dinosaurs. The temporal difference between Bajadasaurus and Amargasaurus, a 15 My younger spiny sauropod from the Neuquén basin, supports that the development of a fence of spines was likely adaptive over a long time period.
SAUROPODA Marsh 1878
DIPLODOCOIDEA Marsh 1884
FLAGELLICAUDATA Harris & Dodson 2004
DICRAEOSAURIDAE Huene 1927
Bajadasaurus pronuspinax gen. et sp. nov.
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.
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).
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).
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 (*).
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).
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).
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).
The cranial bones of Bajadasaurus show several novelties in the skull of dicraeosaurid sauropods. As shown in Fig. 4, this gracile skull with dorsally exposed orbits, dorsoventrally compressed occipital condyle, extremely narrow basipterygoid processes, elongate and slender anterior processes of the squamosals, medially extended post-temporal fenestrae, short lateral temporal fenestrae and a reduced dentition in the maxilla and dentary, largely differs from other known taxa within Dicraeosauridae (Fig. 4). Additionally, the probable contact between the squamosal and quadratojugal, an anteroposteriorly extended and gracile lower jaw, and a narrow, posteriorly extended lateral temporal fenestra are recognized for the first time in a dicraeosaurid skull. The dorsally exposed orbits mean, in the context of a head-down normal position for the Amargasaurus skull26 that eyes were capable of a forward-directed, perhaps stereoscopic view while feeding.
The most striking feature of Bajadasaurus is the presence of extremely long cervical neural spines that curve anteriorly. Axial skeletons with deeply bifid neural spines are common in dicraeosaurid sauropods. In fact, Amargasaurus cazaui shows practically the same development of cervical neural spine elongation as Bajadasaurus, but the spines of the former point backwards rather than forwards. On the contrary, Dicraeosaurus and Brachytrachelopan show anteriorly inclined neural spines in the cervical vertebrae, although the spines are much shorter than in Bajadasaurus.
The discovery of Amargasaurus cazaui opened a field of research and assumptions concerning the function of its spines. Different tetrapods acted as models and the extracorporeal exposition of the main portion of the spines of Amargasaurus was compared to that of iguanodontians as support of a thermoregulatory sail36, a dorsal hump5, a padded crest related to sexual selection37, or an internal core for dorsal horns6. All but the last explanation require that these long and extremely gracile bone projections, now recognized in Bajadasaurus as well, can support enough physical stress to avoid fracturing, based on similar studies in mammals38,39. Conversely, the presence of external keratinous horns in the distal-most two-thirds of the dorsal extension of the neural spines provides a better mechanical solution against a potential fracture.
A recent publication described the supravertebral pneumatic diverticles of Amargasaurus as occupying the ventral 1/3 of the mid-cervical vertebrae, and in anterior and posterior cervicals, the ventral half and the space between the metapophyses6. The remaining 2/3 of the distal spine was recognized as having an undulated and striated surface, comparable to bones bearing keratinized sheath-covered structures. This is also supported by the absence of a supraspinous ligament attachment on the top of neural spines in Bajadasaurus and Amargasaurus, thus differing from the related Dicraeosaurus6.
Although bone is stronger and stiffer in passive situations depending on strain and load, horns and other keratin-based materials are tougher and highly resistant to impact-related fractures in dry to mesic conditions both in mammalian40,41 or sauropsid keratin42. Thus, the cover sheath may transfer the load to the bony core along a radial direction. Additionally, resistance is improved in slightly bent horns39, and in sheaths much longer (double, as in some artiodactyls) than neural spines, thus reducing impulsive loads more than other geometries. This physical characteristic would be biologically beneficial considering that this portion of the neural arch (including its base) is particularly vulnerable because it acts as the osseous roof of the neural cord. Hence, a possible breakage in life could result in a dangerous and traumatic damage for the animal, with serious immunological trauma. Breakages of vertebral laminae in humans (laminectomy) revealed that trauma arises when fragments displace into the spinal canal43. Breakages in Dimetrodon sails revealed a fast-healing system by osteoclastic resorption and deposition of lamellar bone44.
In most extant sauropsids, except for the rostral horn of Trioceros jacksoni, and lateral spines of gerrhosaurid lizards, sheaths do not reach 100% of the bony core length. The discovery of an exceptionally preserved specimen of the ankylosaur Borealopelta permitted examination in extinct archosaurs45. In ankylosaurs, the keratinous sheath of the parascapular spine extends to 25% up the bony core length. Although previous authors considered that horns were no longer than the bone itself in Amargasaurus6, the length ratios of bone core/keratinous sheath in reptiles and mammals and ongoing research on material resistance suggest that the keratinous sheath in Amargasaurus and perhaps Bajadasaurus should have been more than 50% longer than the bone core to improve the bone protection46.
While the extension of the neural spines may be speculative for Bajadasaurus, the bone core itself goes much beyond the anterior limit of the head, becoming a front fence for the body. In this context, whereas the ?fifth vertebra points to a low position respect to a grazing head, we could hypothesize that following neck vertebrae with larger centra and higher reach should logically be longer. A defensive explanation based only on neural spine osseous resistance seems to be incompatible with the 15 My persistence of the Bajadasaurus-Amargasaurus long-spined dicraeosaurid strategy. The vast group of acute spines with long protective sheaths would represent a disturbing fence for a loitering carnivore. Under moderate charge, the breakage would affect only spine tips, preserving the bone core within them.
The phylogenetic position of Bajadasaurus pronuspinax was tested through an equally weighted parsimony analysis in TNT v.1.147. The data matrix used was based on a previously published phylogeny which included a wide array of sauropodomorph taxa7, with the addition of Amargatitanis macni11,12, Pilmatueia faundezi10, and Bajadasaurus pronuspinax. This dataset included 375 characters and 76 taxa (Supplementary Information). The dataset was analyzed starting from 5000 replicates of Wagner trees followed by TBR branch swapping and saving 10 tress per replicate, reaching the best score 1060 times. The trees recovered were subjected to an additional round of branch swapping. Unstable taxa were identified search by Pruned Tree command in TNT. Bremer support values48 were calculated to evaluate the robustness of the nodes in the reduced strict consensus tree.
CM, Carnegie Museum of Natural History, Pittsburgh, PA, United States; MACN, Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Buenos Aires, Argentina; MLL-Pv, Museo Municipal de Las Lajas, Vertebrate Paleontology, Las Lajas, Neuquén, Argentina.
Publisher’s note: Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Janensch, W. Übersicht über die Wirbeltierfauna der Tendaguru-Schichten, nebst einer kurzen Charakterisierung der neu aufgeführten Arten von Sauropoden. Archiv. für Biontologie 3, 81–110 (1914).
Janensch, W. Die Wirbelsäule der Gattung Dicraeosaurus. Palaeontographica Supplement 7, 37–133 (1929).
Salgado, L. & Bonaparte, J. F. Un nuevo saurópodo Dicraeosauridae, Amargasaurus cazaui gen et sp. nov., de la Formación La Amarga, Neocomiano de la provincia del Neuquén, Argentina. Ameghiniana 28, 333–346 (1991).
Paul, G. S. Dinosaur art & restoration notes: Dicraeosaurs. The Dinosaur Report 8 (1994).
Bailey, J. B. Neural spine elongation in dinosaurs: sailbacks or buffalo-backs? J. Paleontol. 71, 1124–1146 (1997).
Schwarz, D., Frey, E. & Meyer, C. A. Pneumaticity and soft-tissue reconstructions in the neck of diplodocid and dicraeosaurid sauropods. Acta Palaeontol. Pol. 52, 167–188 (2007).
Xu, X. et al. A new Middle Jurassic diplodocoid suggests an earlier dispersal and diversification of sauropod dinosaurs. Nat. Comm. 9, 2700 (2018).
Harris, J. D. & Dodson, P. A new diplodocoid sauropod dinosaur from the Upper Jurassic Morrison Formation of Montana, USA. Acta Palaeontol. Pol. 49, 197–210 (2004).
Rauhut, O. W. M., Remes, K., Fechner, R., Cladera, G. & Puerta, P. Discovery of a short-necked sauropod dinosaur from the Late Jurassic period of Patagonia. Nature 435, 670–672 (2005).
Coria, R. A., Windholz, G. J., Ortega, F. & Currie, P. J. A new dicraeosaurid sauropod from the Lower Cretaceous (Mulichinco Formation, Valanginian, Neuquén Basin) of Argentina. Cret. Res. 93, 33–48 (2019).
Apesteguía, S. The sauropod diversity of the La Amarga Formation (Barremian), Neuquén (Argentina). Gondwana Res. 12, 533–546 (2007).
Gallina, P. A. Reappraisal of the Early Cretaceous sauropod dinosaur Amargatitanis macni (Apesteguía, 2007), from northwestern Patagonia, Argentina. Cretaceous Res. 64, 79–87 (2016).
Gallina, P. A., Apesteguía, S. & Canale, J. I. Morphological variability in the skull of dicraeosaurid sauropod dinosaurs. Ameghiniana 54, R21 (2016).
Leanza, H. A. & Hugo, C. A. Hoja Geológica 3969-III - Picún Leufú, provincias del Neuquén y Río Negro. Instituto de Geología y Recursos Naturales. SEGEMAR Boletín 218, 1–135 (1997).
Leanza, H. A. The Jurassic and Cretaceous terrestrial beds from Southern Neuquen Basin, Argentina. Field Guide. Instituto Superior de Correlación Geológica. INSUGEO Serie Misc. 4, 1–30 (1999).
Janensch, W. Die Schädel der Sauropoden Brachiosaurus, Barosaurus und Dicraeosaurus aus den Tendaguruschichten Deutsch-Ostafrikas. Palaeontographica Supplement 7, 145–298 (1935).
McIntosh, J. S. & Berman, D. S. Description of the palate and lower jaw of the sauropod dinosaur Diplodocus (Reptilia: Saurischia) with remarks on the nature of the skull of Apatosaurus. J. Paleontol. 49, 187–199 (1975).
Curry Rogers, K. A. & Forster, C. A. The skull of Rapetosaurus krausei (Sauropoda: Titanosauria) from the Late Cretaceous of Madagascar. J. Vertebr. Paleontol. 24, 121–144 (2004).
Whitlock, J. A., Wilson, J. A. & Lamanna, M. C. Description of a nearly complete juvenile skull of Diplodocus (Sauropoda: Diplodocoidea) from the Late Jurassic of North America. J. Vertebr. Paleontol. 30, 442–457 (2010).
Tschopp, E. & Mateus, O. The skull and neck of a new flagellicaudatan sauropod from the Morrison Formation and its implication for the evolution and ontogeny of diplodocid dinosaurs. J. Syst. Palaeontol. 11, 853–888 (2013).
Sereno, P. C. & Wilson, J. A. In The sauropods: evolution and paleobiology (eds Curry Rogers, K. & Wilson, J. A.) 157–177 (Univ. of California Press, Berkeley, 2005).
Tschopp, E., Mateus, O. & Benson, R. B. J. A specimen-level phylogenetic analysis and taxonomic revision of Diplodocidae (Dinosauria, Sauropoda). PeerJ 3, e857 (2015).
Whitlock, J. A. A phylogenetic analysis of Diplodocoidea (Saurischia: Sauropoda). Zool. J. Linn. Soc. 161, 872–915 (2011).
Wilson, J. A., Pol, D., Carvalho, A. B. & Zaher, H. The skull of the titanosaur Tapuiasaurus macedoi (Dinosauria: Sauropoda), a basal titanosaur from the Lower Cretaceous of Brazil. Zool. J. Linn. Soc. 178, 611–662 (2016).
Salgado, L. & Calvo, J. Cranial osteology of Amargasaurus cazaui Salgado & Bonaparte (Sauropoda, Dicraeosuridae) from the Neocomian of Patagonia. Ameghiniana 29, 337–346 (1992).
Paulina Carabajal, A., Carballido, J. L. & Currie, P. Braincase, neuroanatomy and neck posture of Amargasaurus cazaui (Sauropoda: Dicraeosauridae) and its implications for understanding head posture in sauropods. J. Vertebr. Paleontol. 34, 870–882 (2014).
Whitlock, J. A. & Harris, J. D. The dentary of Suuwassea emilieae (Sauropoda: Diplodocoidea). J. Vertebr. Paleontol. 30, 1637–1641 (2010).
Upchurch, P. The phylogenetic relationships of sauropod dinosaurs. Zool. J. Linn. Soc. 124, 43–103 (1998).
Wilson, J. A. Sauropod dinosaur phylogeny: critique and cladistics analysis. Zool. J. Linn. Soc. 136, 217–276 (2002).
Upchurch, P., Barrett, P. M., & Dodson, P. In The Dinosauria, second edition (eds Weishampel, D. B., Dodson, P. & Osmólska, H.) 259–324 (Univ. of California Press, Berkeley, 2004).
Whitlock, J. A. Was Diplodocus (Diplodocoidea, Sauropoda) capable of propalinal jaw motion? J. Vertebr. Paleontol. 37, e1296457 (2017).
Nowinski, A. Nemegtosaurus mongoliensis n. gen., n. sp. (Sauropoda) from the uppermost Cretaceous of Mongolia. Palaeont. Pol. 25, 57–81 (1971).
Tschopp, E. & Mateus, O. Osteology of Galeamopus pabsti sp. nov. (Sauropoda: Diplodocidae), with implications for neurocentral closure timing, and the cervico-dorsal transition in diplodocids. PeerJ 5, e3179 (2017).
Harris, J. D. The axial skeleton of Suuwassea emilieae (Sauropoda: Flagellicaudata) from the Upper Jurassic Morrison Formation of Montana, USA. Palaeontology 49, 1091–1121 (2006).
Ksepka, D. T. & Norell, M. A. Erketu ellisoni, a long-necked sauropod from Bor Guvé (Dornogov Aimag, Mongolia). Am. Mus. Novit. 3508, 1–16 (2006).
Bramwell, C. D. & Fellgett, P. B. Thermal regulation in sail lizards. Nature 242, 203–205 (1973).
Tomkins, J. L., Lebas, N. R., Witton, M. P., Martill, D. M. & Humphries, S. Positive allometry and the prehistory of sexual selection. Am. Nat. 176, 141–148 (2010).
Tombolato, L., Novitskaya, E. E., Chen, P.-Y., Sheppard, F. A. & McKittrick, J. Microstructure, elastic properties and deformation mechanisms of horn keratin. Acta Biomat. 6, 319–330 (2010).
Drake, A. et al. Horn and horn core trabecular bone of bighorn sheep rams absorbs impact energy and reduces brain cavity accelerations during high impact ramming of the skull. Acta Biomater. 44, 41–50 (2016).
Johnson, K. L. et al. Moisture, anisotropy, stress state, and strain rate effects on bighorn sheep horn keratin mechanical properties. Acta Biomater. 48, 300–308 (2017).
Li, B. W., Zhao, H. P., Feng, X. Q., Guo, W. W. & Shan, S. C. Experimental study on the mechanical properties of the horn sheaths from cattle. J. Exp. Biol. 213, 479–486 (2010).
Bonser, R. H. C. Hydration sensitivity of ostrich claw keratin. J. Mater. Sci. Lett. 21, 1563–1564 (2002).
Bohlman, H. H. Acute fractures and dislocations of the cervical spine. J. Bone Joint Sur. 61, 1119–1142 (1979).
Rega, E. A. et al. Healed Fractures in the Neural Spines of an Associated Skeleton of Dimetrodon: Implications for Dorsal Sail Morphology and Function. Fieldiana Life Earth Sci. 5, 104–111 (2012).
Brown, C. M. An exceptionally preserved armored dinosaur reveals the morphology and allometry of osteoderms and their horny epidermal coverings. PeerJ 5, e4066 (2017).
Apesteguía, S., Gallina, P. A. & Riguetti, F. Dicraeosaurid spines: Reservoir humps, thermoregulatory sails, excessive displays or multiple defensive horn-spines? Ameghiniana 55, R (in press).
Goloboff, P. A., Farris, J. S. & Nixon, K. TNT, a free program for phylogenetic analysis. Cladistics 24, 774–786 (2008).
Bremer, K. Branch support and tree stability. Cladistics 10, 295–304 (1994).
We thank Mr. A. Thaux and Mrs. E. J. Thaux, for kindly allowing us to enter their property and M. Soto, J. Aroca, A. Moretti, L. Ripoll, R. Zapata, M. Romero, C. Albornoz, A. Otero, G. Lio, A. Moretti, J. Pazo, F. Endres, E. Gomez, L. Toledo, V. Paz, A. Fernandez, P. Irazoqui and J.P. Garderes for collaboration in fieldworks. J. Pazo, M. Ripoll, M. Soto, A. Moretti, L. Ripoll and J. Aroca are acknowledged for their skillful preparation of the specimen. J. González helped in the design of Figures 1 and 4. We thank J.L. Carballido who helped with the phylogenetic analysis, and an anonymous reviewer who benefited this work with comments and suggestions. N. Smith generously revised the English of the manuscript. We acknowledge the Secretaría Cultura Neuquén, who provided authorizations for fieldworks, and Municipalidad de Villa El Chocón and Fundación Azara-Universidad Maimónides for logistical support. This study was funded by PICT 2013-0704 (to P.A.G.), National Geographic/Waitt Grant W645-16 (to P.A.G.) and PIP-CONICET 114 201101 00314 (to S.A.).