Bagualia

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Bagualia
Temporal range: Early Jurassic (middle Toarcian), ~179.17 Ma [1]
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Bagualia alba (skeletal reconstruction).png
Reconstructed skeleton and skull of Bagualia with known material in white
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade: Saurischia
Clade:† Sauropodomorpha
Clade:† Sauropoda
Clade:† Eusauropoda
Genus:† Bagualia
Pol et al., 2020
Type species
†Bagualia alba
Pol et al., 2020

Bagualia (meaning "wild horse"), is an extinct genus of eusauropod dinosaur, from the Early Jurassic (Middle Toarcian) Epoch in what is now the Chubut Province of Argentina. The type species, B. alba, was formally described in 2020. Bagualia represents the oldest definitive Eusauropod, and due to the completeness of its material it represents one of the most important taxa for understanding the early evolution of the group.

Contents

Discovery and naming

The Bagualia fossil material was discovered in Bagual Canyon, approximately 4.3 kilometres (2.7 mi) from Cerro Cóndor in Chubut, Argentina within the Early Jurassic deposits of the Cañadón Asfalto Formation. The fossils were excavated by the Museo Paleontológico Egidio Feruglio during fieldwork in 2007 and 2009. [2] The remains were embedded in a dark grey pelitic matrix rich in organic matter. This layer, dated precisely to around 179 million years ago, formed in a lacustrine environment beneath a basaltic layer. The fossils include the holotype, MPEF-PV 3301 (a partial skull with cervical vertebrae), and additional remains from at least three individuals (MPEF-PV 3305–3348). [3] [2]

The generic name, Bagualia comes from "bagual," the Spanish word for "wild horse," referencing the specimens' discovery in the Bagual Canyon ("Cañadón Bagual"). The specific name, alba, is a Spanish word meaning "dawn," highlighting the dinosaur's early age in the sauropod lineage. [3]

Description

Tooth of Bagualia collected during excavation Bagualia teeth at the excavation site.jpg
Tooth of Bagualia collected during excavation

Bagualia is known from many bones from three individuals, including vertebrae from the neck, back, and tail, limb and girdle bones, as well as skull and teeth fragments. The size of Bagualia was likely brought on by a newly formed ecosystem and climate shifts, which were all caused by volcanic activity in the Southern Hemisphere during the Early Jurassic. While the harsh climate and ashes drove most sauropodomorphs to extinction, Bagualia was able to adapt to newly sprouted conifers and plants, using its long neck to snip plant matter from them while staying in place, conserving energy. Its teeth are surrounded by a thick layer of enamel, roughly 7x thicker than other extinct herbivores, enabling the animal to better shear conifer leaves. The digestive system of Bagualia was also a likely reason why it grew to such a large size, and another function of its long neck has been proposed: it may have dissipated heat in a similar fashion to how elephants use their ears. [3]

Skull

The skull of Bagualia is relatively complete. The premaxilla is robust and nearly complete with a tall, lateromedially compressed structure, with a smooth lateral surface with several foramina, and its anterior margin lacks a step. A beak-like process is present at the anteroventral end, unique to Bagualia, which may have supported a larger keratinous structure. The maxilla of Bagualia shows 13 alveoli, with some teeth preserved in varying stages of eruption. It has a prominent premaxillary process and a deep narial fossa. Although the ascending process of the maxilla is missing, the antorbital fenestra and lacrimal processes are well-defined. The maxilla articulates with the jugal and palatine, but lacks contact with the ectopterygoid. The right nasal has a broad but damaged articulation with the frontal and a thinner connection with the prefrontal. The lacrimal is robust and dorsoventrally tall, with distinct articulations for the jugal, maxilla, prefrontal, and nasal, similar to other sauropods like Camarasaurus and Turiasaurus . The rhomboid-shaped left prefrontal features prominent articular facets for the lacrimal, nasal, and frontal bones, characterized by its elongated shape and triangular cross-section. The postorbital forms the posterior and posterodorsal boundaries of the orbit, featuring a slender ventral process typical of early sauropodomorphs. The robust squamosals have four articulating processes, with the longest ventral process contributing to an 'S'-shaped profile. [2]

The braincase is nearly complete and ossified, showcasing a robust and tall structure similar to other eusauropods. It features limited cranial pneumaticity and lacks certain recesses, with an elliptical foramen magnum dorsoventrally oriented, contrasting with the circular shape seen in many non-sauropod sauropodomorphs. The paroccipital process is laterally projected, with a unique morphology that differs from other sauropodomorphs. [2]

The right dentary has 16 alveoli and shows an emerging tooth, while the left dentary has 14 alveoli with five partially erupted teeth. Notably, these dentaries exhibit a U-shaped configuration characteristic of eusauropods, featuring unique structural traits, including well-developed alveoli and a prominent coronoid process on the surangular. The teeth are spoon-shaped with heavily wrinkled enamel, displaying asymmetrical mesial and distal margins, characteristic of many sauropodomorphs, with notable features like a medial convex area and a procumbent arrangement typical of eusauropods. Numerous small pores on the ventral margin, along with little wear on the first erupted tooth, may indicate a vascular function, possibly supporting a keratin-like covering. [2]

Axial skeleton

All cervical vertebrae exhibit an opisthocoelous structure, featuring elongated centra and a ventral keel. The recovered proatlas is robust and rhomboid in shape, while the atlas is distinguished by its elongated neurapophyses. The axis reveals notable features, such as deep lateral fossae and a prominent neural arch, indicating the holotype likely belonged to a subadult individual. Cervical ribs feature a tetraradiate shape at their proximal ends, characterized by a prominent tuberculum, capitulum, and anterior process, along with a long, slender shaft directed posteriorly, consistent with most sauropods. [4]

The preserved dorsal vertebrae, unlike the cervical vertebrae, exhibit more developed zygapophyses, apophyses, and bony laminae. The parapophyses shift from the mid-length of the centrum in the anterior dorsal vertebrae to the neural arch starting from the third dorsal vertebra, a characteristic found in all sauropods. The dorsal ribs are represented by various isolated fragments that cannot be accurately matched. [4]

The pelvic girdle is compressed and misaligned, with left elements shifted posteriorly relative to the right. The sacrum, composed of five vertebrae, has fused sacral ribs, with variations in development and orientation. The neural spines are plate-like and lack lateral fossae, differing from those of some other sauropods, and are fused and posteriorly curved. The sacral ribs are positioned away from the acetabulum, indicating a non-sauropod sauropodomorph structure. [4]

The caudal vertebrae demonstrate distinguishing characteristics including the elongation index, neural spine inclination, and transverse process development. The anterior caudal vertebrae display distinct morphology with amphicoelous centra and well-developed transverse processes, while the middle vertebrae are more elongated with marked articular facets for haemal arches. In the posterior caudal vertebrae, the centra are significantly longer than tall, lacking transverse processes and lateral fossae, with decreasing neural spine angles observed towards the tail's end. The haemal arches contain a canal that occupies roughly 20% of the overall chevron length, exhibiting differences when analyzed alongside other eusauropod lineages. Their concave surfaces, extended ventral blades, and central ridges align with characteristics observed in multiple sauropod taxa. Additionally, the posterior haemal arches tend to become shorter and thicker at their distal ends. [4]

Classification

Bagualia is considered to be an early member of Eusauropoda. Due to its provenance from the Cañadon Asfalto Formation, which is dated to the Toarcian, its describers interpret this as evidence of a eusauropod dominance after an Early Jurassic global warming event, replacing more basal sauropodomorphs. Successive phylogenetic analyses from 2020, 2021, and 2024 have confirmed a close relationship between Bagualia, Nebulasaurus , Patagosaurus , and Spinophorosaurus . The results of Gomez et al. (2024) are shown in the cladogram below: [3] [4] [2]

Sauropoda

Paleoenvironment

Lake Magadi Horizon.jpg
2018-12-30 114345 Waimangu Volcanic Valley anagoria.jpg
Painted Dunes and lava flows (17492501842).jpg
The Chacritas Member hosted and hypersaline and alkaline lake similar to modern Lake Magadi in Kenya, while nearby environments where developed in a similar way to modern Waimangu Volcanic Rift Valley of New Zealand, with nearby volcanic influence of the Chon Aike Province that likely developed in a similar way to modern California volcanic fields

The Chacritas Member of the Cañadón Asfalto Formation hosted a hypersaline and alkaline lake similar to modern Lake Magadi in Kenya, while nearby environments were developed in a similar way to modern Waimangu Volcanic Rift Valley of New Zealand, with the nearby volcanic influence of the Chon Aike Province that likely developed in a similar way to modern California volcanic fields. The holotype of Asfaltovenator comes from the Chacritas Member of the Cañadón Asfalto Formation. This member is mostly made up of two major depositional settings: lacustrine and fluvial deposits. Both of these have intervals of tuffaceous materials, suggesting the presence of volcanic activity. [5] Palustrine littoral environment levels are seen at Cerro Cóndor and Estancia Fossati, characterized by the presence of lacustrine limestones interbedded with shales, tuffs and sandstones. [6] The lacustrine section has been called the "Chacritas Paleolake", and seems to have been a rather saline or even hypersaline hydrologically closed pan lake, shallow in depth, with marginal zones and palustrine subenvironments made of low-energy ramp-like margins. [7] [8]

Bagualia has important paleoecological implications due to its robust skull and broad teeth, which indicate a shift towards bulk browsing on tough vegetation, such as conifers from families like Araucariaceae, Cheirolepidiaceae, and Cupressaceae after the Toarcian Oceanic Anoxic Event, what may have been a key for their success after local environmental change. [3] [2] This adaptation allowed it to process fibrous plant material, reflecting its capacity to exploit new dietary resources during the end of the Early Jurassic. [9] The features of Bagualia highlight a key evolutionary step between early sauropodomorphs and derived eusauropods, suggesting significant ecological interactions as environments changed. [2]

In addition to the Bagualia fossils, the site also yielded remains of different conifer families, turtle fossils, and teeth from at least four theropod dinosaurs. The presence of these diverse remains, mixed in the sediment, suggests a rich and complex ecosystem during the Early Jurassic period. [2]

Related Research Articles

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<i>Piatnitzkysaurus</i> Extinct genus of dinosaurs

Piatnitzkysaurus is a genus of tetanuran theropod dinosaur that lived approximately 179 to 177 million years ago during the lower part of the Jurassic Period in what is now Argentina. Piatnitzkysaurus was a moderately large, lightly built, bipedal, ground-dwelling carnivore that could grow up to 6.6 m (21.7 ft) long.

<i>Tazoudasaurus</i> Extinct genus of dinosaurs

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Volkheimeria is an extinct genus of sauropod dinosaurs that lived in what is now Argentina during the Early Jurassic, 178–179 million years ago. Its type and only species is Volkheimeria chubutensis.

<i>Condorraptor</i> Extinct genus of dinosaurs

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References

  1. ↑ Fantasia, A.; Föllmi, K. B.; Adatte, T.; Spangenberg, J. E.; Schoene, B.; Barker, R. T.; Scasso, R. A. (2021). "Late Toarcian continental palaeoenvironmental conditions: An example from the Cañadón Asfalto Formation in southern Argentina". Gondwana Research. 89 (1): 47–65. Bibcode:2021GondR..89...47F. doi:10.1016/j.gr.2020.10.001. S2CID   225120452 . Retrieved 27 August 2021.
  2. 1 2 3 4 5 6 7 8 9 Gomez, Kevin L.; Carballido, José L.; Pol, Diego (2024-10-14). "Cranial anatomy of Bagualia alba (Dinosauria, Eusauropoda) from the Early Jurassic of Patagonia and the implications for sauropod cranial evolution". Journal of Systematic Palaeontology . 22 (1). doi:10.1080/14772019.2024.2400471. ISSN   1477-2019.
  3. 1 2 3 4 5 D. Pol; J. Ramezani; K. Gomez; J. L. Carballido; A. Paulina Carabajal; O. W. M. Rauhut; I. H. Escapa; N. R. Cúneo (2020). "Extinction of herbivorous dinosaurs linked to Early Jurassic global warming event". Proceedings of the Royal Society B: Biological Sciences. 287 (1939): Article ID 20202310. doi: 10.1098/rspb.2020.2310 . PMC   7739499 . PMID   33203331. S2CID   226982302.
  4. 1 2 3 4 5 Gomez, Kevin; Carballido, Jose; Pol, Diego (2021). "The axial skeleton of Bagualia alba (Dinosauria: Eusauropoda) from the Early Jurassic of Patagonia". Palaeontologia Electronica . doi: 10.26879/1176 . hdl: 11336/166827 .
  5. ↑ Cabaleri, N. G.; Benavente, C. A. (2013). "Sedimentology and paleoenvironments of the Las Chacritas carbonate paleolake, Cañadón Asfalto Formation (Jurassic), Patagonia, Argentina". Sedimentary Geology. 284 (4): 91–105. Bibcode:2013SedG..284...91C. doi:10.1016/j.sedgeo.2012.11.008. hdl: 11336/182449 . Retrieved 29 July 2022.
  6. ↑ Cabaleri, Nora; Volkheimer, Wolfgang; Armella, Claudia; Gallego, Oscar Florencio; Monferran, Mateo Daniel; Cagnoni, Mariana; Silva Nieto, Diego; Páez, Manuhel (2010). "Humedales jurásicos y del J/K en la Cuenca Cañadón Asfalto, río Chubut medio. Argentina". 4º Simposio Argentino del Jurásico. 4 (2): 18.
  7. ↑ Cabaleri, N. G.; Armella, C.; Silva Nieto, D. G. (2005). "Saline paleolake of the Cañadón Asfalto Formation (Middle-Upper Jurassic), Cerro Cóndor, Chubut province (Patagonia), Argentina". Facies. 51 (1): 350–364. Bibcode:2005Faci...51..350C. doi:10.1007/s10347-004-0042-5. S2CID   129090656 . Retrieved 17 August 2022.
  8. ↑ Cabaleri, N.; Volkheimer, W.; Armella, C.; Gallego, O.; Silva Nieto, D.; Páez, M.; Koukharsky, M. (2010). "Estratigrafía, análisis de facies y paleoambientes de la Formación Cañadón Asfalto en el depocentro jurásico Cerro Cóndor, provincia del Chubut". Revista de la Asociación Geológica Argentina. 66 (3): 349–367. Retrieved 2022-09-05.
  9. ↑ Pol, Diego; Gomez, Kevin; Holwerda, Femke M.; Rauhut, Oliver W. M.; Carballido, José L. (2022), "Sauropods from the Early Jurassic of South America and the Radiation of Eusauropoda", Springer Earth System Sciences, Cham: Springer International Publishing, pp. 131–163, ISBN   978-3-030-95958-6 , retrieved 2024-10-17
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