Campananeyen is a genus of rebbachisaurid sauropod dinosaur from the Late Cretaceous (Cenomanian) Candeleros Formation of Argentina. The genus contains a single species, Campananeyen fragilissimus, known from a fragmentary skeleton.
| Campananeyen Temporal range: Late Cretaceous, lower
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Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Dinosauria |
| Clade: | Saurischia |
| Clade: | †Sauropodomorpha |
| Clade: | †Sauropoda |
| Superfamily: | †Diplodocoidea |
| Family: | †Rebbachisauridae |
| Genus: | †Campananeyen Lerzo et al., 2024 |
| Species: | †C. fragilissimus
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| Binomial name | |
| †Campananeyen fragilissimus Lerzo et al., 2024
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Discovery and naming
editThe Campananeyen holotype specimen, MMch-PV 71, was discovered in sediments of the Candeleros Formation (Barda Atravesada de Las Campanas locality) near Villa El Chocón in Neuquén Province, Argentina. The specimen consists of an incomplete skeleton, including the braincase and the right quadrate from the skull, a partial dorsal, sacral, and caudal vertebra, pieces of the ilia, and two ungual phalanges.[1] The cranial remains were described in a scientific paper published in 2016, but left unnamed.[2]
In 2024, Lerzo et al. described the specimen as a new genus and species of rebbachisaurid. The generic name, Campananeyen, is derived from Las Campanas—the name of the type locality—combined with the Mapundungun n'eyen', meaning "air", referring to the extreme pneumatic qualities of the holotype. The specific name, fragilissimus, means "the most fragile" in Latin, in reference to the notably thin ilium.[1]
Description
editThe braincase of Campananeyen exhibits several unique characteristics. The crista prootica was poorly developed, and the foramen for cranial nerve VII, the facial nerve, was open anterior to the crista prootica[1] instead of posterior to it as in Limaysaurus.[2] The paroccipital process was pneumatized. The quadrate fossa, a large fossa on the posterior surface of the quadrate bone, is greatly expanded laterally; all rebbachisaurids have a large quadrate fossa, but that of Campananenyen is 30—70% larger than any other known rebbachisaurid. The quadrate condyle, which formed the jaw joint, was more similar to Nigersaurus than Limaysaurus in that the medial hemicondyle was twice as wide as the lateral condyle.[1]
Most rebbachisaurids lack the hyposphene-hypantrum articulation between the vertebrae, but Campananeyen is one of the few that has hyposphene-hypantrum articulations. The hyposphene of Campananeyen is ovoid and hollow posteriorly, as in Nigersaurus and an unnamed species from the La Amarga Formation, and unlike the usual rhomboid hyposphene of most sauropods.[1]
As in other rebbachisaurids, the ilium contained pneumatic chambers. Due to the extensive pneumatization, the ilium was thin and fragile, and uniquely to Campananeyen the sacral ribs exhibit a dorsal alar arm that would have reinforced the pelvis to better support the leg muscles, particularly the m. iliotibialis.[1]
Classification
editIn their 2024 phylogenetic analyses, Lerzo et al. consistently recovered Campananeyen as the sister taxon of Sidersaura, within the Rebbachisauridae, in a clade also containing Zapalasaurus. Their results are displayed in the cladogram below. Specimen MACN-Pv-N 35, an unnamed rebbachisaurid from the La Amarga Formation represented by a single partial vertebra, may also be closely related to these taxa, but it was removed from most analyses to obtain more resolved results.[1]
Paleoenvironment
editThe Candeleros Formation is interpreted as a desert depositional environment, representing the Kokorkom Desert, with some oases in it, and fossils representing a faunal assemblage typical of Middle Cretaceous ecosystems in the western remnants of Gondwana.[3]
The Barda Atravesada de Las Campanas locality from which Campananeyen was recovered has also yielded partial skeletal remains of another rebbachisaurid,[4] a small unnamed abelisaurid, a chelid turtle, and a sphenodontian.[5] Several animals are also known from other localities within the formation. The dinosaurs include several more rebbachisaurid sauropods (Limaysaurus, Nopcsaspondylus, and Rayososaurus)[6] in addition to titanosaurian sauropods (Andesaurus and an unnamed giant form),[7] diverse theropods (Alnashetri, Bicentenaria, Buitreraptor, Ekrixinatosaurus, and Giganotosaurus),[8] and the enigmatic possible thyreophoran Jakapil.[3] Other animals include rhynchocephalians (Tika and Priosphenodon),[9] the snake Najash, multiple species of the crocodyliform Araripesuchus, and the mammal Cronopio.[10][11]
References
edit- ^ a b c d e f g Lerzo, Lucas N.; Fernández-Baldor, Fidel Torcida; Canale, Juan I.; Whitlock, John A.; Otero, Alejandro; Gallina, Pablo A. (2024-08-13). "They all floated in the Cretaceous: new rebbachisaurid (Sauropoda, Diplodocoidea) with a highly pneumatized skeleton from the Upper Cretaceous (lower Cenomanian) of Patagonia, Argentina". Historical Biology: 1–14. doi:10.1080/08912963.2024.2383708. ISSN 0891-2963.
- ^ a b Paulina Carabajal, A.; Canale, JI.; Haluza, A (2016). "New rebbachisaurid cranial remains (Sauropoda, Diplodocoidea) from the Cretaceous of Patagonia, Argentina, and the first endocranial description for a South American representative of the clade". Journal of Vertebrate Paleontology. 36 (5): e1167067. doi:10.1080/02724634.2016.1167067. hdl:11336/184066.
- ^ a b Riguetti FJ, Apesteguía S, Pereda-Suberbiola X (2022). "A new Cretaceous thyreophoran from Patagonia supports a South American lineage of armoured dinosaurs". Scientific Reports. 12 (1): Article number 11621. Bibcode:2022NatSR..1211621R. doi:10.1038/s41598-022-15535-6. PMC 9372066. PMID 35953515.
- ^ Haluza, Alexander; Canale, Juan Ignacio (2011). New evidence on the anatomy, function and evolutionary constraints in sauropod pedes based on new material from Mupaleo site (Candeleros Formation. Neuquén, Patagonia, Argentina. IV Latin American Congress of Vertebrate Paleontology. Vol. 48.
- ^ Canale, Juan I.; Cerda, Ignacio; Novas, Fernando E.; Haluza, Alejandro (2016). "Small-sized abelisaurid (Theropoda: Ceratosauria) remains from the Upper Cretaceous of northwest Patagonia, Argentina". Cretaceous Research. 62: 18–28. doi:10.1016/j.cretres.2016.02.001. hdl:11336/59930.
- ^ Apesteguía, Sebastián (2007). "The sauropod diversity of the La Amarga Formation (Barremian), Neuquén (Argentina)". Gondwana Research. 12 (4): 533–546. Bibcode:2007GondR..12..533A. doi:10.1016/j.gr.2007.04.007.
- ^ Otero, Alejandro; Carballido, José L.; Salgado, Leonardo; Canudo, José Ignacio; Garrido, Alberto C. (June 2021). "Report of a giant titanosaur sauropod from the Upper Cretaceous of Neuquén Province, Argentina". Cretaceous Research. 122: 104754. doi:10.1016/j.cretres.2021.104754.
- ^ Novas, Fernando E.; Ezcurra, Martín D.; Agnolin, Federico L.; Pol lfirst4=Diego; Ortíz, Raúl (2012). "New Patagonian Cretaceous theropod sheds light about the early radiation of Coelurosauria" (PDF). Revista del Museo Argentino de Ciencias Naturales. Nueva Serie. 14 (1): 57–81. ISSN 1514-5158.
{{cite journal}}: CS1 maint: numeric names: authors list (link) - ^ Apesteguía, Sebastián; Garberoglio, Fernando F.; Gómez, Raúl O. (30 September 2021). "Earliest Tuatara Relative (Lepidosauria: Sphenodontinae) from Southern Continents". Ameghiniana. 58 (5). doi:10.5710/amgh.13.07.2021.3442. ISSN 0002-7014. S2CID 239053594.
- ^ Makovicky, P. J.; Apesteguía, S. N.; Gianechini, F. A. (2012). "A New Coelurosaurian Theropod from the La Buitrera Fossil Locality of Río Negro, Argentina". Fieldiana Life and Earth Sciences. 5: 90–98. doi:10.3158/2158-5520-5.1.90. S2CID 129758444.
- ^ Guillermo W. Rougier; Sebastián Apesteguía; Leandro C. Gaetano (2011). "Highly specialized mammalian skulls from the Late Cretaceous of South America". Nature. 479 (7371): 98–102. Bibcode:2011Natur.479...98R. doi:10.1038/nature10591. PMID 22051679. S2CID 4380850.
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