Portezuelo Formation
| Portezuelo Formation | |
|---|---|
| Stratigraphic range: late Turonian–early Coniacian ~ | |
| Type | Geological formation |
| Unit of | Neuquén Group Río Neuquén Subgroup |
| Underlies | Los Bastos Formation |
| Overlies | Lisandro Formation |
| Thickness | 95–130 m (312–427 ft) |
| Lithology | |
| Primary | Sandstone |
| Other | Conglomerate, limestone |
| Location | |
| Coordinates | 38°30′S 68°42′W / 38.5°S 68.7°W |
| Approximate paleocoordinates | 44°24′S 47°12′W / 44.4°S 47.2°W |
| Region | Mendoza, Río Negro & Neuquén Provinces |
| Country | Argentina |
| Extent | Neuquén Basin |
| Type section | |
| Named for | Sierra del Portezuelo |
  Portezuelo Formation (Argentina) | |
The Portezuelo Formation is a geologic formation of Late Cretaceous (Late Turonian to Early Coniacian) age, outcropping in the Mendoza, Río Negro and Neuquén provinces of Argentina.[1] It is the fourth-oldest formation in the Neuquén Group and the older of the two formations in the Río Neuquén Subgroup. Formerly, that subgroup was treated as a formation, and the Portezuelo Formation was known as the Portezuelo Member.[2]
Description
[edit]The type locality of the Portezuelo Formation is the mountain range known as Sierra del Portezuelo in Neuquén Province.[3] This formation conformably overlies the Lisandro Formation of the Río Limay Subgroup. In the top layers it grades into the Plottier Formation, the younger formation within the Río Neuquén Subgroup.
Sandstones and siltstones, probably deposited under fluvial conditions, make up the Portezuelo Formation. There are also occasional cemented claystone deposits, as well as numerous paleosols (fossil soils). The formation varies between 95 and 130 metres (312 and 427 ft) thick throughout its range.[2][4]
Fossil content
[edit]
Many dinosaur fossils have recently been described from this formation, as well as remains of several other types of animals:
- teleosteid fish including Leufuichthys
- ceratodontiform lungfish including Chaoceratodus[5]
- abundant and diverse turtles including Baalemys[6], Portezueloemys and a species of Prochelidella
- titanosaurian sauropods including Futalognkosaurus, Baalsaurus, Malarguesaurus, Muyelensaurus
- dromaeosaurid theropods including Neuquenraptor, Unenlagia, Pamparaptor[7][8]
- megaraptorid theropods (including Megaraptor and an unnamed form)[7][9]
- an alvarezsaurid theropod Patagonykus[7]
- abelisauroid theropods (Elemgasem, a possible noasaurid and an abelisaurid)[1][10]
- An elasmarian ornithopod (Macrogryphosaurus)[11]
- notosuchian crocodylomorphs (Comahuesuchus, Lomasuchus, Patagosuchus)
- several other theropods, including a modern, possibly galliform bird[7]
- ornithopods including possible iguanodonts
- a possible azdarchoid pterosaur Argentinadraco
See also
[edit]References
[edit]
Wikimedia Commons has media related to Portezuelo Formation.
- ^ a b Portezuelo Formation at Fossilworks.org
- ^ a b Sánchez et al., 2006
- ^ Wichmann, 1929
- ^ Leanza et al., 2004
- ^ Panzeri, K. M.; Guzmán, F. A. (2024). "Unveiling the histology and anatomy of the lungfish Chaoceratodus portezuelensis (Sarcopterygii: Dipnoi) from the Portezuelo and Cerro Lisandro formations (Upper Cretaceous) of Argentine Patagonia". Palaeontologia Electronica. 27 (2). 27.2.a42. doi:10.26879/1408.
- ^ Sarda, M.; Maniel, I. J. (2024). "A new chelid turtle with an ornamented bony shell (Pleurodira: Chelidae) from the Portezuelo Formation (Upper Cretaceous) of Patagonia, Argentina". Historical Biology: An International Journal of Paleobiology. doi:10.1080/08912963.2024.2437832.
- ^ a b c d Agnolin et al., 2006
- ^ Porfiri et al., 2007
- ^ Paulina-Carabajal and Currie, 2017
- ^ Baiano, Mattia A.; Pol, Diego; Bellardini, Flavio; Windholz, Guillermo J.; Cerda, Ignacio A.; Garrido, Alberto C.; Coria, Rodolfo A (2022-09-05). "Elemgasem nubilus: a new brachyrostran abelisaurid (Theropoda, Ceratosauria) from the Portezuelo Formation (Upper Cretaceous) of Patagonia, Argentina". Papers in Palaeontology. 8 (5): e1462. Bibcode:2022PPal....8E1462B. doi:10.1002/spp2.1462.
- ^ Rozadilla, Sebastián; Cruzado-Caballero, Penélope; Calvo, Jorge O. (April 2020). "Osteology of Ornithopod Macrogryphosaurus gondwanicus (Dinosauria, Ornithischia) from the Upper Cretaceous of Patagonia, Argentina". Cretaceous Research. 108: 104311. Bibcode:2020CrRes.10804311R. doi:10.1016/j.cretres.2019.104311. S2CID 213679041.
Bibliography
[edit]- Agnolin, Federico L.; Novas, Fernando E.; Lio, Gabriel (2006). "Neornithine bird coracoid from the Upper Cretaceous of Patagonia". Ameghiniana. 43: 245–248. Retrieved 2019-02-16.
- Leanza, H.A.; Apesteguia, S.; Novas, F.E.; De la Fuente, M.S. (2004). "Cretaceous terrestrial beds from the Neuquén Basin (Argentina) and their tetrapod assemblages". Cretaceous Research. 25 (1): 61–87. Bibcode:2004CrRes..25...61L. doi:10.1016/j.cretres.2003.10.005. Retrieved 2019-02-16.
- Paulina-Carabajal, Ariana; Currie, Philip (2017). "The braincase of the theropod dinosaur Murusraptor: osteology, neuroanatomy and comments on the paleobiological implications of certain endocranial features". Ameghiniana. 54 (5): 617–640. doi:10.5710/AMGH.25.03.2017.3062. hdl:11336/184065. Retrieved 2020-12-11.
- Porfiri, Juan D.; Calvo, Jorge Orlando; Dos Santos, Domenica Diniz; Juárez Valieri, Ruben D. (2007). New record of Neuquenraptor (Theropoda, Dromaeosauridae) from the Late Cretaceous of Patagonia. Jornadas Argentinas de Paleontología de Vertebrados. pp. 34R. Retrieved 2019-02-16.
- Sánchez, María Lidia; Heredia, Susana; Calvo, Jorge O. (2006). "Paleoambientes sedimentarios del Cretácico Superior de la Formación Plottier (Grupo Neuquén), Departamento Confluencia, Neuquén (Sedimentary paleoenvironments in the Upper Cretaceous Plottier Formation (Neuquen Group), Confluencia, Neuquén)". Revista de la Asociación Geológica Argentina. 61: 3–18. Retrieved 2019-02-16.
- Wichmann, R (1929). "Los Estratos con Dinosaurios y su techo en el este del Territorio del Neuquén ("The dinosaur-bearing strata and their upper limit in eastern Neuquén Territory")". Dirección General de Geología, Minería e Hidrogeología Publicación. 32: 1–9.