The Agua de la Piedra Formation (FAP, Spanish names include Estratos de Agua de la Piedra and Complejo Volcano-sedimentario del Terciario inferior) is a Late Oligocene (Deseadan in the SALMA classification) geologic formation of the Malargüe Group that crops out in the southernmost Precordillera and northernmost Neuquén Basin in southern Mendoza Province, Argentina.

The strictly terrestrial tuffs and paleosols of the formation, geologically belonging to Patagonia, have provided a wealth of mammal fossils of various groups at Quebrada Fiera, including Mendozahippus fierensis, Pyrotherium, Coniopternium and Fieratherium. Terror birds reminiscent of the terror bird Andrewsornis and indeterminate remains of the phorusrhacid family have found in conjunction with the mammals.

The Agua de la Piedra is geologically part of the Neuquén Basin, Argentina's most prolific onshore petroleum producing basin of northwestern Patagonia, and crops out in the geographical feature of the Andean orogeny; the Argentinian Precordillera of the higher Andes in the hinterland. The Malargüe Group, of which the Agua de la Piedra Formation is the uppermost unit, hosts among the most spectacular dinosaur fossils and nesting sites in the Allen Formation, the lowermost stratigraphic unit of the group.

The Jagüel Formation, overlying the Allen Formation, hosts the Cretaceous–Paleogene boundary and has provided fossils of marine reptiles including mosasaurs and the marine turtle Euclastes meridionalis. The Roca Formation, overlying the Jagüel Formation shows evidence of Atlantic waters depositing the evaporites, claystones and limestones of the formation.

The Neuquén Basin started forming in the latest Jurassic as one of the rift basins resulting from the break-up of Pangea. While the earlier formations in the basin are mostly distal terrestrial in nature, the Agua de la Piedra Formation is a unique combination of purely terrestrial influence (paleosols) with the early Andean volcanism in the form of tuffs.

Oligocene South America differed quite substantially from the Eocene period preceding it. Isolated from Gondwana for 70 million years, the continent had developed widespread lush forests with their own specific faunas. The climate drastically cooled at the Eocene-Oligocene boundary with global cooling as a result of the formation of the Antarctic Ocean current. The South American landscape became more arid than in the Eocene with ongoing volcanism related to the Andean orogeny affecting the local climates.

The Oligocene of South America is characterized by the arrival of the first monkeys, possibly rafting from Africa, which in the Oligocene was significantly removed from South America. The first rodents had arrived to the island continent in the Late Eocene before, perhaps using similar methods of transoceanic transport. The rodents of South America diversified in the Oligocene. Cabeza Blanca, where the Sarmiento Formation outcrops, has provided the richest and most diverse Oligocene fauna of South America.

The cooler Oligocene climate led to the widespread extension of savanna and other grassland biomes. In the Early Oligocene, these rodents inhabited open and arid landscapes with wind-blown dust and grasslands environments.

The oldest confirmed New World monkey fossils stem from the Deseadan formations Salla in presently Andean Bolivia (the approximately 1,000 grams (2.2 lb) weighing Branisella boliviana and Szalatavus attricuspis half the size of Branisella) and the 2,000 g (4.4 lb) heavy Canaanimico from the Chambira of Amazonian Peru.

The rodents had arrived in the Late Eocene and diversified greatly during the Deseadan following the appearance of Andemys with species A. frassinettii and A. termasi in the Tinguirirican (Abanico Formation; Tinguiririca fauna). Caviomorphs arrived in Patagonia during the latest Eocene or early Oligocene, and by the Late Oligocene they were highly diversified, with representatives of the four main lineages. A great morphological disparity, at least in tooth morphology, was then acquired mainly by the development of hypsodonty in several lineages. The early evolution of each of the major clades was complex, especially for chinchilloids and octodontoids. The first stages of the evolution of cavioids are more obscure because they are recognized through the relatively derived Deseadan species of Cavioidea.

The Oligocene (Tinguirirican and Deseadan SALMAs plus La Cantera fauna) has a rich record of caviomorphs showing a greater morphological disparity than older faunas. Representatives of the four superfamilies, with the archetypal dental features that characterize species of the subsequent SALMAs, can be clearly recognized, at least since the Deseadan SALMA. Although a few genera (e.g., Andemys, Branisamys) cannot be assigned with certainty to any supra generic taxa. The Acaremyidae were likely a group of austral differentiation. The first representatives, the Deseadan Platypittamys brachyodon, Galileomys baios and Changquin woodi, attest to its differentiation into several lineages.

Early Andean volcanism in the Southern Cone of South America dating to the Oligocene has been found in:

• Estratos de Pupunahue
• Estratos de San Pedro
• Caleta Chonos Formation
• Cheuquemó Formation
• Temuco Formation
• Oxaya Formation
• Ancud Volcanic Complex
• Cerro Ratones

The formation comprises the "Rodados Lustrosos" level, formed by clastic heterogeneous conglomerates in a silty matrix, considered as the stratigraphic evidence of the Pehuenche orogenic phase of the Andean orogeny, followed by uniform sequences, variable in thickness, of whitish-ocher tuffaceous paleosols with concretions and whitish-gray tuffs with intercalations of pyroclastic deposits.

The upper part of the Agua de la Piedra Formation consists of 37 metres (121 ft) of white-grayish tuffs and tobaceous paleosols, with laminated or massive parallel stratification constitute the fossiliferous level of Quebrada Fiera. The formation overlies the Pircala-Coihueco Formation.

The studied profiles of the Agua de la Piedra Formation show large lateral lithological varieties, typical of alluvial fan depositional setings. The climate during deposition has been estimated to be semi-arid and the differential thicknesses of facies associations within the Agua de la Piedra Formation may represent the infill of minibasins in the forming foreland of the Andes. Sedimentary loading can enhance the effect of tectonic forces in foreland basins. The variety in volcanic fragments and composition indicates local ash fall caused by contemporaneous volcanism in the area of deposition.

2017 research on the Deseadan fauna (late Oligocene) from Quebrada Fiera, south of Mendoza Province, Argentina, evidences a rich mammal assemblage that shows the existence of common elements with Deseadan faunal associations of Patagonia and those of lower latitudes such as Salla, Bolivia, as well as endemic taxa of different groups.

Endemism refers to Notohippidae (Mendozahippus fierensis), Leontiniidae (Gualta cuyana), Homalodotheriidae (Asmodeus petrasnerus) and Metatheria (Fieratherium sorex); to these mammals a new terrestrial snail has been added in 2016.

Faunal data published in 2019 confirm the Deseadan age, but as per 2020, absolute dating is lacking for Quebrada Fiera.

The Quebrada Fiera site is situated in the Malargüe Department, southern Mendoza Province, Argentina, in the foothills of the Andes Range. The fossiliferous levels are located at around 36°33′13.3″S 69°42′3.5″W / 36.553694°S 69.700972°W / -36.553694; -69.700972 at 1,300 to 1,406 metres (4,265 to 4,613 ft) elevation. The site was discovered during a geological prospection carried out by Yacimientos Petrolíferos Fiscales (YPF) in the late 1970s (Gorroño et al., 1979). Later on, other fossil bearing levels were found at the southern side of the ravine, located at around 36°33′26″S 69°41′35″W / 36.55722°S 69.69306°W / -36.55722; -69.69306, 1,316 metres (4,318 ft) elevation.

The site is one of five recognized fossiliferous sites in Mendoza Province, with Divisadero Largo, where the Santacrucian Mariño Formarion is found, Huaquerías, defining the Huayquerian in the Huayquerías Formation, the Aisol Formation of central Mendoza and the Uspallata Group and Carrizal Formations in the north of the province.

The geological characterization and the preliminary faunal list were published by Gorroño et al. (1979). The faunal assemblage was then assigned to the Late Oligocene (Deseadan SALMA) based on the presence of two typical representatives of the Deseadean fauna of Patagonia; Pyrotherium Ameghino 1888 and Proborhyaena gigantea Ameghino 1897, both also found in the Puesto Almendra member of the Sarmiento Formation.

The species epithet Mendozahippus fierensis and genus Fieratherium refer to Quebrada Fiera.

The formation has provided fossils of:

Group	Clade	Taxa	Site	Images	Notes
Ungulates	Macraucheniidae	Coniopternium andinum	Quebrada Fiera North
	Proterotheriidae	cf. Lambdaconus suinus	Quebrada Fiera North
	Pyrotheriidae	Pyrotherium romeroi	Quebrada Fiera North
		Pyrotherium sp.	Quebrada Fiera South
	Litopterna	Litopterna indet.	Quebrada Fiera North
Cingulata	Dasypodidae	Meteutatus aff. lagenaformis	Quebrada Fiera North
		?Prozaedyus aff. impressus	Quebrada Fiera North
		Stenotatus aff. ornatus	Quebrada Fiera North
Xenarthra	Glyptodontinae	Glyptodontinae indet.	Quebrada Fiera North
	Megalonychidae	?Megalonychidae indet.	Quebrada Fiera North
Notoungulata	Notohippidae	Mendozahippus fierensis	Quebrada Fiera South
			Quebrada Fiera North
		Notohippidae indet.	Quebrada Fiera North
	Archaeohyracidae	cf. Archaeotypotherium sp.	Quebrada Fiera North
		Archaeohyrax suniensis	Quebrada Fiera North
	Hegetotheriidae	Prosotherium garzoni	Quebrada Fiera North
		cf. Prosotherium sp.	Quebrada Fiera North
		Prohegetotherium malalhuense	Quebrada Fiera North
		P. schiaffinoi	Quebrada Fiera North
		P. cf. sculptum	Quebrada Fiera North
		Prohegetotherium sp.	Quebrada Fiera North
		Hegetotheriopsis sulcatus	Quebrada Fiera North
	Homalodotheriidae	Asmodeus petrasnerus	Quebrada Fiera North
	Interatheriidae	Argyrohyrax proavus	Quebrada Fiera North
		Progaleopithecus sp.	Quebrada Fiera North
		Interatheriidae indet.	Quebrada Fiera South
	Leontiniidae	Gualta cuyana	Quebrada Fiera North
	Mesotheriidae	Trachytherus cf. spegazzinianus	Quebrada Fiera North
	Toxodontidae	Proadinotherium sp.	Quebrada Fiera North
		Toxodontidae indet.	Quebrada Fiera North
Rodents	Acaremyidae	Acaremyidae indet.	Quebrada Fiera North
Sparassodonta	Borhyaenidae	Pharsophorus sp.	Quebrada Fiera North
	Proborhyaenidae	Proborhyaena gigantea	Quebrada Fiera North
Theriiformes		Fieratherium sorex	Quebrada Fiera North
Birds	Phorusrhacidae	cf. Andrewsornis sp.	Quebrada Fiera North
		Phorusrhacidae indet.	Quebrada Fiera South
Invertebrates	Gastropods	Gastropoda indet.	Quebrada Fiera North

The Deseadan South American land mammal age (SALMA) is equivalent to the Arikareean in the North American land mammal age (NALMA) and the Harrisonian in the 2000 version of the classification. It overlaps with the Hsandagolian of Asia and the MP 25 zone of Europe, the Waitakian and the Landon epoch of New Zealand.

Deseadan correlations in South America

Formation		Rancahué	Guillermo	Mariño	Deseado	Sarmiento	Salla	Lacayani	Fray Bentos	Moquegua	Chambira	Barzalosa	Tremembé	Cascadas	Map
Basin	Neuquén		Austral	Cuyo	Deseado	San Jorge	Salla	Subandean	Norte	Moquegua	Ucayali	VSM	Taubaté	Panama	Agua de la Piedra Formation (South America)
Country	Argentina						Bolivia		Uruguay	Peru		Colombia	Brazil	Panama
Archaeohyrax
Prohegetotherium
Pyrotherium
Pharsophorus
Trachytherus
Proadinotherium
Proborhyaena
Meteutatus
Andrewsornis
Terror birds
Rodents
Reptiles
Primates
Flora
Insects
Environments	Alluvial		Fluvial	Eolian Alluvial-fluvial	Fluvial		Alluvial	Fluvial-alluvial	Fluvial	Fluvio-lacustrine		Alluvial-fluvial	Lacustrine	Fluvial	Deseadan volcanoclastics Deseadan fauna Deseadan flora
Volcanic	Yes					Yes	Yes	Yes		Yes				Yes

General

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Regional geology

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Oligocene volcanism

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Paleontology

• Schmidt, Gabriela I.; Cerdeño, Esperanza; Hernández del Pino, Santiago (2019), "Macraucheniidae and Proterotheriidae (Mammalia, Litopterna) from Quebrada Fiera (Late Oligocene), Mendoza Province, Argentina", Andean Geology, 46 (2): 368–382, doi:10.5027/andgeoV46n2-3109, hdl:11336/80129, retrieved 2020-08-11 Material was copied from this source, which is available under a Creative Commons Attribution 3.0 International License.
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New World monkeys

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Terror birds

• Sedor, Fernando A.; Vieira Dias, Eliseu; Da Cunha, Renata Floriano; Alvarenga, Herculano (2014), Paleogene phorusrhacid bird (Aves, Phorusrhacidae) from the Guabirotuba Formation, Curitiba Basin, Paraná, South of Brazil, 4th International Palaeontological Congress, p. 807, retrieved 2019-03-04
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South American rodents

• Boivin, Myriam; Marivaux, Laurent; Orliac, Maëva J.; Pujos, François; Salas Gismondi, Rodolfo; Tejada Lara, Julia V.; Antoine, Pierre-Olivier (2017), "Late middle Eocene caviomorph rodents from Contamana, Peruvian Amazonia", Palaeontologia Electronica, 20 (1): Article number 20.1.19A, retrieved 2019-02-12
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  • Ojeda, Ricardo A.; Novillo, Agustina; Ojeda, Agustina A. (2015), "Large-scale richness patterns, biogeography and ecological diversification in caviomorph rodents", SAREM Series A, Chapter 3: 121–138
• Bertrand, Ornella C.; Flynn, John J.; Croft, Darin A.; Wyss, André R. (2012), "Two new taxa (Caviomorpha, Rodentia) from the early Oligocene Tinguiririca fauna (Chile)", American Museum Novitates (3750): 1–36, doi:10.1206/3750.2, retrieved 2019-02-15
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• Cerdeño, Esperanza; Guiomar Vucetich, M. (2007), "The first rodent from the Mariño Formation (Miocene) at Divisadero Largo (Mendoza, Argentina) and its biochronological implications" (PDF), Andean Geology, 34: 199–207, doi:10.5027/andgeoV34n2-a02, retrieved 2017-10-23

Mariño Formation

• Cerdeño, Esperanza; Vera, Bárbara; Combina, Ana María (2018), "A new early Miocene Mesotheriidae (Notoungulata) from the Mariño Formation (Argentina): Taxonomic and biostratigraphic implications", Journal of South American Earth Sciences, 88: 118–131, Bibcode:2018JSAES..88..118C, doi:10.1016/j.jsames.2018.06.016, hdl:11336/158508, retrieved 2019-02-11

Rancahué Formation

• Vera, E.I (2010), "Oligocene ferns from the Rancahué Formation (Aluminé, Neuquén, Argentina): Cuyenopteris patagoniensis nov. gen., nov. sp. (Polypodiales: Blechnaceae/Dryopteridaceae) and Alsophilocaulis calveloi Menéndez emend. Vera (Cyatheales: Cyatheaceae)", Geobios, 43 (4): 465–478, Bibcode:2010Geobi..43..465V, doi:10.1016/j.geobios.2009.12.003
• Menéndez, C.A (1961), "Estípite petrificado de una nueva Cyatheaceae del Terciario de Neuquén", Boletín de la Sociedad Argentina de Botánica, IX: 331–358

Río Guillermo Formation

• Vento, B.; Gandolfo, M. A.; Nixon, K. C.; Prámparo, M. (2017), "Paleofloristic assemblage from the Paleogene Río Guillermo Formation, Argentina: preliminary results of phylogenetic relationships of Nothofagus in South America", Historical Biology, 29 (1): 93–107, Bibcode:2017HBio...29...93V, doi:10.1080/08912963.2015.1136930, hdl:11336/63607

Deseado Formation

• Agnolin, Federico (2006), "Posición sistemática de algunas aves fororracoideas (Ralliformes: Cariamae) Argentinas", Revista del Museo de Ciencias Naturales, 8: 27–33, doi:10.22179/REVMACN.8.348, retrieved 2018-09-10
• Forasiepi, Analía M.; Babot, M. Judith; Zimicz, Natalia (2014), "Australohyaena antiqua (Mammalia, Metatheria, Sparassodonta), a large predator from the Late Oligocene of Patagonia", Journal of Systematic Palaeontology, 13 (6): 503–525, Bibcode:2015JSPal..13..503F, doi:10.1080/14772019.2014.926403, hdl:11336/59430, retrieved 2019-02-12

Sarmiento Formation

• Acosta Hospitaleche, Carolina; Tambussi, Claudia (2005), "Phorusrhacidae Psilopterinae (Aves) en la Formación Sarmiento de la localidad de Gran Hondonada (Eoceno Superior), Patagonia, Argentina [Phorusrhacidae Psilopterinae (Birds) in the Sarmiento Formation from the Gran Hondonada locality (Upper Eocene), Patagonia, Argentina]" (PDF), Revista Española de Paleontología, 20: 127–132, retrieved 2018-09-10
• Arnal, Michelle; Kramarz, Alejandro G.; Vucetich, M. Guiomar; Vieytes, E. Carolina (2014), "A new early Miocene octodontoid rodent (Hystricognathi, Caviomorpha) from Patagonia (Argentina) and a reassessment of the early evolution of Octodontoidea", Journal of Vertebrate Paleontology, 34 (2): 397–406, Bibcode:2014JVPal..34..397A, doi:10.1080/02724634.2013.808203, hdl:11336/29748, retrieved 2019-02-12
• Cheme Arriaga, Lucas; Dozo, María Teresa; Gelfo, Javier N. (2016), "A new Cramaucheniinae (Litopterna, Macraucheniidae) from the early Miocene of Patagonia, Argentina", Journal of Vertebrate Paleontology, 36 (6): e1229672, Bibcode:2016JVPal..36E9672C, doi:10.1080/02724634.2017.1229672, retrieved 2019-02-12
• Dozo, María Teresa; Ciancio, Martín; Bouza, Pablo; Martínez, Gastón (2014), "Nueva asociación de mamíferos del Paleógeno en el este de la Patagonia (provincia de Chubut, Argentina): implicancias biocronológicas y paleobiogeográficas" (PDF), Andean Geology, 41: 224–247, doi:10.5027/andgeoV41n1-a09, retrieved 2017-08-15
• Pérez, María Encarnación; Krause, Marcelo; Vucetich, María Guiomar (2012), "A new species of Chubutomys (Rodentia, Hystricognathi) from the late Oligocene of Patagonia and its implications on the early evolutionary history of Cavioidea sensu stricto", Geobios, 45 (6): 573–580, Bibcode:2012Geobi..45..573P, doi:10.1016/j.geobios.2012.06.001
• Shockey, Bruce J.; Flynn, John J.; Croft, Darin A.; Gans, Phillip; Wyss, André R. (2012), "New leontiniid Notoungulata (Mammalia) from Chile and Argentina : comparative anatomy, character analysis, and phylogenetic hypotheses", American Museum Novitates (3737): 1–64, doi:10.1206/3737.2, retrieved 2019-02-15
• Sterli, Juliana; De la Fuente, Marcelo S.; Krause, J. Marcelo (2015), "A new turtle from the Palaeogene of Patagonia (Argentina) sheds new light on the diversity and evolution of the bizarre clade of horned turtles (Meiolaniidae, Testudinata)", Zoological Journal of the Linnean Society, 174 (3): 519–548, doi:10.1111/zoj.12252, hdl:11336/41594, retrieved 2019-02-13
• Vucetich, M.G.; Dozo, M.T.; Arnal, M.; Pérez, M.E. (2015), "New rodents (Mammalia) from the late Oligocene of Cabeza Blanca (Chubut) and the first rodent radiation in Patagonia", Historical Biology: An International Journal of Paleobiology, 27 (2): 236–257, Bibcode:2015HBio...27..236V, doi:10.1080/08912963.2014.883506, hdl:11336/17958, retrieved 2019-02-13
• Vucetich, María G.; Pérez, María E.; Ciancio, Martín R.; Carlini, Alfredo A.; Madden, Richard H.; Kohn, Matthew J. (2014), "A new acaremyid rodent (Caviomorpha, Octodontoidea) from Scarritt Pocket, Deseadan (late Oligocene) of Patagonia (Argentina)", Journal of Vertebrate Paleontology, 34 (3): 689–698, Bibcode:2014JVPal..34..689V, doi:10.1080/02724634.2013.804414, hdl:11336/17973, retrieved 2019-02-12
• Wyss, André R.; Flynn, John J.; Croft, Darin A. (2018), "New Paleogene notohippids and leontiniids (Toxodontia; Notoungulata; Mammalia) from the Early Oligocene Tinguiririca Fauna of the Andean Main Range, central Chile", Journal of South American Earth Sciences, 3903: 1–42, hdl:2246/6901, retrieved 2019-02-11

Salla Formation

• Reguero, Marcelo A.; Cerdeño, Esperanza (2005), "New late Oligocene Hegetotheriidae (Mammalia, Notoungulata) from Salla, Bolivia", Journal of Vertebrate Paleontology, 25 (3): 674–684, doi:10.1671/0272-4634(2005)025[0674:NLOHMN]2.0.CO;2, retrieved 2018-09-11
• Rincón, Ascanio D.; Shockey, Bruce J.; Anaya, Federico; Solórzano, Andrés (2015), "Palaeothentid Marsupials of the Salla Beds of Bolivia (Late Oligocene): Two New Species and Insights into the Post-Eocene Radiation of Palaeothentoids", Journal of Mammalian Evolution, 22 (4): 455–471, doi:10.1007/s10914-015-9295-8, retrieved 2019-02-13
• Shockey, Bruce J (2017), "New early diverging cingulate (Xenarthra: Peltephilidae) from the Late Oligocene of Bolivia and considerations regarding the origin of crown Xenarthra", Bulletin of the Peabody Museum of Natural History, 58 (2): 371–396, retrieved 2019-02-12

Lacayani fauna

• Billet, Guillaume; De Muizon, Christian; Mamani Quispe, Bernardino (2008), "Late Oligocene mesotheriids (Mammalia, Notoungulata) from Salla and Lacayani (Bolivia): implications for basal mesotheriid phylogeny and distribution", Zoological Journal of the Linnean Society, 152: 153–200, doi:10.1111/j.1096-3642.2007.00388.x, retrieved 2018-09-11

Fray Bentos Formation

• Bond, Mariano; López, Guillermo; Reguero, Marcelo A.; Scillato Yané, Gustavo J.; Vucetich, María G. (1998), "Los mamíferos de la Formación Fray Bentos (Edad mamífero Deseadense, Oligoceno Superior) de las provincias de Corrientes y Entre Ríos, Argentina", Asociación Paleontológica Argentina. Publicación Especial, 5: 41–50, retrieved 2018-09-12
• Tófalo, Ofelia Rita; Morrás, Héctor J.M. (2009), "Evidencias paleoclimáticas en duricostras, paleosuelos y sedimentitas silicoclásticas, del Cenozoico de Uruguay" (PDF), Revista de la Asociación Geológica Argentina: 674–686, retrieved 2018-09-12

Moquegua Formation

• Alván, Aldo; Ramírez, Katerin; von Eynatten, Hilmar; Dunkl, István; Jacay, Javier; Bertone, Gabriela (2017), "Evolución Geológica de las Cuencas de Antearco del Sur de Perú (Moquegua y Camaná-Mollendo): Proveniencia Sedimentaria y Análisis de Facies en Rocas Cenozoicas", Boletín de la Sociedad Geológica del Perú, 112: 53–77, retrieved 2018-09-10
• Shockey, Bruce J.; Billet, Guillaume; Salas Gismondi, Rodolfo (2016), "A new species of Trachytherus (Notoungulata: Mesotheriidae) from the late Oligocene (Deseadan) of Southern Peru and the middle latitude diversification of early diverging mesotheriids", Zootaxa, 4111 (5): 565–583, doi:10.11646/zootaxa.4111.5.3, PMID 27395103, retrieved 2019-02-12

Chambira Formation

• Boivin, Myriam; Marivaux, Laurent; Antoine, Pierre-Olivier (2019), "New insight from the Paleogene record of Amazonia into the early diversification of Caviomorpha (Hystricognathi, Rodentia): phylogenetic, macroevolutionary, and paleobiogeographic implications", Geodiversitas, 41 (4): 143–245, doi:10.5252/geodiversitas2019v41a4, retrieved 2019-02-28
• Boivin, Myriam; Marivaux, Laurent; Candela, Adriana M.; Orliac, Maëva J.; Pujos, François; Salas Gismondi, Rodolfo; Tejada Lara, Julia V.; Antoine, Pierre-Olivier (2016), "Late Oligocene caviomorph rodents from Contamana, Peruvian Amazonia", Papers in Palaeontology, 3 (1): 69–109, doi:10.1002/spp2.1068, hdl:11336/63600, retrieved 2019-02-12
• Marivaux, Laurent; Adnet, Sylvain; Altamirano Sierra, Ali J.; Boivin, Myriam; Pujos, François; Ramdarshan, Anusha; Salas Gismondi, Rodolfo; Tejada, Julia; Antoine, Pierre-Olivier (2016), "Neotropics provide insights into the emergence of New World monkeys: New dental evidence from the late Oligocene of Peruvian Amazonia", Journal of Human Evolution, 97: 159–175, Bibcode:2016JHumE..97..159M, doi:10.1016/j.jhevol.2016.05.011, hdl:11336/182832, PMID 27457552, retrieved 2019-02-04

Barzalosa Formation

• Acosta, Jorge E.; Guatame, Rafael; Caicedo A., Juan Carlos; Cárdenas, Jorge Ignacio (2002), Mapa Geológico de Colombia - Plancha 245 - Girardot - 1:100,000 - Memoria Explicativa, INGEOMINAS, pp. 1–92
• Acosta, Jorge E.; Ulloa, Carlos E. (2001), Mapa Geológico de Colombia - Plancha 246 - Fusagasugá - 1:100,000 - Memoria Explicativa, INGEOMINAS, pp. 1–77

Tremembé Formation

• Do Couto Ribeiro, Graziella (2010), Avaliação morfológica, taxonômica e cronológica dos mamíferos fósseis da Formação Tremembé (Bacia de Taubaté), Estado de São Paulo, Brasil, Universidade de São Paulo, pp. 1–112
• Malabarba, Maria Claudia; Lundberg, John G. (2007), "A fossil loricariid catfish (Siluriformes: Loricarioidea) from the Taubaté Basin, eastern Brazil", Neotropical Ichthyology, 5 (3): 263–270, doi:10.1590/S1679-62252007000300005, retrieved 2018-10-08
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Las Cascadas Formation

• Rincón, A. F.; Bloch, J. I.; Suárez, C.; MacFadden, B. J.; Jaramillo, C. A. (2012), "New floridatragulines (Mammalia, Camelidae) from the early Miocene Las Cascadas Formation, Panama", Journal of Vertebrate Paleontology, 32 (2): 456–475, Bibcode:2012JVPal..32..456R, doi:10.1080/02724634.2012.635736

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