|
Pebas Formation
The Pebas Formation is a lithostratigraphic unit of Miocene age, found in western Amazonia. The formation extends over , including parts of Brazil, Peru, Ecuador and Colombia.Wesselingh et al., 2006 It is interpreted as representing the deposits of a lake ("Lake Pebas") or series of lakes, formed within the foreland basin of the Andes mountain belt. It is known for its abundant fossil ostracods and molluscs and an unusually diverse group of crocodylians.Sala Gismondi et al., 2006 Fossil content Correlations Laventan Huayquerian References Bibliography * * * Further reading * {{cite LSA , first=P. , last=Antoine , first2=J.A. , last2=Abello , first3=S. , last3=Adnet , first4=A.J. , last4=Altamirano Sierra , first5=P. , last5=Baby , first6=G. , last6=Billet , first7=M. , last7=Boivin , first8=Y. , last8=Calderón , last9=Candela and J. Chabain, F. Corfu, D. A. Croft, M. Ganerød, C. Jaramillo, S. Klaus, L. Marivaux, R. E. Navarrete, M. J. Orliac, F. Par ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Pebas
A lake is an area filled with water, localized in a Depression (geology), basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the World Ocean, ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glacier, glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic dra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andean Foreland Basins
The Andean foreland basins or Sub-Andean basins are a group of foreland basins located in the western half of South America immediately east of the Andes mountains. The Andean foreland basins in the Amazon River's catchment area are known as the Amazonian foreland basins. In part sediment accumulation, uplift and subsidence of the Andean foreland basins is controlled by transverse zones of "structural accommodation", likely corresponding to ancient continent-wide faults. From the Bolivian Orocline (20° S, also known as Arica Deflection or Arica Elbow) north these zones of accommodation runs with a NEE-SWW orientation and south of the orocline they run with a NW-SE orientation. The Andean foreland basins in Bolivia have largely accumulated continental sediments, most of them of clastic nature. Beginning in 1920 the Ecuadorian and Peruvian basins were explored for petroleum Petroleum, also known as crude oil, or simply oil, is a naturally occurring yellowish-black liquid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleosuchus
''Paleosuchus'' is a South American genus of reptiles in the subfamily Caimaninae of the family (biology), family Alligatoridae. They are the smallest members of the order Crocodilia in the Americas. The genus contains two extant species and a yet unnamed fossil species. References External links Alligatoridae Reptile genera Taxa named by John Edward Gray Taxonomy articles created by Polbot {{Archosaur-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mourasuchus
''Mourasuchus'' is an extinct genus of giant, aberrant caiman from the Miocene of South America. Its skull has been described as duck-like, being broad, flat, and very elongate, superficially resembling ''Stomatosuchus'' from the Late Cretaceous. History of Discovery ''Mourasuchus'' was first described by Price in 1964 based on a strange and nearly complete skull from the Solimões Formation of Amazonian Brazil, calling it ''Mourasuchus amazoniensis''. Unaware of Price's discovery, Langston described ''"Nettosuchus" atopus'' ("Absurd Duck Crocodile") only a year later based on fragmentary cranial, mandibular and postcranial remains from the middle Miocene La Venta Lagerstätte, a part of the Honda Group. Although he did recognize its similarities to caimans and alligators, Langston reasoned that its bizarre anatomy warranted its own monotypic family, naming it Nettosuchidae.Langston, W. (1965). ''Fossil crocodilians from Colombia and the Cenozoic history of the Crocodilia in So ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kuttanacaiman
''Kuttanacaiman'' is a monotypic genus of extinct caiman represented by the type species ''Kuttanacaiman iquitosensis''. ''Kuttanacaiman'' lived in what is now the Amazon basin during the Middle Miocene, approximately 13 million years ago (Ma). The species was named in 2015 on the basis of one nearly complete skull and a second partial skull from the Pebas Formation near Iquitos, Peru. ''K. iquitosensis'' is characterized by a short, rounded snout and blunt teeth at the back of its jaws that were likely adapted to crushing freshwater bivalves. Its estimated total body length is . Etymology The genus name comes from the Quechua word ''kuttana'', meaning "grinding or crushing machine", and its species name honors the Iquitos native peoples. Habitat ''Kuttanacaiman'' lived in Amazonia at a time before the Amazon River Basin was established; in its place was a massive wetland, called the Pebas Mega-Wetland System, that covered an approximate area of over in a drainage bas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Purussaurus
''Purussaurus'' is an extinct genus of giant caiman that lived in South America during the Miocene epoch, from the Friasian to the Huayquerian in the SALMA classification. It is known from skull material found in the Brazilian and Peruvian Amazon, Colombian Villavieja Formation, Panamanian Culebra Formation and the Urumaco and Socorro Formations of northern Venezuela. Description The skull length of the largest known individual of the type species, ''P. brasiliensis'' is . It has been estimated that ''P. brasiliensis'' reached about in length, weighing about . Another estimate gave a larger size of in length, ranging from , and in weight, ranging from , with a mean daily food intake of . It is also likely that ''Purussaurus'' reached only long and . A 2022 study estimated a length of and a mass of using a phylogenetic approach; and a length of and mass of using a non-phylogenetic approach. As only skulls have been found, the actual length is not certain. Bite force ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gryposuchus
''Gryposuchus'' is an extinct genus of gavialid crocodilian. Fossils have been found from Argentina, Colombia, Venezuela, Brazil and the Peruvian Amazon. The genus existed during the Miocene epoch (Colhuehuapian to Huayquerian). One recently described species, ''G. croizati'', grew to an estimated length of . ''Gryposuchus'' is the type genus of the subfamily Gryposuchinae, although a 2018 study indicates that Gryposuchinae and ''Gryposuchus'' might be paraphyletic and rather an evolutionary grade towards the gharial. Species The type species of ''Gryposuchus'' is ''G. jessei'', named based on a well-preserved rostrum collected along the Pauini River of Brazil in 1912. The specimen was probably destroyed during World War II by the 1943 bombing of Hamburg. Another specimen named UFAC 1272, consisting of a premaxilla and maxilla, was discovered in the nearby Sena Madureia locality of the late Miocene Solimões Formation, in and referred to the species in 1997. ''G. jesse ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gnatusuchus
''Gnatusuchus'' is an extinct genus of caiman represented by the type species ''Gnatusuchus pebasensis'' from the Middle Miocene Pebas Formation of Peru. ''Gnatusuchus'' lived about 13 million years ago (Ma) in a large wetland system called the Pebas mega-wetlands that covered over one million square kilometers of what is now the Amazon Basin (the modern basin had not yet developed at that time and instead of draining from west to east into the Atlantic Ocean, river systems drained northward through the wetlands and into the Caribbean Sea). Discovery and naming Fish and molluscs have long been known from the Pebas Formation, however starting in 2002 systematic surveys of the Peruvian Iquitos area have led to the discovery of many vertebrate remains including further fish remains, mammals, turtles and an abundance of crocodilians, with two contemporaneous lignitic bonebeds preserving a minimum of 7 coexisting taxa. Among the fossils recovered from the Iquitos localities is the holo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caiman Wannlangstoni
''Caiman wannlangstoni'' is an extinct species of caiman that lived in what is now the Amazon Basin and surrounding areas during the Middle and Late Miocene. Fossils of ''C. wannlangstoni'' have been found in the Pebas Formation near Iquitos in Peru and include partial skulls and isolated skull bones. Other fossils were uncovered from the Urumaco Formation in Venezuela and the Laventan Honda Group of Colombia.1 million square kilometers) drainage basin that extended from the Andes to the Caribbean Sea. During this time ''C. wannlangstoni'' would have inhabited oxygen-poor marshes and swamps, feeding on thick-shelled molluscs alongside other caiman species with crushing dentitions like ''Gnatusuchus pebasensis'' and ''Kuttanacaiman iquitosensis''. Beginning around 10.5 Ma, continued uplift of the Andes separated the Pebas region into three smaller basins: the Magdalena, Orinoco and Amazon basins. The youngest remains of ''C. wannlangstoni'' come from the Urumaco Formation, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossilworks
Fossilworks is a portal which provides query, download, and analysis tools to facilitate access to the Paleobiology Database The Paleobiology Database is an online resource for information on the distribution and classification of fossil animals, plants, and microorganisms. History The Paleobiology Database (PBDB) originated in the NCEAS-funded Phanerozoic Marine Pale ..., a large relational database assembled by hundreds of paleontologists from around the world. History Fossilworks was created in 1998 by John Alroy and is housed at Macquarie University. It includes many analysis and data visualization tools formerly included in the Paleobiology Database.{{cite web, title=Frequently asked questions, url=http://www.fossilworks.org/cgi-bin/bridge.pl?page=FAQ, publisher=Fossilworks, access-date=17 December 2021 References {{Reflist External links {{Wikidata property, P842 * [Baidu] |
Octodontoidea
Caviomorpha is the rodent infraorder or parvorder that unites all New World hystricognaths. It is supported by both fossil and molecular evidence. The Caviomorpha was for a time considered to be a separate order outside the Rodentia, but is now accepted as a genuine part of the rodents. Caviomorphs include the extinct Heptaxodontidae (giant hutias) and extant families of chinchilla rats, hutias, guinea pigs and the capybara, chinchillas and viscachas, tuco-tucos, agoutis, pacas, pacaranas, spiny rats, New World porcupines, coypu and octodonts (Vassallo and Antenucci, 2015). Origin The first known rodent fossils in South America are represented by the three taxa ''Cachiyacuy contamanensis'', ''C. kummeli'', and ''Canaanimys maquiensis'', as well as teeth from ''Eobranisamys'' sp. (Dasyproctidae) and ''Eospina'' sp., the latter two found also in the Santa Rosa fauna from the late Eocene or early Oligocene. By the late Oligocene, all superfamilies and most families of ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dinomyidae
The Dinomyidae are a family (biology), family of South American hystricognath rodents: the dinomyids were once a very speciose group, but now contains only a single living species, the pacarana. Several of the extinct dinomyids were among the largest rodents known to date; these included the bison-sized ''Josephoartigasia monesi'' and the smaller ''Josephoartigasia magna''. The dinomyids are thought to have occupied ecological niches associated with large grazing mammals due to their ability to compete with the Meridiungulata, native ungulates of South America. On the other side, they could feed on aquatic or swampy plants along the ancient rivers. These large forms disappeared after the formation of a Great American Interchange, connection to North America. The modern pacarana is only modest in size, considerably smaller than the capybara. The Neoepiblemidae, an entirely extinct family, may actually be part of the Dinomyidae; both groups are undoubtedly closely related. Genera ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
