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Progaleopithecus
''Progaleopithecus'' is an extinct genus of interatheriid notoungulate that lived during the Late Oligocene of Argentina. Fossils of this genus have been found in the Agua de la Piedra, Deseado, and Sarmiento Formations of Argentina. Taxonomy ''Progaleopithecus'' was first named in 1904 by Florentino Ameghino based on remains found in the Sarmiento Formation of Argentina, dating to the Late Oligocene, around 28 to 23 mya. It is a derived member of the Interatheriidae, within the subfamily Interatheriinae. The following cladogram of the Interatheriinae Interatheriinae is an extinct subfamily of interatheriids that consisted of notoungulates dating from the Early Eocene (Casamayoran SALMA) to the Early Pliocene (Montehermosan SALMA). The subfamily includes the genera '' Archaeophylus'', '' Argy ... is based on Vera ''et al.'' 2017, showing the position of ''Progaleopithecus''. References {{Taxonbar, from=Q113638577 Typotheres Prehistoric placental genera Oligoce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deseadan
The Deseadan ( es, Deseadense) age is a period of geologic time (29.0–21.0 Ma) within the Oligocene epoch of the Paleogene to the Early Miocene epoch of the Neogene, used more specifically within the SALMA classification of South America. It follows the Tinguirirican and precedes the Colhuehuapian age. Etymology The age is named after the Deseado Formation of the Deseado Massif in eastern Patagonia, Argentina. Formations Fossils Correlations 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 Landon is a personal name of English origin that means "long hill". It is a variant of Langdon. Landon became popular in the United States in the 1990s, and by 2010 had become the 32nd most popular name for boys. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Interatheriinae
Interatheriinae is an extinct subfamily of interatheriids that consisted of notoungulates dating from the Early Eocene (Casamayoran SALMA) to the Early Pliocene (Montehermosan SALMA). The subfamily includes the genera '' Archaeophylus'', ''Argyrohyrax'', ''Boleatherium'', ''Brucemacfaddenia'', '' Caenophilus'', '' Choichephilum'', ''Cochilius'', ''Eopachyrucos'', ''Federicoanaya'', '' Interatherium'', ''Juchuysillu'', ''Miocochilius'', '' Neoicochilus'', ''Patriarchus'', ''Proargyrohyrax'', ''Progaleopithecus'', ''Protypotherium'', and '' Santiagorothia''. They were small to medium sized interatheres, and when compared to the other subfamily, Notopithecinae, interatheriines are found to occupy an advanced, derived position in the family. Material was copied from this source, which is available under a Creative Commons Attribution 4.0 International License Description Interatheriines were generally small to medium-sized interatheriids, and rarely exceeded the size of a groundhog. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brucemacfaddenia
''Brucemacfaddenia'' is an extinct genus of interatheriine notoungulates that lived during the Late Oligocene in what is now Bolivia. Fossils of this genus have been found in the Salla Formation of Bolivia. Etymology The genus name, ''Brucemacfaddenia'', refers to Bruce MacFadden, known for his significant contributions of Cenozoic mammal evolution in Bolivia. paleontology. The specific name, ''boliviensis'', refers to Bolivia, the country where it was found in. Description ''Brucemacfaddenia'' was a small-sized interatheriid. The derived features of ''Brucemacfaddenia'' that set it apart from other basal interatheriines such as '' Proargyrohyrax'' and ''Santiagorothia'', by having hypselodont cheek teeth an completely persistent lingual sulcus on the upper molars. Its deciduous upper detention had thin enamel. Taxonomy ''Brucemacfaddenia'' was first described in 2008 based on remains found in the Salla Formation, in the La Paz Department, Bolivia, dating to the Lat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Federicoanaya
''Federicoanaya'' is an extinct genus of interatheriine notoungulates that lived during the Late Oligocene in what is now Bolivia. Fossils of this genus have been found in the Salla Formation of Bolivia. Etymology The genus name, ''Federicoanaya'', refers to Federico Anaya, known for his significant contributions to Bolivian paleontology. The specific name, ''sallaensis'', refers to the Salla Formation where it was found. Description ''Federicoanaya'' was a small-sized interatheriid. It can be distinguished from other basal interatheriines such as '' Proargyrohyrax'' and ''Santiagorothia'', by having hypselodont cheek teeth an completely persistent lingual sulcus on the upper molars. Its permanent upper dentition had thin cementum. ''Federicoanaya'', along with ''Brucemacfaddenia'', share upper cheek teeth with a median lobe and a labially extended parastyle in molars. Taxonomy ''Federicoanaya'' was first described in 2008 based on remains found in the Salla Formation, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eopachyrucos
''Eopachyrucos'' is an extinct genus of interatheriid notoungulates that lived from the Middle Eocene to the Late Oligocene of Argentina and Uruguay. Fossils of this genus have been found in the Sarmiento Formation of Argentina and the Fray Bentos Formation of Uruguay. Taxonomy ''Eopachyrucos'' was first named in 1901 by Florentino Ameghino based on fragmentary remains found in the Sarmiento Formation of Argentina. He originally considered it as a member of the family Hegetotheriidae, as an ancestor of ''Pachyrukhos'', as reflected in its name ("dawn ''Pachyrukhos''), however, recent studies have confirmed it to be a member of the family Interatheriidae, more specifically within the subfamily Interatheriinae. The following cladogram of the Interatheriinae Interatheriinae is an extinct subfamily of interatheriids that consisted of notoungulates dating from the Early Eocene (Casamayoran SALMA) to the Early Pliocene (Montehermosan SALMA). The subfamily includes the genera '' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocochilius
''Miocochilius'' is an extinct genus of small notoungulate mammals (typotheres) native to South America. The genus lived during the Middle Miocene epoch ( Laventan in the SALMA classification). The genus contains two described species, the type species ''M. anomopodus'' described in 1953 by Ruben Arthur Stirton and ''M. federicoi'', described and included in the genus by Darin A. Croft. Fossils of ''Miocochilius'' have been found at the Lagerstätte of La Venta in the Honda Group of Colombia, where it is the most abundant mammal, the Honda Group of Bolivia (''M. federicoi'') and the Ipururo Formation in the Ucayali Basin of Peru. The typothere lived alongside a rich faunal assemblage comprising many other mammals, crocodylians, turtles and lizards. Description The genus ''Miocochilius'' was first described by Ruben Arthur Stirton in 1953, based on a nearly complete and numerous incomplete skeletons found in the Honda Group of Colombia. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Protypotherium
''Protypotherium'' is an extinct genus of notoungulate mammals native to South America during the Oligocene and Miocene epochs. A number of closely related animals date back further, to the Eocene. Fossils of ''Protypotherium'' have been found in the Deseadan Fray Bentos Formation of Uruguay, Muyu Huasi and Nazareno Formations of Bolivia, Cura-Mallín and Río Frías Formations of Chile, and Santa Cruz, Salicas, Ituzaingó, Aisol, Cerro Azul, Cerro Bandera, Cerro Boleadoras, Chichinales, Sarmiento and Collón Curá Formations of Argentina. Taxonomy ''Protypotherium'' was a typical representative of the Interatheriidae, a group of typotherian notoungulates with rodent-like appearances, usually with slender forms. The genus has a wide stratigraphic and geographic distribution, around 29 million years. Fossils assigned to ''Protypotherium'' have been found in numerous localities in Argentina, Bolivia, Chile, and Uruguay. Material was copied from this source, which is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sarmiento Formation
The Sarmiento Formation (Spanish: ''Formación Sarmiento''), in older literature described as the Casamayor Formation, is a geological formation in Chubut Province, Argentina, in central Patagonia, which spans around 30 million years from the mid-Eocene to the early Miocene. It predominantly consists of pyroclastic deposits, which were deposited in a semi-arid environment. It is divided up into a number of members. The diverse fauna of the Sarmiento Formation, including a variety of birds, crocodilians, turtles and snakes, also includes many mammals such as South American native ungulates ( notoungulates, litopterns, astrapotheres) as well as armadillo Armadillos (meaning "little armored ones" in Spanish) are New World placental mammals in the order Cingulata. The Chlamyphoridae and Dasypodidae are the only surviving families in the order, which is part of the superorder Xenarthra, al ...s, and caviomorph rodents. Material was copied from this source, which is avail ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Agua De La Piedra Formation
The Agua de la Piedra Formation (FAP, Spanish names include ''Estratos de Agua de la Piedra'' and ''Complejo Volcano-sedimentario del Terciario inferior'')Combina et al., 1994, p.418 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.Agua de la Piedra Formation in the The strictly terrestrial tuffs and paleosols of the formation, geologically belonging to |
Oligocene Mammals Of South America
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain. The name Oligocene was coined in 1854 by the German paleontologist Heinrich Ernst Beyrich from his studies of marine beds in Belgium and Germany. The name comes from the Ancient Greek (''olígos'', "few") and (''kainós'', "new"), and refers to the sparsity of extant forms of molluscs. The Oligocene is preceded by the Eocene Epoch and is followed by the Miocene Epoch. The Oligocene is the third and final epoch of the Paleogene Period. The Oligocene is often considered an important time of transition, a link between the archaic world of the tropical Eocene and the more modern ecosystems of the Miocene. Major changes during the Oligocene included a global expansion o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene Argentina
The Paleogene ( ; also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of the Cretaceous–Paleogene extinction event that ended the preceding Cr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prehistoric Placental Genera
Prehistory, also known as pre-literary history, is the period of human history between the use of the first stone tools by hominins 3.3 million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared 5000 years ago. It took thousands of years for writing systems to be widely adopted, with writing spreading to almost all cultures by the 19th century. The end of prehistory therefore came at very different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilisation, and ancient Egypt were the first civilizations to develop their own scripts and to keep historical records, with their neighbors following. Most other civilizations reached the end of prehistory during the following Iron Age. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
