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Pyrotherium
''Pyrotherium'' ('fire beast') is an extinct genus of South American ungulate in the order Pyrotheria, that lived in what is now Argentina and Bolivia during the Late Oligocene.''Pyrotherium'' at .org It was named ''Pyrotherium'' because the first specimens were excavated from an ancient volcanic ash deposit. Fossils of the genus have been found in the Deseado and s of Argentina and the [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyrotherium Macfaddeni Skull
''Pyrotherium'' ('fire beast') is an extinct genus of South American native ungulates, South American ungulate in the order Pyrotheria, that lived in what is now Argentina and Bolivia during the Oligocene, Late Oligocene.''Pyrotherium'' at Fossilworks.org It was named ''Pyrotherium'' because the first specimens were excavated from an ancient volcanic ash deposit. Fossils of the genus have been found in the Deseado Formation, Deseado and Sarmiento Formations of Argentina and the Salla Formation of Bolivia. So far, two valid species have been described; ''Pyrotherium romeroi'' from Argentina, and ''P. macfaddeni'' from Bolivia, at the end of Oligocene. ''P. romeroi'' in particular is the most recent known pyrothere in the fossil record and best known for its fossil remains, which although incomplete are the best pre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quebrada Fiera
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 |
Deseadan
The Deseadan () 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 The Arikareean North American Stage on the geologic timescale is the North American faunal stage according to the North American Land Mammal Ages chronology (NALMA), typically set from 30,600,000 to 20,800,000 years BP, a period of . It is usuall ... 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 th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyrotheria
Pyrotheria is an order (biology), order of extinct South American native ungulates, meridiungulate mammals. These elephant-like ungulates include the genus, genera ''Baguatherium'', ''Carolozittelia'', ''Colombitherium'', ''Griphodon'', ''Propyrotherium'', ''Proticia'', and ''Pyrotherium''. They had the appearance of large, digitigrade, tapir-like mammals with relatively short, slender limbs and five-toed feet with broad, flat phalanges. Their fossils are restricted to Paleocene through Oligocene deposits of Brazil, Peru and Argentina. Some experts place the clade Xenungulata (which contains several genera, including ''Carodnia'') within Pyrotheria, even when dentition, although bilophodont in both orders, is very different. For most scholars, the two orders remain separated. The dentition is complete with strong, procumbent, chisel-shaped incisors, strong sharp-pointed Canine tooth, canines, and low-crowned cheek teeth with bilophodont molars. The affinities of the Xenungulata ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sarmiento Formation
The Sarmiento Formation (Spanish language, 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 rock, pyroclastic deposits, which were deposited in a Semi-arid climate, 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 (notoungulata, notoungulates, litopterna, litopterns, astrapotheria, astrapotheres) as well as armadillos, and Caviomorpha, caviomorph rodents. Material was copied from this source, which is available under a creativecommons:by/3.0/, Creative Commons Attribution 3.0 International License Paleofauna Amphibians Birds Reptiles Crocodylom ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Florentino Ameghino
Florentino Ameghino (born Giovanni Battista Fiorino Giuseppe Ameghino; September 19, 1853 – August 6, 1911) was an Argentine naturalist, paleontologist, anthropologist and zoologist, whose fossil discoveries on the Argentine Pampas, especially on Patagonia, rank with those made in the western United States during the late 19th century. Along with his two brothers – Carlos and Juan – Florentino Ameghino was one of the most important founding figures in South American paleontology. From 1887 until his death, Ameghino was passionately devoted to the study of fossil mammals from Patagonia, with the valuable support of his brother Carlos Ameghino (1865–1936) who, between 1887 and 1902, made 14 trips to that region, where he discovered and collected numerous fossil faunas and made important stratigraphic observations. Biography Ameghino was born on September 19, 1853, in Tessi, an hamlet of Moneglia, a municipality of Liguria in Italy, in what was then the Kingdom of Sardi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South American Native Ungulates
South American native ungulates, commonly abbreviated as SANUs, are extinct ungulate-like mammals that were indigenous to South America from the Paleocene (from at least 63 million years ago) until the end of the Late Pleistocene (~12,000 years ago). They represented a dominant element of South America's Cenozoic terrestrial mammal fauna prior to the arrival of living ungulate groups in South America during the Pliocene and Pleistocene as part of the Great American Interchange. They comprise five major groups conventionally ranked as orders— Astrapotheria, Litopterna, Notoungulata, Pyrotheria, and Xenungulata—as well as the primitive " condylarth" groups Didolodontidae and Kollpaniinae. It has been proposed that some or all of the members of this group form a clade, named Meridiungulata, though the relationships of South American ungulates remain largely unresolved. The two largest groups of South American ungulates, the notoungulates and the litopterns, were the only grou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frederic Brewster Loomis
Frederic Brewster Loomis (November 22, 1873 – July 28, 1937) was an American paleontologist. Educated at Amherst College and the Ludwig Maximilian University of Munich, he spent his entire professional career at Amherst. His specialty was vertebrate paleontology. Many fossils he uncovered during his extensive field work are still exhibited at Amherst's Beneski Museum of Natural History. He was a fellow of the American Academy of Arts and Sciences, a fellow of the Geological Society of America, and president of the Paleontological Society. Early life and education Loomis was born November 22, 1873, in Brooklyn, New York, to Julie R. Loomis (''née'' Brewster) and Nathaniel H. Loomis, a businessman who ran produce warehouses in New York City. Walter Granger. Memorial to Frederick Brewster Loomis. ''Proceedings of the Geological Society of America for 1937'', Jun. 1938, pp. 173–82. In March 1877 his father died of rabies contracted from a dog bite. The family later moved to Ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oligocene
The Oligocene ( ) is a geologic epoch (geology), epoch of the Paleogene Geologic time scale, Period that 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 Ancient Greek (''olígos'') 'few' and (''kainós'') 'new', and refers to the sparsity of Neontology, extant forms of Mollusca, 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 chang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guide Fossil
Biostratigraphy is the branch of stratigraphy which focuses on correlating and assigning relative ages of rock strata by using the fossil assemblages contained within them.Hine, Robert. "Biostratigraphy." ''Oxford Reference: Dictionary of Biology'', 8th ed., Oxford University Press, 2019. The primary objective of biostratigraphy is ''correlation'', demonstrating that a particular horizon in one geological section represents the same period of time as another horizon at a different section. Fossils within these strata are useful because sediments of the same age can look completely different, due to local variations in the sedimentary environment. For example, one section might have been made up of clays and marls, while another has more chalky limestones. However, if the fossil species recorded are similar, the two sediments are likely to have been laid down around the same time. Ideally these fossils are used to help identify biozones, as they make up the basic biostratigraphy uni ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amherst College
Amherst College ( ) is a Private college, private Liberal arts colleges in the United States, liberal arts college in Amherst, Massachusetts, United States. Founded in 1821 as an attempt to relocate Williams College by its then-president Zephaniah Swift Moore, Amherst is the third oldest institution of higher education in List of colleges and universities in Massachusetts, Massachusetts. The institution was named after the town, which in turn had been named after Jeffery Amherst, 1st Baron Amherst, Jeffery, Lord Amherst, Commander-in-Chief of British forces of North America during the French and Indian War. Originally established as a Men's colleges, men's college, Amherst became Mixed-sex education, coeducational in 1975. Amherst is an exclusively undergraduate four-year institution; 1,971 students were enrolled in fall 2021. Admissions are highly selective. Students choose courses from 42 major programs in an Curriculum#Open curriculum, open curriculum and are not required to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
La Paz Department (Bolivia)
The La Paz Department of Bolivia comprises with a 2024 census population of 3,022,566 inhabitants. It is situated at the western border of Bolivia, sharing Lake Titicaca with the neighboring Peru. It contains the Cordillera Real mountain range, which reaches altitudes of . Northeast of the Cordillera Real are the '' Yungas'', the steep eastern slopes of the Andes Mountains that make the transition to the Amazon River basin to the northeast. The capital of the department is the city of La Paz and is the administrative city and seat of government/national capital of Bolivia. Provinces The Department of La Paz is divided into 20 provinces (''provincias'') which are further subdivided into 85 municipalities (''municipios'') and - on the fourth level - into cantons. The provinces with their capitals are: Government The chief executive office of Bolivia's departments (since May 2010) is the Governor; before then, the office was called the Prefect, and until 2006 the prefec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
