Sclerocalyptus
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Sclerocalyptus
''Neosclerocalyptus'' was an extinct genus of glyptodont that lived during the Pliocene, Pleistocene, and Holocene of Southern South America, mostly Argentina. It was small compared to many Glyptodonts at only around 2 meters long and 360 kilograms. Etymology The genus name ''Neosclerocalyptus'' is a modification of the name of its synonym, ''Sclerocalyptus'', and derived from the Greek roots ''neo-'' meaning "young" or "new", ''scleros'' meaning "hard", and -''calyptos'' meaning "covering", referring to the armored carapace of the animal. The type species, ''N. ornatus'', specific name meaning is "adorned" after the patterns on the holotype osteoderms. History and taxonomy Fossils of ''Neosclerocalyptus'' were first collected by a "Sir Woodbine Parish, KH" from the Pleistocene strata near the Matanzas River in Buenos Aires Province, Argentina, but where later sent to the Royal College of Surgeons in the UK, where they were later described by paleontologist Sir Richard Owen ...
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Sclerocalyptus
''Neosclerocalyptus'' was an extinct genus of glyptodont that lived during the Pliocene, Pleistocene, and Holocene of Southern South America, mostly Argentina. It was small compared to many Glyptodonts at only around 2 meters long and 360 kilograms. Etymology The genus name ''Neosclerocalyptus'' is a modification of the name of its synonym, ''Sclerocalyptus'', and derived from the Greek roots ''neo-'' meaning "young" or "new", ''scleros'' meaning "hard", and -''calyptos'' meaning "covering", referring to the armored carapace of the animal. The type species, ''N. ornatus'', specific name meaning is "adorned" after the patterns on the holotype osteoderms. History and taxonomy Fossils of ''Neosclerocalyptus'' were first collected by a "Sir Woodbine Parish, KH" from the Pleistocene strata near the Matanzas River in Buenos Aires Province, Argentina, but where later sent to the Royal College of Surgeons in the UK, where they were later described by paleontologist Sir Richard Owen ...
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Sclerocalyptus Ornatus Fragment Carapace
''Neosclerocalyptus'' was an extinct genus of glyptodont that lived during the Pliocene, Pleistocene, and Holocene of Southern South America, mostly Argentina. It was small compared to many Glyptodonts at only around 2 meters long and 360 kilograms. Etymology The genus name ''Neosclerocalyptus'' is a modification of the name of its synonym, ''Sclerocalyptus'', and derived from the Greek roots ''neo-'' meaning "young" or "new", ''scleros'' meaning "hard", and -''calyptos'' meaning "covering", referring to the armored carapace of the animal. The type species, ''N. ornatus'', specific name meaning is "adorned" after the patterns on the holotype osteoderms. History and taxonomy Fossils of ''Neosclerocalyptus'' were first collected by a "Sir Woodbine Parish, KH" from the Pleistocene strata near the Matanzas River in Buenos Aires Province, Argentina, but where later sent to the Royal College of Surgeons in the UK, where they were later described by paleontologist Sir Richard Owen ...
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Eosclerocalyptus
''Eosclerocalyptus'' is an extinct genus of glyptodont. It lived during the Late Miocene, and its fossilized remains were discovered in South America. Description This animal, like all glyptodonts, was protected by a carapace covering most of its body. It was very similar to ''Sclerocalyptus'', from which it was only differentiated by its smaller size and some anatomical details, notably on its carapace. The central figures of the osteoderms were depressed, while the caudal tube protecting the tail had fewer lateral figures than those of ''Sclerocalyptus'' (only three pairs), and those were less differentiated. The cephalic shield had a particular ornementation. The skull was tall and narrow, especially in the posterior region, and the choanae were tall and narrow. The teeth were thinner than those of ''Sclerocalyptus'', and only the rearmost ones were trilobed. Classification The genus ''Eosclerocalyptus'' was first described in 1919 by Carlos Ameghino, based on fossils found ...
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Hoplophorus
''Hoplophorus'' is an extinct genus of glyptodont, a subfamily of armadillos . The only confidently known species was ''H. euphractus'', found in Pleistocene deposits in Brazil, though fossils possibly from another species are known from Bolivia. History and taxonomy ''Hoplophorus euphractus'' was first described in 1837 by Danish paleontologist Peter Wilhelm Lund on the basis of fossilized osteoderms and carapace fragments unearthed in the Upper Pleistocene cave deposits in Lagoa Santa, Minas Gérais, Brazil.Lund, P. W. (1837). ''Blik paa Brasiliens dyreverden foÈr sidste jordomvaeltning''. Popp. This was one of the first glyptodonts to be described. Lund attributed many other fossils to the species over several years, including limb bones, teeth, vertebrae, foot remains, and an incomplete skull. Lund later erected 3 more ''Hoplophorus'' species based on the fossils from Lago Santa: ''H. selloi, H. minor,'' & ''H. meyeri.'' All three didn’t receive proper descriptions, ma ...
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Glyptotherium
''Glyptotherium'' (from Greek for 'grooved or carved beast') is a genus of glyptodont (an extinct group of large, herbivorous armadillos) that lived from the Early Pliocene, about 4.9 million years ago, to the Early Holocene, around 7,000 years ago, in the United States, Mexico, Guatemala, Costa Rica, Honduras, El Salvador, Panama, Venezuela, and Brazil. The genus was first described in 1903 by American paleontologist Henry Fairfield Osborn with the type species being, ''G. texanum,'' based on fossils that had been found in the Pliocene Blancan Beds in Llano Estacado, Texas, USA. The genus has since been discovered in many more fossil sites. Another species, ''G. cylindricum'', was named in 1912 by fossil hunter Barnum Brown on the basis of a partial carapace, teeth, and several additional fossils that had been unearthed from the Pleistocene deposits in Jalisco, Mexico. Glyptodonts were typically large, graviportal, herbivorous armadillos with armored carapaces that were made ...
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Glyptodont
Glyptodonts are an extinct subfamily of large, heavily armoured armadillos. They arose in South America around 48 million years ago and spread to southern North America after the continents became connected several million years ago. The best-known genus within the group is ''Glyptodon''. While they were formerly considered to constitute the distinct family Glyptodontidae, in 2016, an analysis of ''Doedicurus'' Mitochondrial DNA (also known as mtDNA / mDNA) found that it was, in fact, nested within the modern armadillos as the sister group of a clade consisting of Chlamyphorinae and Tolypeutinae. For this reason, glyptodonts and all armadillos but '' Dasypus'' were relocated to a new family, Chlamyphoridae, and glyptodonts were demoted from the former family Glyptodontidae to a subfamily. Evolution Glyptodonts first evolved during the Eocene in South America, which remained their center of species diversity. For example, an Early Miocene glyptodont with many primitive feature ...
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Glyptodon
''Glyptodon'' (from Greek for 'grooved or carved tooth': γλυπτός 'sculptured' and ὀδοντ-, ὀδούς 'tooth') is a genus of glyptodont (an extinct group of large, herbivorous armadillos) that lived from the Pleistocene, around 2.5 million years ago, to the Early Holocene, around 11,000 years ago, in Argentina, Uruguay, Paraguay, Bolivia, Peru, Brazil, and Colombia. It was the first named extinct cingulate and is the type genus of Glyptodontinae, and, or, Glyptodontinae. Many species have been named for the genus, though few are considered valid, and it is one of, if not the, best known genus of glyptodont. Hundreds of specimens have been referred to the genus, but the holotype, or name specimen, of the type species, ''G. clavipes'', was described in 1839 by notable British paleontologist Sir Richard Owen. It was roughly the same size and weight as a Volkswagen Beetle, 800–840 kg (1,760–1,850 lb). With its rounded, bony shell and squat limbs, it superfic ...
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Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ...
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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 which helped to support his journal Ameghiniana. Biography Ameghino was born on September 19, 1853 in Tessi, an hamlet of Moneglia, a municipality of Liguria in Ita ...
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Plohophorus
''Plohophorus'' is an extinct genus of Glyptodont. it lived from the Late Miocene to the Late Pliocene, and its fossilized remains were discovered in South America. Description Like all glyptodonts, this animal had a large carapace formed by numerous osteoderms fused together, covering most of its body. ''Plohophorus'' shared similarities with another Miocene glyptodont, ''Phlyctaenopyga'', especially in its rather broad and low skull. The ornamentation of the caudal tube, protecting the tail, was more simplified ; the peripheral figures were partially regressed and marked in the distal part ; the central oval-shaped figures were contiguous to each other and only left space for small triangular areas between each other. Classification The genus ''Plohophorus'' was first described in 1887 by Florentino Ameghino, based on fossil remains found in Upper Miocene terrains of Argentina. The type species is ''Plohophorus figuratus'' ; several other species from the Late Miocene and th ...
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Boreostemma
''Boreostemma'' is an extinct genus of glyptodonts from northern South America. Fossils assigned to the genus were first described as belonging to '' Asterostemma'' from southern South America, but have been placed in the new genus ''Boreostemma'' by Carlini et al. in 2008. The type species is ''B. pliocena''. Fossils of ''Boreostemma'' have been found in the Honda Group of Colombia, in Peru and Venezuela. Etymology The genus name ''Boreostemma'' is a combination of ''stemma'', taken from '' Asterostemma'', and ''boreo'' is derived from borealis, meaning "northern", to distinguish the northern South American genus from the southern ''Asterostemma''. Species Four species have been described in the genus ''Boreostemma''.''Boreostemma''
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Palaehoplophorus
''Palaehoplophorus'' (also spelled, historically, ''Palaeohoplophorus'') is an extinct genus of glyptodont. It lived from the Middle to the Late Miocene, and its fossilized remains were discovered in South America. Description This animal, like all glyptodonts, had a thick carapace, composed of numerous osteoderm fused together, covering a large part of its body. The plates of its carapace bore a medium-sized, depressed central figure, surrounded by a wrinkled peripheral zone, divided by barely defined furrows and irregular tubercles. Large perforations opened in the furrows around the central figure and between the peripheral figures. The tail was protected by a series of mobile osteoderm rings, presenting a similar ornamentation, and by a terminal straight and cylindrical "tube", formed by contiguous, rounded osteoderms, separated by deep grooves with large perforations, similar to those of the carapace. The terminal and lateral osteoderms were almost identical to each other. ...
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