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Fagesia
''Fagesia'' is a small, subglobular ammonite (suborder Ammonitina) belonging to the vascoceratid family of the Acanthocerataceae that lived during the Turonian stage of the Late Cretaceous, 92-88 Ma ago. The shell of ''Fagesia'' is about 9.5 cm (3.47 in) in diameter, typically with blunt umbilical tubercles from which spring 2 or three ribs each, but which are lost in the late growth stage. The suture is ammonitic with long spikey lobes and saddles with rounded subelements. Species * †''Fagesia catinus'' Mantell 1822 - Loma Gorda Formation, Colombia * †''Fagesia fleuryi'' Pervinquière 1907 * †''Fagesia peroni'' Pervinquière 1907 * †''Fagesia pervinquieri'' Bose 1920 * †''Fagesia rudra'' Stoliczka 1865 * †''Fagesia spheroidalis'' Pervinquière 1907 * †''Fagesia superstes'' Kossmat 1897 * †''Fagesia tevesthensis'' Peron 1896 Distribution Fossils of ''Fagesia'' have been found in Brazil, Colombia (El Colegio, Cundinamarca, La Frontera ( Cund ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fagesia Catinus
''Fagesia'' is a small, subglobular ammonite (suborder Ammonitina) belonging to the vascoceratid family of the Acanthocerataceae that lived during the Turonian stage of the Late Cretaceous, 92-88 Ma ago. The shell of ''Fagesia'' is about 9.5 cm (3.47 in) in diameter, typically with blunt umbilical tubercles from which spring 2 or three ribs each, but which are lost in the late growth stage. The suture is ammonitic with long spikey lobes and saddles with rounded subelements. Species * †''Fagesia catinus'' Mantell 1822 - Loma Gorda Formation, Colombia * †''Fagesia fleuryi'' Pervinquière 1907 * †''Fagesia peroni'' Pervinquière 1907 * †''Fagesia pervinquieri'' Bose 1920 * †''Fagesia rudra'' Stoliczka 1865 * †''Fagesia spheroidalis'' Pervinquière 1907 * †''Fagesia superstes'' Kossmat 1897 * †''Fagesia tevesthensis'' Peron 1896 Distribution Fossils of ''Fagesia'' have been found in Brazil, Colombia (El Colegio, Cundinamarca, La Frontera ( Cun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fagesia Spheroidalis
''Fagesia'' is a small, subglobular ammonite (suborder Ammonitina) belonging to the vascoceratid family of the Acanthocerataceae that lived during the Turonian stage of the Late Cretaceous, 92-88 Ma ago. The shell of ''Fagesia'' is about 9.5 cm (3.47 in) in diameter, typically with blunt umbilical tubercles from which spring 2 or three ribs each, but which are lost in the late growth stage. The suture is ammonitic with long spikey lobes and saddles with rounded subelements. Species * †''Fagesia catinus'' Mantell 1822 - Loma Gorda Formation, Colombia * †''Fagesia fleuryi'' Pervinquière 1907 * †''Fagesia peroni'' Pervinquière 1907 * †''Fagesia pervinquieri'' Bose 1920 * †''Fagesia rudra'' Stoliczka 1865 * †''Fagesia spheroidalis'' Pervinquière 1907 * †''Fagesia superstes'' Kossmat 1897 * †''Fagesia tevesthensis'' Peron 1896 Distribution Fossils of ''Fagesia'' have been found in Brazil, Colombia (El Colegio, Cundinamarca, La Frontera ( Cun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fagesia Peroni
''Fagesia'' is a small, subglobular ammonite (suborder Ammonitina) belonging to the vascoceratid family of the Acanthocerataceae that lived during the Turonian stage of the Late Cretaceous, 92-88 Ma ago. The shell of ''Fagesia'' is about 9.5 cm (3.47 in) in diameter, typically with blunt umbilical tubercles from which spring 2 or three ribs each, but which are lost in the late growth stage. The suture is ammonitic with long spikey lobes and saddles with rounded subelements. Species * †''Fagesia catinus'' Mantell 1822 - Loma Gorda Formation, Colombia * †''Fagesia fleuryi'' Pervinquière 1907 * †''Fagesia peroni'' Pervinquière 1907 * †''Fagesia pervinquieri'' Bose 1920 * †''Fagesia rudra'' Stoliczka 1865 * †''Fagesia spheroidalis'' Pervinquière 1907 * †''Fagesia superstes'' Kossmat 1897 * †''Fagesia tevesthensis'' Peron 1896 Distribution Fossils of ''Fagesia'' have been found in Brazil, Colombia (El Colegio, Cundinamarca, La Frontera ( Cun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fagesia Pervinquieri
''Fagesia'' is a small, subglobular ammonite (suborder Ammonitina) belonging to the vascoceratid family of the Acanthocerataceae that lived during the Turonian stage of the Late Cretaceous, 92-88 Ma ago. The shell of ''Fagesia'' is about 9.5 cm (3.47 in) in diameter, typically with blunt umbilical tubercles from which spring 2 or three ribs each, but which are lost in the late growth stage. The suture is ammonitic with long spikey lobes and saddles with rounded subelements. Species * †''Fagesia catinus'' Mantell 1822 - Loma Gorda Formation, Colombia * †''Fagesia fleuryi'' Pervinquière 1907 * †''Fagesia peroni'' Pervinquière 1907 * †''Fagesia pervinquieri'' Bose 1920 * †''Fagesia rudra'' Stoliczka 1865 * †''Fagesia spheroidalis'' Pervinquière 1907 * †''Fagesia superstes'' Kossmat 1897 * †''Fagesia tevesthensis'' Peron 1896 Distribution Fossils of ''Fagesia'' have been found in Brazil, Colombia (El Colegio, Cundinamarca, La Frontera ( Cun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fagesia Tevesthensis
''Fagesia'' is a small, subglobular ammonite (suborder Ammonitina) belonging to the vascoceratid family of the Acanthocerataceae that lived during the Turonian stage of the Late Cretaceous, 92-88 Ma ago. The shell of ''Fagesia'' is about 9.5 cm (3.47 in) in diameter, typically with blunt umbilical tubercles from which spring 2 or three ribs each, but which are lost in the late growth stage. The suture is ammonitic with long spikey lobes and saddles with rounded subelements. Species * †''Fagesia catinus'' Mantell 1822 - Loma Gorda Formation, Colombia * †''Fagesia fleuryi'' Pervinquière 1907 * †''Fagesia peroni'' Pervinquière 1907 * †''Fagesia pervinquieri'' Bose 1920 * †''Fagesia rudra'' Stoliczka 1865 * †''Fagesia spheroidalis'' Pervinquière 1907 * †''Fagesia superstes'' Kossmat 1897 * †''Fagesia tevesthensis'' Peron 1896 Distribution Fossils of ''Fagesia'' have been found in Brazil, Colombia (El Colegio, Cundinamarca, La Frontera ( Cun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fagesia Fleuryi
''Fagesia'' is a small, subglobular ammonite (suborder Ammonitina) belonging to the vascoceratid family of the Acanthocerataceae that lived during the Turonian stage of the Late Cretaceous, 92-88 Ma ago. The shell of ''Fagesia'' is about 9.5 cm (3.47 in) in diameter, typically with blunt umbilical tubercles from which spring 2 or three ribs each, but which are lost in the late growth stage. The suture is ammonitic with long spikey lobes and saddles with rounded subelements. Species * †''Fagesia catinus'' Mantell 1822 - Loma Gorda Formation, Colombia * †''Fagesia fleuryi'' Pervinquière 1907 * †''Fagesia peroni'' Pervinquière 1907 * †''Fagesia pervinquieri'' Bose 1920 * †''Fagesia rudra'' Stoliczka 1865 * †''Fagesia spheroidalis'' Pervinquière 1907 * †''Fagesia superstes'' Kossmat 1897 * †''Fagesia tevesthensis'' Peron 1896 Distribution Fossils of ''Fagesia'' have been found in Brazil, Colombia (El Colegio, Cundinamarca, La Frontera ( Cun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fagesia Rudra
''Fagesia rudra'' is a small, subglobular ammonite (suborder Ammonitina) belonging to the vascoceratid family. This species lived during the Turonian The Turonian is, in the ICS' geologic timescale, the second age in the Late Cretaceous Epoch, or a stage in the Upper Cretaceous Series. It spans the time between 93.9 ± 0.8 Ma and 89.8 ± 1 Ma (million years ago). The Turonian is preceded by t ... stage of the late Cretaceous, 92-88 Ma ago. References *W.J. Kennedy, C.W. WrighVascoceratid ammonites from the type turonian Global Names [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fagesia Superstes
''Fagesia superstes'' is a small, subglobular ammonite (suborder Ammonitina) belonging to the vascoceratid family. This species lived during the Turonian The Turonian is, in the ICS' geologic timescale, the second age in the Late Cretaceous Epoch, or a stage in the Upper Cretaceous Series. It spans the time between 93.9 ± 0.8 Ma and 89.8 ± 1 Ma (million years ago). The Turonian is preceded by t ... stage of the late Cretaceous, 92-88 Ma ago. ReferencesPaleobiology Database Acanthoceratoidea {{ammonitina-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
La Frontera Formation
The La Frontera Formation ( es, Formación La Frontera, K2F, Ksf) is a geological formation, part of the Villeta Group, of the Altiplano Cundiboyacense and neighbouring areas of the Eastern Ranges of the Colombian Andes. The sequence of limestones and lydites dates to the Late Cretaceous period; Turonian epoch and has a maximum thickness of . Fossils of '' Yaguarasaurus columbianus'' were said to be found in this formation (listed as "La Frontera Member"), although the geological mapping of the area state the time-equivalent Hondita Formation as the stratigraphic unit present in the Quebradas El Ocal and Itaibe in Huila. The La Frontera Formation does not outcrop south of Cundinamarca. A high diversity of ammonites has been found in the La Frontera Formation. Etymology The formation was first described by Hubach in 1931 and elevated to formation in 1969 by Cáceres and Etayo.Montoya & Reyes, 2005, p.24 The formation is named after the quarry La Frontera near Albán, Cundinama ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loma Gorda Formation
The Loma Gorda Formation ( es, Formación Loma Gorda, Kl, Kslg) is a fossiliferous geological formation of the Upper Magdalena Valley (VSM) and surrounding Central and Eastern Ranges of the Colombian Andes, extending from Cundinamarca in the north to Huila and easternmost Tolima in the south. The uppermost unit of the Güagüaquí Group, a sequence of laminated siltstones and shales, dates to the Late Cretaceous period; Turonian to Coniacian epochs, and has a maximum thickness of . Etymology The formation was named in 1966 by De Porta, named Loma Gorda ("Fat Hill") in Ricaurte, Cundinamarca.Acosta & Ulloa, 2002, p.23 Description Lithologies The Loma Gorda Formation is characterised by laminated siltstones and shales with calcareous concretions.Acosta & Ulloa, 2002, p.24 The formation has provided fossils of '' Ankinatsytes venezolanus'', '' Barroisiceras onilahyense'', '' Codazziceras ospinae'', '' Eulophoceras jacobi'', ''Fagesia catinus'', '' Hauericeras madagascaren ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vascoceratidae
The Vascoceratidae is a family of Upper Cretaceous ammonites in the superfamily Acanthoceratoidea characterized by shells that are either smooth or bluntly tuberculate, or have sparse, coarse ribs. Sutural elements are shallow, irregular, and slightly indented, or deep and very indented. Whorl section and degree of involution vary, even within species. The Vascoceratidae is a short lived family restricted to the early and middle Turonian stage. Its duration, no more than a few million years. They are derived from the Acanthoceratidae and are the predecessors of the Tissotiidae Tissotiidae is a family of ammonites (Ammonitina) belonging to the Acanthoceratoidea. The Tissotiidae are derived from the Vascoceratidae, another acanthoceratoid family, and gave rise to the Coilopoceratidae. They have been divided into two su ..., which in turn gave rise to the Coilopoceratidae; all taking place in a short time span in the Turonian. Ammonitida families Acanthoceratoidea Turoni ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aipe
Aipe is a town and municipality in the Huila Department, Colombia. It is located on the west bank of the Magdalena River in the Central Ranges of the Colombian Andes at altitudes between . Aipe borders Natagaima, Ataco and Planadas of the department of Tolima in the north and west, Villavieja and Tello in the east, and the departmental capital Neiva in the south. History In early 1741, Doña Teresa and Don Enríque Cortés, descendants of Mr. Jacinto Cortés, gave 80 hectares to establish a new town, and are considered the founders of the Aipe. In 1770, the church hierarchy and government in Neiva records the construction of the church of Our Lady of Sorrows. In 1874, Aipe acquired autonomy from Neiva, as a member of the canton district of Villavieja and on 8 April 1912 by Ordinance No. 26, was created as a municipality by the Departmental Assembly. Geography The municipality of Aipe is located on the left bank of the Magdalena River. It is located in the northwest of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |