|
Yarengian Supergorizont
The Yarenskian Gorizont ("Yarenskian Horizon") is a major biostratigraphic unit in Russia corresponding to Upper Olenekian-age terrestrial sediments. It lies above the Ustmylian Gorizont of the Vetlugian Supergorizont, and is located below a short unconformity overlain by the Donguz Gorizont. Some paleontologists elevate the Yarenskian to a supergorizont and subdivide it into two smaller units: the older Fedorovskian Gorizont and the younger Gamskian Gorizont. Others prefer to consider the Fedorovskian and Gamskian to be subgorizonts or members of the Yarenskian. Vertebrate index fossils of the Fedorovskian include the lungfish ''Gnathorhiza,'' the trematosaurid ''Inflectosaurus,'' and the procolophonid '' Burtensia''. In the Gamskian, these index fossils are replaced by ''Ceratodus'', ''Trematosaurus'', and ''Kapes'', respectively. The Yarenskian as a whole is characterized by the capitosaur amphibian ''Parotosuchus'', and has also been known as the ''Parotosuchus'' fauna. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Parotosuchus Orenb12DB
''Parotosuchus'' is an extinct genus of capitosaurian temnospondyl amphibians within the family (biology), family Mastodonsauridae. Fossils are known from the Early Triassic of Europe, Africa, Australia, and Antarctica. It was about long and likely lived in aquatic environments such as lakes and rivers. ''Parotosuchus'' was covered in a scaly skin, unlike the smooth skin of modern-day amphibians, and probably moved with an eel-like motion in the water. ''Parotosuchus'' was originally named ''Parotosaurus''. However, the name ''Parotosaurus'' was preoccupied by a genus of skinks, and in 1968 the name ''Parotosuchus'' was proposed as a replacement. The name ''Archotosaurus'' was also proposed as a replacement name in 1976, although the author who proposed this was unaware that ''Parotosuchus'' was already in use. Because the name ''Parotosuchus'' was erected earlier than ''Archotosaurus'', it has priority. References Further reading *Parotosuchus (Temnospondyli: Mastodonsa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trematosaurus
''Trematosaurus'' is an extinct genus of trematosaurid temnospondyl amphibian found in Germany and Russia. It was first named by Hermann Burmeister in 1849 and the type species is ''Trematosaurus brauni''. History of study ''Trematosaurus'' was one of the first temnospondyls to be described. The type locality, called Merkel's Quarry, is in east-central Germany at Bernburg an der Saale within the Bausandstein (Olenekian) and was collected for several decades from the 1840s into the early 20th century, producing extensive cranial remains, although the majority of these are preserved as internal molds (steinkerns) or natural molds. The name ''Trematosaurus'' was in fact coined in 1842 by Carl von Braun, a frequent collector who used the Greek suffix ''trema'' ('hole') in reference to the pineal foramen to form the generic epithet, but as he provided no formal description, the name was not considered valid until the work of Burmeister, who named the type species after Braun. Burm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volgograd Oblast
Volgograd Oblast (russian: Волгогра́дская о́бласть, ''Volgogradskaya oblast'') is a federal subjects of Russia, federal subject (an oblast) of Russia, located in the Volga region, Volga region of Southern Russia. Its administrative center is Volgograd. The population of the oblast was 2,610,161 in the Russian Census (2010), 2010 Census. Formerly known as Stalingrad Oblast, it was given its present name in 1961, when the city of Stalingrad was renamed Volgograd as part of de-Stalinization. Volgograd Oblast borders Rostov Oblast in the southwest, Voronezh Oblast in the northwest, Saratov Oblast in the north, Astrakhan Oblast and the Republic of Kalmykia in the southeast, and has an Kazakhstan–Russia border, international border with Kazakhstan in the east. The two main rivers in European Russia, the Don River (Russia), Don and the Volga River, Volga, run through the oblast and are connected by the Volga–Don Canal. Volgograd Oblast's strategic waterway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Don (river)
The Don ( rus, Дон, p=don) is the fifth-longest river in Europe. Flowing from Central Russia to the Sea of Azov in Southern Russia, it is one of Russia's largest rivers and played an important role for traders from the Byzantine Empire. Its basin is between the Dnieper basin to the west, the lower Volga basin immediately to the east, and the Oka basin (tributary of the Volga) to the north. Native to much of the basin were Slavic nomads. The Don rises in the town of Novomoskovsk southeast of Tula (in turn south of Moscow), and flows 1,870 kilometres to the Sea of Azov. The river's upper half ribbles (meanders subtly) south; however, its lower half consists of a great eastern curve, including Voronezh, making its final stretch, an estuary, run west south-west. The main city on the river is Rostov-on-Don. Its main tributary is the Seversky Donets, centred on the mid-eastern end of Ukraine, thus the other country in the overall basin. To the east of a series of three ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lipovskaya Formation
The Yarenskian Gorizont (geology), Gorizont ("Yarenskian Horizon") is a major biostratigraphic unit in Russia corresponding to Upper Olenekian-age terrestrial sediments. It lies above the Ustmylian Gorizont of the Vetlugian Supergorizont, and is located below a short unconformity overlain by the Donguz Gorizont. Some paleontologists elevate the Yarenskian to a supergorizont and subdivide it into two smaller units: the older Fedorovskian Gorizont and the younger Gamskian Gorizont. Others prefer to consider the Fedorovskian and Gamskian to be subgorizonts or members of the Yarenskian. Vertebrate index fossils of the Fedorovskian include the lungfish ''Gnathorhiza,'' the Trematosauridae, trematosaurid ''Inflectosaurus,'' and the procolophonid ''Burtensia''. In the Gamskian, these index fossils are replaced by ''Ceratodus'', ''Trematosaurus'', and ''Kapes (genus), Kapes'', respectively. The Yarenskian as a whole is characterized by the capitosaur amphibian ''Parotosuchus'', and has also ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orenburg Oblast
Orenburg Oblast (russian: Оренбургская область, ''Orenburgskaya oblast'') is a federal subject of Russia (an oblast). Its administrative center is the city of Orenburg. From 1938 to 1957, it bore the name ''Chkalov Oblast'' () in honor of Valery Chkalov. Population: 2,033,072 ( 2010 Census). Geography Orenburg Oblast's internal borders are with the republics of Bashkortostan and Tatarstan to the north, Chelyabinsk Oblast to the north-east, and with Samara and Saratov oblasts to the west. Orenburg Oblast also shares an international border with Kazakhstan to the east and south. The oblast is situated on the boundary between Europe and Asia. The majority of its territory lies west of the continental divide in European Russia and smaller sections in the east situated on the Asian side of the divide. The most important river of the oblast is the Ural and the largest lake Shalkar-Yega-Kara. Orenburg is traversed by the northeasterly line of equal latitude and longi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ural River
The Ural (russian: Урал, ), known before 1775 as Yaik (russian: Яик, ba, Яйыҡ, translit=Yayıq, ; kk, Жайық, translit=Jaiyq, ), is a river flowing through Russia and Kazakhstan in the continental border between Europe and Asia. It originates in the southern Ural Mountains and discharges into the Caspian Sea. At , it is the third-longest river in Europe after the Volga and the Danube, and the 18th-longest river in Asia. The Ural is conventionally considered part of the boundary between the continents of Europe and Asia. The Ural arises near Mount Kruglaya in the Ural Mountains, flows south parallel and west of the north-flowing Tobol, through Magnitogorsk, and around the southern end of the Urals, through Orsk where it turns west for about , to Orenburg, where the river Sakmara joins. From Orenburg it continues west, passing into Kazakhstan, then turning south again at Oral, and meandering through a broad flat plain until it reaches the Caspian a few miles be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Petropavlovskaya Svita
The Yarenskian Gorizont ("Yarenskian Horizon") is a major biostratigraphic unit in Russia corresponding to Upper Olenekian-age terrestrial sediments. It lies above the Ustmylian Gorizont of the Vetlugian Supergorizont, and is located below a short unconformity overlain by the Donguz Gorizont. Some paleontologists elevate the Yarenskian to a supergorizont and subdivide it into two smaller units: the older Fedorovskian Gorizont and the younger Gamskian Gorizont. Others prefer to consider the Fedorovskian and Gamskian to be subgorizonts or members of the Yarenskian. Vertebrate index fossils of the Fedorovskian include the lungfish ''Gnathorhiza,'' the trematosaurid ''Inflectosaurus,'' and the procolophonid '' Burtensia''. In the Gamskian, these index fossils are replaced by ''Ceratodus'', ''Trematosaurus'', and ''Kapes'', respectively. The Yarenskian as a whole is characterized by the capitosaur amphibian ''Parotosuchus'', and has also been known as the ''Parotosuchus'' fauna. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geological Formations
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics ( lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exposed in a geographical region (the stratigraphic column). It is the fundamental unit of lithostratigraphy, the study of strata or rock layers. A formation must be large enough that it can be mapped at the surface or traced in the subsurface. Formations are otherwise not defined by the thickness of their rock strata, which can vary widely. They are usually, but not universally, tabular in form. They may consist of a single lithology (rock type), or of alternating beds of two or more lithologies, or even a heterogeneous mixture of lithologies, so long as this distinguishes them from adjacent bodies of rock. The concept of a geologic formation goes back to the beginnings of modern scientific geology. The term was used by Abraham Gottlob Wer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rauisuchidae
Rauisuchidae is a group of large (up to or more) predatory Triassic archosaurs. There is some disagreement over which genera should be included in Rauisuchidae and which should be in the related Prestosuchidae and Poposauridae, and indeed whether these should even be thought of as separate valid families. Rauisuchids occurred throughout much of the Triassic, and may have first occurred in the Early Triassic if some archosaurian taxa such as ''Scythosuchus'' and ''Tsylmosuchus'' are considered to be within the family. An early cladistic analysis of crocodylotarsan (pseudosuchian) archosaurs included ''Lotosaurus ''Lotosaurus'' is an extinct genus of sail-backed poposauroid Poposauroidea is a clade of advanced pseudosuchians (archosaurs closer to crocodilians than to dinosaurs). It includes poposaurids, shuvosaurids, ctenosauriscids, and other unusual ...'', ''Fasolasuchus'', ''Rauisuchus'', and "the Kupferzell rauisuchid" (later called ''Batrachotomus'') within Rauisuchidae ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhytidosteidae
Rhytidosteidae is a family of Temnospondyli that lived in the Permian and Triassic. Phylogeny Below is a cladogram A cladogram (from Greek ''clados'' "branch" and ''gramma'' "character") is a diagram used in cladistics to show relations among organisms. A cladogram is not, however, an evolutionary tree because it does not show how ancestors are related to ... from Dias-da-Silva and Marsicano (2011): References *Yates, AM (2000), A new tiny rhytidosteid (Temnospondyli: Stereospondyi) from the Early Triassic of Australia and the possibility of hidden temnospondyl diversity. J. Vert Paleontol. 20:484-489. External linksRhytidosteidae at Palaeos. Stereospondyls Permian temnospondyls Triassic temnospondyls Amphibian families Lopingian first appearances Early Triassic extinctions {{Temnospondyli-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erythrosuchidae
Erythrosuchidae (meaning "red crocodiles" in Greek) are a family of large basal archosauriform carnivores that lived from the later Early Triassic (Olenekian) to the early Middle Triassic (Anisian). Naming The family Erythrosuchidae was named by David Meredith Seares Watson in 1917.D.M.S. Watson. 1917. "A sketch classification of the Pre-Jurassic tetrapod vertebrates". ''Proceedings of the Zoological Society of London'' 1917: 167–186 Description They were the apex predators of their day, with lengths of to almost . Their fossil remains are known to date from South Africa (Beaufort Group of the Karoo Basin), China, India and European Russia, from the Early to Middle Triassic. Erythrosuchids were unusually large and robust archosauromorphs. Several features set them apart from other archosauriformes and are also seen in later, more derived archosaurs. For example, they lack teeth on the palate, which are found in other early archosauriformes, such as ''Doswellia'' and eupar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
