|
Schilfsandstein
The Stuttgart Formation is a Formation (geology), geologic formation in Germany. It preserves fossils dating back to the Carnian stage of the Triassic Period (geology), period.Stuttgart Formation at Fossilworks.org Fossil content Temnospondyls * ''Cyclotosaurus, Cyclotosaurus buechneri''Witzmann et al., 2016 * ''Cyclotosaurus, C. robustus''Schoch & Milner, 2000 * ''Hyperokynodon, Hyperokynodon keuperinus'' * ''Mastodonsaurus, Mastodonsaurus andriani''Münster, 1839 * ''Metoposaurus, Metoposaurus diagnosticus''Sulej, 2002 * ''Gerrothorax, Gerrothorax sp.''[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metoposaurus
''Metoposaurus'' meaning "front lizard" is an extinct genus of stereospondyl temnospondyl amphibian, known from the Late Triassic of Germany, Italy, Poland, and Portugal. https://www.app.pan.pl/archive/published/app47/app47-535.pdf This mostly aquatic animal possessed small, weak limbs, sharp teeth, and a large, flat head. This highly flattened creature mainly fed on fish, which it captured with its wide jaws lined with needle-like teeth. ''Metoposaurus'' was up to 3 m (10 feet) long and weighed about 450 kg (1,000 pounds). Many ''Metoposaurus'' mass graves have been found, probably from creatures that grouped together in drying pools during drought. Discovery and species Discovery The earliest mention of Metoposauridae dates back to 1842 when Von Meyer described the dorsal view of the skull roof of a labyrinthodont from the Keuper Schilfsandstein of Feuerbacher Haide near Stuttgart. Later, Meyer attempted a reconstruction of the same specimen and named it ''Metopias ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hyperokynodon
''Hyperokynodon'' is an extinct genus of trematosaurian temnospondyl within the family Trematosauridae. Fossils have been found in Germany. While most trematosaurids existed during the Early Triassic, ''Hyperokynodon'' has been found in Late Triassic deposits, making it the youngest known trematosaurid. ''Hyperokynodon'' was known since 1852, but it was not identified as a trematosaurid until 1987. The type and only species is ''H. keuperinus''. Description ''Hyperokynodon'' is known only from two specimens: a holotype snout and a cast of the underside of the skull roof. The holotype was found in Heilbronn, Germany, in the mid-1800s. It likely came from deposits in the Wartberg, a mountain that had several active quarries at the time. The cast, known as SMNS 55910, was found in a sandstone quarry east of the city of Heilbronn. SMNS 55910 is an impression of the underside of the skull table and includes parts of the palate and the edge of the orbit. Based on the cast, the total ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cyclotosaurus
''Cyclotosaurus'' is an extinct genus of temnospondyl within the family Mastodonsauridae. It was of great size for an amphibian, had an elongated skull up to . Etymology The name means "round eared lizard" in Ancient Greek, derived from round openings or fenestrae in the cheeks, which are thought to contain structures of the middle ear. History German naturalist Eberhard Fraas erected the genus ''Cyclotosaurus'' in 1889, with ''C. robustus'' (previously ''Mastodonsaurus robustus'') as the type species. Several species are known, mainly from Germany and Poland in Central Europe, as well as East Greenland and Thailand. The relationships between species is unclear. ''"Labyrinthodon" pachygnathus'' Owen, 1842 and ''"L." leptognathus'' Owen, 1842 were transferred to ''Cyclotosaurus'', as ''C. pachygnathus'' and ''C. leptognathus'', by Paton (1974). However, Damiani (2001) assigned the two species to Mastodonsauroidea indeterminate and Stereospondyli indeterminate. Palaeontology ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Formation (stratigraphy)
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 (geology), 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeobates
''Palaeobates'' is an extinct genus of prehistoric elasmobranch sharks in the order Hybodontiformes. It lived during the Triassic period. It was a small shark about long. ''Palaeobates'' had a grinding-type dentition, which it used to crush hard-shelled prey. The teeth exhibit an orthodont histology. See also * List of prehistoric cartilaginous fish This list of prehistoric cartilaginous fish genera is an attempt to create a comprehensive listing of all genera that have ever been included in the class chondrichthyes ''and'' are known from the fossil record. This list excludes purely vernacula ... References Hybodontiformes Prehistoric shark genera {{Triassic-fish-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lissodus
''Lissodus'' is an extinct genus of freshwater shark. It lived from the Early Carboniferous stage to the Albian age of the Cretaceous. It was about long and had flat teeth that it used for eating clams Clam is a common name for several kinds of bivalve molluscs. The word is often applied only to those that are edible and live as infauna, spending most of their lives halfway buried in the sand of the seafloor or riverbeds. Clams have two .... References Prehistoric shark genera Mesozoic fish of Asia Jurassic sharks Mesozoic fish of Europe Hasle Formation {{Triassic-fish-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zanclodon
''Zanclodon'' ("scythe tooth") is an extinct genus of archosauriform found in Middle Triassic deposits in southern Germany. Taxonomy ''Zanclodon'' was originally named ''Smilodon'' by Plieninger (1846), but this name had previously been used for the saber-toothed cat (a preoccupied name), prompting Plieninger to erect the replacement name ''Zanclodon''. It was formerly placed in the Teratosauridae, within the Theropoda, and at times, plateosaurid material was mistakenly referred to ''Zanclodon'' (see Galton 2001). The type species, ''Zanclodon laevis'', is based on a left maxilla that represents an indeterminate archosaurian. Therefore, the genus is not unambiguously identifiable.Galton, P.M. (2001). The prosauropod dinosaur ''Plateosaurus'' Meyer, 1837 (Saurischia: Sauropodomorpha; Upper Triassic). II. Notes on the referred species. ''Revue de Paléobiologie'', Genève 20(2): 435–502. Species * ''Z. laevis'' (Plieninger, 1846) riginally "Smilodon"( type) * ''Z. crenat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kannemeyeriiformes
Kannemeyeriiformes is a group of large-bodied Triassic dicynodonts. As a clade, Kannemeyeriiformes has been defined to include the species ''Kannemeyeria simocephalus'' and all dicynodonts more closely related to it than to the species '' Lystrosaurus murrayi''. Evolutionary history Despite being the most species-rich group of dicynodonts in the Triassic Period, kannemeyeriiforms exhibit much less diversity in terms of their anatomy and ecological roles than the dicynodonts from the Permian Period. Lystrosauridae is thought to be the most closely related group (sister taxon) to Kannemeyeriiformes, and since the earliest lystrosaurids are known from the Late Permian, the divergence of these two groups must have occurred at least as far back as this time, implying that a long ghost lineage must exist. Although no kannemeyeriiforms have been found in the Late Permian yet, the recent discovery of ''Sungeodon'' helps fill a gap in the early fossil record of the group by showing that k ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gerrothorax
''Gerrothorax'' ("wicker chest") is an extinct genus of temnospondyl amphibian from the Triassic period of Greenland, Germany, Poland, Sweden, and possibly Thailand. It is known from a single species, ''G. pulcherrimus'', although several other species such as ''G. pustuloglomeratus'' have been named in the past. ''Gerrothorax'' was about long, and had a remarkably flattened body. It probably hid under sand or mud on river and lake bottoms, scanning for prey with its large, upward-facing eyes. ''Gerrothorax'' had an unusually shaped skull with angular protrusions on the sides. This looked vaguely similar to the skull of the earlier, unrelated, amphibian ''Diplocaulus'', but was not so developed. Some ''Gerrothorax'' fossils preserved hypobranchials anceratobranchials(bony gill arches) near the neck. This shows that ''Gerrothorax'' was pedomorphic, retaining its larval gills as an adult. When originally described in 1946, these bones were considered to correspond to feather-lik ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
