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Saurosphargid
Saurosphargidae is an extinct family of marine reptiles known from the early Middle Triassic (Anisian stage) of Europe and China. The type species of the family is '' Saurosphargis volzi'', named by Friedrich von Huene in 1936 based on a single specimen collected from the lower Anisian Lower Muschelkalk of Gogolin, Poland - a section of 12 incomplete back vertebrae with ribs. The generic name of ''Saurosphargis'' is derived from Greek ''sauros'', "lizard", and ''sphargis'', the old genus name for the leatherback turtle, in reference to the dorsal osteoderm "body armor" and broadened ribs forming a closed chest rib basket, traits that are seemingly transitional between turtles and other reptiles. However, due to the only known specimen' destruction during World War II, many authors considered ''Saurosphargis'' to be a ''nomen dubium''. Nevertheless, even based on surviving descriptions alone, many differences were noted even from its closest known relative at the time, '' Eusaur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sinosaurosphargis
''Sinosaurosphargis'' is an extinct genus of basal marine saurosphargid reptile known from the Middle Triassic (Anisian age) Guanling Formation of Yunnan and Guizhou Provinces, southwestern China. It contains a single species, ''Sinosaurosphargis yunguiensis''. Discovery ''Saurosphargis'' is known from several individuals, all of which were collected from Member II of the Guanling Formation, dating to the Pelsonian substage of the latest Anisian stage of the early Middle Triassic, about 243 million years ago. The holotype IVPP V 17040 and paratype IVPP V 16076 are housed at the Institute of Vertebrate Paleontology and Paleoanthropology in Beijing, and represent a nearly complete articulated skeleton and skull, and a partial disarticulated postcranial skeleton including dorsal vertebra, ribs, with osteoderms and gastral rib fragments, respectively. ZMNH M 8797, an incomplete postcranial skeleton showing a very well preserved right forelimb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sinosaurosphargis Yunguiensis
''Sinosaurosphargis'' is an extinct genus of basal marine saurosphargid reptile known from the Middle Triassic (Anisian age) Guanling Formation of Yunnan and Guizhou Provinces, southwestern China. It contains a single species, ''Sinosaurosphargis yunguiensis''. Discovery ''Saurosphargis'' is known from several individuals, all of which were collected from Member II of the Guanling Formation, dating to the Pelsonian substage of the latest Anisian stage of the early Middle Triassic, about 243 million years ago. The holotype IVPP V 17040 and paratype IVPP V 16076 are housed at the Institute of Vertebrate Paleontology and Paleoanthropology in Beijing, and represent a nearly complete articulated skeleton and skull, and a partial disarticulated postcranial skeleton including dorsal vertebra, ribs, with osteoderms and gastral rib fragments, respectively. ZMNH M 8797, an incomplete postcranial skeleton showing a very well preserved right forelimb housed a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eusaurosphargis Dalsassoi
''Eusaurosphargis'' is an extinct genus of a diapsid reptile, known from the Middle Triassic (Anisian and Ladinian age) Besano Formation of northern Italy and Prosanto Formation of south-eastern Switzerland. It contains a single species, ''Eusaurosphargis dalsassoi''. It was a small reptile, measuring long. Discovery The holotype of ''Eusaurosphargis dalsassoi'' (BES SC 390) is a partial skeleton of a single individual found disarticulated but in close association. BES SC 390 was collected from an oil shale at Cava di Besano of the Besano Formation (Grenzbitumenzone). These lagoonal beds are equivalent to those at Monte San Giorgio, dating to the Anisian-Ladinian boundary, probably to the latest Anisian at this location, of the early Middle Triassic, about 243 million years ago. Nicole Klein and Oliver J. Sichelschmidt (2014) described disarticulated remains they referred to ''Eusaurosphargis sp''. These remains were collected from the Dutch Winterswijk Quar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Largocephalosaurus
''Largocephalosaurus'' is an extinct genus of basal saurosphargid, a marine reptile known from the Middle Triassic (Anisian age) Guanling Formation of Yunnan and Guizhou Provinces, southwestern China. It contains a type species, ''Largocephalosaurus polycarpon'', and a second species ''L. qianensis''. ''L. polycarpon'' was initially interpreted as an eosauropterygian sauropterygian closely related to European pachypleurosaurs and nothosaurids. However following additional preparation of the postcranial skeleton and the discovery of a second better known species ''L. qianensis'', Li ''et al.'' (2014) reinterpreted ''Largocephalosaurus'' as a basal member of the family Saurosphargidae and a close relative of ''Saurosphargis'' and '' Sinosaurosphargis''. According to Li ''et al.'' (2014), saurosphargids did not belong to Sauropterygia, although they were closely related to it, forming its sister taxon. Discovery The type species of ''Largocephalosaurus'', ''L. polycarpon'' is kno ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saurosphargis
''Saurosphargis'' is an extinct genus of a basal marine reptile, saurosphargid, known from the Middle Triassic (Anisian age) of southwestern Poland and eastern Netherlands. It contains a single species, ''Saurosphargis volzi''. Discovery ''Saurosphargis'' is known solely from the unnumbered holotype that was housed at the Breslaw Museum, a partial postcranial skeleton that included a section of 12 incomplete back vertebrae with ribs. The specimen collected at Gogolin, Gorny Slask of Upper Silesia, Poland, from the Chorzower Schichten horizon of the Lower Muschelkalk, dating to the early Anisian stage of the early Middle Triassic, about 246 million years ago. Rieppel (1995) described an isolated vertebra MGU Wr. 3873s housed at Institute of Geological Sciences, University of Wroclaw, that is possibly referable to ''Saurosphargis'', collected from the same general location. The holotype was destroyed during World War II, and as a result many authors considered ''S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saurosphargis Volzi
''Saurosphargis'' is an extinct genus of a basal marine reptile, saurosphargid, known from the Middle Triassic (Anisian age) of southwestern Poland and eastern Netherlands. It contains a single species, ''Saurosphargis volzi''. Discovery ''Saurosphargis'' is known solely from the unnumbered holotype that was housed at the Breslaw Museum, a partial postcranial skeleton that included a section of 12 incomplete back vertebrae with ribs. The specimen collected at Gogolin, Gorny Slask of Upper Silesia, Poland, from the Chorzower Schichten horizon of the Lower Muschelkalk, dating to the early Anisian stage of the early Middle Triassic, about 246 million years ago. Rieppel (1995) described an isolated vertebra MGU Wr. 3873s housed at Institute of Geological Sciences, University of Wroclaw, that is possibly referable to ''Saurosphargis'', collected from the same general location. The holotype was destroyed during World War II, and as a result many authors considered ''Sauro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Helveticosaurus
''Helveticosaurus'' is an extinct genus of diapsid marine reptile known from the Middle Triassic (Anisian-Ladinian boundary) of southern Switzerland. It contains a single species, ''Helveticosaurus zollingeri'', known from the nearly complete holotype T 4352 collected at Cava Tre Fontane of Monte San Giorgio, an area well known for its rich record of marine life during the Middle Triassic. Description and paleobiology ''Helveticosaurus'' is known from a nearly complete holotype which includes the premaxilla, maxilla, prefrontal, postfrontal, postorbital, squamosal, dentary and a postcranial skeleton. Several disarticulated elements are also known including teeth, portions of the snout and poscranial elements. ''Helveticosaurus'' is estimated to be about long from snout to tail. It possessed many features that were adaptations to a marine lifestyle in the shallow-sea environment that existed in Europe at the time when much of the continent was part of the Tethys Ocean. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sauropterygia
Sauropterygia ("lizard flippers") is an extinct taxon of diverse, aquatic reptiles that developed from terrestrial ancestors soon after the end-Permian extinction and flourished during the Triassic before all except for the Plesiosauria became extinct at the end of that period. The plesiosaurs would continue to diversify until the end of the Mesozoic. Sauropterygians are united by a radical adaptation of their pectoral girdle, adapted to support powerful flipper strokes. Some later sauropterygians, such as the pliosaurs, developed a similar mechanism in their pelvis. Uniquely among reptiles, sauropterygians moved their tail vertically like modern cetaceans and sirenians. Origins and evolution The earliest sauropterygians appeared about 247 million years ago (Ma), at the start of the Middle Triassic: the first definite sauropterygian with exact stratigraphic datum lies within the Spathian division of the Olenekian era in South China. Early examples were small (around 60 c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Placodont
Placodonts (" Tablet teeth") are an extinct order of marine reptiles that lived during the Triassic period, becoming extinct at the end of the period. They were part of Sauropterygia, the group that includes plesiosaurs. Placodonts were generally between in length, with some of the largest measuring long. The first specimen was discovered in 1830. They have been found throughout central Europe, North Africa, the Middle East and China. Palaeobiology The earliest forms, like ''Placodus'', which lived in the early to middle Triassic, resembled barrel-bodied lizards superficially similar to the marine iguana of today, but larger. In contrast to the marine iguana, which feeds on algae, the placodonts ate molluscs and so their teeth were flat and tough to crush shells. In the earliest periods, their size was probably enough to keep away the top sea predators of the time: the sharks. However, as time passed, other kinds of carnivorous reptiles began to colonize the seas, such as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Leatherback Turtle
The leatherback sea turtle (''Dermochelys coriacea''), sometimes called the lute turtle or leathery turtle or simply the luth, is the largest of all living turtles and the heaviest non-crocodilian reptile, reaching lengths of up to and weights of . It is the only living species in the genus ''Dermochelys'' and family Dermochelyidae. It can easily be differentiated from other modern sea turtles by its lack of a bony shell; instead, its carapace is covered by oily flesh and flexible, leather-like skin, for which it is named. Taxonomy and evolution Taxonomy ''Dermochelys coriacea'' is the only species in genus ''Dermochelys''. The genus, in turn, contains the only extant member of the family Dermochelyidae. Domenico Agostino Vandelli named the species first in 1761 as ''Testudo coriacea'' after an animal captured at Ostia and donated to the University of Padua by Pope Clement XIII. In 1816, French zoologist Henri Blainville coined the term ''Dermochelys''. The leatherback was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alps
The Alps () ; german: Alpen ; it, Alpi ; rm, Alps ; sl, Alpe . are the highest and most extensive mountain range system that lies entirely in Europe, stretching approximately across seven Alpine countries (from west to east): France, Switzerland, Italy, Liechtenstein, Austria, Germany, and Slovenia. The Alpine arch generally extends from Nice on the western Mediterranean to Trieste on the Adriatic and Vienna at the beginning of the Pannonian Basin. The mountains were formed over tens of millions of years as the African and Eurasian tectonic plates collided. Extreme shortening caused by the event resulted in marine sedimentary rocks rising by thrusting and folding into high mountain peaks such as Mont Blanc and the Matterhorn. Mont Blanc spans the French–Italian border, and at is the highest mountain in the Alps. The Alpine region area contains 128 peaks higher than . The altitude and size of the range affect the climate in Europe; in the mountains, precipitation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nomen Dubium
In binomial nomenclature, a ''nomen dubium'' (Latin for "doubtful name", plural ''nomina dubia'') is a scientific name that is of unknown or doubtful application. Zoology In case of a ''nomen dubium'' it may be impossible to determine whether a specimen belongs to that group or not. This may happen if the original type series (i. e. holotype, isotype, syntype or paratype) is lost or destroyed. The zoological and botanical codes allow for a new type specimen, or neotype, to be chosen in this case. A name may also be considered a ''nomen dubium'' if its name-bearing type is fragmentary or lacking important diagnostic features (this is often the case for species known only as fossils). To preserve stability of names, the ''International Code of Zoological Nomenclature'' allows a new type specimen, or neotype, to be chosen for a ''nomen dubium'' in this case. 75.5. Replacement of unidentifiable name-bearing type by a neotype. When an author considers that the taxonomic identity of a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
