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Necrosauridae
Palaeovaranidae, formerly known as Necrosauridae, is an extinct clade of anguimorph lizards known from the Paleogene of Europe. They have sometimes been recovered as members of Varanoidea. It contains three genera. Genera * '' Eosaniwa'' Haubold, 1977 Geiseltal, Germany, Eocene * '' Palaeovaranus'' Zittel, 1887 (Formerly ''Necrosaurus'') Messel Pit, Germany, Quercy Phosphorites Formation, France, Eocene * '' Paranecrosaurus'' Smith & Habersetzer, 2021 (Formerly "''Saniwa" feisti'') Messel Pit, Germany, Eocene References † † A dagger, obelisk, or obelus is a typographical mark that usually indicates a footnote if an asterisk has already been used. The symbol is also used to indicate death (of people) or extinction (of species or languages). It is one of the mo ... Eocene lizards {{Paleo-lizard-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeovaranus
''Palaeovaranus'' is an extinct genus of Varanoidea, varanoid lizards from the Late Eocene of France and Germany. It contains two species, ''Palaeovaranus cayluxensis'' and ''Palaeovaranus giganteus'' (formerly assigned to a separate genus ''Melanosauroides''). The genus was first named by Henri Filhol in 1877, but he had named the species ''Palaeovaranus cayluxi'' earlier as ''Palaeosaurus cayluxi'' in 1873, and as ''Necrosaurus cuxleyi'' in 1876 after it was discovered that ''Palaeosaurus'' was preoccupied. However, he failed to provide any kind of valid description, which renders Karl Alfred Ritter von Zittel's 1887 description of the taxon as the valid authority on its validity. Despite this, the name ''Necrosaurus'' was the widely used name in the literature afterwards until 2017, when the name ''Palaeovaranus'' was revived. It is placed in the family Palaeovaranidae. References External links Anguimorpha, † Eocene lizards Eocene reptiles of Europe Eocene Fran ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paranecrosaurus
''Paranecrosaurus'' is an extinct genus of lizard from the Eocene Messel Pits of Germany. It contains a single species, ''Paranecrosaurus feisti,'' originally described as a species of ''Saniwa.'' It was carnivorous, as indicated by the presence of the lizard ''Cryptolacerta'' as stomatch contents. It is placed in the family Palaeovaranidae. References † A dagger, obelisk, or obelus is a typographical mark that usually indicates a footnote if an asterisk has already been used. The symbol is also used to indicate death (of people) or extinction (of species or languages). It is one of the mo ... Eocene lizards Fossil taxa described in 2021 {{Paleo-lizard-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anguimorph
The Anguimorpha is a suborder of squamates. The group was named by Fürbringer in 1900 to include all autarchoglossans closer to '' Varanus'' and ''Anguis'' than ''Scincus''. These lizards, along with iguanians and snakes, constitute the proposed "venom clade" Toxicofera of all venomous reptiles. Evolution The oldest widely accepted member of Anguimorpha is '' Dorsetisaurus'' from the Late Jurassic of Europe and North America. In 2022, the genus '' Cryptovaranoides'' was described from the latest Triassic (Rhaetian) of England. ''Cryptovaranoides'' was recovered in the study as a crown-group anguimorph, and therefore the oldest crown group-squamate, 35 million years older than any previously known crown-group squamate. However, a 2023 study found that ''Cryptovaranoides'' most likely represents an archosauromorph that was only distantly related to squamates. Families Anguidae There are 9 genera found within the Anguidae family. They are characterized by being heavily arm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene
The Paleogene Period ( ; also spelled Palaeogene or Palæogene) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period Ma (million years ago) to the beginning of the Neogene Period Ma. It is the first period of the Cenozoic Era, the tenth period of the Phanerozoic and is divided into the Paleocene, Eocene, and Oligocene epochs. The earlier term Tertiary Period was used to define the time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognized as a formal stratigraphic term, "Tertiary" still sometimes remains in informal use. Paleogene is often abbreviated "Pg", although the United States Geological Survey uses the abbreviation "" for the Paleogene on the Survey's geologic maps. Much of the world's modern vertebrate diversity originated in a rapid surge of diversification in the early Paleogene, as survivors of the Cretaceous–Paleogene extinction event took advantage of empty ecolo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Varanoidea
Varanoidea is a superfamily of lizards, including the well-known family Varanidae (the monitors and goannas). Also included in the Varanoidea are the Lanthanotidae ( earless monitor lizards), and the extinct Palaeovaranidae. Throughout their long evolutionary history, varanoids have exhibited great diversity, both in habitat and form. This superfamily includes the largest-known terrestrial lizard, Megalania (~5 meters), and the largest extant lizard, the Komodo dragon (''Varanus komodoensis'', ~3 meters). Evolution Either synonymous with, or a subgroup of, the group Platynota, the varanoids first appear in the fossil record in the latter part of Early Cretaceous, but possible varanoid ancestors have been traced back as far as Early Jurassic times. Among the earliest known varanoids are the monitor-like necrosaurids '' Palaeosaniwa canadensis'' from the Campanian (roughly 71–82 mya) of North America and '' Estesia mongoliensis'' and '' Telmasaurus grangeri'', both from the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geisel Valley
The Geisel valley () is a valley in Saxony-Anhalt, Germany, situated west of Merseburg, Saalekreis district. It is named after the River Geisel which rises in Mücheln and is a tributary of the Saale, just under long. Its main settlements are Braunsbedra and Mücheln, which in the future will merge into the 'collective municipality' of ''Geiseltal''. The Geisel valley was quarried for coal from 1698 until the mines were closed in 1994; The mining of brown coal is first attested for 1698 near the Zöbigker grove but is most likely to be older. Initially, only twelve smaller pits emerged at the beginning of the Industrial Revolution in the late 19th century, which spread to large areas; ultimately, the Braunsbedra-Geiseltal mines became one of the largest connected mining regions in Germany. Coal/Lignite mining At the beginning of the twentieth century, the region was characterized by mostly independent pits (Elisabeth 1906, Großkayna 1907, Beuna 1907, Cecilie 1907, Rheinland 19 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Messel Pit
The Messel Formation is a Formation (geology), geologic formation in Hesse, central Germany, dating back to the Eocene Epoch (geology), epoch (about 47 Ma). Its geographic range is restricted to the Messel pit. There it unconformably overlies crystalline Variscan basement and its Permian cover (Rotliegend) as well as Eocene volcanic breccias derived from the basement rocks. The formation mainly comprises lacustrine laminated bituminous shale (‘oil shale’) renowned for its content of fossils in exceptional preservation, particularly plants, arthropods and vertebrates (e.g. ''Darwinius masillae''). Messel pit The Messel pit () is a disused quarry near the village of Messel (Landkreis Darmstadt-Dieburg, Hesse) about southeast of Frankfurt am Main, Germany. Bituminous shale was mined there. Because of its abundance of well-preserved fossils of the Messel Formation dating from the middle of the Eocene, it has significant geological and scientific importance. Over 1400 taxa o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quercy Phosphorites Formation
The Quercy Phosphorites Formation (French language, French: ''Phosphorites du Quercy''; ) is a Formation (geology), geologic formation and lagerstätte in Occitania (administrative region), Occitanie, southern France. It preserves fossils dated to the Paleogene Period (geology), period (Bartonian, latest Bartonian to Late Oligocene),Quercy Phosphorites Formation at Fossilworks.orgPhosphorites du Quercy Formation at Fossilworks.org or MP16 to MP28 zones of the Eu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anguimorpha
The Anguimorpha is a suborder of Squamata, squamates. The group was named by Fürbringer in 1900 to include all autarchoglossans closer to ''Varanus'' and ''Anguis'' than ''Scincus''. These lizards, along with iguanians and snakes, constitute the proposed "venom clade" Toxicofera of all venomous reptiles. Evolution The oldest widely accepted member of Anguimorpha is ''Dorsetisaurus'' from the Late Jurassic of Europe and North America. In 2022, the genus ''Cryptovaranoides'' was described from the latest Triassic (Rhaetian) of England. ''Cryptovaranoides'' was recovered in the study as a crown-group anguimorph, and therefore the oldest crown group-squamate, 35 million years older than any previously known crown-group squamate. However, a 2023 study found that ''Cryptovaranoides'' most likely represents an Archosauromorpha, archosauromorph that was only distantly related to squamates. Families Anguidae There are 9 genera found within the Anguidae family. They are characteriz ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lizard Families
This is a list of the extant lizard families. Lizards are an paraphyly, informal group of Squamata, squamates. Taxonomy There are five infraorders which separate the lizards, these are- Diploglossa, Gekkota, Iguania, Platynota and Scincomorpha. This separation is based mainly on morphological similarities between family groups. The Diploglossans and Platynotans are two closely related infraorders which are very diverse families. Very few generalisations can be placed upon these families morphologically. Many species are limbless, while others have fully formed limbs. It is believed that these lizards are the closest lizard relation to the snakes. The Gekkotans are the second most diverse group of lizards. They can be morphologically distinguished by the absence of temporal arches, which allows greater moveability of the head. Most species also have cloacal sacs and fixed eyelids. The Iguanians are another diverse group of lizards. All iguanians are fully limbed. Most species amb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
