Eophycis Temporal range: | |
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Restoration of E. jamnesis | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Actinopterygii |
Order: | Gadiformes |
Family: | Moridae |
Genus: | † Eophycis Jerzmanska, 1968 |
Type species | |
Eophycis jamnensis Jerzmanska, 1968 | |
Species | |
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Eophycis ("dawn Phycis ") is an extinct genus of prehistoric morid gadiform fish that lived during the early Oligocene epoch in the Paratethys Sea, where it is known from both the eastern and western regions. It represents the oldest fossil record of the Moridae. [1] [2]
It contains three species: [2]
Several articulated, well-preserved specimens of E. jamnensis are known from Poland. [2]
Lates is a genus of freshwater and euryhaline lates perches belonging to the family Latidae. The generic name is also used as a common name, lates, for many of the species.
The Moridae are a family of cod-like fishes, known as codlings, hakelings, and moras.
Palaeobatrachus is an extinct genus of frogs from Europe that existed from the middle Eocene to the middle Pleistocene, spanning almost 50 million years. They were obligately aquatic, and would have not spent much time on dry land. They are one of two genera and by far the largest genus in the family Palaeobatrachidae, which are considered to be members of Pipimorpha, related to the South American-African family Pipidae, which includes the African clawed frog and Surinam toad.
The Paratethys sea, Paratethys ocean, Paratethys realm or just Paratethys, was a large shallow inland sea that covered much of mainland Europe and parts of western Asia during the middle to late Cenozoic, from the late Paleogene to the late Neogene. At its greatest extent, it stretched from the region north of the Alps over Central Europe to the Aral Sea in Central Asia.
Berycomorus is an extinct genus of prehistoric marine ray-finned fish that lived during the late Eocene epoch. It contains a single species, B. firdoussi, from the Pabdeh Formation of Iran.
Balistomorphus is an extinct genus of prehistoric triggerfish during the early Oligocene epoch in what is now Canton Glarus, Switzerland, where fossils are known from the Matt Formation. It inhabited the marine environment of the Paratethys.
Acanthopleurus is an extinct genus of marine triplespine that lived in the seas over what is now Europe during the early Oligocene epoch.
Eolamprogrammus is an extinct genus of prehistoric marine cusk-eel that lived during the earliest Eocene. It contains a single species, E. senectus from the earliest Ypresian-aged Danata Formation of Turkmenistan. It may potentially represent an early member of the Neobythitinae.
Properca is an extinct genus of marine percomorph ray-finned fish that lived in Europe throughout much of the Cenozoic, from the Paleocene to the Miocene epochs.
Bregmacerina is an extinct genus of prehistoric marine ray-finned fish, most likely a codlet, that lived during the early part of the Miocene epoch. It contains a single species, B. antiqua, from the Burdigalian Sakaraul Horizon Formation of North Caucasus, Russia.
Aluvarus praeimperialis is an extinct ray-finned fish, known from two headless larval fossil specimens found in the Pabdeh Formation, a Late Eocene stratum from the Priabonian epoch, of what is now Iran. A. praeimperialis was originally thought to be a luvar, described as "Luvarus praeimperialis", as it was thought to be a predecessor to the modern luvar. A later reexamination of the specimens showed that they were too incomplete to demonstrate such a conclusion and had no clear exclusive shared traits with luvar, and were renamed "Aluvarus", meaning "not luvar" or "different than luvar". However, some authorities still retain it as a luvar.
Carpathichthys is an extinct genus of prehistoric slickhead fish from the Oligocene. It contains a single species, C. polonicus, from the Menilite Formation in the Carpathian Flysch Belt of Poland, in what was formerly the Paratethys Sea.
Caprovesposus is an extinct, prehistoric surgeonfish that inhabited the Paratethys Sea during the Oligocene. It is known from a single species, C. parvus, from what is now the North Caucasus, Russia. Potential specimens are known from the Miocene of Egypt, but these are poorly preserved and this attribution is uncertain.
Diaphyodus is an extinct genus of prehistoric marine ray-finned fish, generally considered a drumfish, from the Late Paleocene and Eocene, and potentially to the mid-Oligocene of Europe and North America.
Dapalis is an extinct genus of prehistoric glassfish known from the Middle Eocene to the Early Miocene. It is known from both freshwater and estuarine habitats of much of mainland Europe.
Eolates is an extinct genus of prehistoric lates perch from the Paleogene of Europe. It contains three species, two marine and one freshwater, known from the early-middle Eocene and Late Oligocene.
Eomyctophum is an extinct genus of lanternfish that inhabited the Paratethys Sea during the Oligocene. It is the only member of the extinct subfamily Eomyctophinae, although Eokrefftia may also belong in it. Its remains are known from throughout eastern Europe & western Asia in both the Caucasus and Carpathians, and comprise both articulated skeletons and otoliths, suggesting it was a particularly common fish.
Palimphyes is an extinct genus of marine ray-finned fish known from the Paleogene period. It was a euzaphlegid, an extinct family of scombroid fish related to the escolars and snake mackerels.
The Alosidae, or the shads, are a family of clupeiform fishes. The family currently comprises four genera worldwide, and about 32 species.
The Matt Formation is an Early Oligocene-aged marine geological formation that outcrops in the Glarus Alps of the Canton of Glarus, Switzerland. It is most notable for its fossiliferous slates found near Engi, known as the Engi slates, Glarner Schiefer or Glarner Fischschiefer, which contain the well-preserved fossils of fishes, birds, and sea turtles. The metamorphization of the rock has led to many of the fossils appearing somewhat distorted.