Anoual Formation, the Glossary
Table of Contents
49 relations: Albanerpetontidae, Alocodon, Amphibian, Amphitheriidae, Annual, Morocco, Arganodus, Atoposauridae, Bathonian, Caudata, Choristodera, Coelacanth, Crocodyliformes, Cteniogenys, Dinosaur, Dryolestida, Figuig Province, Fish, Geological formation, High Atlas, Ksar Metlili Formation, Lepidosauria, Lepidotes, Limestone, Lissamphibia, Lungfish, Marl, Mawsoniidae, Morocco, Mudstone, Ornithischia, Osteoglossiformes, Parviraptor, Pholadomya, Pterosaur, Rhamphorhynchidae, Rhynchocephalia, Sandstone, Scheenstia, Scincomorpha, Squamata, Stegosauria, Teleosauridae, Testudinata, Thalattosuchia, Theriosuchus, Theropoda, Turtle, Unconformity, Wukongopteridae.
- Jurassic Morocco
- Jurassic System of Africa
- Paleontology in Morocco
Albanerpetontidae
The Albanerpetontidae (also spelled Albanerpetidae and Albanerpetonidae) are an extinct family of small amphibians, native to the Northern Hemisphere during the Mesozoic and Cenozoic.
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Alocodon
Alocodon is a genus of ornithischian dinosaur known from multiple teeth from the Middle or Late Jurassic Cabaços Formation of Portugal, and also the Forest Marble and Chipping Norton Formations of England.
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Amphibian
Amphibians are ectothermic, anamniotic, four-limbed vertebrate animals that constitute the class Amphibia.
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Amphitheriidae
Amphitheriidae is a family of Mesozoic mammals restricted to the Middle Jurassic of Britain, with indeterminate members also possibly known from the equivalently aged Itat Formation in Siberia and the Anoual Formation of Morocco.
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Annual, Morocco
Annual or Anoual (Berber language: Anwal) is a small town in northeastern Morocco about 60 km west of Nador.
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Arganodus
Arganodus is an extinct genus of freshwater lungfish that had a wide global distribution throughout much of the Triassic period, with a single species surviving across Gondwana into the Cretaceous.
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Atoposauridae
Atoposauridae is a family of crocodile-like archosaurs belonging to Neosuchia.
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Bathonian
In the geologic timescale the Bathonian is an age and stage of the Middle Jurassic.
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Caudata
The Caudata are a group of amphibians containing the extant salamanders (the order Urodela) and all extinct species of amphibians more closely related to salamanders than to frogs.
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Choristodera
Choristodera (from the Greek χωριστός chōristos + δέρη dérē, 'separated neck') is an extinct order of semiaquatic diapsid reptiles that ranged from the Middle Jurassic, or possibly Triassic, to the Miocene (168 to 20 or possibly 11.6 million years ago).
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Coelacanth
Coelacanths (order Coelacanthiformes) are an ancient group of lobe-finned fish (Sarcopterygii) in the class Actinistia.
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Crocodyliformes
Crocodyliformes is a clade of crurotarsan archosaurs, the group often traditionally referred to as "crocodilians".
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Cteniogenys
Cteniogenys is a genus of choristodere, a morphologically diverse group of aquatic reptiles.
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Dinosaur
Dinosaurs are a diverse group of reptiles of the clade Dinosauria.
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Dryolestida
Dryolestida is an extinct order of mammals, known from the Jurassic and Cretaceous.
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Figuig Province
The Figuig Province (Arabic: إقليمفكيك) is a province in the Oriental Region of Morocco.
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Fish
A fish (fish or fishes) is an aquatic, anamniotic, gill-bearing vertebrate animal with swimming fins and a hard skull, but lacking limbs with digits.
Geological formation
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).
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High Atlas
The High Atlas, also called the Grand Atlas, is a mountain range in central Morocco, North Africa, the highest part of the Atlas Mountains.
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Ksar Metlili Formation
The Ksar Metlili Formation is a geological formation in eastern High Atlas of Morocco, it is late Tithonian to Berriasian in age. Anoual Formation and Ksar Metlili Formation are Jurassic Morocco, Jurassic System of Africa, Mudstone formations, Paleontology in Morocco and Sandstone formations.
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Lepidosauria
The Lepidosauria (from Greek meaning scaled lizards) is a subclass or superorder of reptiles, containing the orders Squamata and Rhynchocephalia.
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Lepidotes
Lepidotes (from λεπιδωτός, 'covered with scales') (previously known as Lepidotus) is an extinct genus of Mesozoic ray-finned fish.
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Limestone
Limestone (calcium carbonate) is a type of carbonate sedimentary rock which is the main source of the material lime.
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Lissamphibia
The Lissamphibia (from Greek λισσός (lissós, "smooth") + ἀμφίβια (amphíbia), meaning "smooth amphibians") is a group of tetrapods that includes all modern amphibians.
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Lungfish
Lungfish are freshwater vertebrates belonging to the class Dipnoi.
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Marl
Marl is an earthy material rich in carbonate minerals, clays, and silt.
Mawsoniidae
Mawsoniidae is an extinct family of prehistoric coelacanth fishes which lived during the Triassic to Cretaceous periods.
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Morocco
Morocco, officially the Kingdom of Morocco, is a country in the Maghreb region of North Africa.
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Mudstone
Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds.
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Ornithischia
Ornithischia is an extinct clade of mainly herbivorous dinosaurs characterized by a pelvic structure superficially similar to that of birds.
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Osteoglossiformes
Osteoglossiformes (Greek: "bony tongues") is a relatively primitive order of ray-finned fish that contains two sub-orders, the Osteoglossoidei and the Notopteroidei.
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Parviraptor
Parviraptor is a genus of squamate containing one species, Parviraptor estesi, from the Late Jurassic (Tithonian) or Early Cretaceous (Berriasian) Purbeck Limestone Formation of Dorset, England.
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Pholadomya
Pholadomya is a genus of saltwater clams, marine bivalve molluscs in the family Pholadomyidae.
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Pterosaur
Pterosaurs (from Greek pteron and sauros, meaning "wing lizard") are an extinct clade of flying reptiles in the order Pterosauria.
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Rhamphorhynchidae
Rhamphorhynchidae is a group of early pterosaurs named after Rhamphorhynchus, that lived in the Late Jurassic.
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Rhynchocephalia
Rhynchocephalia is an order of lizard-like reptiles that includes only one living species, the tuatara (Sphenodon punctatus) of New Zealand.
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains, cemented together by another mineral.
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Scheenstia
Scheenstia is an extinct genus of neopterygian ray-finned fish from the Late Jurassic–Early Cretaceous of Europe.
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Scincomorpha
Scincomorpha is an infraorder and clade of lizards including skinks (Scincidae) and their close relatives.
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Squamata
Squamata (Latin squamatus, 'scaly, having scales') is the largest order of reptiles, comprising lizards and snakes.
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Stegosauria
Stegosauria is a group of herbivorous ornithischian dinosaurs that lived during the Jurassic and early Cretaceous periods.
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Teleosauridae
Teleosauridae is a family of extinct typically marine crocodylomorphs similar to the modern gharial that lived during the Jurassic period.
See Anoual Formation and Teleosauridae
Testudinata
Testudinata is the group of all tetrapods with a true turtle shell.
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Thalattosuchia
Thalattosuchia is a clade of mostly marine crocodylomorphs from the Early Jurassic to the Early Cretaceous that had a cosmopolitan distribution.
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Theriosuchus
Theriosuchus is an extinct genus of atoposaurid neosuchian from Late Jurassic to Early Cretaceous of Europe (Hungary & southern England), Southeast Asia (Thailand) and western North America (Wyoming), with fragmentary records from Middle Jurassic and Early Cretaceous sites in China, Morocco, and Scotland.
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Theropoda
Theropoda (from ancient Greek whose members are known as theropods, is a dinosaur clade that is characterized by hollow bones and three toes and claws on each limb. Theropods are generally classed as a group of saurischian dinosaurs. They were ancestrally carnivorous, although a number of theropod groups evolved to become herbivores and omnivores.
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Turtle
Turtles are reptiles of the order Testudines, characterized by a special shell developed mainly from their ribs.
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Unconformity
An unconformity is a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous.
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Wukongopteridae
Wukongopteridae is a group of basal pterosaurs, found in China and the UK.
See Anoual Formation and Wukongopteridae
See also
Jurassic Morocco
- Aganane Formation
- Anoual Formation
- Atlasaurus
- Azilal Formation
- Berberosaurus
- Cetiosaurus
- Docidoceras
- Donodon
- El Mers Group
- Guettioua Formation
- Imi-n-Ifri Formation
- Iouaridène Formation
- Ksar Metlili Formation
- Spicomellus
- Tafraout Group
- Tazoudasaurus
- Thyreosaurus
- Tilougguit Formation
Jurassic System of Africa
- Adigrat Sandstone
- Aganane Formation
- Anoual Formation
- Antalo Limestone
- Assaouas Formation
- Azilal Formation
- Batoka Formation
- Bemaraha Formation
- Bushveld Sandstone
- Clarens Formation
- Drakensberg Group
- El Mers Group
- Elliot Formation
- Enon Formation
- Etjo Sandstone
- Forest Sandstone
- Guettioua Formation
- Imi-n-Ifri Formation
- Iouaridène Formation
- Irhazer Shale
- Isalo III Formation
- Kadzi Formation
- Kandreho Formation
- Ksar Metlili Formation
- Mabdi Formation
- Mpandi Formation
- Mugher Mudstone
- Stormberg Group
- Tafraout Group
- Tendaguru Formation
- Tilougguit Formation
- Tiourarén Formation
- Upper Karoo Group
Paleontology in Morocco
- Aganane Formation
- Anoual Formation
- Aoufous Formation
- Argana Group
- Azilal Formation
- El Mers Group
- Fezouata Formation
- Guettioua Formation
- Imi-n-Ifri Formation
- Kem Kem Group
- Ksar Metlili Formation
- Tafraout Group