Related Research Articles
Liopleurodon is a genus of large, carnivorous marine reptile belonging to the Pliosauroidea, a clade of short-necked plesiosaurs. The two species of Liopleurodon lived from the Callovian Stage of the Middle Jurassic to the Kimmeridgian stage of the Late Jurassic Period. It was the apex predator of the Middle to Late Jurassic seas that covered Europe. The largest species, L. ferox, is estimated to have grown up to 6.4 metres (21 ft) in length.
Cetiosaurus meaning 'whale lizard', from the Greek keteios/κήτειος meaning 'sea monster' and sauros/σαυρος meaning 'lizard', is a herbivorous sauropod dinosaur from the Middle Jurassic Period, living about 167 million years ago in what is now Europe.
Teinurosaurus is a genus of carnivorous theropod dinosaur. Teinurosaurus lived during the Late Jurassic in what is now Portugal. The type species is Teinurosaurus sauvagei. It's been estimated to be 11.4 m in length and 3.6 tonnes in weight.
Morinosaurus was a genus of sauropod dinosaur from an unnamed formation of Kimmeridgian-age Upper Jurassic rocks from Boulogne-sur-Mer, Départment du Pas-de-Calais, France. It is an obscure tooth genus sometimes referred to the Lower Cretaceous English wastebasket taxon Pelorosaurus.
Neosodon was a genus of sauropod dinosaur from the Late Tithonian-age Upper Jurassic Sables et Gres a Trigonia gibbosa of Départment du Pas-de-Calais, France. It has never been formally given a species name, but is often seen as N. praecursor, which actually comes from a different animal. Often in the past, it had been assigned to the wastebasket taxon Pelorosaurus, but restudy has suggested that it could be related to Turiasaurus, a roughly-contemporaneous giant Spanish sauropod. It is only known from six teeth.
Erectopus is a basal allosauroid theropod from the Lower Cretaceous of France.
Machimosaurus is an extinct genus of teleosaurid crocodyliform from the Late Jurassic and Early Cretaceous. The type species, Machimosaurus hugii, was found in Switzerland. Other fossils have been found in England, France, Germany, Portugal, Switzerland and Tunisia. Machimosaurus rex is the largest named teleosaurid and thalattosuchian, with an estimated length of approximately 7.2 metres ,. Machimosaurus is the largest known crocodyliform of the Jurassic.
The Caranguejeira Conglomerate is an Aptian to Cenomanian geologic formation in Portugal. Dinosaur remains diagnostic to the genus level are among the fossils that have been recovered from the formation.
Joseph Henri Ferdinand Douvillé, also known as Henri Douvillé, was French paleontologist, geologist and malacologist. Douvillé worked as a mining engineer in Bourges (1872) and Limoges (1874), afterwards serving as professeur suppléant of paleontology at the École des Mines. From 1881 to 1911 he was a professor of paleontology at the École des Mines.
Philippe-Charles or Philip Carel Schmerling was a Dutch/Belgian prehistorian, pioneer in paleontology, and geologist. He is often considered the founder of paleontology.
Henri Émile Sauvage was a French paleontologist, ichthyologist, and herpetologist. He was a leading expert on Mesozoic fish and reptiles.
Georges de Tribolet was a Swiss geologist. He was the older brother of geologist and paleontologist, Maurice de Tribolet (1852–1929).
Eugène Dumortier was a French paleontologist.
Louis Édouard Gourdan de Fromentel was a French physician and paleontologist known for his study of fossil coral polyps and sponges.
Nicolas Robert Bouchard-Chantereaux was a French geologist and zoologist interested in malacology and marine biology. He was President de l'Administration du Muséum d'Histoire Naturelle Boulogne.
Philippe Thomas was a French veterinarian and amateur geologist who discovered large deposits of phosphates in Tunisia. Despite the huge economic importance of his discovery, he received little recognition during his life. Monuments to Thomas in Tunisia were destroyed after the country gained independence.
Victor-Auguste Gauthier was a French school teacher and amateur palaeontologist. He specialized in the study of fossilized sea urchins, contributing meticulous descriptions of many fossils found in southern France, Algeria, Tunisia and Persia.
Alphonse Péron was a French soldier and amateur naturalist. He used his spare time to pursue his interest in paleontology, and authored or coauthored several important works on the geology and paleontology of France and Algeria.
The Bulletin de la Société Géologique de France, otherwise known as BSGF - Earth Sciences Bulletin is a peer-reviewed open access scientific journal covering Earth sciences. The journal publishes articles, short communications, reviews, comments and replies. It is published by EDP Sciences and the editor-in-chief is Laurent Jolivet. The journal was established in 1830. It is a publication of the Société géologique de France. Most of the older content, published before 1924 is available online at the Biodiversity Heritage Library.
The Azilal Formation, also known as Toundute Continental Series and Wazzant Formation, is a geological unit in the Azilal & Ouarzazate provinces of the High Atlas of Morocco, that cover the middle Toarcian to early Aalenian stages of the Jurassic Period. It is a terrestrial deposit which overlies marine dolomites of equivalent age to the Budoš Limestone of Montenegro or the Marne di Monte Serrone of Italy. Dinosaur remains, such the Sauropod Tazoudasaurus and the Basal Ceratosaur Berberosaurus are known from the unit, along with several undescribed genera. The Units inside the group have been considered individual on the past, being a division of the so-called "Couches rouges", and subdivided by a supposed geological scale. The strata of the group extends towards the Central High Atlas, covering different anticlines, and topographic accidents along the range of the Mountains. Although new studies have suggested that the strata is coeval in age, and should be referred to as a unique unit. The Group is believed to have been a mostly deltaic, and river channels filled a succession of seashore and inland environments, covering the late Liassic coast of modern northern Africa. Based on observed halokinetic strata, the Tazoult Ridge evolved as a Salt Wall forming a 20 km long NE-SW trending structural and sedimentary high for at least 20 million years, between Pliensbachian-Bajocian periods. This emerged small landmass generated a great local Diapir, with continuous Diapirism until the end of the Aalenian.
References
- ↑ Sauvage, H. E. (1880). Synopsis des poissons et des reptiles des terrains jurassiques de Boulogne-sur-mer. Bulletin de la Société Géologique de France13:524-547.
- ↑ Sauvage, H. E. (1874). Memoire sur les dinosauriens et les crocodiliens des terrains jurassiques de Boulogne-sur-Mer. Mémoires de la Société Géologique de France, second series10:1-58.
- ↑ Kuhn, O. (1934) Sauropterygia: Fossilia Catalogous 69:1-127.
- ↑ Sepkoski, J. J. (2002). A compendium of fossil marine animal genera. Bulletins of American Paleontology363:1-560
