Information about Mosasaur
| Mosasaurs Fossil range: Cretaceous | ||||||||||||
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An etching of Mosasaur An etching of Mosasaur | ||||||||||||
| Conservation status | ||||||||||||
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Extinct (fossil) | ||||||||||||
| Scientific classification | ||||||||||||
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| Subfamilies | ||||||||||||
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Halisaurinae Mosasaurinae Plioplatecarpinae Tylosaurinae | ||||||||||||
Known genera include Clidastes, Mosasaurus, Prognathodon, Globidens, Plotosaurus, Plesiotylosaurus, Carinodens, Dallasaurus, Igdamanosaurus, Halisaurus, Tylosaurus, Platecarpus, Selmasaurus, Plioplatecarpus, Amphekepubis, Goronyosaurus, Liodon, Moanasaurus, Pluridens, Lakumasaurus, Yaguarasaurus, Eonatator, Hainosaurus, Tethysaurus, Angolasaurus, Kourisodon and Russellosaurus.
Description
Mosasaur skull Oxford University Museum of Natural History.
The smallest-known mosasaur was Carinodens belgicus, which was about 3 to 3.5 m long and probably lived in shallow waters near shore, cracking mollusks and sea urchins with its bulbous teeth. Larger mosasaurs were more typical: mosasaurs ranged in size up to 17 m. Hainosaurus holds the record for longest mosasaur, at 17.5 m.
Mosasaurs had a body shape similar to that of modern-day monitor lizards (varanids), but were more elongated and streamlined for swimming. Their limb bones were reduced in length and their paddles were formed by webbing between their elongated digit-bones. Their tails were broad and supplied the locomotive power. This method of locomotion may have been similar to that used by the conger eel or sea snakes today. The animal may have lurked and pounced rapidly and powerfully on passing prey, rather than hunting for it.
Mosasaurs had a double-hinged jaw and flexible skull (much like that of a snake), which enabled them to gulp down their prey almost whole, a snakelike habit that has helped identify the unmasticated gut contents fossilized within mosasaur skeletons. A skeleton of Tylosaurus proriger from South Dakota included remains of the diving seabird Hesperornis, a marine bony fish, a possible shark and another, smaller mosasaur (Clidastes). Mosasaur bones have also been found with shark teeth embedded in them.
Based on features such as the double row of pterygoid ("flanged") teeth on the palate, the double-hinged jaw, modified/reduced limbs and probable methods of locomotion, many researchers believe that snakes and mosasaurs may have had a common ancestor. This theory was first suggested in 1869, by Edward Drinker Cope, who coined the term "Pythonomorpha" to include them. The idea lay dormant for more than a century, before being revived in the 1990s.[2] [3]
Environment
Sea levels were high during the Cretaceous Period, causing marine transgressions in many parts of the world and a great inland seaway in what is now North America. Mosasaur fossils have been found in the Netherlands, in Sweden, in Africa, in Australia, in New Zealand and on Vega Island, off the coast of Antarctica. In Canada and the United States, complete or partial specimens have been found in Alabama, Mississippi, Tennessee, and Georgia and in almost all the states covered by the seaway: Texas, southwest Arkansas, New Mexico, Kansas,[4] Colorado, Nebraska, the Dakotas and Montana. Mosasaurs are also known from California, Mexico, Peru and Denmark.Many of the 'dinosaur' remains found on New Zealand—a volcanic island arc that has never been part of a continent—are actually mosasaurs and plesiosaurs, another group of Mesozoic predatory marine reptiles.
Discovery
The Mosasaur discovered in a Maastricht limestone quarry, 1780 (contemporary engraving).
Dr. Hoffman's correspondence among men of science made the find famous. When the Revolutionary forces occupied Maastricht, the carefully-hidden fossil was uncovered, betrayed, it is said, by a case of wine and transported to Paris, where Georges Cuvier was able to describe it for science, although le grand animal fossile de Maastricht was not actually described as a Mosasaur ('Meuse reptile') until 1822 and not given its official name, Mosasaurus hoffmanni, until 1829. Several sets of mosasaur remains, that had been discovered earlier at Maastricht but were not identified as mosasaurs until the nineteenth century, have been on display in the Teylers Museum, Haarlem, since about 1770.
The Maastricht limestone beds were rendered so famous they have given their name to the ultimate 6-million-year epoch of the Cretaceous: the Maastrichtian.
Evolutionary antecedents
Based on features such as the loosely-hinged jaw, modified/reduced limbs and probable locomotion, many researchers believe that snakes may be descended from mosasaurs, a suggestion advanced in 1869, by Edward Drinker Cope, who coined the term "Pythonomorpha" to include them. The idea lay dormant for more than a century, to be revived in the 1990s.[2]On 2005-11-16, research reported in Netherlands Journal of Geosciences, confirmed that the recently uncovered Dallasaurus turneri is an early link between land-based monitor lizards (such as the Komodo dragon) and the aquatic mosasaurs.[6]
In popular culture
Mosasaurs appear in the BBC television series Sea Monsters. Mosasaurs also feature heavily in the ITV television series Primeval. In this show, the mosasaurs are depicted as having skin more similar to a crocodile's (which is incorrect).A highly evolved mosasaur appeared in an episode of . It was inhabiting Loch Ness as the legendary Loch Ness Monster.
Purported modern sightings
Although paleontologists have determined that all mosasaurs went extinct around the same time as the dinosaurs, and there is no fossil evidence of them beyond the end of the Cretaceous (Maastrichtian), some cryptozoologists feel that sporadic reports of crocodile-like sea serpents may be surviving mosasaurs. The Taniwha of Māori lore has also been connected to mosasaurs by journalists. However, there is no scientific evidence of any mosasaur remains since the end of the Cretaceous, 65 million years ago.References
1. ^ Lee, 1997, "The phylogeny of varanoid lizards and the affinities of snakes," in Phil. Trans. R. Soc. Lond. B 352: 53-91.
2. ^ [1]
3. ^ [2]
4. ^ Everhart, M.J. 2005. "Enter the Mosasaurs," Chapter 9 in "Oceans of Kansas: A Natural History of the Western Interior Sea." Indiana University Press, Bloomington, 322 p.
5. ^ [3]
6. ^ [4]
2. ^ [1]
3. ^ [2]
4. ^ Everhart, M.J. 2005. "Enter the Mosasaurs," Chapter 9 in "Oceans of Kansas: A Natural History of the Western Interior Sea." Indiana University Press, Bloomington, 322 p.
5. ^ [3]
6. ^ [4]
External links
- Palaeos: Vertebrates: Mosasaurs
- BBC Science and Nature: Mosasaurs
- Mike Everhart and David Lewis, "Mesozoic marine monsters of the Mangahouanga": New Zealand fossil fauna
- Mike Everhart, "A day in the life of a Mosasaur": life in the Sea of Kansas, illus. by Carl Buell
- Mike Everhart, "Mosasaurus hoffmani" until 1829.
- Mosasaurus maximus mounted skeleton at University of Texas Memorial Museum
- Canadian Fossil Discovery Centre
The Cretaceous Period is one of the major divisions of the geologic timescale, reaching from the end of the Jurassic Period (i.e. from 145.5 ± 4.0 million years ago (Ma)) to the beginning of the Paleocene epoch of the Tertiary Period (about 65.5 ± 0.3 Ma).
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Etching is the process of using strong acid to cut into the unprotected parts of a metal surface to create a design in intaglio in the metal (the original process - in modern manufacturing other chemicals may be used on other types of material).
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conservation status of a species is an indicator of the likelihood of that species continuing to survive either in the present day or the future. Many factors are taken into account when assessing the conservation status of a species: not simply the number remaining, but the
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- For other uses of the term, see Fossil (disambiguation)
FOSSIL is a standard for allowing serial communication for telecommunications programs under the DOS operating system.
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Scientific classification or biological classification is a method by which biologists group and categorize species of organisms. Scientific classification also can be called scientific taxonomy, but should be distinguished from folk taxonomy, which lacks scientific basis.
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Chordata
Bateson, 1885
Typical Classes
See below
Chordates (phylum Chordata) are a group of animals that includes the vertebrates, together with several closely related invertebrates.
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Bateson, 1885
Typical Classes
See below
Chordates (phylum Chordata) are a group of animals that includes the vertebrates, together with several closely related invertebrates.
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Sauropsida*
Goodrich, 1916
Subclasses
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Goodrich, 1916
Subclasses
- Anapsida
- Diapsida
- Reptilia Laurenti, 1768
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Squamata
Oppel, 1811
Suborders
see text
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Oppel, 1811
black: range of Squamata
Suborders
see text
- This article is about the Squamata order of reptiles. For the Roman scale armour see: Lorica squamata.
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Lacertilia*
Günther, 1867
Families
Many, see text.
Lizards are reptiles of the order Squamata, normally possessing four legs, external ear openings and movable eyelids.
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Günther, 1867
Families
Many, see text.
Lizards are reptiles of the order Squamata, normally possessing four legs, external ear openings and movable eyelids.
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Paul Gervais full name François Louis Paul Gervaise (September 26, 1816 - February 10, 1879) was a French palaeontologist and entomologist.
Gervais was born at Paris, where he obtained the diplomas of doctor of science and of medicine, and in 1835 he began
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Gervais was born at Paris, where he obtained the diplomas of doctor of science and of medicine, and in 1835 he began
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family (Latin: familia, plural familiae) is a rank, or a taxon in that rank. Exact details of formal nomenclature depend on the Nomenclature Code which applies.
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Halisaurinae
Bardet et al., 2005
Genera
See text.
Halisaurinae (Bardet et al., 2005) is a subfamily of mosasaurs, a diverse group of Late Cretaceous marine squamates.
Bardet et al. (2005, p.
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Bardet et al., 2005
Genera
See text.
Halisaurinae (Bardet et al., 2005) is a subfamily of mosasaurs, a diverse group of Late Cretaceous marine squamates.
Bardet et al. (2005, p.
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Mosasaurinae
Mosasaurinae (Gervais, 1853; Williston, 1897) is a subfamily of mosasaurs, a diverse group of Late Cretaceous marine squamates.
Russell (1967, pp.
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Mosasaurinae (Gervais, 1853; Williston, 1897) is a subfamily of mosasaurs, a diverse group of Late Cretaceous marine squamates.
Russell (1967, pp.
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Plioplatecarpinae
Dollo, 1884; Williston, 1897
Genera
See text.
Plioplatecarpinae is a subfamily of mosasaurs, a diverse group of late Cretaceous marine squamates.
Russell (1967, pp.
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Dollo, 1884; Williston, 1897
Genera
See text.
Plioplatecarpinae is a subfamily of mosasaurs, a diverse group of late Cretaceous marine squamates.
Russell (1967, pp.
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Tylosaurinae
Williston, 1895
Genera
See text.
Tylosaurinae (Williston, 1895; Williston, 1897) is a subfamily of mosasaurs, a diverse group of Late Cretaceous marine squamates.
Russell (1967, pp.
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Williston, 1895
Genera
See text.
Tylosaurinae (Williston, 1895; Williston, 1897) is a subfamily of mosasaurs, a diverse group of Late Cretaceous marine squamates.
Russell (1967, pp.
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Latin}}}
Official status
Official language of: Vatican City
Used for official purposes, but not spoken in everyday speech
Regulated by: Opus Fundatum Latinitas
Roman Catholic Church
Language codes
ISO 639-1: la
ISO 639-2: lat
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Official status
Official language of: Vatican City
Used for official purposes, but not spoken in everyday speech
Regulated by: Opus Fundatum Latinitas
Roman Catholic Church
Language codes
ISO 639-1: la
ISO 639-2: lat
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Origin France
Mouth Hollands Diep
Basin countries France, Belgium, Netherlands
Length 925 km (575 mi)
Source elevation 409 m (1,342 ft)
Avg.
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Mouth Hollands Diep
Basin countries France, Belgium, Netherlands
Length 925 km (575 mi)
Source elevation 409 m (1,342 ft)
Avg.
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Ancient Greek refers to the second stage in the history of the Greek language[1] as it existed during the Archaic (9th–6th centuries BC) and Classical (5th–4th centuries BC) periods in Greece.
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Sauropsida*
Goodrich, 1916
Subclasses
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Goodrich, 1916
Subclasses
- Anapsida
- Diapsida
- Reptilia Laurenti, 1768
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Serpentes
Linnaeus, 1758
Infraorders and Families
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Linnaeus, 1758
Infraorders and Families
- Alethinophidia - Nopcsa, 1923
- Acrochordidae- Bonaparte, 1831
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Dinosauria *
Owen, 1842
Orders & Suborders
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Owen, 1842
Orders & Suborders
- Ornithischia
- Cerapoda
- Thyreophora
- Saurischia
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Lepidosauria
Orders
The Lepidosauria are reptiles with overlapping scales. They include the tuataras, lizards, snakes and amphisbaenians. Lepidosaurians are the most successful of modern reptiles.
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Orders
- Sphenodontia
- Squamata
The Lepidosauria are reptiles with overlapping scales. They include the tuataras, lizards, snakes and amphisbaenians. Lepidosaurians are the most successful of modern reptiles.
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Squamata
Oppel, 1811
Suborders
see text
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Oppel, 1811
black: range of Squamata
Suborders
see text
- This article is about the Squamata order of reptiles. For the Roman scale armour see: Lorica squamata.
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Aigialosauridae
Genera
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Genera
- Aigialosaurus
- Carsosaurus
- Mesoleptos
- Opetiosaurus
- Proaigialosaurus
- Coniasaurus
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Varanidae
Genus: Varanus
Merrem, 1820
Species
Many, see text.
Monitor lizards are the family Varanidae
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Genus: Varanus
Merrem, 1820
Species
Many, see text.
Monitor lizards are the family Varanidae
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The Cretaceous Period is one of the major divisions of the geologic timescale, reaching from the end of the Jurassic Period (i.e. from 145.5 ± 4.0 million years ago (Ma)) to the beginning of the Paleocene epoch of the Tertiary Period (about 65.5 ± 0.3 Ma).
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A geologic period is a subdivision of geologic time that divides an era into smaller timeframes. The equivalent term used to demarcate rock layers and the fossil record is the system; thus the rocks of the Devonian System were laid down during the Devonian Period.
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The Turonian is a stage of the Late Cretaceous Epoch. It spans the time between 93.5 ± 0.8 Ma and 89.3 ± 1 Ma (million years ago).
The Turonien was definied by the French paleontologist Alcide d'Orbigny (1802 - 1857), who named it after the city of Tours in the French
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The Turonien was definied by the French paleontologist Alcide d'Orbigny (1802 - 1857), who named it after the city of Tours in the French
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The Maastrichtian is the last stage of the Cretaceous period, and therefore of the Mesozoic era. It spanned from 70.6 ± 0.6 Ma to 65.5 ± 0.3 Ma (million years ago).
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Herod_Archelaus