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Chaeteessidae
Chaeteessidae is a family of praying mantises. It contains a single extant genus, '' Chaeteessa'', native to South America which is thought to be the most primitive and earliest diverging lineage of living mantises. Fossil genera are known from the Paleogene of Eurasia and North America. Fossil genera * †'' Arvernineura'' Piton 1940 Menat Formation, France, Paleocene (Selandian) * †'' Louispitonia'' Schubnel and Nel 2019 (=''Archaeophlebia'' Piton 1940) Menat Formation, France, Paleocene (Selandian) * †'' Lithophotina'' Cockerell 1908 Florissant Formation, Colorado, United States, Eocene * †'' Megaphotina'' Gratshev and Zherikhin 1993 Bol'shaya Svetlovodnaya, Primorsky, Russia, Eocene Indeterminate species are also known from French Oise amber, dating to the Eocene (Ypresian) See also *List of mantis genera and species The following list of mantis genera and species is based on the "Mantodea Species File", which is the primary reference for the taxonomy shown here. ...
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Mantodea
Mantises are an order (Mantodea) of insects that contains over 2,400 species in about 460 genera in 33 families. The largest family is the Mantidae ("mantids"). Mantises are distributed worldwide in temperate and tropical habitats. They have triangular heads with bulging eyes supported on flexible necks. Their elongated bodies may or may not have wings, but all Mantodea have forelegs that are greatly enlarged and adapted for catching and gripping prey; their upright posture, while remaining stationary with forearms folded, has led to the common name praying mantis. The closest relatives of mantises are termites and cockroaches (Blattodea), which are all within the superorder Dictyoptera. Mantises are sometimes confused with stick insects (Phasmatodea), other elongated insects such as grasshoppers (Orthoptera), or other more distantly related insects with raptorial forelegs such as mantisflies (Mantispidae). Mantises are mostly ambush predators, but a few ground-dwelling spe ...
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Praying Mantis
Mantises are an order (Mantodea) of insects that contains over 2,400 species in about 460 genera in 33 families. The largest family is the Mantidae ("mantids"). Mantises are distributed worldwide in temperate and tropical habitats. They have triangular heads with bulging eyes supported on flexible necks. Their elongated bodies may or may not have wings, but all Mantodea have forelegs that are greatly enlarged and adapted for catching and gripping prey; their upright posture, while remaining stationary with forearms folded, has led to the common name praying mantis. The closest relatives of mantises are termites and cockroaches (Blattodea), which are all within the superorder Dictyoptera. Mantises are sometimes confused with stick insects ( Phasmatodea), other elongated insects such as grasshoppers (Orthoptera), or other more distantly related insects with raptorial forelegs such as mantisflies (Mantispidae). Mantises are mostly ambush predators, but a few ground-dwelling s ...
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List Of Mantis Genera And Species
The following list of mantis genera and species is based on the "Mantodea Species File", which is the primary reference for the taxonomy shown here. The insect Order (biology), order Mantodea consists of over 2,400 species of mantises in about 460 genus, genera. 75 of these genera are in the Family (biology), family Mantidae (the mantids), which formerly was sole family recognized within the order. In some cases, common names in the English language are loosely applied to several different members of a particular genus, or even for species in various genera. For example, "giant Asian mantis" is used for various members of ''Hierodula'', "dead leaf mantis" may refer not only to various species of ''Deroplatys'', but to all brown mantises that use leaf mimicry for camouflage. "flower mantis" refers to numerous mantises, especially those belonging to or similar to those of genus ''Creobroter'', and so on. ---For citation of common nomenclature and additional references, see individua ...
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Chaeteessa
''Chaeteessa'' is a genus of mantis. It is the only extant member the family Chaeteessidae Chaeteessidae is a family of praying mantises. It contains a single extant genus, '' Chaeteessa'', native to South America which is thought to be the most primitive and earliest diverging lineage of living mantises. Fossil genera are known from th ..., which is the most primitive lineage of living mantises. It contains six species found in South America: Species *'' Chaeteessa burmeisteri'' *'' Chaeteessa caudata'' *'' Chaeteessa filata'' *'' Chaeteessa nana'' *'' Chaeteessa nigromarginata'' *'' Chaeteessa valida'' References Mantodea genera Taxa named by Hermann Burmeister {{Mantodea-stub ...
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Menat Formation
The Menat Formation is a geologic formation in France. It preserves fossils dating back to the Paleocene. It is a maar deposit located on top of an ancient volcano, the extent is very localised with the outcropping area being around 600 by 1000 metres. Numerous species of fossil insects, plants and fish are known, as well as some isolated mammals, including the primate '' Plesiadapis insignis'', the choristodere reptile ''Lazarussuchus'', and birds, including members of Halcyornithidae and Messelasturidae Messelasturidae is an extinct family of birds known from the Eocene of North America and Europe. Their morphology is a mosiac that in some aspects are strongly convergent with modern hawks and falcons, but in others are more similar to parrots. ... and relatives of Songziidae. See also * List of fossiliferous stratigraphic units in France References * Paleogene France {{Paleogene-stub ...
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Paleocene
The Paleocene, ( ) or Palaeocene, is a geological epoch (geology), epoch that lasted from about 66 to 56 mya (unit), million years ago (mya). It is the first epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name is a combination of the Ancient Greek ''palaiós'' meaning "old" and the Eocene Epoch (which succeeds the Paleocene), translating to "the old part of the Eocene". The epoch is bracketed by two major events in Earth's history. The K–Pg extinction event, brought on by Chicxulub impact, an asteroid impact and possibly volcanism, marked the beginning of the Paleocene and killed off 75% of living species, most famously the non-avian dinosaurs. The end of the epoch was marked by the Paleocene–Eocene Thermal Maximum (PETM), which was a major climatic event wherein about 2,500–4,500 gigatons of carbon were released into the atmosphere and ocean systems, causing a spike in global temperatures and ocean acidification. In the Pal ...
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Selandian
The Selandian is a stage in the Paleocene. It spans the time between . It is preceded by the Danian and followed by the Thanetian. Sometimes the Paleocene is subdivided in subepochs, in which the Selandian forms the "middle Paleocene". Stratigraphic definition The Selandian was introduced in scientific literature by Danish geologist Alfred Rosenkrantz in 1924. It is named after the Danish island of Zealand (Danish: ''Sjælland'') given its prevalence there.Selandien
The base of the Selandian is close to the boundary between

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Florissant Formation
The Florissant Formation is a sedimentary geologic formation outcropping around Florissant, Teller County, Colorado. The formation is noted for the abundant and exceptionally preserved insect and plant fossils that are found in the mudstones and shales. Based on argon radiometric dating, the formation is Eocene (approximately 34 million years old ) in age and has been interpreted as a lake environment. The fossils have been preserved because of the interaction of the volcanic ash from the nearby Thirtynine Mile volcanic field with diatoms in the lake, causing a diatom bloom. As the diatoms fell to the bottom of the lake, any plants or animals that had recently died were preserved by the diatom falls. Fine layers of clays and muds interspersed with layers of ash form "paper shales" holding beautifully-preserved fossils. The Florissant Fossil Beds National Monument is a national monument established to preserve and study the geology and history of the area. History The name ''Fl ...
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Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope Carbon-13, 13C in the atmosphere was exceptionally low in comparison with the more common isotope Carbon-12, 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Popigai impact structure, Siberia and in what is now ...
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