HOME





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. ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Chaeteessa
''Chaeteessa'' is a genus of mantis. It is the only extant member the family Chaeteessidae, 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 ''Chaeteessa valida'' is a species of praying mantis in 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 primitiv ...'' References Mantodea genera Taxa named by Hermann Burmeister {{Mantodea-stub ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Ypresian
In the geologic timescale the Ypresian is the oldest age or lowest stratigraphic stage of the Eocene. It spans the time between , is preceded by the Thanetian Age (part of the Paleocene) and is followed by the Eocene Lutetian Age. The Ypresian is consistent with the lower Eocene. Events The Ypresian Age begins during the throes of the Paleocene–Eocene Thermal Maximum (PETM). The Fur Formation in Denmark, the Messel shales in Germany, the Oise amber of France and Cambay amber of India are of this age. The Eocene Okanagan Highlands are an uplands subtropical to temperate series of lakes from the Ypresian. Stratigraphic definition The Ypresian Stage was introduced in scientific literature by Belgian geologist André Hubert Dumont in 1850. The Ypresian is named after the Flemish city of Ypres in Belgium (spelled ''Ieper'' in Dutch). The definitions of the original stage were totally different from the modern ones. The Ypresian shares its name with the Belgian Ieper Group (French: ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Oise Amber
Oise ( ; ; pcd, Oése) is a departments of France, department in the north of France. It is named after the river Oise (river), Oise. Inhabitants of the department are called ''Oisiens'' () or ''Isariens'', after the Latin name for the river, Isara. It had a population of 829,419 in 2019.Populations légales 2019: 60 Oise
INSEE


History

Oise is one of the original 83 departments created during the French Revolution on March 4, 1790. It was created from part of the provinces of France, province of Île-de-France and Picardy. After the coalition victory at Battle of Waterloo, Waterloo, the department was occupied by Great Britain, British British army, troops between June 1815 and November 1818. In March 2021, local Member of Parliament (France), Member of Parliament Olivier Da ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Primorsky Krai
Primorsky Krai (russian: Приморский край, r=Primorsky kray, p=prʲɪˈmorskʲɪj kraj), informally known as Primorye (, ), is a federal subject (a krai) of Russia, located in the Far East region of the country and is a part of the Far Eastern Federal District. The city of Vladivostok is the administrative center of the krai, and the second largest city in the Russian Far East, after Khabarovsk. The krai has the largest economy among the federal subjects in the Russian Far East, and a population of 1,956,497 as of the 2010 Census. The krai shares Russia's only border with North Korea, along the Tumen River in Khasansky District in the southwestern corner of the krai. Peter the Great Gulf, the largest gulf in the Sea of Japan, is located along the south coast. Historically part of Manchuria, Primorsky Krai was ceded to the Russian Empire by Qing China in 1860 as part of a region known as Outer Manchuria, forming most of the territory of Primorskay ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Eocene
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic 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 13C in the atmosphere was exceptionally low in comparison with the more common isotope 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 Siberia and in what is now Chesapeake Bay. As with other geologic periods, the strata that define the start and e ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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-dwelli ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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