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Microphysidae
The Microphysidae are a very small family of bugs, comprising only 5 extant genera. Systematics Until recently, many authors considered these bugs to belong within the family Anthocoridae. The following genera belong to this family: Subfamily Microphysinae * Genus '' Chinaola'' Blatchley * Genus '' Loricula'' Curtis (= ''Microphysa'') * Genus '' Mallochiola'' Bergroth * Genus '' Myrmedobia'' Bärensprung * Genus †'' Myrmericula'' Popov * Genus †'' Popovophysa'' McKellar & Engel 2011, Canadian amber, Campanian * Genus †'' Tytthophysa'' Popov & Herczek 2009 Baltic amber, 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'', ... *Subfamily Ciorullinae * Genus '' Ciorulla'' Péricart Cimicomorpha Heteroptera families {{Cimicomorpha-stub ...
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Loricula
''Loricula'' is a genus of minute bladder bugs in the family Microphysidae The Microphysidae are a very small family of bugs, comprising only 5 extant genera. Systematics Until recently, many authors considered these bugs to belong within the family Anthocoridae. The following genera belong to this family: Subfamil .... There are more than 20 described species in ''Loricula''. Species These 25 species belong to the genus ''Loricula'': * '' Loricula bedeli'' (Montandon, 1887) * '' Loricula bipunctata'' (Perris, 1857) * '' Loricula blascoi'' Ribes & Pericart, 1996 * '' Loricula distinguenda'' Reuter, 1884 * '' Loricula elegantula'' (Bärensprung, 1858) * '' Loricula freyi'' (Lindberg, 1932) * '' Loricula hispanica'' Pericart, 1972 * '' Loricula jakovlevi'' Pericart, 1969 * '' Loricula josifovi'' Simov, 2008 * '' Loricula lundbladi'' China, 1938 * '' Loricula meinanderi'' Pericart, 1972 * '' Loricula pselaphiformis'' Curtis, 1833 * '' Loricula ruficeps'' (Reuter, 1884) * '' ...
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Microphysidae
The Microphysidae are a very small family of bugs, comprising only 5 extant genera. Systematics Until recently, many authors considered these bugs to belong within the family Anthocoridae. The following genera belong to this family: Subfamily Microphysinae * Genus '' Chinaola'' Blatchley * Genus '' Loricula'' Curtis (= ''Microphysa'') * Genus '' Mallochiola'' Bergroth * Genus '' Myrmedobia'' Bärensprung * Genus †'' Myrmericula'' Popov * Genus †'' Popovophysa'' McKellar & Engel 2011, Canadian amber, Campanian * Genus †'' Tytthophysa'' Popov & Herczek 2009 Baltic amber, 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'', ... *Subfamily Ciorullinae * Genus '' Ciorulla'' Péricart Cimicomorpha Heteroptera families {{Cimicomorpha-stub ...
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Mallochiola
''Mallochiola'' is a genus of minute bladder bugs in the family Microphysidae The Microphysidae are a very small family of bugs, comprising only 5 extant genera. Systematics Until recently, many authors considered these bugs to belong within the family Anthocoridae. The following genera belong to this family: Subfamil .... There is one described species in ''Mallochiola'', ''M. gagates''. References Further reading * * Cimicomorpha genera Articles created by Qbugbot Microphysidae {{Cimicomorpha-stub ...
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Myrmedobia
''Myrmedobia'' is a genus of minute bladder bugs in the family Microphysidae The Microphysidae are a very small family of bugs, comprising only 5 extant genera. Systematics Until recently, many authors considered these bugs to belong within the family Anthocoridae. The following genera belong to this family: Subfamil .... There are about five described species in ''Myrmedobia''. Species These five species belong to the genus ''Myrmedobia'': * '' Myrmedobia coleoptrata'' (Fallén, 1807) * '' Myrmedobia distinguenda'' Reuter, 1884 * '' Myrmedobia exilis'' (Fallén, 1807) * '' Myrmedobia inconspicua'' (Douglas & Scott, 1871) * † '' Loricula pericarti'' Popov, 2004 References Further reading * * Cimicomorpha genera Articles created by Qbugbot Microphysidae {{Cimicomorpha-stub ...
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Cimicomorpha
The Cimicomorpha are an infraorder of insects in the order Hemiptera, the true bugs. The rostrum and other morphology of all members apparently is adapted to feeding on animals as their prey or hosts. Members include bed bugs, bat bugs, assassin bugs, and pirate bugs. The two infraorders Cimicomorpha and Pentatomorpha have very similar characteristics, possibly as a result of the evolution of plant feeding. The key similarity that unites the Cimicomorpha and Pentatomorpha is the loss of the arolia (adhesive pads) on the pretarsi of the insects. These two infraorders comprise 90% of Heteroptera species. These insects are a part of the old, informal classification of “Geocorisae” (land bugs). Among these bugs, parental care has evolved several times. Parental care varies from brooding of the eggs by the female, to a more active form that involves protection of young against predators and the female covering the nymphs under her body. Superfamilies and families ''BioLib ...
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Canadian Amber
Canadians (french: Canadiens) are people identified with the country of Canada. This connection may be residential, legal, historical or cultural. For most Canadians, many (or all) of these connections exist and are collectively the source of their being ''Canadian''. Canada is a multilingual and multicultural society home to people of groups of many different ethnic, religious, and national origins, with the majority of the population made up of Old World immigrants and their descendants. Following the initial period of French and then the much larger British colonization, different waves (or peaks) of immigration and settlement of non-indigenous peoples took place over the course of nearly two centuries and continue today. Elements of Indigenous, French, British, and more recent immigrant customs, languages, and religions have combined to form the culture of Canada, and thus a Canadian identity. Canada has also been strongly influenced by its linguistic, geographic, and e ...
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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 ...
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Baltic Amber
The Baltic region is home to the largest known deposit of amber, called Baltic amber or succinite. It was produced sometime during the Eocene epoch, but exactly when is controversial. It has been estimated that these forests created more than 100,000 tons of amber. Today, more than 90% of the world's amber comes from Kaliningrad Oblast of Russia. It is a major source of income for the region; the local Kaliningrad Amber Combine extracted 250 tonnes of it in 2014, 400 tonnes in 2015. "Baltic amber" was formerly thought to include amber from the Bitterfeld brown coal mines in Saxony (Eastern Germany). Bitterfeld amber was previously believed to be only 20–22 million years old (Miocene), but a comparison of the animal inclusions in 2003 suggested that it was possibly Baltic amber that was redeposited in a Miocene deposit. Further study of insect taxa in the ambers has shown Bitterfeld amber to be from the same forest as the Baltic amber forest, but separately deposited from a ...
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Campanian
The Campanian is the fifth of six ages of the Late Cretaceous Epoch on the geologic timescale of the International Commission on Stratigraphy (ICS). In chronostratigraphy, it is the fifth of six stages in the Upper Cretaceous Series. Campanian spans the time from 83.6 (± 0.2) to 72.1 (± 0.2) million years ago. It is preceded by the Santonian and it is followed by the Maastrichtian. The Campanian was an age when a worldwide sea level rise covered many coastal areas. The morphology of some of these areas has been preserved: it is an unconformity beneath a cover of marine sedimentary rocks. Etymology The Campanian was introduced in scientific literature by Henri Coquand in 1857. It is named after the French village of Champagne in the department of Charente-Maritime. The original type locality was a series of outcrop near the village of Aubeterre-sur-Dronne in the same region. Definition The base of the Campanian Stage is defined as a place in the stratigraphic colu ...
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