Dascillidae
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Dascillidae
Dascillidae is a family of beetles within the clade Elateriformia. There are about 100 extant species in 11 genera, which are found worldwide. Dascillidae together with Rhipiceridae form the super family Dascilloidea. Taxonomy The family was named by Guérin-Méneville, Guérin Méneville in 1843. The family is divided up into two poorly defined subfamilies Karumiinae, and Dascillinae. Description Adult Dascillidae are 4.5–25 mm long with an elongate body that is somewhat convex in cross-section. They are covered in dense grey/brown hairs. Karumiines have highly modified soft-bodies, similar to some members of Elateroidea. Ecology The adults can be found on grass during the springtime. The larvae occur in moist soil or under rocks. The larvae are thought to feed on roots or decaying plant matter. Some karumiines like ''Karumia'' are associated with termites. Genera * ''Anorus'' * ''Dascillus'' * ''Karumia'' * ''Notodascillus'' * ''Coptocera'' Murray * ''Metallid ...
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Dascilloidea
Dascilloidea is a superfamily of polyphagan beetles, comprising two families Family (from la, familia) is a group of people related either by consanguinity (by recognized birth) or affinity (by marriage or other relationship). The purpose of the family is to maintain the well-being of its members and of society. Ideal ...: Dascillidae (soft bodied plant beetles) and Rhipiceridae (cicada beetle and cicada parasite beetles).bugguide.net-Dascilloidea
(Accessed 18 August 2007)


References

Elateriformia Beetle superfamilies
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Anorus
''Anorus'' is a genus of soft-bodied plant beetles in the family Dascillidae Dascillidae is a family of beetles within the clade Elateriformia. There are about 100 extant species in 11 genera, which are found worldwide. Dascillidae together with Rhipiceridae form the super family Dascilloidea. Taxonomy The family was na .... There are at least three described species in ''Anorus''. Species These three species belong to the genus ''Anorus'': * '' Anorus arizonicus'' Blaisdell, 1934 * '' Anorus parvicollis'' Horn, 1894 * '' Anorus piceus'' LeConte, 1859 References Further reading * * Polyphaga Articles created by Qbugbot {{polyphaga-stub ...
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Dascillus
''Dascillus'' is a genus of soft-bodied plant beetles in the family Dascillidae. There are more than 20 described species in ''Dascillus''. Species These 24 species belong to the genus ''Dascillus'': * ''Dascillus cervinus'' (Linnaeus, 1758) * '' Dascillus chifengi'' Jin, Ślipiński & Pang, 2013 * '' Dascillus congruus'' Pascoe, 1860 * '' Dascillus corporaali'' Pic, 1923 * '' Dascillus davidsoni'' (LeConte, 1859) * '' Dascillus elongatus'' Zhang, 1989 * '' Dascillus flatus'' Zhang, 1989 * '' Dascillus formosanus'' Jin, Ślipiński & Pang, 2013 * '' Dascillus lanceus'' Jin, Ślipiński & Pang, 2013 * '' Dascillus latahensis'' Lewis, 1973 * '' Dascillus lateralis'' Megerle * '' Dascillus levigatus'' Li, Ślipiński & Jin, 2017 * ''Dascillus liangshanensis'' * '' Dascillus lithographicus'' Wickham, 1911 * ''Dascillus malachiticus'' Knoch * ''Dascillus musculus'' Zhang & al., 1994 * ''Dascillus plumbeus'' (Horn, 1880) * ''Dascillus relictus'' Zhang, 1989 * ''Dascillus shandongianus ...
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Rhipiceridae
Rhipiceridae is a family of beetles found worldwide. The larva of rhipicerids are parasitoids of cicada nymphs. Rhipiceridae and Dascillidae form the super family Dascilloidea, within the Elateriformia. Taxonomic History The taxonomic history of Rhipiceridae began with J. Fabricius who described ''Hispa mystacina'' in 1775, which was later included in the new genus ''Rhipicera'' by Latreille (1817) who rightly noticed that the Fabrician species did not belong to ''Hispa'' and placed it in the tribe ‘Cebrionites’ along with ''Cebrio'', ''Dascillus'' and ''Scirtes''. Since then W. Kirby, J. O. Westwood and others described several new species of ''Rhipicera'' from Australia and South America. Subfamilies and Distribution Rhipiceridae includes seven genera and about a hundred described species divided into two subfamilies, Rhipicerinae and Sandalinae. Sandalinae include most of the species and are known from North and South America, Africa, south-eastern Europe and Asia, whil ...
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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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Yixian Formation
The Yixian Formation (; formerly transcribed as Yihsien Formation) is a geological formation in Jinzhou, Liaoning, People's Republic of China, that spans the late Barremian and early Aptian stages of the Early Cretaceous. It is known for its exquisitely preserved fossils, and is mainly composed of basalts interspersed with siliciclastic sediments. History Japanese occupation The potential importance of the Yixian Formation was initially recognized during the time the Empire of Japan occupied China's Rehe ("Jehol") Province after the First battle of Hopei in 1933. Many Japanese scientists had noticed fossil remains of extinct fish and reptiles, possibly the champsosaurs. These initial fossil discoveries made by Japanese scientists vanished once World War II ended in 1945. Chinese rediscovery By 1949, when administration of the area passed to the Chinese Communist Party and its leader Mao Zedong, the fossils of Yixian were studied only by Chinese scientists. It was not unt ...
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Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ...
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Aptian
The Aptian is an age in the geologic timescale or a stage in the stratigraphic column. It is a subdivision of the Early or Lower Cretaceous Epoch or Series and encompasses the time from 121.4 ± 1.0 Ma to 113.0 ± 1.0 Ma (million years ago), approximately. The Aptian succeeds the Barremian and precedes the Albian, all part of the Lower/Early Cretaceous. The Aptian partly overlaps the upper part of the Western European Urgonian Stage. The Selli Event, also known as OAE1a, was one of two oceanic anoxic events in the Cretaceous Period, which occurred around 120 Ma and lasted approximately 1 to 1.3 million years. The Aptian extinction was a minor extinction event hypothesized to have occurred around 116 to 117 Ma.Archangelsky, Sergio.The Ticó Flora (Patagonia) and the Aptian Extinction Event" ''Acta Paleobotanica'' 41(2), 2001, pp. 115-22. Stratigraphic definitions The Aptian was named after the small city of Apt in the Provence region of France, which is also known for its cry ...
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