Schizopodidae
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Schizopodidae
Schizopodidae is a family of beetles, in the large suborder Polyphaga. It was a subfamily until 1991, when it was elevated to family status. The family of Schizopodidae is a part of the superfamily, Buprestoidea, which is a member of the suborder of polyphaga beetles, defined by the coxa not being fused to the thorax. Buprestoidea contains bullet-shaped beetles, known for their distinctive metallic colors. Little is known about Schizopodidae, but the adults are often found clinging to plants. The family contains the following genera: * '' Dystaxia'' LeConte, 1866 * †'' Electrapate'' Iablokoff-Khnzorian, 1962 Baltic amber, Eocene * '' Glyptoscelimorpha'' Horn, 1893 * †'' Mesoschizopus'' Cai et al., 2015Cai, C., Ślipiński, A., & Huang, D. (2015). First false jewel beetle (Coleoptera: Schizopodidae) from the Lower Cretaceous of China. ''Cretaceous Research'' 52, 490-94. Yixian Formation, China, Early Cretaceous (Aptian The Aptian is an age in the geologic timescale or a ...
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Schizopodidae
Schizopodidae is a family of beetles, in the large suborder Polyphaga. It was a subfamily until 1991, when it was elevated to family status. The family of Schizopodidae is a part of the superfamily, Buprestoidea, which is a member of the suborder of polyphaga beetles, defined by the coxa not being fused to the thorax. Buprestoidea contains bullet-shaped beetles, known for their distinctive metallic colors. Little is known about Schizopodidae, but the adults are often found clinging to plants. The family contains the following genera: * '' Dystaxia'' LeConte, 1866 * †'' Electrapate'' Iablokoff-Khnzorian, 1962 Baltic amber, Eocene * '' Glyptoscelimorpha'' Horn, 1893 * †'' Mesoschizopus'' Cai et al., 2015Cai, C., Ślipiński, A., & Huang, D. (2015). First false jewel beetle (Coleoptera: Schizopodidae) from the Lower Cretaceous of China. ''Cretaceous Research'' 52, 490-94. Yixian Formation, China, Early Cretaceous (Aptian The Aptian is an age in the geologic timescale or a ...
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Electrapate
''Electrapate martynovi'' is an extinct species of beetles in the family Schizopodidae Schizopodidae is a family of beetles, in the large suborder Polyphaga. It was a subfamily until 1991, when it was elevated to family status. The family of Schizopodidae is a part of the superfamily, Buprestoidea, which is a member of the suborde ..., the only species in the genus ''Electrapate''. References Schizopodidae † † {{Schizopodidae-stub ...
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Dystaxia (beetle)
''Dystaxia'' is a genus of beetles in the family Schizopodidae Schizopodidae is a family of beetles, in the large suborder Polyphaga. It was a subfamily until 1991, when it was elevated to family status. The family of Schizopodidae is a part of the superfamily, Buprestoidea, which is a member of the suborde ..., containing the following species: * '' Dystaxia elegans'' Fall, 1905 * '' Dystaxia murrayi'' LeConte, 1866 References Schizopodidae Buprestoidea genera {{Schizopodidae-stub ...
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Glyptoscelimorpha
''Glyptoscelimorpha'' is a genus of beetles in the family Schizopodidae Schizopodidae is a family of beetles, in the large suborder Polyphaga. It was a subfamily until 1991, when it was elevated to family status. The family of Schizopodidae is a part of the superfamily, Buprestoidea, which is a member of the suborde ..., containing the following species: * '' Glyptoscelimorpha juniperae'' (Knull, 1940) * '' Glyptoscelimorpha marmorata'' Horn, 1893 * '' Glyptoscelimorpha viridis'' Chamberlin, 1931 References Schizopodidae Buprestoidea genera {{Schizopodidae-stub ...
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Schizopus
''Schizopus'' is a genus of beetles in the family Schizopodidae Schizopodidae is a family of beetles, in the large suborder Polyphaga. It was a subfamily until 1991, when it was elevated to family status. The family of Schizopodidae is a part of the superfamily, Buprestoidea, which is a member of the suborde ..., containing the following species: * '' Schizopus laetus'' LeConte, 1858 * '' Schizopus sallei'' Horn, 1885 References Schizopodidae Buprestoidea genera {{Schizopodidae-stub ...
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Beetle
Beetles are insects that form the order Coleoptera (), in the superorder Endopterygota. Their front pair of wings are hardened into wing-cases, elytra, distinguishing them from most other insects. The Coleoptera, with about 400,000 described species, is the largest of all orders, constituting almost 40% of described insects and 25% of all known animal life-forms; new species are discovered frequently, with estimates suggesting that there are between 0.9 and 2.1 million total species. Found in almost every habitat except the sea and the polar regions, they interact with their ecosystems in several ways: beetles often feed on plants and fungi, break down animal and plant debris, and eat other invertebrates. Some species are serious agricultural pests, such as the Colorado potato beetle, while others such as Coccinellidae (ladybirds or ladybugs) eat aphids, scale insects, thrips, and other plant-sucking insects that damage crops. Beetles typically have a particularly hard e ...
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Polyphaga
Polyphaga is the largest and most diverse suborder of beetles. It comprises 144 families in 16 superfamilies, and displays an enormous variety of specialization and adaptation, with over 350,000 described species, or approximately 90% of the beetle species so far discovered. Key characteristics of Polyphaga are that the hind coxa (base of the leg) does not divide the first and second abdominal/ventral plates which are known as sternites. Also, the notopleural suture (found under the pronotal shield) is not present. Etymology The name of ''polyphaga'' is derived from two Greek words: , meaning 'many', and , meaning 'to eat', so the suborder is called the “eaters of many things”. Classification The five main infraorders are: * Bostrichiformia — including furniture beetles and skin beetles * Cucujiformia — includes lady beetles, longhorn beetles, weevils, checkered beetles and leaf beetles * Elateriformia — includes click beetles and fireflies * Scarabaeiformia — ...
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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 Lignite, 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 f ...
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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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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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