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Yuripopovinidae
Yuripopovinidae is an extinct family of Coreoidea Hemipteran true bugs. Member species are known from the Early Cretaceous and early Late Cretaceous of Asia and northern Gondwana. Among the distinguishing characters are "the hemelytral costal vein apically much thickened and pterostigma-like, the corium with two large cells separated by one longitudinal straight vein." Dehiscensicoridae, described from the Yixian Formation of China has been deemed a junior synonym of Yuripopovinidae per Du ''et al.'' (2019). The family was named after Russian paleoentomologist Yuri Alexandrovich Popov. Genera * †'' Caulisoculus'' Burmese amber, Myanmar, Cenomanian * †'' Changirostrus'' Yixian Formation, China, Aptian * †'' Crassiantenninus'' Yixian Formation, China, Aptian * †'' Dehiscensicoris'' Yixian Formation, China, Aptian * †'' Minuticoris'' Yixian Formation, China, Aptian * †'' Megaoptocoris'' Burmese amber, Myanmar, Cenomanian * †'' Pingquanicoris'' Yixian Formatio ...
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Coreoidea
Coreoidea is a superfamily of true bugs in the infraorder Pentatomomorpha which includes leaf-footed bugs and allies. There are more than 3,300 described species in Coreoidea. There are five extant families presently recognized, but the Coreoidea as a whole are part of a close-knit group with the Lygaeoidea and Pyrrhocoroidea and it is likely that these three superfamilies are paraphyletic to a significant extent; they are therefore in need of revision and redelimitation. The families are: * Alydidae Amyot & Serville, 1843 – broad-headed bugs * Coreidae Leach, 1815 – leaf-footed bugs and squash bugs * Hyocephalidae Bergroth, 1906 * Rhopalidae – scentless plant bugs * Stenocephalidae Amyot & Serville, 1843 * † Trisegmentatidae Zhang, Sun & Zhang, 1994 * † Yuripopovinidae Yuripopovinidae is an extinct family of Coreoidea Hemipteran true bugs. Member species are known from the Early Cretaceous and early Late Cretaceous of Asia and northern Gondwana. Among ...
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Yuri Alexandrovich Popov
Yuri Alexandrovich Popov (Russian: Юрий Александрович Попов) (5 March 1936 – 16 November 2016) was a Soviet and Russian paleoentomologist, an authority on the taxonomy and evolution of fossil true bugs ( Heteroptera) and Coleorrhyncha. He described more than 20 new families and subfamilies and 300 new genera and species from the Mesozoic and Cenozoic. He also was one of the founders of the modern higher classification of true bugs: three of seven heteropteran infraorders have been established by him ( Nepomorpha Popov, 1968, Gerromorpha Popov, 1971, and Leptopodomorpha Popov, 1971). He was the author of more than 170 publications, including a classic monograph on the evolution of water bugs. Selected publications *Popov, Yu.A. (1971) Historical development of true bugs of the infraorder Nepomorpha (Heteroptera). Trudy Paleontologicheskogo Instituta AN SSSR 129: 1–230 (in Russian). *Popov, Yu.A. & Shcherbakov, D.E. (1991) Mesozoic Peloridioidea and t ...
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Burmese Amber
Burmese amber, also known as Burmite or Kachin amber, is amber from the Hukawng Valley in northern Myanmar. The amber is dated to around 100 million years ago, during the latest Albian to earliest Cenomanian ages of the mid-Cretaceous period. The amber is of significant palaeontological interest due to the diversity of flora and fauna contained as inclusions, particularly arthropods including insects and arachnids but also birds, lizards, snakes, frogs and fragmentary dinosaur remains. The amber has been known and commercially exploited since the first century AD, and has been known to science since the mid-nineteenth century. Research on the deposit has attracted controversy due to its alleged role in funding internal conflict in Myanmar and hazardous working conditions in the mines where it is collected. Geological context, depositional environment and age The amber is found within the Hukawng Basin, a large Cretaceous-Cenozoic sedimentary basin within northern Myanmar. The s ...
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Late Cretaceous
The Late Cretaceous (100.5–66 Ma) is the younger of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', the Latin word for the white limestone known as chalk. The chalk of northern France and the white cliffs of south-eastern England date from the Cretaceous Period. Climate During the Late Cretaceous, the climate was warmer than present, although throughout the period a cooling trend is evident. The tropics became restricted to equatorial regions and northern latitudes experienced markedly more seasonal climatic conditions. Geography Due to plate tectonics, the Americas were gradually moving westward, causing the Atlantic Ocean to expand. The Western Interior Seaway divided North America into eastern and western halves; Appalachia and Laramidia. India maintained a northward course towards Asia. In the Southern Hemisphere, Australia and Ant ...
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