Heptasteornis Andrewsi
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Heptasteornis Andrewsi
''Heptasteornis'' is the name given to a potentially dubious genus of alvarezsaurid dinosaur from the Late Cretaceous. The type (and only known) species is ''Heptasteornis andrewsi'', described as a presumed gigantic prehistoric owl in 1975. It was previously included in ''Elopteryx nopcsai'' and indeed the holotypes of both were believed to be from the same individual as they were discovered, and initially were assigned the same specimen number. This appears to be in error however (see below).Harrison & Walker (1975) The material was discovered in Romania by Franz Nopcsa, in the late Maastrichtian Sânpetru Formation ( Rognacian faunal stage, deposited c. 68 - 66 million years ago) of the Haţeg Basin in Transylvania. The scientific name means "C.W. Andrews' Transylvanian bird", after the namer of ''Elopteryx'', and Ancient Greek ''hepta'' (ἑπτά) "seven" + ''asty'' (άστυ) "city" + ''ornis'' (όρνις) "bird"; the Latin ''septum urbium'' or the German ''Siebenbürgen ...
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Maastrichtian
The Maastrichtian () is, in the ICS geologic timescale, the latest age (uppermost stage) of the Late Cretaceous Epoch or Upper Cretaceous Series, the Cretaceous Period or System, and of the Mesozoic Era or Erathem. It spanned the interval from . The Maastrichtian was preceded by the Campanian and succeeded by the Danian (part of the Paleogene and Paleocene). The Cretaceous–Paleogene extinction event (formerly known as the Cretaceous–Tertiary extinction event) occurred at the end of this age. In this mass extinction, many commonly recognized groups such as non-avian dinosaurs, plesiosaurs and mosasaurs, as well as many other lesser-known groups, died out. The cause of the extinction is most commonly linked to an asteroid about wide colliding with Earth, ending the Cretaceous. Stratigraphic definitions Definition The Maastrichtian was introduced into scientific literature by Belgian geologist André Hubert Dumont in 1849, after studying rock strata of the Chalk Group c ...
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