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Prosyntexis
''Prosyntexis'' is an extinct genus of stem sawflies in the family Sepulcidae. There are at least four described species in ''Prosyntexis''. The species ''Prosyntexis okhotensis'' and ''Prosyntexis gobiensis'' were formerly included in the genus '' Trematothorax''. Species These four species belong to the genus ''Prosyntexis'': * †''Prosyntexis gobiensis'' (Rasnitsyn, 1993) - Dzun-Bain Formation, Aptian * †''Prosyntexis gouleti'' Sharkey, 1990 - Crato Formation, Aptian * †''Prosyntexis montsecensis'' Rasnitsyn & Ansorge, 2000 La Pedrera de Rúbies Formation, Barremian * †''Prosyntexis okhotensis'' (Rasnitsyn, 1993) - Ola Formation, 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 s ... References Sawflies {{cretaceous-insect-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
La Pedrera De Rúbies Formation
The La Pedrera de Rúbies Formation is an Early Cretaceous ( late Berriasian to early Barremian geologic formation in Catalonia, Spain. The formation crops out in the area of the Montsec in the Organyà Basin. At the La Pedrera de Meià locality, the formation consists of rhythmically laminated, lithographic limestones that formed in the distal areas of a large, shallow coastal lake. It is noted for the exceptional preservation of articulated small vertebrates and insects, similar to that of the Solnhofen Limestone. Fossil content The La Pedrera de Rúbies Formation has yielded the enantiornithine bird '' Noguerornis'' and the scincogekkomorph lizard '' Pedrerasaurus'',Weishampel et al., 2004, pp. 517-607 and two species of Teiid lizard ''Meyasaurus'', ''M. fauri'' and ''M. crusafonti,'' the indeterminate avialan '' Ilerdopteryx'',Kellner, 2002 frogs '' Neusibatrachus wilferti'',Báez & Sanchiz, 2007, p.477 and '' Montsechobatrachus''. A crocodyliform ''Montsecosuchus'' and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sepulcidae
Sepulcidae is an extinct family of stem sawflies in the order Hymenoptera. The family is known primarily from late Mesozoic fossils found in 1968 in Transbaikalia. The insects were distant relatives of modern sawflies and are part of the living superfamily Cephoidea. The genus '' Sepulca'' was identified by Alexandr Pavlovich Rasnitsyn. It was named by his colleague and a science-fiction author Kirill Eskov after fictional entities called '' sepulki'', found in Stanisław Lem's ''The Star Diaries'' and '' Observation on the Spot''. The relation to Lem's ''sepulki'' is understandable in both Polish and Russian, but their English translation obscures their association with ancient insects as they are translated as ''Scrupts'' in English editions of Lem's novels. Genera These 17 genera belong to the family Sepulcidae: * Subfamily Sepulcinae Rasnitsyn, 1968 ** †'' Sepulca'' Rasnitsyn, 1968 ** †'' Sepulenia'' Rasnitsyn, 1968 * Subfamily Parapamphiliinae Rasnitsyn, 1968 ** †... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crato Formation
The Crato Formation is a geologic formation of Early Cretaceous ( Aptian) age in northeastern Brazil's Araripe Basin. It is an important Lagerstätte (undisturbed fossil accumulation) for palaeontologists. The strata were laid down mostly during the Aptian age, about 113 million years ago. It thought to have been deposited in a semi-arid lacustrine wetland environment.Ribeiro et al., 2021 The Crato Formation earns the designation of Lagerstätte due to an exceedingly well preserved and diverse fossil faunal assemblage. Some 25 species of fossil fishes are often found with stomach contents preserved, enabling paleontologists to study predator-prey relationships in this ecosystem. There are also fine examples of pterosaurs, reptiles and amphibians, invertebrates (particularly insects), and plants. Even dinosaurs are represented: a new maniraptor was described in 1996. The unusual taphonomy of the site resulted in limestone accretions that formed nodules around dead organisms, pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barremian
The Barremian is an age in the geologic timescale (or a chronostratigraphic stage) between 129.4 ± 1.5 Ma (million years ago) and 121.4 ± 1.0 Ma). It is a subdivision of the Early Cretaceous Epoch (or Lower Cretaceous Series). It is preceded by the Hauterivian and followed by the Aptian Stage.See Gradstein ''et al.'' (2004) or the online geowhen database (link below) Stratigraphic definitions The original type locality for the Barremian Stage is in the vicinity of the village of Barrême, Alpes-de-Haute-Provence, France. Henri Coquand defined the stage and named it in 1873. The base of the Barremian is determined by the first appearance of the ammonites ''Spitidiscus hugii'' and ''Spitidiscus vandeckii''. The end of the Barremian is determined by the geomagnetic reversal at the start of the M0r chronozone, which is biologically near the first appearance of the ammonite '' Paradeshayesites oglanlensis''. Regional equivalents The Barremian falls in the Gallic epoch, a su ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ola Formation
Ola may refer to: Places Panama *Olá, a subdistrict in Coclé Province * Olá District Russia * Ola, Russia, an urban settlement in Magadan Oblast * Ola District, an administrative division in Magadan Oblast * Ola (river), a river in Magadan Oblast United States *Ola, Arkansas, a city *Ola, Georgia, an unincorporated community *Ola, Idaho, an unincorporated community *Ola, South Dakota, a census-designated place *Ola, Kaufman County, Texas, an unincorporated community *Casa Linda Estates, Dallas, formerly known as Ola People * Ola (given name), a list of men and women with the name * Ola (surname), a list of men and women with the surname * Ola Svensson (born 1986), also known by the mononym Ola, Swedish singer-songwriter * Ola Nordmann, a national personification of Norwegians * Ola people, another name for the ''Wurla'', an indigenous people of Western Australia Other uses *Ola High School (other), the name of several high schools * Ola Cabs, an Indian online cab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 column wher ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
