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Pinophilini
Pinophilini is a tribe of rove beetles in the family Staphylinidae. Genera These genera belong to the tribe Pinophilini: * ''Lathropinus'' Sharp, 1866 * ''Mimopinophilus'' Coiffait, 1978 * ''Oedichirus'' Erichson, 1839 * ''Palaminus'' Erichson, 1839 * ''Pinophilus'' Gravenhorst, 1802 * ''Procirrus'' Latreille, 1829 c g *†''Cretoprocirrus'' Shaw et al., 2020 Burmese amber, Myanmar, Cenomanian Data sources: i = ITIS, c = Catalogue of Life, g = GBIF, b = Bugguide.net References Further reading * * * * * * * * * * * * * * External links * Paederinae {{staphylinidae-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rove Beetle
The rove beetles are a family (Staphylinidae) of beetles, primarily distinguished by their short elytra (wing covers) that typically leave more than half of their abdominal segments exposed. With roughly 63,000 species in thousands of genera, the group is currently recognized as the largest extant family of organisms. It is an ancient group, with fossilized rove beetles known from the Triassic, 200 million years ago, and possibly even earlier if the genus ''Leehermania'' proves to be a member of this family. They are an ecologically and morphologically diverse group of beetles, and commonly encountered in terrestrial ecosystems. One well-known species is the devil's coach-horse beetle. For some other species, see list of British rove beetles. Anatomy As might be expected for such a large family, considerable variation exists among the species. Sizes range from <1 to , with most in the 2–8 mm range, and the form is generally elongated, with some rove beetles being ovoid i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pinophilus P1610351a
''Pinophilus'' is a genus of rove beetles in the family Staphylinidae. Species (list incomplete) * '' Pinophilus cayennensis'' Laporte de Castelnau, 1835 * '' Pinophilus chinensis'' Bernhauer, 1938 * '' Pinophilus femoratus'' Schubert, 1911 * '' Pinophilus formosae'' Bernhauer, 1935 * '' Pinophilus gracilis'' * ''Pinophilus insigniventris'' Bernhauer, 1918 * ''Pinophilus javanus'' Erichson, 1840 * ''Pinophilus latipes'' Gravenhorst, 1802 * ''Pinophilus lewisius'' Sharp, 1874 * ''Pinophilus melanocephalus'' Motschulsky, 1858 * ''Pinophilus parapunctatissimus'' Li & Chen, 1993 * ''Pinophilus parcus'' * ''Pinophilus punctatissimus'' Sharp, 1889 * ''Pinophilus rufipennis'' Sharp, 1874 * ''Pinophilus sachtlebeni'' Bernhauer, 1935 * ''Pinophilus sautteri'' Bernhauer, 1935 * ''Pinophilus tenuis'' Fagel, 1963 g Data sources: i = ITIS, c = Catalogue of Life, g = GBIF, b = Bugguide.net References Further reading * * * * * * * * * External links * Paederinae {{ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaminus
''Palaminus'' is a genus of rove beetles in the family Staphylinidae. There are about 16 described species in ''Palaminus''. Species These 16 species belong to the genus ''Palaminus'': * '' Palaminus aequalis'' Bernhauer, ms * '' Palaminus apterus'' Bernhauer, 1918 * '' Palaminus dubius'' Notman, 1929 * '' Palaminus formosae'' Cameron, 1949 * '' Palaminus formosanus'' Bernhauer, ms * '' Palaminus hudsonicus'' Casey, 1910 * '' Palaminus iaponicus'' Cameron * '' Palaminus insularis'' Cameron, 1913 * '' Palaminus japonicus'' Cameron, 1930 * '' Palaminus larvalis'' * '' Palaminus lumiventris'' Herman, 2003 * '' Palaminus luteus'' Casey, 1910 * '' Palaminus montanus'' Cameron, 1947 * '' Palaminus parvus'' Cameron, 1918 * '' Palaminus rufulus'' Coiffait, 1978 * '' Palaminus variabilis'' Erichson, 1840 g Data sources: i = ITIS, c = Catalogue of Life, g = GBIF, b = Bugguide.net References Further reading * * * * * * * * * External links * Paederinae {{staphy ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pinophilus
''Pinophilus'' is a genus of rove beetles in the family Staphylinidae. Species (list incomplete) * '' Pinophilus cayennensis'' Laporte de Castelnau, 1835 * '' Pinophilus chinensis'' Bernhauer, 1938 * '' Pinophilus femoratus'' Schubert, 1911 * '' Pinophilus formosae'' Bernhauer, 1935 * '' Pinophilus gracilis'' * ''Pinophilus insigniventris'' Bernhauer, 1918 * ''Pinophilus javanus'' Erichson, 1840 * ''Pinophilus latipes'' Gravenhorst, 1802 * ''Pinophilus lewisius'' Sharp, 1874 * ''Pinophilus melanocephalus'' Motschulsky, 1858 * ''Pinophilus parapunctatissimus'' Li & Chen, 1993 * ''Pinophilus parcus'' * ''Pinophilus punctatissimus'' Sharp, 1889 * ''Pinophilus rufipennis'' Sharp, 1874 * ''Pinophilus sachtlebeni'' Bernhauer, 1935 * ''Pinophilus sautteri'' Bernhauer, 1935 * ''Pinophilus tenuis'' Fagel, 1963 g Data sources: i = ITIS, c = Catalogue of Life, g = GBIF, b = Bugguide.net References Further reading * * * * * * * * * External links * Paederinae {{ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cenomanian
The Cenomanian is, in the ICS' geological timescale, the oldest or earliest age of the Late Cretaceous Epoch or the lowest stage of the Upper Cretaceous Series. An age is a unit of geochronology; it is a unit of time; the stage is a unit in the stratigraphic column deposited during the corresponding age. Both age and stage bear the same name. As a unit of geologic time measure, the Cenomanian Age spans the time between 100.5 and 93.9 million years ago (Mya). In the geologic timescale, it is preceded by the Albian and is followed by the Turonian. The Upper Cenomanian starts around at 95 Mya. The Cenomanian is coeval with the Woodbinian of the regional timescale of the Gulf of Mexico and the early part of the Eaglefordian of the regional timescale of the East Coast of the United States. At the end of the Cenomanian, an anoxic event took place, called the Cenomanian-Turonian boundary event or the "Bonarelli event", that is associated with a minor extinction event for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
