Phloeostichidae
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Phloeostichidae
Phloeostichidae is a family of beetles in the superfamily Cucujoidea. They are typically found under the bark of dead trees. Larvae have been found to consume plant tissue and some fungi, while the adults appear to be exclusively fungivores. The family contains four extant genera, '' Phloeostichus'' is native to the Palearctic, '' Rhopalobrachium'' is native to central-southern South America and eastern Australia, '' Hymaea'' is native to southeastern Australia, and '' Bunyastichus'' is found in Tasmania. Genera * '' Bunyastichus'' Leschen, Lawrence & Ślipiński, 2005 * '' Phloeostichus'' Redtenbacher, 1842 * '' Rhopalobrachium'' Boheman, 1858 * '' Hymaea'' Pascoe, 1869 *†'' Pleuroceratos'' Poinar and Kirejtshuk 2008 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 ...
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Cucujoidea
Cucujoidea is a superfamily of beetles. This group formerly included all of the families now included in the superfamily Coccinelloidea. They include some fungus beetles and a diversity of lineages of "bark beetles" unrelated to the "true" bark beetles ( Scolytinae), which are weevils (superfamily Curculionoidea). Morphology The morphology of Cucujoidea is varied and there are no features uniting all members of the superfamily. Adults can be recognised by the procoxal cavities being internally open in most taxa, females having tarsal formula 5-5-5 and males 5-5-5 or 5-5-4 (rarely 4-4-4), females with tergite VIII concealed dorsally by tergite VII, and males with tergite X completely membraneous. Larvae have frontal arms usually lyriform, the mandible mesal surface usually with well-developed mola, a maxillary articulating area usually present, a hypopharyngeal sclerome usually present, and two pretarsal setae. Taxonomy According to a 2015 revision, the following 25 families ...
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Hymaea
''Hymaea'' is a genus of beetles in the family Phloeostichidae Phloeostichidae is a family of beetles in the superfamily Cucujoidea. They are typically found under the bark of dead trees. Larvae have been found to consume plant tissue and some fungi, while the adults appear to be exclusively fungivores. The .... Species These species belong to the genus ''Hymaea'' * '' Hymaea parallela'' Carter, 1936 * '' Hymaea magna'' Sen Gupta & Crowson, 1966 * '' Hymaea succinifera'' Pascoe, 1869 References Cucujoidea genera {{cucujoidea-stub ...
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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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Palearctic
The Palearctic or Palaearctic is the largest of the eight biogeographic realms of the Earth. It stretches across all of Eurasia north of the foothills of the Himalayas, and North Africa. The realm consists of several bioregions: the Euro-Siberian region; the Mediterranean Basin; the Sahara and Arabian Deserts; and Western, Central and East Asia. The Palaearctic realm also has numerous rivers and lakes, forming several freshwater ecoregions. The term 'Palearctic' was first used in the 19th century, and is still in use as the basis for zoogeographic classification. History In an 1858 paper for the ''Proceedings of the Linnean Society'', British zoologist Philip Sclater first identified six terrestrial zoogeographic realms of the world: Palaearctic, Aethiopian/Afrotropic, Indian/Indomalayan, Australasian, Nearctic, and Neotropical. The six indicated general groupings of fauna, based on shared biogeography and large-scale geographic barriers to migration. Alfred Wallace a ...
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Rhopalobrachium (insect)
''Rhopalobrachium'' was a genus of flowering plants in the family Rubiaceae but is no longer recognized. It has been sunk into synonymy with ''Cyclophyllum''. It was originally described by Rudolf Schlechter and Kurt Krause in 1908 to accommodate two New Caledonian species, ''R. congestum'' and ''R. fragrans''. No type species was selected. Former species * ''Rhopalobrachium congestum'' Schltr. & K.Krause = ''Aidia congesta'' * ''Rhopalobrachium fragrans'' Schltr. & K.Krause = ''Cyclophyllum fragrans ''Cyclophyllum'' is a genus of flowering plants in the family Rubiaceae. It is found from New Guinea, Australia and on islands in many parts of the Pacific. Species * '' Cyclophyllum baladense'' Guillaumin * '' Cyclophyllum balansae'' (Baill.) ...'' * ''Rhopalobrachium megacarpum'' (Kaneh.) Kaneh. = '' Atractocarpus carolinensis'' References External links World Checklist of Rubiaceae Historically recognized Rubiaceae genera Vanguerieae {{Ixoroideae-stub ...
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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 marine spec ...
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