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Embolemidae
Embolemidae is a family of small solitary parasitoid wasps with around 70 species in 2 genera distributed around the world.van Achterberg, Cornelis & Kats, R.. (2000). Revision of the Palaearctic Embolemidae (Hymenoptera). Zoöl. Med. 74 (2000), 17: 251-269. The few species whose biology is known are parasites on planthopper nymphs of the families Achilidae and Cixiidae. There is debate regarding the status of the genus named ''Ampulicomorpha'' by Ashmead in 1893, generally considered now to be a junior synonym of ''Embolemus'' (e.g.,), though some authorities dispute this (e.g.,) Biology Females are wingless while males have wings, and in temperate regions emerge later than the females, which overwinter as adults. The wingless females have been recorded from the nests of ants and small mammal burrows, or under stones in pastures and grasslands, and they appear to be ant mimics. A Palearctic species, ''Embolemus ruddii'', has been found in association with the ant species ''For ...
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Embolemus Nearcticus
''Embolemus'' is a genus of wasps belonging to the family Embolemidae. There is debate regarding the status of the genus named ''Ampulicomorpha'' by Ashmead in 1893, generally considered now to be a junior synonym of ''Embolemus'' (e.g.,van Achterberg, Cornelis & Kats, R.. (2000). Revision of the Palaearctic Embolemidae (Hymenoptera). Zoöl. Med. 74 (2000), 17: 251-269.), as a few authorities dispute this (e.g.,). The genus has cosmopolitan distribution. Species Extant * '' Embolemus africanus'' (Risbec, 1957) * '' Embolemus ambrensis'' Olmi, 2004 * '' Embolemus andersoni'' Olmi, 1998 * '' Embolemus angustipennis'' (Kieffer, 1912) * ''Embolemus apertus'' Azevedo & Amarante, 2005 * '' Embolemus australis'' (Olmi, 1996) * '' Embolemus bestelmeyeri'' Olmi, 1997 * ''Embolemus boraceia'' Amarante, Brandão & Carpenter, 1999 * '' Embolemus brandaoi'' Azevedo & Amarante, 2005 * '' Embolemus brothersi'' Olmi, 2006 * ''Embolemus burundensis'' Olmi, 2011 * '' Embolemus capensis'' Olmi, 1 ...
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Embolemus
''Embolemus'' is a genus of wasps belonging to the family Embolemidae. There is debate regarding the status of the genus named ''Ampulicomorpha'' by Ashmead in 1893, generally considered now to be a junior synonym of ''Embolemus'' (e.g.,van Achterberg, Cornelis & Kats, R.. (2000). Revision of the Palaearctic Embolemidae (Hymenoptera). Zoöl. Med. 74 (2000), 17: 251-269.), as a few authorities dispute this (e.g.,). The genus has cosmopolitan distribution. Species Extant * '' Embolemus africanus'' (Risbec, 1957) * '' Embolemus ambrensis'' Olmi, 2004 * '' Embolemus andersoni'' Olmi, 1998 * '' Embolemus angustipennis'' (Kieffer, 1912) * ''Embolemus apertus'' Azevedo & Amarante, 2005 * '' Embolemus australis'' (Olmi, 1996) * '' Embolemus bestelmeyeri'' Olmi, 1997 * ''Embolemus boraceia'' Amarante, Brandão & Carpenter, 1999 * '' Embolemus brandaoi'' Azevedo & Amarante, 2005 * '' Embolemus brothersi'' Olmi, 2006 * ''Embolemus burundensis'' Olmi, 2011 * '' Embolemus capensis'' Olmi, 1 ...
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Embolemus Confusus
''Embolemus'' is a genus of wasps belonging to the family Embolemidae. There is debate regarding the status of the genus named ''Ampulicomorpha'' by Ashmead in 1893, generally considered now to be a junior synonym of ''Embolemus'' (e.g.,van Achterberg, Cornelis & Kats, R.. (2000). Revision of the Palaearctic Embolemidae (Hymenoptera). Zoöl. Med. 74 (2000), 17: 251-269.), as a few authorities dispute this (e.g.,). The genus has cosmopolitan distribution. Species Extant * '' Embolemus africanus'' (Risbec, 1957) * '' Embolemus ambrensis'' Olmi, 2004 * '' Embolemus andersoni'' Olmi, 1998 * '' Embolemus angustipennis'' (Kieffer, 1912) * ''Embolemus apertus'' Azevedo & Amarante, 2005 * '' Embolemus australis'' (Olmi, 1996) * '' Embolemus bestelmeyeri'' Olmi, 1997 * ''Embolemus boraceia'' Amarante, Brandão & Carpenter, 1999 * '' Embolemus brandaoi'' Azevedo & Amarante, 2005 * '' Embolemus brothersi'' Olmi, 2006 * ''Embolemus burundensis'' Olmi, 2011 * '' Embolemus capensis'' Olmi, 1 ...
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Embolemus Walkeri
''Embolemus'' is a genus of wasps belonging to the family Embolemidae. There is debate regarding the status of the genus named ''Ampulicomorpha'' by Ashmead in 1893, generally considered now to be a junior synonym of ''Embolemus'' (e.g.,van Achterberg, Cornelis & Kats, R.. (2000). Revision of the Palaearctic Embolemidae (Hymenoptera). Zoöl. Med. 74 (2000), 17: 251-269.), as a few authorities dispute this (e.g.,). The genus has cosmopolitan distribution. Species Extant * '' Embolemus africanus'' (Risbec, 1957) * '' Embolemus ambrensis'' Olmi, 2004 * '' Embolemus andersoni'' Olmi, 1998 * '' Embolemus angustipennis'' (Kieffer, 1912) * '' Embolemus apertus'' Azevedo & Amarante, 2005 * '' Embolemus australis'' (Olmi, 1996) * '' Embolemus bestelmeyeri'' Olmi, 1997 * '' Embolemus boraceia'' Amarante, Brandão & Carpenter, 1999 * '' Embolemus brandaoi'' Azevedo & Amarante, 2005 * '' Embolemus brothersi'' Olmi, 2006 * '' Embolemus burundensis'' Olmi, 2011 * '' Embolemus capensis'' Olm ...
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Wessex Formation
The Wessex Formation is a fossil-rich English geological formation that dates from the Berriasian to Barremian stages (about 145–125 million years ago) of the Early Cretaceous. It forms part of the Wealden Group and underlies the younger Vectis Formation and overlies the Durlston Formation. The dominant lithology of this unit is mudstone with some interbedded sandstones. It is part of the strata of the Wessex Basin, exposed in both the Isle of Purbeck and the Isle of Wight. While the Purbeck sections are largely barren of vertebrate remains, the Isle of Wight sections are well known for producing the richest and most diverse fauna in Early Cretaceous Europe. Nomenclatural History The Wessex Formation has historically alternately been called the "Variegated Marls And Sandstones", a name used by W. J. Arkell in his 1947 map of the Isle of Purbeck as well as the "Wealden Marls" It was given its current formal name by Daley and Stewart in 1979 Stratigraphy and Lithology In ...
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Embolemus Ruddii
''Embolemus ruddii'' is a small aculeate wasp in the family Embolemidae Embolemidae is a family of small solitary parasitoid wasps with around 70 species in 2 genera distributed around the world.van Achterberg, Cornelis & Kats, R.. (2000). Revision of the Palaearctic Embolemidae (Hymenoptera). Zoöl. Med. 74 (2000), .... Biology Females are apterous whilst males are winged. It is a widespread, yet rarely recorded palearctic species. They are believed to parasitise tree root-feeding planthoppers in the family Cixiidae. Varrone, R. & Olmi, M. (2010). First record of host of Embolemus ruddii Westwood (Hymenoptera Embolemidae). Frustula entomologica, 33, 91-95. References {{Taxonbar, from=Q14583547 Chrysidoidea Insects described in 1833 ...
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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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Cixiidae
The Cixiidae are a family of fulgoroid insects, one of many families commonly known as planthoppers, distributed worldwide and comprising more than 2,000 species from over 150 genera. The genera are placed into three subfamilies, Borystheninae, Bothriocerinae and Cixiinae with sixteen tribes currently accepted in Cixiinae. Description Cixiid species are typically comparatively small (body size less than a centimeter) and usually inconspicuous. The face is longer than wide and the head is narrower than the pronotum. The forewings are at least partly transparent and the veins bear minute setae. The hind tibiae end in a cluster of spines and may sometimes have spines along their length. Nymphs live underground, feeding on roots. Adults feed on herbs, shrubs and/or trees; some are polyphagous, while others are specialised on their host plants (monophagous). A couple of species are cavernicolous, feeding on roots in volcanic caves. Females occasionally bear impressive "wax tails ...
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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 ...
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Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope Carbon-13, 13C in the atmosphere was exceptionally low in comparison with the more common isotope Carbon-12, 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Popigai impact structure, Siberia and in what is now ...
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Baltic Amber
The Baltic region is home to the largest known deposit of amber, called Baltic amber or succinite. It was produced sometime during the Eocene epoch, but exactly when is controversial. It has been estimated that these forests created more than 100,000 tons of amber. Today, more than 90% of the world's amber comes from Kaliningrad Oblast of Russia. It is a major source of income for the region; the local Kaliningrad Amber Combine extracted 250 tonnes of it in 2014, 400 tonnes in 2015. "Baltic amber" was formerly thought to include amber from the Bitterfeld Lignite, brown coal mines in Saxony (Eastern Germany). Bitterfeld amber was previously believed to be only 20–22 million years old (Miocene), but a comparison of the animal inclusions in 2003 suggested that it was possibly Baltic amber that was redeposited in a Miocene deposit. Further study of insect taxa in the ambers has shown Bitterfeld amber to be from the same forest as the Baltic amber forest, but separately deposited f ...
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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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