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Asaphus
''Asaphus'' () is a genus of trilobites that is known from the Lower (upper Arenig) and Middle Ordovician of northwestern Europe (Sweden, Estonia, Saint Petersburg Area). Etymology The generic name is derived from the Greek word ''asaphes'', meaning "indistinct." Description The headshield (or cephalon) and tailshield (or pygidium) are semicircular and without a border (defined by a furrow or a change in convexity parallel to its margin). The cephalon is of approximately equal size as the pygidium (or isopygous). The central raised area of the cephalon (or glabella) is long, reaching the frontal margin. It may have faint lateral glabellar furrows or be smooth, and sometimes an inconspicuous tubercle is present just in front of the hardly discernible occipital ring. The natural fracture lines (sutures) of the head run along the top edges of the compound eye. From the back of the eye these cut to the back of the head (or is said to be opisthoparian) and not to the side. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Asaphus Expansus
''Asaphus expansus'' () is the type species of the asaphid trilobite genus ''Asaphus''. It was previously classified as ''Entomostracites expansus'' before being split off into its own genus. Location Most specimens have been obtained in Northern Europe, with one known exeption being in North America North America is a continent in the Northern Hemisphere, Northern and Western Hemisphere, Western hemispheres. North America is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the southeast by South Ameri .... Characteristics ''Asaphus expansus'' differs from related species in its genus by having a cranidium that is considered broad, as opposed to its more medium sized counterparts. Examples of these other species are ''A. fallax'' and ''A. raniceps''. References Trilobites of Asia Asaphidae Ordovician trilobites Asaphida {{asaphida-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Asaphus Kowalewskii
''Asaphus kowalewskii'' () is one of the 35 species of trilobites of the genus ''Asaphus'' (this particular species is sometimes placed in its own genus, ''Neoasaphus''). Fossils of this species are popular among collectors because of their prominent stalked eyes (termed "peduncles"), many an inch or more in length. In the Ordovician period, an inland sea formed in what is now Eastern Europe. The sea contained a remarkably diverse trilobite fauna. Over a dozen species of ''Asaphus'' developed in this sea, with many species, including unrelated species, developing long eyestalks in various lengths. That so many species of trilobite developed eyestalks suggests that they were trying to overcome increased turbidity, or there was some sort of massive selective pressure leading these trilobites to bury themselves in the substrate up to their eyes. This species may have lain in wait buried in a benthic layer of loose debris or sediment with only its periscope eyestalks protruding ab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charles Stokes (collector)
Charles Stokes ( – 28 December 1853) was a London stockbroker who gained a reputation both as an amateur scientist and as an art collector. Biography According to the 1851 England Census, Stokes was born in the City of London, Middlesex around 1784. A baptism was recorded at St Andrew's in Holborn, City of London on 9 June 1783 for Charles Stokes, son of John Stokes and Agnes Partridge Stokes of Shoe Lane (off Fleet Street) in the City of London). Upon his death in December 1853, Stokes was widely reported to be in his 70th year (typically meaning aged 69). Stokes was also listed as age 69 when his death was recorded.''London, England, Church of England Deaths and Burials, 1813-2003'' He seems never to have married. He is recorded as being a partner in the stockbroking firm of Hodges & Stokes, Threadneedle Street. Between 1835 and 1851, he is recorded as living in Gray's Inn Road, at Verulam Buildings, a housing development which had been designed for the professional clas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trilobite
Trilobites (; meaning "three-lobed entities") are extinction, extinct marine arthropods that form the class (biology), class Trilobita. One of the earliest groups of arthropods to appear in the fossil record, trilobites were among the most successful of all early animals, existing in oceans for almost 270million years, with over 22,000 species having been described. Because trilobites had wide diversity and an easily fossilized mineralised exoskeleton made of calcite, they left an extensive fossil record. The study of their fossils has facilitated important contributions to biostratigraphy, paleontology, evolution, evolutionary biology, and plate tectonics. Trilobites are placed within the clade Artiopoda, which includes many organisms that are morphologically similar to trilobites, but are largely unmineralised. The relationship of Artiopoda to other arthropods is uncertain. Trilobites evolved into many ecological niches; some moved over the seabed as predators, scavengers, or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Entomostracites
''Entomostracites'' is a scientific name for several trilobites, now assigned to various other genera Genus (; : genera ) is a taxonomic rank above species and below family as used in the biological classification of living and fossil organisms as well as viruses. In binomial nomenclature, the genus name forms the first part of the binomial s .... * ''E. bucephalus'' = '' Paradoxides paradoxissimus'' * ''E. crassicauda'' = '' Illaenus crassicauda'' * ''E. expansus'' = '' Asaphus expansus'' * ''E. gibbosus'' = '' Olenus gibbosus'' * ''E. granulatus'' = '' Nankinolithus granulatus'' * ''E. laciniatus'' = '' Lichas laciniatus'' * ''E. laticauda'' = '' Eobronteus laticauda'' * ''E. paradoxissimus'' = '' Paradoxides paradoxissimus'' * ''E. pisiformis'' = '' Agnostus pisiformis'' * ''E. punctatus'' = '' Encrinurus punctatus'' * ''E. scarabaeoides'' = '' Peltura scarabaeoides'' * ''E. spinulosus'' = '' Parabolina spinulosa'' References {{Set index article, animals Disused tri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Entomolithus
''Entomolithus'' (petrified insect) is an obsolete scientific name for several trilobites, first published by Linnaeus in 1753, before the starting point of zoological nomenclature in a list under the heading "Paradoxus: 3. Entomolithus Monoculi". This is why this first name has no formal status. After the starting point of the zoological nomenclature, the name was published again in 1759, but with a different description. Because scholars incorrectly considered ''Entomolithus'' Linnaeus, 1759 a junior homonym, it was later replaced by ''Entomostracites'' Wahlenberg, 1818. Although the name as published in 1759 was in fact valid, the International Commission on Zoological Nomenclature decided to suppress ''Entomolithus'' Linnaeus, 1759, because this name had gone out of use for a very long time. Species originally assigned to ''Entomolithus'' have been renamed. * ''E. paradoxus'' = '' Paradoxides paradoxissimus'' * ''E. paradoxus α expansus'' = ''Asaphus expansus ''Asaphus ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coronura
''Coronura'' is a trilobite in the order Phacopida, that existed during the Middle Devonian in what is now New York, U.S.A. It was described by Hall and Clarke in 1888, and the type species is ''Coronura aspectans'', which was originally described under the genus ''Asaphus'' by Conrad in 1841. The species was described from the Onondaga Formation. P.A. Jell and J.M. Adrain. Fossils of ''Coronura'' have also been found in Indiana,''Coronura'' at the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era, and the second of twelve periods of the Phanerozoic Eon (geology), Eon. The Ordovician spans 41.6 million years from the end of the Cambrian Period Megaannum, Ma (million years ago) to the start of the Silurian Period Ma. The Ordovician, named after the Celtic Britons, Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same Rock (geology), rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed Stratum, strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official per ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
