|
Campanile (gastropod)
''Campanile'' is a genus of large sea snails, marine gastropod molluscs in the family Campanilidae. Biology All species in this genus have become extinct, except ''Campanile symbolicum'' Iredale, 1917 from southwestern Australia. They used to flourish in the Tethys Sea and underwent a widespread adaptive radiation in the Cenozoic. Species Species within the genus ''Campanile'' include: * † ''Campanile auvertianum'' * † ''Campanile brookmani'' Cox 1930 * † ''Campanile claytonense'' * † '' Campanile cornucopiae'' * † '' Campanile dilloni'' * † '' Campanile elongatum'' * † '' Campanile giganteum'' (Lamarck, 1804) - a gigantic fossil species from the Eocene * † ''Campanile gigas'' Martin 1881 * † ''Campanile greenellum'' * † ''Campanile hebertianum'' * † ''Campanile houbricki'' * † ''Campanile parisiense'' * † ''Campanile paratum'' * ''Campanile symbolicum'' Iredale, 1917 - a living Australian species. This is the only extant species of Campanilidae. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Campanile Giganteum
†''Campanile giganteum'' is a species of exceptionally large fossil sea snail, marine gastropod molluscs in the family Campanilidae Campanilidae are a taxonomic family of sea snails, marine gastropod molluscs in the clade Sorbeoconcha (an alternative representation of the clade Caenogastropoda).Bouchet, P. (2013). Campanilidae. Accessed through: World Register of Marine Speci .... This species dates from the Eocene epoch. With a shell length of or even more than from 28 July 2016. this is considered to be one of [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Campanile Auvertianum
''Campanile auvertianum'' is a species of fossil sea snail, a marine gastropod mollusc in the family Campanilidae. This species lived during the 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' ... epoch, Bartonian age (from 38.0 to 41.3 Ma). Shells of ''Campanile auvertianum'' can reach a length of about . References External links Museum Nationale d’histoire Naturelle Campanilidae Eocene gastropods Paleogene gastropods of Europe Paleogene gastropods of North America Fossil taxa described in 1850 {{paleo-gastropod-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Campanile Trevorjacksoni
A bell tower is a tower that contains one or more bells, or that is designed to hold bells even if it has none. Such a tower commonly serves as part of a Christian church, and will contain church bells, but there are also many secular bell towers, often part of a municipal building, an educational establishment, or a tower built specifically to house a carillon. Church bell towers often incorporate clocks, and secular towers usually do, as a public service. The term campanile (, also , ), deriving from the Italian ''campanile'', which in turn derives from ''campana'', meaning "bell", is synonymous with ''bell tower''; though in English usage campanile tends to be used to refer to a free standing bell tower. A bell tower may also in some traditions be called a belfry, though this term may also refer specifically to the substructure that houses the bells and the ringers rather than the complete tower. The tallest free-standing bell tower in the world, high, is the Mortegliano ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Freiberger Forschungshefte
The Freiberger, also known as Franches-Montagnes, is a horse breed from Switzerland, from the Jura region, described as either a "heavy warmblood" or a "light coldblood". It was widely used as draft and pack horse in the Swiss army. It has a good disposition and is versatile, suitable for both driving and riding. Each year at the ''Marché Concours'' in Saignelégier in the Franches-Montagnes district of the Swiss canton of Jura, on the second weekend in August, a variety of shows and competitions are held. Breed characteristics History The presence of an autochthonous horse breed in the Jura traces to the year 1619. By the early 19th century, there were active breeders in the district of Franches-Montagnes. In 1817, there were 4,000 breeding mares on record. The horses were bred for use in agriculture and by the army as pack animals and artillery draft horses. There are records of imports of Anglo-Norman horses for the year 1821, and of other horses from England, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Campanile Houbricki
A bell tower is a tower that contains one or more bells, or that is designed to hold bells even if it has none. Such a tower commonly serves as part of a Christian church, and will contain church bells, but there are also many secular bell towers, often part of a municipal building, an educational establishment, or a tower built specifically to house a carillon. Church bell towers often incorporate clocks, and secular towers usually do, as a public service. The term campanile (, also , ), deriving from the Italian ''campanile'', which in turn derives from ''campana'', meaning "bell", is synonymous with ''bell tower''; though in English usage campanile tends to be used to refer to a free standing bell tower. A bell tower may also in some traditions be called a belfry, though this term may also refer specifically to the substructure that houses the bells and the ringers rather than the complete tower. The tallest free-standing bell tower in the world, high, is the Mortegliano ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic 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 13C in the atmosphere was exceptionally low in comparison with the more common isotope 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 Siberia and in what is now Chesapeake Bay. As with other geologic periods, the strata that define the start and e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.JPG "Click for more on -> Campanile Trevorjacksoni")
