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Archaeonycteris Trigonodon
''Archaeonycteris'' is an archaic bat genus whose fossilised remains have been found in Germany, France, England and India. The genus was established in 1917, when Pierre Revilliod described the material excavated at the Messel Pit as the fossil species '' Archaeonycteris trigonodon''. *''Archaeonycteris trigonodon'' Revilliod, 1917 - Messel Pit (Lutetian), Germany *''Archaeonycteris pollex'' Storch & Habersetzer, 1988 - Messel Pit (Lutetian), Germany *''Archaeonycteris brailloni'' Russell ''et al.'', 1973 - Avenay quarry (Ypresian In the geologic timescale the Ypresian is the oldest age (geology), age or lowest stage (stratigraphy), stratigraphic stage of the Eocene. It spans the time between , is preceded by the Thanetian Age (part of the Paleocene) and is followed by th ...), France *''Archaeonycteris relicta'' Harrison & Hooker, 2010 - Creechbarrow Limestone Formation, England *''Archaeonycteris storchi'' Smith ''et al.'', 2007 - Vastan Lignite Mines (Ypresian), Indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Early Eocene
In the geologic timescale the Ypresian is the oldest age or lowest stratigraphic stage of the Eocene. It spans the time between , is preceded by the Thanetian Age (part of the Paleocene) and is followed by the Eocene Lutetian Age. The Ypresian is consistent with the lower Eocene. Events The Ypresian Age begins during the throes of the Paleocene–Eocene Thermal Maximum (PETM). The Fur Formation in Denmark, the Messel shales in Germany, the Oise amber of France and Cambay amber of India are of this age. The Eocene Okanagan Highlands are an uplands subtropical to temperate series of lakes from the Ypresian. Stratigraphic definition The Ypresian Stage was introduced in scientific literature by Belgian geologist André Hubert Dumont in 1850. The Ypresian is named after the Flemish city of Ypres in Belgium (spelled ''Ieper'' in Dutch). The definitions of the original stage were totally different from the modern ones. The Ypresian shares its name with the Belgian Ieper Group (French: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ypresian
In the geologic timescale the Ypresian is the oldest age (geology), age or lowest stage (stratigraphy), stratigraphic stage of the Eocene. It spans the time between , is preceded by the Thanetian Age (part of the Paleocene) and is followed by the Eocene Lutetian Age. The Ypresian is consistent with the lower Eocene. Events The Ypresian Age begins during the throes of the Paleocene–Eocene Thermal Maximum (PETM). The Fur Formation in Denmark, the Messel shales in Germany, the Oise amber of France and Cambay amber of India are of this age. The Eocene Okanagan Highlands are an uplands subtropical to temperate series of lakes from the Ypresian. Stratigraphic definition The Ypresian Stage was introduced in scientific literature by Belgium, Belgian geologist André Hubert Dumont in 1850. The Ypresian is named after the Flanders, Flemish city of Ypres in Belgium (spelled ''Ieper'' in Dutch). The definitions of the original stage were totally different from the modern ones. The Ypresi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene Mammals Of Asia
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 end of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene Mammals Of Europe
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 end of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene Bats
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 end of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Archaeonycteris Trigonodon 4
''Archaeonycteris'' is an archaic bat genus whose fossilised remains have been found in Germany, France, England and India. The genus was established in 1917, when Pierre Revilliod described the material excavated at the Messel Pit as the fossil species ''Archaeonycteris trigonodon''. *''Archaeonycteris trigonodon'' Revilliod, 1917 - Messel Pit (Lutetian), Germany *''Archaeonycteris pollex'' Storch & Habersetzer, 1988 - Messel Pit (Lutetian), Germany *''Archaeonycteris brailloni'' Russell ''et al.'', 1973 - Avenay quarry (Ypresian), France *''Archaeonycteris relicta'' Harrison & Hooker, 2010 - Creechbarrow Limestone Formation, England *''Archaeonycteris storchi'' Smith ''et al.'', 2007 - Vastan Lignite Mines Vastan ( fa, واستان, also Romanized as Vāstān) is a village in Tangeh Soleyman Rural District, Kolijan Rostaq District, Sari County, Mazandaran Province, Iran Iran, officially the Islamic Republic of Iran, and also call ... (Ypresian), India ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Archaeonycteris Praecursor
''Archaeonycteris'' is an archaic bat genus whose fossilised remains have been found in Germany, France, England and India. The genus was established in 1917, when Pierre Revilliod described the material excavated at the Messel Pit as the fossil species ''Archaeonycteris trigonodon''. *''Archaeonycteris trigonodon'' Revilliod, 1917 - Messel Pit (Lutetian), Germany *''Archaeonycteris pollex'' Storch & Habersetzer, 1988 - Messel Pit (Lutetian), Germany *''Archaeonycteris brailloni'' Russell ''et al.'', 1973 - Avenay quarry (Ypresian), France *''Archaeonycteris relicta'' Harrison & Hooker, 2010 - Creechbarrow Limestone Formation, England *''Archaeonycteris storchi'' Smith ''et al.'', 2007 - Vastan Lignite Mines Vastan ( fa, واستان, also Romanized as Vāstān) is a village in Tangeh Soleyman Rural District, Kolijan Rostaq District, Sari County, Mazandaran Province, Iran Iran, officially the Islamic Republic of Iran, and also call ... (Ypresian), India ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vastan Lignite Mines
Vastan ( fa, واستان, also Romanized as Vāstān) is a village in Tangeh Soleyman Rural District, Kolijan Rostaq District, Sari County, Mazandaran Province, Iran Iran, officially the Islamic Republic of Iran, and also called Persia, is a country located in Western Asia. It is bordered by Iraq and Turkey to the west, by Azerbaijan and Armenia to the northwest, by the Caspian Sea and Turkmeni .... At the 2006 census, its population was 120, in 39 families. References Populated places in Sari County {{Sari-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Avenay-Val-d'Or
Avenay-Val-d'Or () is a commune in the Marne department, northeastern France. Located in the Vallée de la Marne, part of the Champagne region, its primary industry is viticulture. History A number of Roman remains have been discovered nearby, including a fort and medals showing Emperors Marcus Aurelius and his son Commodus. It was formerly the site of a Benedictine abbey founded by Bertha of Avenay at the end of the sixth century CE, later destroyed during the French Revolution. One of the most prestigious religious institutions in Champagne, it became so popular in the 12th century that limits were placed on the number of nuns accepted. Population See also *Communes of the Marne department *Montagne de Reims Regional Natural Park Montagne de Reims Regional Natural Park (French: ''Parc naturel régional de la Montagne de Reims'') is a protected area in the Grand Est region of France. It is organized around the Montagne de Reims, a wooded range of hills covered by vineyard ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle 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 end of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lutetian
The Lutetian is, in the geologic timescale, a stage or age in the Eocene. It spans the time between . The Lutetian is preceded by the Ypresian and is followed by the Bartonian. Together with the Bartonian it is sometimes referred to as the Middle Eocene Subepoch. Stratigraphic definition The Lutetian was named after Lutetia, the Latin name for the city of Paris. The Lutetian Stage was introduced in scientific literature by French geologist Albert de Lapparent in 1883 and revised by A. Blondeau in 1981. The base of the Lutetian Stage is at the first appearance of the nanofossil ''Blackites inflatus'', according to an official reference profile (GSSP) established in 2011. Of two candidates located in Spain, the Gorrondatxe section was chosen.See thwebsite of Eustoquio Molinafor these candidates. The top of the Lutetian (the base of the Bartonian) is at the first appearance of calcareous nanoplankton species ''Reticulofenestra reticulata''. The Lutetian overlaps with the Geisel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
