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Palaeocarpilius
''Palaeocarpilius'' is an Extinction, extinct genus of crabs belonging to the family Carpiliidae. The type species of this genus is ''Palaeocarpilius macrocheilus''. These Fauna, epifaunal Carnivore, carnivores lived in the Eocene and the Oligocene, from 48.6 to 28.4 Ma. Species *''Palaeocarpilius aquitanicus'' Milne-Edwards 1862 *''Palaeocarpilius ignotus'' Milne-Edwards 1862 *''Palaeocarpilius intermedius'' Stubblefield 1927 *''Palaeocarpilius laevis'' Imaizumi 1939 *''Palaeocarpilius macrocheilus'' Desmarest 1822 *''Palaeocarpilius mississippiensis'' Rathbun 1935 *''Palaeocarpilius rugifer'' Stoliczka 1871 *''Palaeocarpilius valrovinensis'' De Gregorio 1895 Distribution Fossils of this genus have been found in the Eocene of Italy and in the Oligocene of India, Libya and United States. References Crabs Prehistoric Malacostraca Prehistoric crustacean genera Eocene crustaceans Oligocene crustaceans Fossils of Italy Fossils of the United States Fossils of India Eocene ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeocarpilius Valrovinensis
''Palaeocarpilius'' is an extinct genus of crabs belonging to the family Carpiliidae. The type species of this genus is '' Palaeocarpilius macrocheilus''. These epifaunal carnivores lived in the Eocene and the Oligocene, from 48.6 to 28.4 Ma. Species *'' Palaeocarpilius aquitanicus'' Milne-Edwards 1862 *'' Palaeocarpilius ignotus'' Milne-Edwards 1862 *'' Palaeocarpilius intermedius'' Stubblefield 1927 *''Palaeocarpilius laevis'' Imaizumi 1939 *'' Palaeocarpilius macrocheilus'' Desmarest 1822 *'' Palaeocarpilius mississippiensis'' Rathbun 1935 *''Palaeocarpilius rugifer'' Stoliczka 1871 *'' Palaeocarpilius valrovinensis'' De Gregorio 1895 Distribution Fossils of this genus have been found in the Eocene of Italy and in the Oligocene The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified bu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeocarpilius Ignotus
''Palaeocarpilius'' is an extinct genus of crabs belonging to the family Carpiliidae. The type species of this genus is ''Palaeocarpilius macrocheilus''. These epifaunal carnivores lived in the Eocene and the Oligocene, from 48.6 to 28.4 Ma. Species *''Palaeocarpilius aquitanicus'' Milne-Edwards 1862 *'' Palaeocarpilius ignotus'' Milne-Edwards 1862 *''Palaeocarpilius intermedius'' Stubblefield 1927 *''Palaeocarpilius laevis'' Imaizumi 1939 *''Palaeocarpilius macrocheilus'' Desmarest 1822 *''Palaeocarpilius mississippiensis'' Rathbun 1935 *''Palaeocarpilius rugifer'' Stoliczka 1871 *''Palaeocarpilius valrovinensis'' De Gregorio 1895 Distribution Fossils of this genus have been found in the Eocene of Italy and in the Oligocene The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but ... ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeocarpilius Macrocheilus
''Palaeocarpilius'' is an extinct genus of crabs belonging to the family Carpiliidae. The type species of this genus is '' Palaeocarpilius macrocheilus''. These epifaunal carnivores lived in the Eocene and the Oligocene, from 48.6 to 28.4 Ma. Species *'' Palaeocarpilius aquitanicus'' Milne-Edwards 1862 *'' Palaeocarpilius ignotus'' Milne-Edwards 1862 *''Palaeocarpilius intermedius'' Stubblefield 1927 *''Palaeocarpilius laevis'' Imaizumi 1939 *'' Palaeocarpilius macrocheilus'' Desmarest 1822 *''Palaeocarpilius mississippiensis'' Rathbun 1935 *''Palaeocarpilius rugifer'' Stoliczka 1871 *''Palaeocarpilius valrovinensis'' De Gregorio 1895 Distribution Fossils of this genus have been found in the Eocene of Italy and in the Oligocene The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeocarpilius Aquitanicus
''Palaeocarpilius'' is an extinct genus of crabs belonging to the family Carpiliidae. The type species of this genus is ''Palaeocarpilius macrocheilus''. These epifaunal carnivores lived in the Eocene and the Oligocene, from 48.6 to 28.4 Ma. Species *'' Palaeocarpilius aquitanicus'' Milne-Edwards 1862 *'' Palaeocarpilius ignotus'' Milne-Edwards 1862 *''Palaeocarpilius intermedius'' Stubblefield 1927 *''Palaeocarpilius laevis'' Imaizumi 1939 *''Palaeocarpilius macrocheilus'' Desmarest 1822 *''Palaeocarpilius mississippiensis'' Rathbun 1935 *''Palaeocarpilius rugifer'' Stoliczka 1871 *''Palaeocarpilius valrovinensis'' De Gregorio 1895 Distribution Fossils of this genus have been found in the Eocene of Italy and in the Oligocene The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but .. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Italy
Italy ( it, Italia ), officially the Italian Republic, ) or the Republic of Italy, is a country in Southern Europe. It is located in the middle of the Mediterranean Sea, and its territory largely coincides with the homonymous geographical region. Italy is also considered part of Western Europe, and shares land borders with France, Switzerland, Austria, Slovenia and the enclaved microstates of Vatican City and San Marino. It has a territorial exclave in Switzerland, Campione. Italy covers an area of , with a population of over 60 million. It is the third-most populous member state of the European Union, the sixth-most populous country in Europe, and the tenth-largest country in the continent by land area. Italy's capital and largest city is Rome. Italy was the native place of many civilizations such as the Italic peoples and the Etruscans, while due to its central geographic location in Southern Europe and the Mediterranean, the country has also historically b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oligocene
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain. The name Oligocene was coined in 1854 by the German paleontologist Heinrich Ernst Beyrich from his studies of marine beds in Belgium and Germany. The name comes from the Ancient Greek (''olígos'', "few") and (''kainós'', "new"), and refers to the sparsity of extant forms of molluscs. The Oligocene is preceded by the Eocene Epoch and is followed by the Miocene The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" ... Epoch. The Oligocene is the third and final epoch of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oligocene Crustaceans
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain. The name Oligocene was coined in 1854 by the German paleontologist Heinrich Ernst Beyrich from his studies of marine beds in Belgium and Germany. The name comes from the Ancient Greek (''olígos'', "few") and (''kainós'', "new"), and refers to the sparsity of extant forms of Mollusca, molluscs. The Oligocene is preceded by the Eocene Epoch and is followed by the Miocene Epoch. The Oligocene is the third and final epoch of the Paleogene The Paleogene ( ; also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (Mya) to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene Crustaceans
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] |
