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Palaeotherium
''Palaeotherium'' (Ancient Greek for 'old beast') is an extinct genus of perissodactyl ungulate known from the Mid Eocene to earliest Oligocene of Europe. First described by French naturalist Georges Cuvier in 1804, ''Palaeotherium'' was among the first Paleogene mammals to be described. Taxonomy ''Palaeotherium'' belongs to the family Palaeotheriidae, a group proposed to consist of two subfamilies, the Palaeotheriinae representing ''Palaeotherium'' and the Plagiolophinae containing the closely related '' Plagiolophus''. Although at times proposed to be ancestral to modern horses the palaeotheres are now considered a sister taxon to the Equidae, and not part of the same lineage. The species and subspecies referable to ''Palaeotherium'' are a subject of debate, due in part to the diversity of species within the genus. Species and subspecies are mainly assigned based on dental and cranial characteristics. Description ''Palaeotherium'' was a diverse genus of herbivorous perissod ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeotherium Magnum 4
''Palaeotherium'' (Ancient Greek for 'old beast') is an extinct genus of perissodactyl ungulate known from the Mid Eocene to earliest Oligocene of Europe. First described by French naturalist Georges Cuvier in 1804, ''Palaeotherium'' was among the first Paleogene mammals to be described. Taxonomy ''Palaeotherium'' belongs to the family Palaeotheriidae, a group proposed to consist of two subfamilies, the Palaeotheriinae representing ''Palaeotherium'' and the Plagiolophinae containing the closely related '' Plagiolophus''. Although at times proposed to be ancestral to modern horses the palaeotheres are now considered a sister taxon to the Equidae, and not part of the same lineage. The species and subspecies referable to ''Palaeotherium'' are a subject of debate, due in part to the diversity of species within the genus. Species and subspecies are mainly assigned based on dental and cranial characteristics. Description ''Palaeotherium'' was a diverse genus of herbivorous perissod ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeotherium
''Palaeotherium'' (Ancient Greek for 'old beast') is an extinct genus of perissodactyl ungulate known from the Mid Eocene to earliest Oligocene of Europe. First described by French naturalist Georges Cuvier in 1804, ''Palaeotherium'' was among the first Paleogene mammals to be described. Taxonomy ''Palaeotherium'' belongs to the family Palaeotheriidae, a group proposed to consist of two subfamilies, the Palaeotheriinae representing ''Palaeotherium'' and the Plagiolophinae containing the closely related '' Plagiolophus''. Although at times proposed to be ancestral to modern horses the palaeotheres are now considered a sister taxon to the Equidae, and not part of the same lineage. The species and subspecies referable to ''Palaeotherium'' are a subject of debate, due in part to the diversity of species within the genus. Species and subspecies are mainly assigned based on dental and cranial characteristics. Description ''Palaeotherium'' was a diverse genus of herbivorous perissod ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeotheriidae
Palaeotheriidae is an extinct family of herbivorous perissodactyl mammals related to equids. They ranged across Europe and Asia from the Eocene through to the early Oligocene 55–33 Ma, existing for approximately . Living in dense forests, they ate soft leaves, shoots, berries, and leaf matter picked up from the forest floor. Morphology Palaeothere sizes ranged from at the shoulder, and weighed an estimated .S. Legendre. 1988. Les communautes de mammiferes du Paleogene (Eocene superieur et Oligocene) d'Europe occidentale: structure, milieux et evolution. Ph.D. thesis, Universite des Sciences et Techniques du Languedoc, Montpellier, France. 2 volumes. 1-265 Extinction Evidence suggests that the palaeotheriidae went extinct in Eurasia during the Early Oligocene, approximately 33 Ma, as part of a faunal turnover event known as the Grande Coupure. The Eocene-Oligocene transition marked a significant global cooling event caused by the onset of Antarctic glaciation. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
George Cuvier
Jean Léopold Nicolas Frédéric, Baron Cuvier (; 23 August 1769 – 13 May 1832), known as Georges Cuvier, was a French naturalist and zoologist, sometimes referred to as the "founding father of paleontology". Cuvier was a major figure in natural sciences research in the early 19th century and was instrumental in establishing the fields of comparative anatomy and paleontology through his work in comparing living animals with fossils. Cuvier's work is considered the foundation of vertebrate paleontology, and he expanded Linnaean taxonomy by grouping classes into phyla and incorporating both fossils and living species into the classification. Cuvier is also known for establishing extinction as a fact—at the time, extinction was considered by many of Cuvier's contemporaries to be merely controversial speculation. In his ''Essay on the Theory of the Earth'' (1813) Cuvier proposed that now-extinct species had been wiped out by periodic catastrophic flooding events. In this way, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buttes Chaumont
The Parc des Buttes Chaumont () is a public park situated in northeastern Paris, France, in the 19th arrondissement. Occupying , it is the fifth-largest park in Paris, after the Bois de Vincennes, Bois de Boulogne, Parc de la Villette and Tuileries Garden. Opened in 1867, late in the regime of Napoleon III, it was built according to plans by Jean-Charles Adolphe Alphand, who created all the major parks demanded by the Emperor. The park has of roads and of paths. The most famous feature of the park is the Temple de la Sibylle, inspired by the Temple of Vesta in Tivoli, Italy, and perched at the top of a cliff fifty metres above the waters of the artificial lake. History The park took its name from the bleak hill which occupied the site, which, because of the chemical composition of its soil, was almost bare of vegetation – it was called ''Chauve-mont'', or bare hill. The area, just outside the limits of Paris until the mid-19th century, had a sinister reputation; it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Georges Cuvier
Jean Léopold Nicolas Frédéric, Baron Cuvier (; 23 August 1769 – 13 May 1832), known as Georges Cuvier, was a French natural history, naturalist and zoology, zoologist, sometimes referred to as the "founding father of paleontology". Cuvier was a major figure in natural sciences research in the early 19th century and was instrumental in establishing the fields of comparative anatomy and paleontology through his work in comparing living animals with fossils. Cuvier's work is considered the foundation of vertebrate paleontology, and he expanded Linnaean taxonomy by grouping classes into phylum, phyla and incorporating both fossils and living species into the classification. Cuvier is also known for establishing extinction as a fact—at the time, extinction was considered by many of Cuvier's contemporaries to be merely controversial speculation. In his ''Essay on the Theory of the Earth'' (1813) Cuvier proposed that now-extinct species had been wiped out by periodic catastrophi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Montmartre
Montmartre ( , ) is a large hill in Paris's northern 18th arrondissement. It is high and gives its name to the surrounding district, part of the Right Bank. The historic district established by the City of Paris in 1995 is bordered by Rue Caulaincourt and Rue Custine on the north, the Rue de Clignancourt on the east and the Boulevard de Clichy and Boulevard de Rochechouart to the south, containing . Montmartre is primarily known for its artistic history, the white-domed Basilica of the Sacré-Cœur on its summit, as well as a nightclub district. The other church on the hill, Saint Pierre de Montmartre, built in 1147, was the church of the prestigious Montmartre Abbey. On 15 August 1534, Saint Ignatius of Loyola, Saint Francis Xavier and five other companions bound themselves by vows in the Martyrium of Saint Denis, 11 Rue Yvonne Le Tac, the first step in the creation of the Jesuits. Near the end of the 19th century and at the beginning of the 20th, during the Belle Époqu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bartonian
The Bartonian is, in the ICS's geologic time scale, a stage or age in the middle Eocene Epoch or Series. The Bartonian Age spans the time between . It is preceded by the Lutetian and is followed by the Priabonian Age. Stratigraphic definition The Bartonian Stage was introduced by Swiss stratigrapher Karl Mayer-Eymar in 1857. The name derives from the coastal village Barton-on-Sea (part of New Milton) in southern England. The Barton Group, a lithostratigraphic unit from the south English Hampshire Basin, is of Bartonian age. The distinction between group and stage was made in the second part of the 20th century, when stratigraphers saw the need to distinguish between litho- and chronostratigraphy. The base of the Bartonian is at the first appearance of the calcareous nanoplankton species ''Reticulofenestra reticulata''. In 2009, an official reference profile (GSSP) for the base of the Bartonian had not yet been established. The top of the Bartonian Stage (the base of the Pria ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hordle
Hordle is a village and civil parish in the county of Hampshire, England. It is situated between the Solent coast and the New Forest, and is bordered by the towns of Lymington and New Milton. Like many New Forest parishes Hordle has no village centre. The civil parish includes the hamlets of Tiptoe and Everton as well as part of Downton. The parish was originally much larger; stretching from the New Forest boundary to Hurst Castle. The village Hordle has several shops including a post office, a pharmacy, and Co-operative Stores.History – HordlePC The village also has a primary school, and a : ''The Three Bells''. The present civil parish is somewhat smaller than the it used to cont ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hampshire
Hampshire (, ; abbreviated to Hants) is a ceremonial county, ceremonial and non-metropolitan county, non-metropolitan counties of England, county in western South East England on the coast of the English Channel. Home to two major English cities on its south coast, Southampton and Portsmouth, Hampshire is the 9th-most populous county in England. The county town of Hampshire is Winchester, located in the north of the county. The county is bordered by Dorset to the south-west, Wiltshire to the north-west, Berkshire to the north, Surrey to the north-east, and West Sussex to the south east. The county is geographically diverse, with upland rising to and mostly south-flowing rivers. There are areas of downland and marsh, and two national parks: the New Forest National Park, New Forest and part of the South Downs National Park, South Downs, which together cover 45 per cent of Hampshire. Settled about 14,000 years ago, Hampshire's recorded history dates to Roman Britain, when its chi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Creechbarrow Limestone
The Creechbarrow Limestone is a geologic formation in England. It preserves fossils dating back to the Paleogene period. See also * List of fossiliferous stratigraphic units in England See also *Lists of fossiliferous stratigraphic units in Europe * Lists of fossiliferous stratigraphic units in the United Kingdom References * {{DEFAULTSORT:Fossiliferous stratigraphic units in England England England is a country ... References * Paleogene England Limestone formations {{England-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
