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Catenipora
''Catenipora'' is an extinct genus of tabulate corals in the family Halysitidae ''Halysitidae'' is an extinct family of tabulate coral Tabulata, commonly known as tabulate corals, are an order of extinct forms of coral. They are almost always colonial, forming colonies of individual hexagonal cells known as corallites ..., known from the Ordovician to the Silurian. ''C. elegans'' is known from the Silurian of Estonia. Species * †''Catenipora approximata'' * †''Catenipora arctica'' * †''Catenipora capilliformis'' * †''Catenipora copulata'' * †''Catenipora crassaeformis'' * †''Catenipora distans'' * †''Catenipora elegans'' * †''Catenipora escharoides'' * †''Catenipora exilis'' * †''Catenipora gotlandica'' * †''Catenipora jingyangensis'' * †''Catenipora maxima'' * †''Catenipora obliqua'' * †''Catenipora panga'' * †''Catenipora robusta'' * †''Catenipora rubraeformis'' * †''Catenipora septosa'' * †''Catenipora tapaensis' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Halysitidae
''Halysitidae'' is an extinct family of tabulate coral Tabulata, commonly known as tabulate corals, are an order of extinct forms of coral. They are almost always colonial, forming colonies of individual hexagonal cells known as corallites defined by a skeleton of calcite, similar in appearance to ...s. These tabulate corals lived from Ordovician to Devonian (from 471.8 to 412.3 Ma). Fossil corals of the family ''Halysitidae'' have been found in the sediments of Afghanistan, Canada, United States, Venezuela and Australia. Genera * '' Acanthohalysites'' Hamada 1957 * '' Catenipora'' Lamarck 1816 * '' Cystihalysites'' Chernyshev 1941 * '' Eocatenipora'' Hamada 1957 * '' Falsicatenipora'' Hamada 1958 * '' Halysites'' von Waldheim 1828 * '' Hexismia'' Sokolov 1955 * '' Quepora'' Sinclair 1955 * '' Schedohalysites'' Hamada 1957 * '' Solenihalysites'' Stasinska 1967 * '' Spumaeolites'' Zhizhina 1967 References Tabulata Prehistoric cnidarian families Ordovician first appe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Museum Of Man And Nature
:''This about the German museum; for the Canadian one, see Manitoba Museum''. The Museum Mensch und Natur (English language, English Museum of Man and Nature) is a natural history museum. It is a tenant of the Nymphenburg Palace in Munich, Germany. Bear exhibit In 2006, the museum received the stuffed and mounted body of "Bear JJ1", nicknamed "Bruno" in the German-language press, which was a brown bear that was shot dead by a hunter as a public safety measure after several unsuccessful efforts to capture him alive. JJ1 had been part of a wildlife restoration program in Italy but walked across Austria into Germany. The bear was put on display next to the last bear previously killed (in 1835) in Bavaria. See also *List of museums in Germany *List of natural history museums References External links Museum Mensch und Natur website Natural history museums in Germany Museums in Munich {{Germany-museum-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jean-Baptiste Lamarck
Jean-Baptiste Pierre Antoine de Monet, chevalier de Lamarck (1 August 1744 – 18 December 1829), often known simply as Lamarck (; ), was a French naturalist, biologist, academic, and soldier. He was an early proponent of the idea that biological evolution occurred and proceeded in accordance with natural laws. Lamarck fought in the Seven Years' War against Prussia, and was awarded a commission for bravery on the battlefield. Posted to Monaco, Lamarck became interested in natural history and resolved to study medicine. Packard (1901), p. 15. He retired from the army after being injured in 1766, and returned to his medical studies. Lamarck developed a particular interest in botany, and later, after he published the three-volume work ''Flore françoise'' (1778), he gained membership of the French Academy of Sciences in 1779. Lamarck became involved in the Jardin des Plantes and was appointed to the Chair of Botany in 1788. When the French National Assembly founded the Mus� ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tabulata
Tabulata, commonly known as tabulate corals, are an order of extinct forms of coral. They are almost always colonial, forming colonies of individual hexagonal cells known as corallites defined by a skeleton of calcite, similar in appearance to a honeycomb. Adjacent cells are joined by small pores. Their distinguishing feature is their well-developed horizontal internal partitions (''tabulae'') within each cell, but reduced or absent vertical internal partitions ( ''septa''). They are usually smaller than rugose corals, but vary considerably in shape, from flat to conical to spherical. Around 300 species have been described. Among the most common tabulate corals in the fossil record are '' Aulopora'', '' Favosites'', '' Halysites'', '' Heliolites'', '' Pleurodictyum'', ''Sarcinula'' and '' Syringopora''. Tabulate corals with massive skeletons often contain endobiotic symbionts, such as cornulitids and '' Chaetosalpinx''. Like rugose corals, they lived entirely during the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prehistoric Anthozoa Genera
Prehistory, also known as pre-literary history, is the period of human history between the use of the first stone tools by hominins 3.3 million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared 5000 years ago. It took thousands of years for writing systems to be widely adopted, with writing spreading to almost all cultures by the 19th century. The end of prehistory therefore came at very different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilisation, and ancient Egypt were the first civilizations to develop their own scripts and to keep historical records, with their neighbors following. Most other civilizations reached the end of prehistory during the following Iron Age. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleozoic Cnidarians
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in the ocean but e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossil Taxa Described In 1816
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absolut ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleozoic Life Of Ontario
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in the ocean but e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_im_Museum_Mensch_und_Natur_002.jpg "Click for more on -> Museum Of Man And Nature")
