Charixa
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Charixa
''Charixa'' is a genus of bryozoans belonging to the family Electridae. Extant species of this genus are found in Northern America. Species: * '' Charixa bispinata'' Martha, Taylor & Rader, 2019 * '' Charixa burdonaria'' Taylor, Lazo & Aguirre-Urreta, 2008 * ''Charixa lhuydi'' (Pitt, 1976) (fossil, Cretaceous The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of th ... of England) References {{Taxonbar, from=Q39261161 Cheilostomatida ...
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Charixa Bispinata
''Charixa'' is a genus of bryozoans belonging to the family Electridae. Extant species of this genus are found in Northern America. Species: * '' Charixa bispinata'' Martha, Taylor & Rader, 2019 * '' Charixa burdonaria'' Taylor, Lazo & Aguirre-Urreta, 2008 * ''Charixa lhuydi'' (Pitt, 1976) (fossil, Cretaceous The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of th ... of England) References {{Taxonbar, from=Q39261161 Cheilostomatida ...
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Charixa Burdonaria
''Charixa'' is a genus of bryozoans belonging to the family Electridae. Extant species of this genus are found in Northern America. Species: * ''Charixa bispinata'' Martha, Taylor & Rader, 2019 * '' Charixa burdonaria'' Taylor, Lazo & Aguirre-Urreta, 2008 * ''Charixa lhuydi'' (Pitt, 1976) (fossil, Cretaceous The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of th ... of England) References {{Taxonbar, from=Q39261161 Cheilostomatida ...
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Electridae
Electridae is a family of bryozoans in the order Cheilostomatida. Genera The World Register of Marine Species lists the following genera: *'' Arbocuspis'' Nikulina, 2010 *'' Arbopercula'' Nikulina, 2010 *'' Aspidelectra'' Levinsen, 1909 *'' Bathypora'' MacGillivray, 1885 *''Charixa'' Lang, 1915 *''Conopeum'' Gray, 1848 **''Conopeum seurati'' *'' Einhornia'' Nikulina, 2007 *'' Electra'' Lamouroux, 1816 **'' Electra pilosa'' **'' Electra posidoniae'' *'' Gontarella'' Grischenko, Taylor & Mawatari, 2002 *'' Harpecia'' Gordon, 1982 *'' Lapidosella'' Gontar, 2010 *'' Mychoplectra'' Gordon & Parker, 1991 *'' Osburnea'' Nikulina, 2010 *''Pyripora ''Pyripora'' is a genus of bryozoans belonging to the family Electridae. The genus has almost cosmopolitan distribution In biogeography, cosmopolitan distribution is the term for the range of a taxon that extends across all or most of the w ...'' d'Orbigny, 1849 *'' Tarsocryptus'' Tilbrook, 2011 *'' Villicharixa'' Gordon, 1989 Referenc ...
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Bryozoans
Bryozoa (also known as the Polyzoa, Ectoprocta or commonly as moss animals) are a phylum of simple, aquatic invertebrate animals, nearly all living in sedentary colonies. Typically about long, they have a special feeding structure called a lophophore, a "crown" of tentacles used for filter feeding. Most marine bryozoans live in tropical waters, but a few are found in oceanic trenches and polar waters. The bryozoans are classified as the marine bryozoans (Stenolaemata), freshwater bryozoans (Phylactolaemata), and mostly-marine bryozoans (Gymnolaemata), a few members of which prefer brackish water. 5,869living species are known. At least two genera are solitary (''Aethozooides'' and ''Monobryozoon''); the rest are colonial. The terms Polyzoa and Bryozoa were introduced in 1830 and 1831, respectively. Soon after it was named, another group of animals was discovered whose filtering mechanism looked similar, so it was included in Bryozoa until 1869, when the two groups were n ...
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Fossil
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 ...
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Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ...
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