Spongioradsia
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Spongioradsia
''Spongioradsia'' is an genus of polyplacophoran molluscs. ''Spongioradsia'' became extinct during the Oligocene period. MolluscaBase eds. (2022). MolluscaBase. Spongioradsia Pilsbry, 1894. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=385630 on 2022-06-22 Species * '' Spongioradsia aleutica'' (Dall, 1878) ;Synonyms: * ''Spongioradsia foveolata'' Is. Taki, 1938: synonym of ''Callochiton foveolatus ''Callochiton'' is a genus of chitons in the family Callochitonidae. MolluscaBase eds. (2022). MolluscaBase. Callochiton Gray, 1847. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=1 ...'' (Is. Taki, 1938) (original combination) * ''Spongioradsia subaleutica'' Sirenko, 1976: synonym of ''Lepidochitona (Lepidochitona) subaleutica'' (Sirenko, 1976) (original combination) References External links Pilsbry, H. A. (1893-1895). Manual of conchology, struc ...
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Spongioradsia Aleutica
''Spongioradsia'' is an genus of polyplacophoran molluscs. ''Spongioradsia'' became extinct during the Oligocene period. MolluscaBase eds. (2022). MolluscaBase. Spongioradsia Pilsbry, 1894. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=385630 on 2022-06-22 Species * '' Spongioradsia aleutica'' (Dall, 1878) ;Synonyms: * ''Spongioradsia foveolata'' Is. Taki, 1938: synonym of ''Callochiton foveolatus ''Callochiton'' is a genus of chitons in the family Callochitonidae. MolluscaBase eds. (2022). MolluscaBase. Callochiton Gray, 1847. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=1 ...'' (Is. Taki, 1938) (original combination) * ''Spongioradsia subaleutica'' Sirenko, 1976: synonym of ''Lepidochitona (Lepidochitona) subaleutica'' (Sirenko, 1976) (original combination) References External links Pilsbry, H. A. (1893-1895). Manual of conchology, struc ...
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Chiton
Chitons () are marine molluscs of varying size in the class Polyplacophora (), formerly known as Amphineura. About 940 extant and 430 fossil species are recognized. They are also sometimes known as gumboots or sea cradles or coat-of-mail shells or suck-rocks, or more formally as loricates, polyplacophorans, and occasionally as polyplacophores. Chitons have a shell composed of eight separate shell plates or valves. These plates overlap slightly at the front and back edges, and yet articulate well with one another. Because of this, the shell provides protection at the same time as permitting the chiton to flex upward when needed for locomotion over uneven surfaces, and even allows the animal to curl up into a ball when dislodged from rocks. The shell plates are encircled by a skirt known as a girdle. Habitat Chitons live worldwide, from cold waters through to the tropics. They live on hard surfaces, such as on or under rocks, or in rock crevices. Some species live quite hi ...
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Mollusc
Mollusca is the second-largest phylum of invertebrate animals after the Arthropoda, the members of which are known as molluscs or mollusks (). Around 85,000  extant species of molluscs are recognized. The number of fossil species is estimated between 60,000 and 100,000 additional species. The proportion of undescribed species is very high. Many taxa remain poorly studied. Molluscs are the largest marine phylum, comprising about 23% of all the named marine organisms. Numerous molluscs also live in freshwater and terrestrial habitats. They are highly diverse, not just in size and anatomical structure, but also in behaviour and habitat. The phylum is typically divided into 7 or 8  taxonomic classes, of which two are entirely extinct. Cephalopod molluscs, such as squid, cuttlefish, and octopuses, are among the most neurologically advanced of all invertebrates—and either the giant squid or the colossal squid is the largest known invertebrate species. The gastr ...
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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 Epoch. The Oligocene is the third and final epoch of the Paleogene Period. The Oligocene is often considered an important time of transition, a link between the archaic world of the tropical Eocene and the more modern ecosystems of the Miocene. Major changes during the Oligocene included a global expansi ...
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Callochiton Foveolatus
''Callochiton'' is a genus of chitons in the family Callochitonidae. MolluscaBase eds. (2022). MolluscaBase. Callochiton Gray, 1847. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=138085 on 2022-06-22 Species * '' Callochiton crocinus'' (Reeve, 1847) * '' Callochiton dentatus'' Spengler, 1797 * ''Callochiton empleurus ''Callochiton empleurus'' is a species of chiton in the family Family (from la, familia) is a group of people related either by consanguinity (by recognized birth) or affinity (by marriage or other relationship). The purpose of the family ...'' (Hutton, 1872) * '' Callochiton kapitiensis'' Mestayer, 1926 * '' Callochiton laevis'' * '' Callochiton mortenseni'' Odhner, 1924 * '' Callochiton puniceus'' (Gould, 1846) * '' Callochiton septemvalvis'' ( Montagu, 1803) * '' Callochiton subeudoxa'' ( Iredale and Hull, 1930 * '' Callochiton sulculatus'' Suter, 1907 References * * ...
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Oligocene Animals
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 Epoch. The Oligocene is the third and final epoch of the Paleogene Period. The Oligocene is often considered an important time of transition, a link between the archaic world of the tropical Eocene and the more modern ecosystems of the Miocene. Major changes during the Oligocene included a global expansion ...
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