Protomonaxonida
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Protomonaxonida
Protomonaxonida is an extinct order of sea sponges. It is a paraphyletic group gathering the most ancient species from the Burgess Shale to modern sponges. Families and genera * Family † Choiidae Laubenfels, 1925 ** Genus †'' Allantospongia'' Rigby & Hou, 1995 ** Genus †''Choia'' Walcott, 1920 ** Genus †'' Choiaella'' Rigby & Hou, 1995 ** Genus †'' Lenica'' Goryanskiy, 1977 * Family † Halichondritidae Rigby, 1986 ** Genus †'' Halichondrites'' Walcott, 1920 ** Genus †'' Pohlispongia'' Rigby & von Bitter, 2005 * Family † Hamptoniidae De Laubenfels, 1955 ** Genus †'' Hamptonia'' Walcott, 1920 ** Genus †'' Hamptoniella'' Rigby & Collins, 2004 * Family † Hazeliidae De Laubenfels, 1955 ** Genus †'' Crumillospongia'' Rigby, 1986 ** Genus †'' Falospongia'' Rigby, 1986 ** Genus †'' Hazelia'' Walcott, 1920 * Family † Leptomitidae De Laubenfels, 1955 ** Genus †'' Leptomitus'' Walcott, 1886 ** Genus †'' Paraleptomitella'' Chen et al., 1989 ** Genus † ...
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Pirania
''Pirania'' is an extinct genus of sea sponge known from the Middle Cambrian Burgess Shale and the Ordovician Fezouata formation. It is named after Mount St. Piran, a mountain situated in the Bow River Valley in Banff National Park, Alberta Alberta ( ) is one of the thirteen provinces and territories of Canada. It is part of Western Canada and is one of the three prairie provinces. Alberta is bordered by British Columbia to the west, Saskatchewan to the east, the Northwest Ter .... It was first described in 1920 by Charles Doolittle Walcott. 198 specimens of ''Pirania'' are known from the Greater Phyllopod bed, where they comprise 0.38% of the community. References External links * Burgess Shale fossils Protomonaxonida Burgess Shale sponges Prehistoric sponge genera Cambrian first appearances Middle Ordovician extinctions Taxa named by Charles Doolittle Walcott Fossil taxa described in 1920 {{paleo-sponge-stub Cambrian genus extinctions ...
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Choiaella
''Choiaella'' is an extinct genus of sea sponge ranging from the Chengjiang lagerstatten until the Lower Silurian. It is closely related to the genera ''Choia'' and '' Allantospongia'', which the Chengjiang fauna species ''C. radiata'' coexisted sympatrically with. The species ''C. scotica'' is known from the Caradoc-aged fine sandstone of Wallace's Cast, Southern Uplands of Scotland Scotland (, ) is a country that is part of the United Kingdom. Covering the northern third of the island of Great Britain, mainland Scotland has a border with England to the southeast and is otherwise surrounded by the Atlantic Ocean to the .... The Silurian species has not been formally named. References Maotianshan shales fossils Protomonaxonida Silurian extinctions Cambrian first appearances Prehistoric sponge genera Fossil taxa described in 1995 {{silurian-animal-stub ...
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Hazeliidae
Hazeliidae is an extinct family of spicular Cambrian sea sponges known from the Burgess Shale, the Marjum Formation of Utah, and possibly Chengjiang Chengjiang (; earlier Tchinkiang) is a city located in Yuxi, Yunnan Province, China, just north of Fuxian Lake. Administrative divisions Chengjiang City has 2 subdistricts and 4 townships. ;2 subdistricts * Fenglu () * Longjie () ;4 towns C .... It was described by Charles Walcott in 1920. References Protomonaxonida Ordovician invertebrates Cambrian sponges Prehistoric sponge families Cambrian first appearances Middle Ordovician extinctions {{demosponge-stub ...
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Leptomitus
''Leptomitus'' is a genus of demosponge known from the Middle Cambrian The Cambrian Period ( ; sometimes symbolized C with bar, Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million ... Burgess Shale. Its name is derived from the Greek ''lept'' ("slender") and ''mitos'' ("thread"), referring to the overall shape of the sponge. 138 specimens of ''Leptomitus'' are known from the Greater Phyllopod bed, where they comprise 0.26% of the community. References External links * Burgess Shale fossils Protomonaxonida Prehistoric sponge genera Burgess Shale sponges Cambrian genus extinctions {{paleo-sponge-stub ...
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Hazelia
''Hazelia'' is a genus of spicular Cambrian demosponge known from the Burgess Shale, the Marjum formation The Marjum Formation is a Cambrian geological formation that overlies the Wheeler Shale in the House Range, Utah. It is known for its occasional preservation of soft-bodied tissue, and is slightly younger than the Burgess Shale The Burgess S ... of Utah, and possibly Chengjiang. It was described by Charles Walcott in 1920. Its tracts are mainly radial and anastomose to form an irregular skeleton. Its oxeas form a fine net in the skin of the sponge. References External links * Protomonaxonida Burgess Shale sponges Maotianshan shales fossils Cambrian first appearances Middle Ordovician extinctions Prehistoric sponge genera Taxa named by Charles Doolittle Walcott Fossil taxa described in 1920 {{demosponge-stub Cambrian genus extinctions ...
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Falospongia
''Falospongia'' is a genus of sponge made up of radiating fronds, known from the Middle Cambrian Burgess Shale. Its name is derived from the Latin Latin (, or , ) is a classical language belonging to the Italic branch of the Indo-European languages. Latin was originally a dialect spoken in the lower Tiber area (then known as Latium) around present-day Rome, but through the power of the ... ''fala'' ("scaffold") and ''spongia'' ("sponge"), referring to the open framework of the skeleton. It superficially resembles '' Haplistion'' but is monaxial. 5 specimens of ''Falospongia'' are known from the Greater Phyllopod bed, where they comprise under 0.1% of the community. References External links * Burgess Shale fossils Protomonaxonida Burgess Shale sponges Prehistoric sponge genera Cambrian genus extinctions {{paleo-sponge-stub ...
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Crumillospongia
''Crumillospongia'' is a genus of middle Cambrian sponges known from the Burgess Shale and other localities from the Lower and Middle Cambrian. Its name is derived from the Latin ''crumilla'' ("money purse") and ''spongia'' ("sponge"), a reflection of its similarity to a small leathery money purse A money bag (or money sack) is a bag normally used to hold and transport coins and banknotes, often closed with a drawstring.Phyllopod bed, where they comprise 0.1% of the community.


References


External links


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Hamptoniella
''Hamptoniella'' is an extinct genus of sponges known from the Middle Cambrian Middle or The Middle may refer to: * Centre (geometry), the point equally distant from the outer limits. Places * Middle (sheading), a subdivision of the Isle of Man * Middle Bay (other) * Middle Brook (other) * Middle Creek (di ... Burgess Shale. References External links * Protomonaxonida Burgess Shale sponges Prehistoric sponge genera Cambrian genus extinctions {{paleo-sponge-stub ...
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Hamptonia
''Hamptonia'' is an extinct genus of sea sponge known from the Middle Cambrian Burgess Shale and the Lower Ordovician Fezouata formation The Fezouata Formation or Fezouata Shale is a geological formation in Morocco which dates to the Early Ordovician.
. It was first described in 1920 by Charles Doolittle Walcott. 48 specimens of ''Hamptonia'' are known from the Greater Phyllopod bed, where they comprise < 0.1% of the community.


References


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Halichondrites
''Halichondrites'', sometimes mis-spelt ''Halicondrites'' is an extinct genus of sea sponge known from the Middle Cambrian Burgess Shale. 7 specimens of ''Halichondrites'' are known from the Greater Phyllopod bed, where they comprise < 0.1% of the community.


Taxonomy and species

The genus ''Halichondrites'' was erected by John William Dawson in 1889, who described the species ''Halichondrites confusus'' from the Ordovician of at Little Métis. In 1920, Charles Doolittle Walcott, considering ''H. confusus'' to be ina ...
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Choia
''Choia'' is a genus of extinct demosponge ranging from the Cambrian until the Lower Ordovician periods. Fossils of ''Choia'' have been found in the Burgess Shale in British Columbia; the Maotianshan shales of China; the Wheeler Shale in Utah; and the Lower Ordovician Fezouata formation. It was first described in 1920 by Charles Doolittle Walcott. Life habit ''Choia'' was originally thought to be not attached to the sea bed: the living animal was originally thought to rest directly on the substrate, with the radiating spines from the edge of its flattish, conical body, giving an appearance not unlike that of the peak of a big top, with guy lines. Recently discovered fossils from Lower Ordovician Morocco show that the living animal was actually suspended high above the seafloor, attached via stalk-like spines derived from spicules. Water is assumed to have entered the sponge parallel to the spines, being expelled, presumably, from a central opening. Species reached up to ...
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