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Polygnathus Communis
''Polygnathus'' is an extinct genus of conodonts. Species * †''Polygnathus acrinodosus'' Aboussalam 2003 * †''Polygnathus alkhovikovae'' Baranov, Slavík & Blodgett 2014 * †''Polygnathus angustipennatus'' Bischoff and Ziegler 1957 * †''Polygnathus aragonensis'' Martínez-Pérez & Valenzuela-Ríos 2014 * †''Polygnathus arthuri'' Baranov, Slavík & Blodgett 2014 * †''Polygnathus bardashevi'' Baranov, Slavík & Blodgett 2014 * †''Polygnathus bicristatus'' Mossoni et al. 2015 * †''Polygnathus burretti'' Savage 2013 * †''Polygnathus chongqingensis'' Wang in Gong et al. 2012 * †''Polygnathus carlsi'' Martínez-Pérez & Valenzuela-Ríos 2014 * †''Polygnathus communis'' ** †''Polygnathus communis hanensis'' Savage 2013 ** †''Polygnathus communis longanensis'' Qie et al. 2014 ** †''Polygnathus communis namdipensis'' Savage 2013 ** †''Polygnathus communis phaphaensis'' Savage 2013 * †''Polygnathus costatus'' Klapper 1971 ** †''Polygnathus costatus part ...
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Animal
Animals are multicellular, eukaryotic organisms in the Kingdom (biology), biological kingdom Animalia. With few exceptions, animals Heterotroph, consume organic material, Cellular respiration#Aerobic respiration, breathe oxygen, are Motility, able to move, can Sexual reproduction, reproduce sexually, and go through an ontogenetic stage in which their body consists of a hollow sphere of Cell (biology), cells, the blastula, during Embryogenesis, embryonic development. Over 1.5 million Extant taxon, living animal species have been Species description, described—of which around 1 million are Insecta, insects—but it has been estimated there are over 7 million animal species in total. Animals range in length from to . They have Ecology, complex interactions with each other and their environments, forming intricate food webs. The scientific study of animals is known as zoology. Most living animal species are in Bilateria, a clade whose members have a Symmetry in biology#Bilate ...
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2016 In Paleontology
Flora Plants Fungi Cnidarians Research * '' Yunnanoascus haikouensis'', previously thought to be a member of Ctenophora, is reinterpreted as a crown-group medusozoan by Han ''et al.'' (2016). * A study on the fossil corals from the Late Triassic (Norian) outcrops in Antalya Province (Turkey), indicating that the corals lived in symbiosis with photosynthesizing dinoflagellate algae, is published by Frankowiak ''et al.'' (2016). New taxa Arthropods Bryozoans Brachiopods Molluscs Echinoderms Conodonts Fishes Amphibians Research * A study on the histology and growth histories of the humeri of the specimens of '' Acanthostega'' recovered from the mass-death deposit of Stensiö Bjerg (Greenland) is published by Sanchez ''et al.'' (2016), who argue that even the largest individuals from this deposit are juveniles. * Fossils of a tetrapod resembling ''Ichthyostega'' and a probable whatcheeriid- grade tetrapod are described from two Devonian (Famennian) localit ...
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Ozarkodinida Genera
Ozarkodinida is an extinct conodont order. It is part of the clade Prioniodontida, also known as the "complex conodonts". Name Ozarkodinida is named after the Ozark Mountains of Missouri Missouri is a U.S. state, state in the Midwestern United States, Midwestern region of the United States. Ranking List of U.S. states and territories by area, 21st in land area, it is bordered by eight states (tied for the most with Tennessee ..., United States. Elements The feeding apparatus of ozarkodinids is composed at the front of an axial Sa element, flanked by two groups of four close-set elongate Sb and Sc elements which were inclined obliquely inwards and forwards. Above these elements lay a pair of arched and inward pointing (makellate) M elements. Behind the S-M array lay transversely oriented and bilaterally opposed (pectiniform, i.e. comb-shaped) Pb and Pa elements. References External links * * Prehistoric jawless fish orders {{Conodont-stub ...
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Fossilworks
Fossilworks is a portal which provides query, download, and analysis tools to facilitate access to the Paleobiology Database, a large relational database assembled by hundreds of paleontologists from around the world. History Fossilworks was created in 1998 by John Alroy and is housed at Macquarie University. It includes many analysis and data visualization tools formerly included in the Paleobiology Database.{{cite web, title=Frequently asked questions, url=http://www.fossilworks.org/cgi-bin/bridge.pl?page=FAQ, publisher=Fossilworks, access-date=17 December 2021 References {{Reflist External links {{Wikidata property, P842 * [Baidu]  




List Of Global Boundary Stratotype Sections And Points
This is a list of Global Boundary Stratotype Sections and Points. Since 1977, Global Boundary Stratotype Sections and Points (abbreviated GSSPs) are internationally agreed upon reference points on stratigraphic sections of rock which define the lower boundaries of stages on the geologic time scale. They are selected by the International Commission on Stratigraphy based on multiple factors, but their accessibility and the degree to which they are representative of the same boundary on sections worldwide are among the most important. Since GSSPs require well-preserved sections of rock without interruptions in sedimentation, and since most are defined by different stages of animal life, defining them becomes progressively more difficult as one goes further back in time. Organization of this list This list is divided first into the geologic eras of the Phanerozoic (the Cenozoic, the Mesozoic, and the Paleozoic) and then into the geologic periods of each era. Each period is marke ...
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Patrognathus
''Patrognathus'' is an extinct genus of conodonts. Use in stratigraphy The Tournaisian, the oldest age of the Mississippian Mississippian may refer to: * Mississippian (geology), a subperiod of the Carboniferous period in the geologic timescale, roughly 360 to 325 million years ago *Mississippian culture, a culture of Native American mound-builders from 900 to 1500 AD ... (also known as Lower Carboniferous) contains eight conodont biozones, four of which contain ''Patrognathus'' species: * the zone of '' Siphonodella quadruplicata'' and ''Patrognathus andersoni'' (upper zone of ''Patrognathus andersoni'') * the lower zone of ''Patrognathus andersoni'' * the zone of ''Patrognathus variabilis'' * the zone of ''Patrognathus crassus'' References External links * * Ozarkodinida genera Mississippian conodonts Tournaisian life Fossil taxa described in 1969 Mississippian first appearances Mississippian extinctions {{conodont-stub ...
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Siphonodella
''Siphonodella'' is an extinct genus of conodonts. ''Siphonodella banraiensis'' is from the Late Devonian of Thailand. ''Siphonodella nandongensis'' is from the Early Carboniferous of the Baping Formation in China.New material of the Early Carboniferous conodonts from the lower member of the Baping Formation in Nandong, Guangxi, China. Zhihong Li, Zhongqin Peng, Long Cheng, Chuanshang Wang and Baozhong Wang, Acta Micropalaeontologica Sinica, 2014, volume 31, issue 3, pages 271–284 Use in stratigraphy The Tournaisian, the oldest age of the Mississippian (also known as Lower Carboniferous) contains eight conodont biozones, two of which are characterized by ''Siphonodella'' species: * the zone of '' Gnathodus typicus'' and ''Siphonodella isosticha'' * the zone of ''Siphonodella quadruplicata'' and '' Patrognathus andersoni'' (upper zone of ''Patrognathus andersoni'') The GSSP Golden Spike for the Tournaisian The Tournaisian is in the ICS geologic timescale the lowest sta ...
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Dollymae Bouckaerti
''Dollymae'' is an extinct genus of conodonts.Les conodontes du Tournaisien supérieur de la Belgique: note préliminaire. E Groessens, 1971, Service Géologique de Belgique Use in stratigraphy The Tournaisian, the oldest age of the Mississippian Mississippian may refer to: * Mississippian (geology), a subperiod of the Carboniferous period in the geologic timescale, roughly 360 to 325 million years ago *Mississippian culture, a culture of Native American mound-builders from 900 to 1500 AD ... (also known as Lower Carboniferous) contains eight conodont biozones, one of which is the zone of ''Dollymae bouckaerti''. References External links * * Mississippian conodonts Conodont genera Fossil taxa described in 1959 {{conodont-stub ...
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Scaliognathus Anchoralis
Mississippian may refer to: *Mississippian (geology), a subperiod of the Carboniferous period in the geologic timescale, roughly 360 to 325 million years ago *Mississippian culture, a culture of Native American mound-builders from 900 to 1500 AD *Mississippian Railway, a short line railroad *A native of Mississippi Mississippi () is a state in the Southeastern region of the United States, bordered to the north by Tennessee; to the east by Alabama; to the south by the Gulf of Mexico; to the southwest by Louisiana; and to the northwest by Arkansas. Mis ... See also * Mississippi (other) {{Disambiguation ...
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Gnathodus
''Gnathodus'' is an extinct conodont genus in the family Idiognathodontidae. Use in stratigraphy The Tournaisian, the oldest age of the Mississippian (also known as Lower Carboniferous), contains eight conodont biozones, 3 of which are defined by ''Gnathodus species'': * the zone of ''Gnathodus pseudosemiglaber'' and ''Scaliognathus anchoralis'' * the zone of ''Gnathodus semiglaber'' and ''Polygnathus communis'' * the zone of ''Gnathodus typicus'' and ''Siphonodella isosticha'' The Visean, the second age of the Mississippian, contains four conodont biozones, two of which are defined by ''Gnathodus'' species: * the ''Gnathodus bilineatus'' Zone * the ''Gnathodus texanus'' Zone The Serpukhovian, the third or youngest age of the Mississippian, includes four conodont biozones, two of which are defined by ''Gnathodus'' species: * the ''Gnathodus postbilineatus'' Zone * the ''Gnathodus bollandensis'' Zone References * Proposal of Gnathodus bilineatus (Roundy, 1926) as type s ...
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Tournaisian
The Tournaisian is in the ICS geologic timescale the lowest stage or oldest age of the Mississippian, the oldest subsystem of the Carboniferous. The Tournaisian age lasted from Ma to Ma. It is preceded by the Famennian (the uppermost stage of the Devonian) and is followed by the Viséan. Name and regional alternatives The Tournaisian was named after the Belgian city of Tournai. It was introduced in scientific literature by Belgian geologist André Hubert Dumont in 1832. Like many Devonian and lower Carboniferous stages, the Tournaisian is a unit from West European regional stratigraphy that is now used in the official international time scale. The Tournaisian correlates with the regional North American Kinderhookian and lower Osagean stages and the Chinese Tangbagouan regional stage. In British stratigraphy, the Tournaisian contains three substages: the Hastarian, Ivorian and lower part of the Chadian (the upper part falls in the Viséan). Stratigraphy The base of ...
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2019 In Paleontology
Flora Plants Fungi Paleomycological research * Fossil sporocarps indistinguishable from sporocarps of members of the extant genus ''Stemonitis'' are described from the Cretaceous amber from Myanmar by Rikkinen, Grimaldi & Schmidt (2019). * A study on the impact of major historical events such as the Cretaceous–Paleogene extinction event on the evolution of two major subclasses of lichen-forming fungi ( Lecanoromycetidae and Ostropomycetidae) is published by Huang ''et al.'' (2019). * Description of crustose lichens from European Paleogene amber is published by Kaasalainen ''et al.'' (2019). * Fungi belonging to the genera ''Periconia'', ''Penicillium'' and ''Scopulariopsis'', representing the first and the oldest known fossil record of these taxa, are described from the Eocene Baltic amber by Tischer ''et al.'' (2019). Sponges Research * Sponge spicules and spicule-like structures that probably represent sponge fossils are described from four sections of the Ediacaran-C ...
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