Ancyrodella

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Ancyrodella
Temporal range: Late Devonian
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Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class:Conodonta
Genus:Ancyrodella
Ulrich & Bassler, 1926 [1]
Species
  • Ancyrodella buckeyensis
  • Ancyrodella recta
  • Ancyrodella rotundiloba

Ancyrodella is an extinct genus of conodonts from the Late Devonian.

Conodont Extinct agnathan chordates resembling eels

Conodonts are extinct agnathan chordates resembling eels, classified in the class Conodonta. For many years, they were known only from tooth-like microfossils found in isolation and now called conodont elements. Knowledge about soft tissues remains limited. The animals are also called Conodontophora to avoid ambiguity.

During the Famennian stage of the Late Devonian, a biologic event occurred (Upper Kellwasser Extinction of all Ancyrodella and Ozarkodina and most Palmatolepis , Polygnathus and Ancyrognathus ).

The Famennian is the latter of two faunal stages in the Late Devonian epoch. It lasted from 372.2 million years ago to 358.9 million years ago. It was preceded by the Frasnian stage and followed by the Tournaisian stage.

Late Devonian extinction One of the five most severe extinction events in the history of the Earths biota

The Late Devonian extinction was one of five major extinction events in the history of life on Earth. A major extinction, the Kellwasser event, occurred at the boundary that marks the beginning of the last phase of the Devonian period, the Famennian faunal stage, about 376–360 million years ago. Overall, 19% of all families and 50% of all genera became extinct. A second, distinct mass extinction, the Hangenberg event, closed the Devonian period.

Ozarkodina is an extinct genus of conodonts in the family Spathognathodontidae.

Related Research Articles

The Devonian is a geologic period and system of the Paleozoic, spanning 60 million years from the end of the Silurian, 419.2 million years ago (Mya), to the beginning of the Carboniferous, 358.9 Mya. It is named after Devon, England, where rocks from this period were first studied.

Edward Oscar Ulrich was an invertebrate paleontologist specializing in the study of Paleozoic fossils.

Heinz Christian Pander Russian geologist

Heinz Christian Pander, also Christian Heinrich Pander, was a Baltic German biologist and embryologist born in Riga.

The Exshaw Formation is a stratigraphic unit in the Western Canada Sedimentary Basin. It takes the name from the hamlet of Exshaw, Alberta in the Canadian Rockies, and was first described from outcrops on the banks of Jura Creek north of Exshaw by P.S. Warren in 1937. The formation is of Late Devonian to Early Mississippian age as determined by conodont biostratigraphy, and it straddles the Devonian-Carboniferous boundary.

Palliser Formation

The Palliser Formation is a stratigraphic unit of Late Devonian (Famennian) age in the Western Canada Sedimentary Basin. It is a thick sequence of limestone and dolomitic limestone that is present in the Canadian Rockies and foothills of western Alberta. Tall cliffs formed of the Palliser Formation can be seen throughout Banff and Jasper National Parks.

Keyser Formation

The Late Silurian to Early Devonian Keyser Formation is a mapped limestone bedrock unit in Pennsylvania, Maryland, Virginia, and West Virginia.

Wurmiella is an extinct conodont genus.

Spathognathodontidae is an extinct conodont family ranging from the Silurian to the Devonian.

Palmatolepis is an extinct conodont genus in the family Palmatolepidae. It was the most abundant genus of conodonts of the Late Devonian, disappearing during the Devonian/Carboniferous crisis.

Icriodus is an extinct conodont genus in the family Gnathodontidae.

Alternognathus is an extinct conodont genus in the family Elictognathidae. An extensive study on its population dynamics and lifespan has recently been published.

Eolinguipolygnathus is an extinct genus of conodont from the Early Devonian (Emsian).

Pseudopolygnathus is an extinct genus of conodonts in the family Polygnathidae.

Conodonts are an extinct class of animals whose feeding apparatuses called teeth or elements are common microfossils found in strata dating from the Stage 10 of the Furongian, the fourth and final series of the Cambrian, to the Rhaetian stage of the Late Triassic. These elements can be used alternatively to or in correlation with other types of fossils in the subfield of the stratigraphy named biostratigraphy.

Ancyrognathus is an extinct genus of conodonts.

Siphonodella is an extinct genus of conodonts.

Cryptotaxis is an extinct genus of conodonts in the family Cryptotaxidae from the Famennian.

Oulodus is a genus of conodonts in the family Prioniodinidae.

References

  1. A classification of the toothlike fossils, conodonts, with descriptions of American Devonian and Mississippian species. EO Ulrich and RS Bassler, 1926
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