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Pseudooneotodus ✝
Source Data |
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Rank | genus | ||||||||||||||||||||||||||||||||||||
Taxonomy (GBIF) | Life : Animalia : Chordata : Strachanognathidae : Pseudooneotodus | ||||||||||||||||||||||||||||||||||||
Taxonomy (PBDB) | Life : Animalia : Chordata : Conodonta : Strachanognathidae : Pseudooneotodus | ||||||||||||||||||||||||||||||||||||
Taxonomic Status (GBIF) | accepted | ||||||||||||||||||||||||||||||||||||
Classification (PBDB,GBIF) |
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Scientific Name | Pseudooneotodus Drygant, 1974 | ||||||||||||||||||||||||||||||||||||
Name Published In | Paleont. Sb. Lemberg No. 10 (2) | ||||||||||||||||||||||||||||||||||||
Opinions (PBDB) |
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Status (PBDB) | extinct | ||||||||||||||||||||||||||||||||||||
Taxon Size (PBDB) | 7 | ||||||||||||||||||||||||||||||||||||
First Recorded Appearance | 485 - 470 Ma Paleozoic | ||||||||||||||||||||||||||||||||||||
Last Recorded Appearance | 408 - 393 Ma Early/Lower Devonian | ||||||||||||||||||||||||||||||||||||
Environment | marine (based on Vertebrata) | ||||||||||||||||||||||||||||||||||||
Motility | actively mobile (based on Conodonta) | ||||||||||||||||||||||||||||||||||||
Vision | well-developed (based on Conodonta) | ||||||||||||||||||||||||||||||||||||
Diet | carnivore (based on Conodonta) | ||||||||||||||||||||||||||||||||||||
Taphonomy | hydroxylapatite (based on Conodonta) | ||||||||||||||||||||||||||||||||||||
Primary Reference (PBDB) | D. M. Drygant. 1974. Simple conodonts form the Silurian and lowermost Devonian of the Volyno-Podolian area. Paleontologicheskiy Sbornik 10:64-70 |
Fossil Distribution
Subtaxa
Name | Status | Common Name(s) | Fossil Occurrences | Oldest | Youngest |
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Oneotodus beckmanni ✝ species | accepted (GBIF) listed (PBDB) | 567 | 461 Ma Middle Ordovician | 408 Ma Early/Lower Devonian | |
Pseudooneotodus bicornis ✝ species | accepted (GBIF) listed (PBDB) | 321 | 450 Ma Late/Upper Ordovician | 423 Ma Silurian | |
Pseudooneotodus boreensis ✝ species | accepted (GBIF) listed (PBDB) | 6 | 439 Ma Silurian | 431 Ma Silurian | |
Pseudooneotodus coniformis ✝ species | accepted (GBIF) listed (PBDB) | 19 | 433 Ma Silurian | 431 Ma Silurian | |
Pseudooneotodus linguicornis ✝ species | accepted (GBIF) listed (PBDB) | 28 | 433 Ma Silurian | 431 Ma Silurian | |
Pseudooneotodus tricornis ✝ species | accepted (GBIF) listed (PBDB) | 17 | 441 Ma Silurian | 431 Ma Silurian |
Synonymy List
Year | Name and Author |
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1974 | Pseudooneotodus Drygant |
1984 | Pseudooneotodus Stouge p. 59 |
2002 | Pseudooneotodus Sepkoski, Jr. |
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!