|Silurian||Pridoli||no faunal stages defined||older|
|Subdivision of the Devonian system|
according to the ICS, as of 2017.
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.
It was during this age that tetrapods first appeared. In the seas, a novel major group of ammonoid cephalopods called clymeniids appeared, underwent tremendous diversification and spread worldwide, then just as suddenly went extinct.
North American subdivisions of the Famennian include the Chautauquan, Canadaway, Conneaut, Conneautan, Conewango and Conewangan.
Name and definitionEdit
The Famennian stage was proposed in 1855 by Belgian geologist André Hubert Dumont and was accepted for the upper stage of the Upper Devonian by the Subcommission on Devonian Stratigraphy in 1981. It is named after Famenne, a natural region in southern Belgium.
|Cartilaginous fish of the Fammenian|
|Placoderms of the Fammenian|
|Tetrapodomorphs of the Fammenian|
|Catskill Formation, Red Hill Shale, Pennsylvania|
|Tetrapods of the Fammenian|
|Amphibians of the Fammenian|
|Andreyevka, Tula Oblast, Russia|
- Thorez, Jacques; Dreesen, Roland; Streel, Maurice (2006). "Frasnian". Geologica Belgica. 9 (1–2): 27–45. Retrieved 16 March 2013.