is one of two faunal stages
in the Late Devonian
period. It lasted from 382.7 million years ago to 372.2 million years ago. It was preceded by the Givetian
stage and followed by the Famennian
Major reef-building was under way during the Frasnian stage, particularly in western Canada and Australia. On land, the first forests were taking shape. In North America, the Antler and Taconic orogenies peaked, which were contemporary with the Bretonic phase of the Variscan orogeny in Europe.
The Frasnian coincides with the second half of the "charcoal gap" in the fossil record, a time when atmospheric oxygen levels were below 13%, the minimum necessary to sustain wildfires.
North American subdivisions of the Frasnian include
The Frasnian stage was proposed in 1879 by French geologist Jules Gosselet and was accepted for the lower stage of the Upper Devonian by the Subcommission on Devonian Stratigraphy in 1981. It is named after the village of Frasnes-lez-Couvin in Belgium.
Coordinates: 43°30′12″N 3°05′12″E / 43.5032°N 3.0868°E
This page was last edited on 22 February 2018, at 22:11 (UTC)
under CC BY-SA license.