The Frasnian is one of two faunal stages in the Late Devonian Period.

Major reef-building was under way during the Frasnian Stage, particularly in western Canada and Australia.

The Frasnian coincides with the second half of the "charcoal gap" in the fossil record, a time when atmospheric oxygen levels were below 13 percent, the minimum necessary to sustain wildfires.

[7] 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.

[8] It is named after the village of Frasnes-lez-Couvin, in the district of Couvin, in Belgium.