Katian
The Katian is the second stage of the Upper Ordovician. It is preceded by the Sandbian and succeeded by the Hirnantian stage. The Katian began million years ago and lasted for about 7.8 million years until the beginning of the Hirnantian million years ago.
During the Katian climate cooled which started the Late Ordovician glaciationNaming
The name Katian is derived from Katy Lake.The GSSP of the Katian stage is the Black Knob Ridge Section in southeastern Oklahoma. It is an outcrop of the Womble Shale and the Bigfork Chert, the latter containing the lower boundary of the Katian. The lower boundary is defined as the first appearance datum of the graptolite species Diplacanthograptus caudatus. This horizon is 4.0 m above the base of the Bigfork Chert.Palaeontology
Molluscs
Cephalopods
Endocerids