Percha Formation


The Percha Formation is a geologic formation in southern New Mexico. It preserves fossils dating back to the Famennian Age of the late Devonian period.

Description

The formation consists mostly of black to gray shale and minor limestone. It rests on a regional unconformity, so that the underlying formation may be the Fusselman Formation, the Sly Gap Formation, or the Onate Formation. It underlies the Lake Valley Limestone, Caballero Formation, Escabrosa Limestone, or other Mississippian formations. Total thickness is about.
The formation is divided into two members. The Ready Pay Member is mostly black fissile shale nearly devoid of fossils and with a total thickness of about. The Box Member , which is much less limited in areal extent, is about of gray to green calcareous shale with limestone nodules and beds. It is highly fossiliferous.

Fossils

The base of the formation contains fossils of arthrodiran fish, shark teeth, late Fammenian conodonts, brachiopods, and corals. The Box Member contains fossils of brachiopods, crinoids, bryozoans, sponges, corals, and late Fammenian conodonts.

History of investigation

The formation was first named as the Percha Shale by C.H. Gordon in 1907 for exposures at Percha Creek. However, a type section was not designated until 1945, by F.V. Stevenson. Stevenson also divided the formation into the lower Ready Pay Member and the upper Box Member. D. Schumacher and coinvestigators mapped the formation into southeastern Arizona and renamed it the Percha Formation in 1976.