Ighas mountain

Ighas mountain

Geological time
Devonian Carboniferous
Age
~360 million years ago
Period
Late Devonian (famennian)
Formation
Achguig Formation
Depositional environment
Current-swept, shallow open-marine carbonate ramp
Fossil types
Ammonoids (Clymeniids, Goniatitids), orthoconic cephalopods, conodonts
Paleoecology highlights
Strong bottom currents, highly condensed sedimentation, cephalopod shell accumulations

During the late Devonian, this area lay beneath an open sea, on a broad seafloor that sloped gently across the western Tafilalt Platform. Dim blue-green light filtered down to a bed of soft carbonate mud. Most of the time the water was quiet and deposition almost imperceptibly slow, but distant storms sent strong currents sweeping across the bottom, stirring the mud and scattering broken shells.

Ighas mountain shown on the globe Map

†Ammonoidea

11 specimens

Bivalvia

1 specimen

Gastropoda

1 specimen

Orthoceratoidea

5 specimens

Unclassified

1 specimen