Turonian Prionocyclids
from the Mancos Shale in East-Central Utah

Shown from youngest (on top) to oldest
all about natural size


  P. wyomingensis & P. novamexicanus
 
Prionocyclus wyomingensis Meek 1876         Prionocyclus novimexicanus (Marcou) 1858
 
    Gracile form of P. wyomingensis on left was found associated with Scaphites cf. S. whitfieldi east of Clawson.  The ammonite on the right is the robust form of P. novimexicanus found with S. whitfieldi high in the Juana Lopez Member S.E. of Green River.  P. wyomingensis has a double row of ventro-lateral nodes while P. novimexicanus has a single row, with a groove on each side of the keel.

See parts of a crushed P. novimexicanus? here

Ammonites from the P. novamexicanus Biozone

P. wyomingensis
Prionocyclus wyomingensis Meek 1876

Gracile form on left, robust form on right, both associated with Scaphites cf. S. ferronensis .  These ammonites can be found all along the outcrop of the Juana Lopez Member from east of Ferron, around the north end of the San Rafael Swell, to the Colorado border.

See a large adult P. wyomingensis here

Ammonites from the P. wyomingensis Biozone

P. macombi

Prionocyclus macombi Meek 1876

Gracile form on left, robust form on right.  From the Juana Lopez Member S.E. of Green River.  P. macombi has a single row of ventro-lateral clavi and low flattened ribs.

See a large adult P. macombi here

Ammonites from the P. macombi Biozone

P. hyatti

Prionocyclus hyatti (Stanton) 1893

Gracile form on left, robust form on right.  Found in the lower Ferron Sandstone Member near Mounds.  P. hyatti has a much wider umbilicus than the other prionocyclids.

Ammonites from the P. hyatti Biozone


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