Multilamella Orłowski, 1989

Emended diagnosis. Sets of thin, straight or undulating shingled lamellae, parallel to one another, but bent in one direction on the sole of bed or within the bed. The sets of the lamellae are inclined at diverse angles to the bedding

Diagnosis. - Groups of thin laminae parallel to each other, straight to undulating, covering the surface on the sole of sandstone beds or situated inside the beds near the sole. As a rule, the groups are parallel to the bedding plane, rarely slightly oblique. Single laminae are convex in the same direction. Laminae situated perpendicularly to bedding plane. Groups of laminae are sometimes associated with single, meandering track, oval in cross section, with concave laminae insi;de, retrusive. Longitudinal tracks often perpendicular to bedding plane and to groups of laminae.

Origin.-These trace fossils probably represent feeding burrows of an animal with longitudinal and narrow body, perhaps a worm or worm-like organism. The laminae were made by the sides of the animal's body. The single, meandering tracks were made by the same animal, which was moving forward horizontally or vcrtically.