A new paper was published in Ichnos by Luis Buatois, Euridice Solórzano, Williams Rodríguez, and Gabriela Mángano examining Precambrian continental trace fossils in Venezuela.
This study documents a specific type of simple ichnofabric referred to as an unconformity-bound simple ichnofabric. The well cores in this study feature the Precambrian basement of the Orinoco Oil Belt hosting continental ichnofossils attributed to Taenidium. The bioturbation is interpreted to have be produced in the Miocene in a regolith formed on top of the Precambrian basement. The ichnofabric found here is similar to ultracomposite ichnofabrics in that it involves a significant difference in time, but it is still considered a simple ichnofabric due to representing a single bioturbation event. This study highlights the importance of recognizing temporal disjunctions in the stratigraphic record that may mislead researchers about evolutionary events.

Check out the paper in Ichnos here.
Written by Zane Gabriel Goodell
