Description

Dickinsonia costata
Ediacaran
Late Precambrian (Vendian)
Penega Formation
East Angelsk, White Sea, Russia

35mm on 200mm slab.

Here’s the classic Ediacaran form.  Its relationships to Paleozoic groups are uncertain and it disappeared by the end of the Vendian Period.  It may belong to a kingdom of early animals separate from all others and yet its body nearly shows the complete bilateral symmetry of phyla we know including the Chordata.

The Vendian Period spans about the last 110 million years of the Proterozoic Eon from about 540 to 650 million years ago.  It is during this time that soft-bodied, macroscopic life appeared.  By the end of the Vendian the supercontinent, Rodinia, which formed from the collisions of the major land masses approximately 1.2 billion years ago, had started to fragment into continents that would reconnect at the end of the Paleozoic Era over 300 million years later.