Trace fossils of these Avalon organisms have been found worldwide, with many found in Newfoundland, in Canada and the Charnwood Forest in England, representing the earliest known complex multicellular organisms. The Avalon explosion theoretically produced the Ediacaran biota. The biota largely disappeared contemporaneously with the rapid increase in biodiversity known as the Cambrian explosion. At this time, all living animal groups were present in the Cambrian oceans.
The Avalon explosion appears similar to the Cambrian explosion in the rapid increase in diversity of morphologies in a relatively small-time frame, followed by diversification within the established body plans, a pattern similar to that observed in other evolutionary events.
The Avalon explosion was a time of early evolution and low diversity in species. There were over 270 species defined, with 50 different morphological characteristics categories, many of whose anatomical structures had to be inferred with fossils and casts. These species were placed into 20 different genera.
During this time, animals became bilateral and along with increasing complexity. Many animals during this time fit into the annelid, arthropod, echinoderm, and cnidarian phyla. Animals at this time developed bilateral symmetry with a clear anterior and posterior side, which included species like Spriggina, Charniodiscus and Yorgia.
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