EON CODEX
Precambrian Era

Ediacaran Period

635–541 Million Years Ago

The Ediacaran Period is the last period of the Precambrian, named after the Ediacara Hills in South Australia where its characteristic fossils were first discovered. It witnessed the appearance of the first large, complex multicellular organisms — the enigmatic Ediacara biota. These soft-bodied creatures, including Dickinsonia, Charnia, and Kimberella, represent some of the earliest experiments in animal body plans. Many have no clear modern descendants, making their biological affinities one of paleontology's great mysteries.

Environment

Climate & Environment

The Ediacaran followed the extreme Cryogenian glaciations (Snowball Earth). Climate warmed significantly, ocean chemistry changed, and oxygen levels rose — conditions thought to have enabled the evolution of large multicellular life.

Fauna & Flora

Signature Life Forms

Dickinsonia — enigmatic flat organism

Charnia — frond-like deep-sea organism

Kimberella — possible early mollusc relative

Cloudina — first organism with a mineral skeleton