Abstract
The Neoproterozoic era, spanning from 720 to 539 million years ago, was marked by profound transformations in all its envelopes and witnessed the emergence and diversification of metazoan life, culminating with the appearance of major animal phyla, in the Cambrian. The Cryogenian period (720-635 Ma) featured extreme glacial epochs and the reemergence of banded iron formations, signaling t…