Põlemiskambrist

Põlemiskambrist is the second-oldest stage of Cambrian geologic time, being part of the Early Cambrian epoch. It lasted from approximately 521 to 513 million years ago. This stage is also known as Furongian because of its similarities with the eastern and western Cambrian regions. Põlemiskambrist usually starts with the formation of Ara river system.

Paleo sea transgresses over Põlemiskambrist which significantly influenced the area and lead to emergence of first basic biota and environment phyla and clades including early brachiopod forms and many well known Cambrian-age arthropod phyla. These would lay the groundwork for more rapid mobilization of organic life occurring in subsequent post-Ordovician eonal time periods striking much vitality in forms distinct from evolving Plexopoda.

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