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The lower boundary of the Vendian could have a biostratigraphic substantiation as well taking into consideration the worldwide occurrence of the Pertatataka assemblage of giant acanthomorph acritarchs. 635-542 Mya) represents the time from the end of global Marinoan glaciation to the first appearance worldwide of somewhat complicated trace fossils (Treptichnus pedum (Seilacher, 1955)).Although the Ediacaran Period does contain soft-bodied fossils, it is unusual in comparison to later periods because its beginning is not defined by a change in the fossil record.Plus you really cannot get to know Russian brides unless you spend time with them in their home environment.

The fossil record from the Ediacaran Period is sparse, as more easily fossilized hard-shelled animals had yet to evolve.

), spans 94 million years from the end of the Cryogenian Period 635 million years ago (Mya), to the beginning of the Cambrian Period 541 Mya.

It marks the end of the Proterozoic Eon, and the beginning of the Phanerozoic Eon.

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