Described as an explosion of multi-cellular organisms and major diversification, FTP, identify this period that started 540 million years ago and ended around 488 million years ago at the start of the Ordovician period.
A later epoch of this period is the Furongian. During this epoch, Laurentia, Baltica, and Siberia separated from the Neoproterozoic supercontinent Pannotia. This is due to Geologists claim that continental drift rates in this period were unusually higher than those in layer periods. Panthalassa also covered most of the southern hemisphere. Described as an explosion of multi-cellular organisms and major diversification, FTP, identify this period that started 540 million years ago and ended around 488 million years ago at the start of the Ordovician period.
A later epoch of this period is the Furongian. During this epoch, Laurentia, Baltica, and Siberia separated from the Neoproterozoic supercontinent Pannotia.
{Cambrian}