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Eras

Cryogenian

Proterozoic

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The second period of the Neoproterozoic era, spanning about 720 to 635 million years ago. It is defined by two severe global glaciations, the Sturtian and Marinoan, in which ice sheets may have reached or nearly reached the equator in a so called Snowball Earth or Slushball Earth state that severely disrupted the biosphere.

Facts
Rank
Period 1
Start (Million Years Ago)
720 1
End (Million Years Ago)
635 1
Key Event
Sturtian Glaciation, about 717 to 660 Ma, the first major ice age; Marinoan Glaciation, about 639 to 632.3 Ma, the second, ending near the Cryogenian-Ediacaran boundary. 1
Cross-Tradition Connections

Anticipated By

Tonian, Eras

In Discipline

Part Of

Neoproterozoic, Eras

Precursor To

Ediacaran, Eras
Sources
1. Cryogenian (Wikipedia)
Wikimedia FoundationLead section
Quote, Lead section
The second of the three periods of the Neoproterozoic era, preceded by the Tonian and followed by the Ediacaran.
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1. Cryogenian (Wikipedia)
Wikimedia FoundationGlaciations section
Quote, Glaciations section
Sturtian Glaciation, about 717 to 660 Ma, the first major ice age; Marinoan Glaciation, about 639 to 632.3 Ma, the second, ending near the Cryogenian-Ediacaran boundary.
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