Olduvai subchron

E1740070 UNEXPLORED

The Olduvai subchron is a brief interval of normal geomagnetic polarity within the predominantly reversed Matuyama chron, dated to the early Pleistocene and widely used for geological and paleoanthropological dating.

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All labels observed (1)

Label	Occurrences
Olduvai subchron canonical	1

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Matuyama reversed chron → contains → Olduvai subchron ⓘ