The Neoarchean ( //; also spelled Neoarchaean) is a geologic era within the Archaean. It spans the period of time from —the period being defined chronometrically and not referenced to a specific level in a rock section on Earth. Oxygenic photosynthesis first evolved in this era and was accountable for the oxygen catastrophe which was to happen later in the paleoproterozoic from a poisonous buildup of oxygen in the atmosphere, produced by these oxygen producing photoautotrophs, which evolved earlier in the Neoarchean. The supercontinent Kenorland formed during this period, about 2.7 billion years ago.
Archean Eon Eoarchean Paleoarchean Mesoarchean Neoarchean This geochronology article is a stub. You can help Wikipedia by expanding it.