Precambrian 3 divisions? Based on Radiometric dates
Protozoic Eon (542 my - 2.5 by) youngest
Archean Eon (4.0 by - 2.5 by) oldest
Hadean Eon (4.6 by - 4.0 by) formation of Earth
Hadean Formation
No rock record during this time, only at the end when Zircon crystals started forming
Meteorite bombardment, volcanism, extreme temperatures
A sea of magma covered much of the Earth’s surface
An early atmosphere started to form
Komatiite - what forms it?
Only formed during Early Earth when the temperatures were extreme.
Lots of heat is needed to form Komatiite
Archean tectonics overview
Small continent mass
Plate tectonic movement was rapid
Passive continental Margins
Occurs where the transition from land to sea such as a divergent boundary
Archean atmosphere
Formed by outgassing
No free oxygen at first
Oxygen began to appear
Photochemical dissociation of H2O by UV radiation
Photosynthesis
Oceans began to accumulate
Evidence of oxygen present
Banded Iron Formation: BIFs
Made of hematite layered with Fe-rich chert. The hematite is FE2O3. In the presence of free O2 in the atmosphere the Fe would oxidize before forming this mineral.
First supercontinent in Proterozoic
Gonawanaland formed
Consists of southern continents.
Luarentia and Gondawanaland formed a supercontinent known as Rodinia at the end of Proterozoic Eon
Rock evidence in Proterozoic
Banded Iron Formations (BIFs) – Reflect increasing oxygen levels.
Glacial Tillite – Evidence for early ice ages, such as the Snowball Earth.
Sedimentary – Show evidence of more stable continental environments. (
Stromatolites
Produce O2
BIFs became common 2.5 - 2.0 by
Continental red beds appeared 1.8 by
Atmosphere oxidizing
First oxygen in aquatic areas then in the atmosphere
First multicellular organism
It may have developed from specialized colonies
Ediacaran
Soft-bodied, Nearshore, shallow marine
670 - 570 my