Editing Banded iron formation (section)

===The Great Oxidation Event===
[[Image:Oxygenation-atm-2.svg|thumb|upright=2|[[Great Oxidation Event|Oxygen (O<sub>2</sub>) build-up]] in the [[Earth's atmosphere]]. Red and green lines represent the range of the estimates while time is measured in billions of years ago (Ga).<ref name="holland-2006"/>
<br />Banded formation iron deposition peaks at the beginning of Stage 2 and pauses at the beginning of Stage 3.]]
{{Main|Great Oxidation Event}}
The peak of deposition of banded iron formations in the late Archean, and the end of deposition in the Orosirian, have been interpreted as markers for the Great Oxygenation Event. Prior to 2.45 billion years ago, the high degree of [[mass-independent fractionation]] of sulfur (MIF-S) indicates an extremely oxygen-poor atmosphere. The peak of banded iron formation deposition coincides with the disappearance of the MIF-S signal, which is interpreted as the permanent appearance of oxygen in the atmosphere between 2.41 and 2.35 billion years ago. This was accompanied by the development of a stratified ocean with a deep anoxic layer and a shallow oxidized layer. The end of deposition of BIF at 1.85 billion years ago is attributed to the oxidation of the deep ocean.<ref name="holland-2006"/>