1/7
Looks like no tags are added yet.
Six Archean characteristics
Stabilized, much hotter inside, oceans, earliest life, stromatolites, almost no free O₂
Old stable continental crust
Craton
Rock indicating an extremely hot mantle
Komatiite
Basaltic lava erupted underwater
Pillow Basalt
Layered structure built by microbial mats
Stromatolite
Layered iron-rich sediment from O₂ + dissolved iron
Banded Iron Formation (BIF)
Why was atmospheric O₂ low if microbes made oxygen?
It reacted with dissolved iron and volcanic gases first
How do BIFs show oxygen production began?
O₂ reacted with dissolved iron, making iron oxide layers