Fortunately for life, oxygen levels in the atmosphere have been stable over Earth's history.
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Q5: The Pacific Ocean is in the later
Q6: The Grenville orogeny was the culminating event
Q7: Sandstone-carbonate-shale assemblages are characteristic of the early
Q8: The evolution of Laurentia can be described
Q9: Banded iron formations precipitated in oxygen-rich ocean
Q11: Glaciers were rare during the Proterozoic, as
Q12: Both the presence of banded iron formations
Q13: Orogens are belts of igneous and metamorphic
Q14: Passive margin deposits are rare or absent
Q15: The Ediacaran fauna of Australia includes many
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