A new theory on the thermal evolution of Earth explains why the planet’s upper mantle was cool enough to produce diamonds in the Archean Eon between 4 billion and 2.5 billion years ago, rather than turning into lumps of common graphite. After studying thousands of rocks samples dating at least 2.5 billion years old, Kamber & Tomlinson determined the Earth’s upper mantle was much cooler than previously thought. Image credit: NASA / JPL-Caltech. Queensland...
