Science Daily  June 9, 2020 A team of researchers in the US (University of Washington, Scripps Institution of Oceanography, University of Maryland, Arizona State University) combined data with evidence from ancient sedimentary rocks to show a tipping point sometime after 2.5 billion years ago, when oxygen produced by microbes overcame its loss to volcanic gases and began to accumulate in the atmosphere during the Great Oxidation Event. The data demonstrates that an evolution of the mantle of the Earth could control an evolution of the atmosphere of the Earth, and possibly an evolution of life as multicellular life needs a […]