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A new study, published today in Nature, offers the most detailed picture to date of the 3-D makeup of the Earth's early atmosphere. Although the gases were enriched in carbon dioxide, or CO2, compared with the air today, they were lacking in oxygen, or O2. This led scientists to conclude that Earth's atmosphere was very different than what we experience today. The new details of Earth's earliest atmosphere could affect how scientists think about the early evolution of life on Earth. From the perspective of life as we know it today, the first significant concentration of CO2 to accumulate in Earth's atmosphere was approximately 450 million years ago. In comparison, O2 began to accumulate in Earth's atmosphere some 490 million years ago.. Recently, O2 levels were high in the Earth's atmosphere and, thus, the oceans were more acidic. Furthermore, there were large quantities of organic molecules. These molecules occurred as primitive organisms metabolized organic carbon. The global environment was home to many different organisms including soft-bodied protists, primitive plants, and probably primitive single-celled creatures. All of these were consuming organic carbon. All these organisms required O2 as an oxidant. The first primitive plants and animals were green in color. Some of these green organisms would have produced oxygen when they died. Free oxygen in Earth's atmosphere would have reacted with the organic carbon and created gas that would have been lost into the atmosphere, since there was no way to hold these gases for a long time in water. This would have caused an increase in the concentration of these carbon-based molecules in the Earth's atmosphere. Free oxygen in the Earth's atmosphere would have reacted with the organic carbon and created gas that would have been lost into the atmosphere, since there was no way to hold these gases for a long time in water. This would have caused an increase in the concentration of these carbon-based molecules in the Earth's atmosphere. This increased concentration would have brought about the initial rise in atmospheric oxygen concentration. Bill McKane and Charles Paul from the University of Iowa are co-authors of the study. Paul and McKane arrived at their conclusions based on their analyses of gas from ancient rock and the diversity of marine and terrestrial organisms found in that rock. The senior author of the study, James Wayman, from the University of California, Berkeley, is the senior author. Wayman and his team members are all professors at Berkeley, and they study the evolution of the Earth's atmosphere. In the early 1990s, Way 595f342e71


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