Atmospheric oxygenation three billion years ago

The distribution of chromium isotopes and redox-sensitive metals in the Nsuze palaeosol and in the Ijzermyn iron formation from the Pongola Supergroup, in South Africa, suggests that there were appreciable levels of atmospheric oxygen about three billion years ago, some 300–400 million years earlier than previous indications for Earth surface oxygenation. Atmospheric oxygen before the Event The first long-term oxygenation of the Earth's atmosphere — the Great Oxidation Event — is thought to have occurred around 2.3 billion years ago, although there is some geochemical evidence for transient atmospheric oxygenation as early as 2.7 billion years ago. Sean Crowe et al . examine the distribution of chromium isotopes and other metals that act as indicators for oxidative weathering in ancient soil and rock samples from South Africa. Their measurements suggest that oxygen-driven weathering was taking place 3 billion years ago, implying the presence of appreciable levels of atmospheric oxygen. This oxygen was probably produced by photosynthesis, indicating that cyanobacteria may have evolved by this time. This suggests an early evolution of oxygenic photosynthesis, 600 million years before the Great Oxidation Event. It is widely assumed that atmospheric oxygen concentrations remained persistently low (less than 10 −5 times present levels) for about the first 2 billion years of Earth’s history 1 . The first long-term oxygenation of the atmosphere is thought to have taken place around 2.3 billion years ago, during the Great Oxidation Event 2 , 3 . Geochemical indications of transient atmospheric oxygenation, however, date back to 2.6–2.7 billion years ago 4 , 5 , 6 . Here we examine the distribution of chromium isotopes and redox-sensitive metals in the approximately 3-billion-year-old Nsuze palaeosol and in the near-contemporaneous Ijzermyn iron formation from the Pongola Supergroup, South Africa. We find extensive mobilization of redox-sensitive elements through oxidative weathering. Furthermore, using our data we compute a best minimum estimate for atmospheric oxygen concentrations at that time of 3 × 10 −4 times present levels. Overall, our findings suggest that there were appreciable levels of atmospheric oxygen about 3 billion years ago, more than 600 million years before the Great Oxidation Event and some 300–400 million years earlier than previous indications for Earth surface oxygenation.