A Threshold in Phanerozoic Oxygen Concentrations: Evidence from Carbonate Sediment Color and Physiological Requirements of Marine Fauna

In his book The Nature of the Stratigraphical Record, Derek Ager made the remarkable observation that the geologic eras of the Phanerozoic could be identified by coloration patterns of carbonate sediments in outcrops. This observation, however, was never quantified nor explained by Ager. Here, we present a record of spectral reflectance of carbonate sediments collected from sections worldwide. While sediment color is governed by many factors, global and abrupt shifts in sediment color across depositional envrionments observed here may represent a shift towards rising oxygen concentrations. Such a shift would explain changes in redox state of iron or organic matter concentrations, both factors which influence sediment color. This record is combined with a simple model of physiological requirements of marine fauna in order to infer a minimum pO2 in the atmosphere to support life. Results indicate a strong threshold change in the Earth system near the Triassic-Jurassic boundary, potentially reflecting rising atmospheric oxygen concentrations not previously recorded.