Oxidation of the Ediacaran Ocean

TLDR: High-resolution carbon isotope and sulphur isotope records from the Huqf Supergroup, Sultanate of Oman, that cover most of the Ediacaran period indicate that the ocean became increasingly oxygenated after the end of the Marinoan glaciation and allow us to identify three distinct stages of oxidation.

Abstract: Oxygenation of the Earth's surface is thought to have occurred in two main steps. The first, about 2,300 million years ago, saw a significant increase in atmospheric and surface ocean oxygen levels and has been widely studied. Much less is known about the second step, which took place around 800–540 million years ago and appears to have been associated with the evolution of complex animals. Now carbon and sulphur isotope records from sediments in the Sultanate of Oman have been used to construct a record of the amount of oxygen in the ocean during the Ediacaran period (635–542 million years ago). The data suggest that there were three distinct stages of oxidation within this period: the second stage involved an increase in oxygen in the deep ocean and appears to have been associated with the evolution of complex animals. Reconstruction of the amount of oxygen in the ocean during the Ediacaran period using carbon- and sulphur-isotope records identifies three distinct stages of oxidation over this interval. Complex animals may have evolved during the second stage, indicating that this event may have played a key role in the evolution of eukaryotic organisms. Oxygenation of the Earth’s surface is increasingly thought to have occurred in two steps. The first step, which occurred ∼2,300 million years (Myr) ago, involved a significant increase in atmospheric oxygen concentrations and oxygenation of the surface ocean1,2. A further increase in atmospheric oxygen appears to have taken place during the late Neoproterozoic period3,4 (∼800–542 Myr ago). This increase may have stimulated the evolution of macroscopic multicellular animals and the subsequent radiation of calcified invertebrates4,5, and may have led to oxygenation of the deep ocean6. However, the nature and timing of Neoproterozoic oxidation remain uncertain. Here we present high-resolution carbon isotope and sulphur isotope records from the Huqf Supergroup, Sultanate of Oman, that cover most of the Ediacaran period (∼635 to ∼548 Myr ago). These records indicate that the ocean became increasingly oxygenated after the end of the Marinoan glaciation, and they allow us to identify three distinct stages of oxidation. When considered in the context of other records from this period7,8,9,10,11,12,13,14,15, our data indicate that certain groups of eukaryotic organisms appeared and diversified during the second and third stages of oxygenation. The second stage corresponds with the Shuram excursion in the carbon isotope record16 and seems to have involved the oxidation of a large reservoir of organic carbon suspended in the deep ocean6, indicating that this event may have had a key role in the evolution of eukaryotic organisms. Our data thus provide new insights into the oxygenation of the Ediacaran ocean and the stepwise restructuring of the carbon6,16,17 and sulphur cycles3,18,19 that occurred during this significant period of Earth’s history.