Extremely cold ocean temperatures in iron formation brine pools of snowball Earth.

For the severe low-latitude "snowball Earth" glaciations, glacial deposits occurring on all continents is well-established. However, cold, salty, ice-covered oceans-a salient prediction of snowball Earth-is difficult to establish geologically. Here we demonstrate that anomalously high iron isotope values (δ56Fe) of snowball iron formation-never observed in earlier anoxic Archaean oceans-can be attributed to additional temperature-dependent fractionation in extremely cold brine pools in the snowball ocean. Experiments and modeled fractionations relevant to the precipitation of iron formation demonstrate temperature-dependent δ56Fe fractionation, where colder temperatures correspond with more positive δ56Fe. Assuming the ~ 0.9‰ differential in δ56Fe values of snowball iron formation in excess of those preceding the Great Oxidation Event is due to temperature-dependent fractionation, we calculate that the temperature of the iron formation brine pools was -15 ± 7°C. Such cold snowball brine pools, colder than those in Antarctic margins today, represent Earth's coldest recorded ocean temperatures.