CHANGES IN THE SR/CA AND MG/CA RATIOS OF CRETACEOUS SEAWATER DERIVED FROM THE COMPOSITION OF BIOLOGICAL LOW-MG CALCITE
In sclerochronological sections which allow for the evaluation of intra-shell variations, Sr concentrations show only minor variations, so that an increase from mean values of 900 µg/g in Aptian-Albian samples to 1500 µg/g in Campanian samples is believed to reflect changes in the Sr/Ca ratio of seawater. Applying partition coefficients for modern mollusk calcite results in a Sr/Ca ratio of Campanian seawater that was 1.5 times that of modern seawater. This is consistent with data derived from benthic foraminifera by Lear et al.
Estimating Mg/Ca ratios of seawater from Mg concentrations in biological calcite is difficult due to a pronounced temperature control. At the same d18O, Early Cretaceous specimens have much less Mg than Late Cretaceous samples. This is consistent with an increasing Mg/Ca ratio of seawater from the Barremian to the Maastrichtian, also reported by others from studies of fluid inclusions in halite. Importantly, the seawater Mg/Ca ratio was low before sea-floor spreading rates are believed to have increased during the mid-Cretaceous. This indicates that hydrothermal alteration of oceanic crust was not the major controlling factor of the seawater Mg/Ca ratio.
Changing Sr/Ca ratios of Cretaceous seawater are consistent with patterns of aragonite versus calcite predominance in marine carbonates, suggesting that the changing mode of carbonate sedimentation, triggered by the seawater Mg/Ca ratio, controlled the Sr/Ca ratio of seawater.