The magnitude of sea - level estimates for the past 100 million years rely heavily on
foraminiferal calcite oxygen isotopes (δ18O), which are influenced by temperature, evaporation and precipitation, and diagenesis2.
Cenozoic deep - sea temperatures and global ice volumes from Mg / Ca in benthic
foraminiferal calcite
This shows the effect of historically invisible confounding influences on T: dO18 proxy reconstructions, and explicitly refutes your claim, Kau, that, «ONLY a change in temperature or a change in seawater δ18O can alter the δ18O ratio of
foraminiferal calcite.