Multiple independent studies across marine, lacustrine, and glacial archives confirm that oxygen isotope ratios serve as a reliable and widely utilized proxy for reconstructing past temperatures. While certain contexts present methodological challenges or diagenetic alterations, refined calibration techniques continue to validate the accuracy of oxygen isotopes in paleothermometry.
The claim is that oxygen isotopes serve as a reliable proxy for reconstructing past temperatures. Multiple retrieved papers across diverse archives (otoliths, lake sediments, marine bivalves, ice cores) explicitly support this premise by using oxygen isotopes to successfully reconstruct past water and air temperatures. One paper notes complications and unrealistic temperature outputs from chironomid head capsules due to diagenetic alteration, which provides a partial counterpoint regarding specific conditions, but does not overturn the extensive literature supporting the overall reliability of oxygen isotopes as temperature proxies when properly calibrated. The weight of evidence strongly supports the claim.