Evidence item

The quoted passage directly supports the 7.5 °C maximum-likelihood estimate and its comparison with earlier benthic-isotope reconstructions. DIRECT_TEXT

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Source: Model-data synthesis of benthic isotopes suggests a warmer Miocene Climatic Optimum · locator {} · excerpt hash sha256:c2be294d53aabeae67c36c428020eed84b55bfb70bdd135f6c4ce03ded4aa21f

Our approach yields a maximum likelihood estimate of MCO global mean surface temperature of 7.5 °C above preindustrial, significantly warmer than previous benthic δ18O-based reconstructions, implying a higher MCO-derived estimate of Earth system sensitivity.