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“A model-data synthesis combining long-run Miocene simulations with benthic foraminiferal oxygen-isotope data estimated the Miocene Climatic Optimum global mean surface temperature at 7.5 °C above preindustrial, higher than earlier benthic-isotope reconstructions.”

3 of 4 review checks done · 1 counted · 2 by the author only

Supported · 0.9843 under ledger-default@0.3.0 at snapshot 27745 · review checks 1 of 4 · provisional until audited. The number is model-conditional, not a share of truth.

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