2023
DOI: 10.5194/egusphere-egu23-8831
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Sea surface temperature evolution of the North Atlantic Ocean across the Eocene-Oligocene Transition

Abstract: <p>When a permanent ice cap developed on Antarctica during the Eocene–Oligocene transition (EOT; ~34.44 to 33.65 million years ago (Ma)), Earth witnessed a transition from a greenhouse towards a glacially driven climate. Evidence of high-latitude cooling and increased latitudinal temperature gradients across the EOT has been found in both marine and terrestrial environments. However, the timing and magnitude of temperature change in the North Atlantic remains poorly constrained.&… Show more

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