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  1. 26 wrz 2016 · During the late Miocene epoch, about seven million years ago, large areas of the continents experienced drying, enhanced seasonality, and a restructuring of terrestrial plant and animal...

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  2. 18 paź 2021 · During the Miocene, major global cooling occurred during two intervals: the middle Miocene (∼14–13 Ma) and the late Miocene (∼7-6 Ma). The Antarctic Ice Sheet expanded substantially at ∼14–13 Ma, and glaciation in the Northern Hemisphere was initiated at ∼7–6 Ma.

  3. 23 gru 2020 · 5.1.3 Late Miocene (Tortonian and Messinian) Vegetation. The late Miocene ushered in major changes in vegetation linked to paleogeographic changes and a drying, cooling climate.

  4. 6 cze 2012 · Measurements from several ocean cores reveal that ocean warmth persisted throughout the late Miocene epoch despite CO2 levels of only 200–350 p.p.m.v., probably driven by a deep thermocline...

  5. During the late Miocene epoch, about seven million years ago, large areas of the continents experienced drying, enhanced seasonality, and a restructuring of terrestrial plant and animal...

  6. 26 wrz 2016 · We find that a sustained late Miocene cooling occurred synchronously in both hemispheres, and culminated with ocean temperatures dipping to near-modern values between about 7 and 5.4 million...

  7. 23 gru 2020 · Miocene climate was dynamic: long periods of early and late glaciation bracketed a ∼2 Myr greenhouse interval—the Miocene Climatic Optimum (MCO). Floras, faunas, ice sheets, precipitation, p CO 2, and ocean and atmospheric circulation mostly (but not ubiquitously) covaried with these large changes in climate.

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