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Creators/Authors contains: "Swann, G. E."

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  1. ; ; ; ; ; ; ; ; ; ; et al (, Reviews of Geophysics)
    Key Points The “stable” warm late Pliocene ∼3.3–3.1 million years ago was a time of climate transition, especially in the southern hemisphere Ocean temperatures and ice sheets evolved asynchronously 3.3–2.4 Ma during the onset and intensification of Northern Hemisphere Glaciation Climate variability evolved in complex, non‐uniform ways, most strongly expressed in northern mid‐latitude sea‐surface temperature records 
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