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      Temperate rainforests near the South Pole during peak Cretaceous warmth

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          The least-squares line and plane and the analysis of palaeomagnetic data

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            The Phanerozoic record of global sea-level change.

            K. Miller (2005)
            We review Phanerozoic sea-level changes [543 million years ago (Ma) to the present] on various time scales and present a new sea-level record for the past 100 million years (My). Long-term sea level peaked at 100 +/- 50 meters during the Cretaceous, implying that ocean-crust production rates were much lower than previously inferred. Sea level mirrors oxygen isotope variations, reflecting ice-volume change on the 10(4)- to 10(6)-year scale, but a link between oxygen isotope and sea level on the 10(7)-year scale must be due to temperature changes that we attribute to tectonically controlled carbon dioxide variations. Sea-level change has influenced phytoplankton evolution, ocean chemistry, and the loci of carbonate, organic carbon, and siliciclastic sediment burial. Over the past 100 My, sea-level changes reflect global climate evolution from a time of ephemeral Antarctic ice sheets (100 to 33 Ma), through a time of large ice sheets primarily in Antarctica (33 to 2.5 Ma), to a world with large Antarctic and large, variable Northern Hemisphere ice sheets (2.5 Ma to the present).
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              A Dynamic Thermodynamic Sea Ice Model

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                Author and article information

                Journal
                Nature
                Nature
                Springer Science and Business Media LLC
                0028-0836
                1476-4687
                April 2020
                April 1 2020
                April 2020
                : 580
                : 7801
                : 81-86
                Article
                10.1038/s41586-020-2148-5
                32238944
                d21306b8-b709-4127-acaf-377e15b77e01
                © 2020

                http://www.springer.com/tdm

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