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      The Bering Strait was flooded 10,000 years before the Last Glacial Maximum

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          Abstract

          The cyclic growth and decay of continental ice sheets can be reconstructed from the history of global sea level. Sea level is relatively well constrained for the Last Glacial Maximum (LGM, 26,500 to 19,000 y ago, 26.5 to 19 ka) and the ensuing deglaciation. However, sea-level estimates for the period of ice-sheet growth before the LGM vary by > 60 m, an uncertainty comparable to the sea-level equivalent of the contemporary Antarctic Ice Sheet. Here, we constrain sea level prior to the LGM by reconstructing the flooding history of the shallow Bering Strait since 46 ka. Using a geochemical proxy of Pacific nutrient input to the Arctic Ocean, we find that the Bering Strait was flooded from the beginning of our records at 46 ka until 35.7 - 2.4 + 3.3 ka. To match this flooding history, our sea-level model requires an ice history in which over 50% of the LGM’s global peak ice volume grew after 46 ka. This finding implies that global ice volume and climate were not linearly coupled during the last ice age, with implications for the controls on each. Moreover, our results shorten the time window between the opening of the Bering Land Bridge and the arrival of humans in the Americas.

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          Bedmap2: improved ice bed, surface and thickness datasets for Antarctica

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            A bacterial method for the nitrogen isotopic analysis of nitrate in seawater and freshwater.

            We report a new method for measurement of the isotopic composition of nitrate (NO3-) at the natural-abundance level in both seawater and freshwater. The method is based on the isotopic analysis of nitrous oxide (N20) generated from nitrate by denitrifying bacteria that lack N2O-reductase activity. The isotopic composition of both nitrogen and oxygen from nitrate are accessible in this way. In this first of two companion manuscripts, we describe the basic protocol and results for the nitrogen isotopes. The precision of the method is better than 0.2/1000 (1 SD) at concentrations of nitrate down to 1 microM, and the nitrogen isotopic differences among various standards and samples are accurately reproduced. For samples with 1 microM nitrate or more, the blank of the method is less than 10% of the signal size, and various approaches may reduce it further.
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              Space geodesy constrains ice age terminal deglaciation: The global ICE-6G_C (VM5a) model

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                Author and article information

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                Journal
                Proceedings of the National Academy of Sciences
                Proc. Natl. Acad. Sci. U.S.A.
                Proceedings of the National Academy of Sciences
                0027-8424
                1091-6490
                January 03 2023
                December 27 2022
                January 03 2023
                : 120
                : 1
                Affiliations
                [1 ]Department of Geosciences, Princeton University, Princeton, NJ 08544
                [2 ]Max Planck Institute for Chemistry, Mainz 55128, Germany
                [3 ]Earth and Planetary Sciences, University of California-Santa Cruz, Santa Cruz, CA 95064
                [4 ]Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138
                [5 ]Department of Marine Sciences, University of Connecticut, Groton, CT 06340
                [6 ]Florence Bascom Geoscience Center, United States Geological Survey, Reston, VA 20192
                [7 ]Department of Geosciences, Environment and Society, Université Libre de Bruxelles, Brussels 1050, Belgium
                [8 ]Department of Earth Sciences, ETH Zürich, Zürich 8092, Switzerland
                Article
                10.1073/pnas.2206742119
                f1c73383-3e18-4e89-a2a8-c7957ab4e714
                © 2023

                https://creativecommons.org/licenses/by-nc-nd/4.0/

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