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

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          Significance

          The Bering Strait was a land bridge during the peak of the last ice age (the Last Glacial Maximum, LGM), when sea level was ~130 m lower than today. This study reconstructs the history of sea level at the Bering Strait by tracing the influence of Pacific waters in the Arctic Ocean. We find that the Bering Strait was open from at least 46,000 until 35,700 y ago, thus dating the last formation of the land bridge to within 10,000 y of the LGM. This history requires that ice volume increased rapidly into the LGM. In addition, it appears that humans migrated to the Americas as soon as the formation of the land bridge allowed for their passage.

          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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          Most cited references71

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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

                Contributors
                Journal
                Proc Natl Acad Sci U S A
                Proc Natl Acad Sci U S A
                PNAS
                Proceedings of the National Academy of Sciences of the United States of America
                National Academy of Sciences
                0027-8424
                1091-6490
                27 December 2022
                3 January 2023
                27 December 2022
                : 120
                : 1
                : e2206742119
                Affiliations
                [1] aDepartment of Geosciences, Princeton University , Princeton, NJ 08544
                [2] bMax Planck Institute for Chemistry , Mainz 55128, Germany
                [3] cEarth and Planetary Sciences, University of California-Santa Cruz , Santa Cruz, CA 95064
                [4] dDepartment of Earth and Planetary Sciences, Harvard University , Cambridge, MA 02138
                [5] eDepartment of Marine Sciences, University of Connecticut , Groton, CT 06340
                [6] fFlorence Bascom Geoscience Center, United States Geological Survey , Reston, VA 20192
                [7] gDepartment of Geosciences, Environment and Society, Université Libre de Bruxelles , Brussels 1050, Belgium
                [8] hDepartment of Earth Sciences, ETH Zürich , Zürich 8092, Switzerland
                Author notes
                1To whom correspondence may be addressed. Email: jesse.farmer@ 123456umb.edu or tpico@ 123456ucsc.edu .

                Edited by Claire Waelbroeck, Laboratoire d'Océanographie et du Climat: Expérimentations et Approches Numériques, Institut Pierre-Simon Laplace, Paris, France; received April 18, 2022; accepted October 21, 2022 by Editorial Board Member Jean Jouzel

                2Present address: Department of Atmospheric Sciences, University of Washington, Seattle, WA 98195.

                Author information
                https://orcid.org/0000-0001-5200-6429
                https://orcid.org/0000-0002-3629-0922
                https://orcid.org/0000-0002-0852-1922
                https://orcid.org/0000-0001-9985-9242
                https://orcid.org/0000-0002-2643-0979
                https://orcid.org/0000-0002-2591-6301
                https://orcid.org/0000-0002-7206-5079
                https://orcid.org/0000-0001-7534-4420
                https://orcid.org/0000-0002-7923-1973
                Article
                202206742
                10.1073/pnas.2206742119
                9910591
                36574665
                f1c73383-3e18-4e89-a2a8-c7957ab4e714
                Copyright © 2022 the Author(s). Published by PNAS.

                This open access article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND).

                History
                : 18 April 2022
                : 21 October 2022
                Page count
                Pages: 7, Words: 5728
                Funding
                Funded by: National Science Foundation (NSF), FundRef 100000001;
                Award ID: OCE-2054780
                Award Recipient : Jesse R Farmer Award Recipient : Tamara Pico Award Recipient : Ona M Underwood Award Recipient : Daniel M Sigman
                Funded by: National Science Foundation (NSF), FundRef 100000001;
                Award ID: OCE-2054757
                Award Recipient : Jesse R Farmer Award Recipient : Tamara Pico Award Recipient : Ona M Underwood Award Recipient : Daniel M Sigman
                Funded by: DOI | U.S. Geological Survey (USGS), FundRef 100000203;
                Award ID: Climate Research and Development Program
                Award Recipient : Thomas M Cronin
                Funded by: Max-Planck-Institut für Chemie (MPIC), FundRef 501100017039;
                Award ID: n/a
                Award Recipient : Jesse R Farmer Award Recipient : Alfredo Martinez-Garcia Award Recipient : Gerald H. Haug
                Categories
                dataset, Dataset
                research-article, Research Article
                earth-sci, Earth, Atmospheric, and Planetary Sciences
                413
                Physical Sciences
                Earth, Atmospheric, and Planetary Sciences

                arctic ocean,bering strait,sea level,foraminifera-bound n isotopes,glacial isostatic adjustment

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