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

Author:

Farmer Jesse R.12ORCID,Pico Tamara3ORCID,Underwood Ona M.1,Cleveland Stout Rebecca4ORCID,Granger Julie5ORCID,Cronin Thomas M.6ORCID,Fripiat François27ORCID,Martínez-García Alfredo2ORCID,Haug Gerald H.28ORCID,Sigman Daniel M.1ORCID

Affiliation:

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

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.

Funder

National Science Foundation

DOI | U.S. Geological Survey

Max-Planck-Institut für Chemie

Publisher

Proceedings of the National Academy of Sciences

Subject

Multidisciplinary

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