Articles | Volume 13, issue 8
https://doi.org/10.5194/cp-13-991-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/cp-13-991-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Post-glacial flooding of the Bering Land Bridge dated to 11 cal ka BP based on new geophysical and sediment records
Martin Jakobsson
CORRESPONDING AUTHOR
Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Christof Pearce
Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Department of Geoscience, Aarhus University, 8000 Aarhus, Denmark
Thomas M. Cronin
US Geological Survey MS926A, Reston, Virginia 20192, USA
Jan Backman
Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Leif G. Anderson
Department of Marine Sciences, University of Gothenburg, 412 96
Gothenburg, Sweden
Natalia Barrientos
Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Göran Björk
Department of Marine Sciences, University of Gothenburg, 412 96
Gothenburg, Sweden
Helen Coxall
Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Agatha de Boer
Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Larry A. Mayer
Center for Coastal and Ocean Mapping, University of New Hampshire, Durham, New
Hampshire 03824, USA
Carl-Magnus Mörth
Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Johan Nilsson
Department of Meteorology, Stockholm University, 106 91 Stockholm,
Sweden
Jayne E. Rattray
Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Christian Stranne
Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Center for Coastal and Ocean Mapping, University of New Hampshire, Durham, New
Hampshire 03824, USA
Igor Semiletov
Pacific Oceanological Institute, Far Eastern Branch of the Russian
Academy of Sciences, 690041 Vladivostok, Russia
Tomsk Polytechnic University, Tomsk, Russia
Matt O'Regan
Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
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- Younger-Dryas cooling and sea-ice feedbacks were prominent features of the Pleistocene-Holocene transition in Arctic Alaska B. Gaglioti et al. 10.1016/j.quascirev.2017.05.012
- The deglaciation of the Americas during the Last Glacial Termination D. Palacios et al. 10.1016/j.earscirev.2020.103113
- Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming V. Meyer et al. 10.1088/1748-9326/ab2653
- Molecular Genetic Analysis of the Relationships and Origin of Smelt (Hypomesus, Osmeridae), a New Component of the Fauna of the Barents Sea L. Skurikhina et al. 10.1134/S1022795419070135
- Sea level fingerprinting of the Bering Strait flooding history detects the source of the Younger Dryas climate event T. Pico et al. 10.1126/sciadv.aay2935
- GLOBAL CHOKE POINTS MAY LINK SEA LEVEL AND HUMAN SETTLEMENT AT THE LAST GLACIAL MAXIMUM J. Dobson et al. 10.1080/00167428.2020.1728195
- Functional immune diversity in reindeer reveals a high Arctic population at risk M. Lukacs et al. 10.3389/fevo.2022.1058674
- Deglacial floods in the Beaufort Sea preceded Younger Dryas cooling L. Keigwin et al. 10.1038/s41561-018-0169-6
- Late Pleistocene and Holocene transgression inferred from the sediments of the Gulf of San Jorge, central Patagonia, Argentina P. Desiage et al. 10.1002/jqs.3511
- Late Holocene Paleomagnetic Secular Variation in the Chukchi Sea, Arctic Ocean G. West et al. 10.1029/2021GC010187
- Holocene paleoenvironmental change based on diatom records from the continental shelf of the Chukchi Sea in the Arctic Ocean Y. Bak & S. Nam 10.1007/s12303-023-0040-7
- Sedimentary proxies for Pacific water inflow through the Herald Canyon, western Arctic Ocean H. Swärd et al. 10.1007/s41063-018-0055-x
- A new 30 000-year chronology for rapidly deposited sediments on the Lomonosov Ridge using bulk radiocarbon dating and probabilistic stratigraphic alignment F. Muschitiello et al. 10.5194/gchron-2-81-2020
- Methane flux from Beringian coastal wetlands for the past 20,000 years M. Fuchs et al. 10.1016/j.quascirev.2024.108976
- Holocene dynamics in the Bering Strait inflow to the Arctic and the Beaufort Gyre circulation based on sedimentary records from the Chukchi Sea M. Yamamoto et al. 10.5194/cp-13-1111-2017
- Intermediate- and Deep-Water Oxygenation History in the Subarctic North Pacific During the Last Deglacial Period E. Ovsepyan et al. 10.3389/feart.2021.638069
- A stable isotope record of late Quaternary hydrologic change in the northwestern Brooks Range, Alaska (eastern Beringia) A. King et al. 10.1002/jqs.3368
- Deglacial records of terrigenous organic matter accumulation off the Yukon and Amur rivers based on lignin phenols and long-chain n-alkanes M. Cao et al. 10.5194/cp-19-159-2023
- Late Holocene paleoceanography in the Chukchi and Beaufort Seas, Arctic Ocean, based on benthic foraminifera and ostracodes J. Seidenstein et al. 10.1007/s41063-018-0058-7
- NEW EVIDENCE OF THE EARLIEST DOMESTIC DOGS IN THE AMERICAS A. Perri et al. 10.1017/aaq.2018.74
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Discussed (preprint)
Latest update: 23 Nov 2024
Short summary
The Arctic and Pacific oceans are connected by the presently ~53 m deep Bering Strait. During the last glacial period when the sea level was lower than today, the Bering Strait was exposed. Humans and animals could then migrate between Asia and North America across the formed land bridge. From analyses of sediment cores and geophysical mapping data from Herald Canyon north of the Bering Strait, we show that the land bridge was flooded about 11 000 years ago.
The Arctic and Pacific oceans are connected by the presently ~53 m deep Bering Strait. During...
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