Ice and ocean constraints on early human migrations into North America along the Pacific coast
Founding populations of the first Americans likely occupied parts of Beringia during the Last Glacial Maximum (LGM). The timing, pathways, and modes of their southward transit remain unknown, but blockage of the interior route by North American ice sheets between ~26 and 14 cal kyr BP (ka) favors a...
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ftpubmed:oai:pubmedcentral.nih.gov:9963817 2023-05-15T18:17:25+02:00 Ice and ocean constraints on early human migrations into North America along the Pacific coast Praetorius, Summer K. Alder, Jay R. Condron, Alan Mix, Alan C. Walczak, Maureen H. Caissie, Beth E. Erlandson, Jon M. 2023-02-06 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9963817/ http://www.ncbi.nlm.nih.gov/pubmed/36745804 https://doi.org/10.1073/pnas.2208738120 en eng National Academy of Sciences http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9963817/ http://www.ncbi.nlm.nih.gov/pubmed/36745804 http://dx.doi.org/10.1073/pnas.2208738120 Copyright © 2023 the Author(s). Published by PNAS. https://creativecommons.org/licenses/by-nc-nd/4.0/This open access article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND) (https://creativecommons.org/licenses/by-nc-nd/4.0/) . CC-BY-NC-ND Proc Natl Acad Sci U S A Physical Sciences Text 2023 ftpubmed https://doi.org/10.1073/pnas.2208738120 2023-03-05T02:11:05Z Founding populations of the first Americans likely occupied parts of Beringia during the Last Glacial Maximum (LGM). The timing, pathways, and modes of their southward transit remain unknown, but blockage of the interior route by North American ice sheets between ~26 and 14 cal kyr BP (ka) favors a coastal route during this period. Using models and paleoceanographic data from the North Pacific, we identify climatically favorable intervals when humans could have plausibly traversed the Cordilleran coastal corridor during the terminal Pleistocene. Model simulations suggest that northward coastal currents strengthened during the LGM and at times of enhanced freshwater input, making southward transit by boat more difficult. Repeated Cordilleran glacial-calving events would have further challenged coastal transit on land and at sea. Following these events, ice-free coastal areas opened and seasonal sea ice was present along the Alaskan margin until at least 15 ka. Given evidence for humans south of the ice sheets by 16 ka and possibly earlier, we posit that early people may have taken advantage of winter sea ice that connected islands and coastal refugia. Marine ice-edge habitats offer a rich food supply and traversing coastal sea ice could have mitigated the difficulty of traveling southward in watercraft or on land over glaciers. We identify 24.5 to 22 ka and 16.4 to 14.8 ka as environmentally favorable time periods for coastal migration, when climate conditions provided both winter sea ice and ice-free summer conditions that facilitated year-round marine resource diversity and multiple modes of mobility along the North Pacific coast. Text Sea ice Beringia PubMed Central (PMC) Pacific Proceedings of the National Academy of Sciences 120 7 |
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Physical Sciences |
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Physical Sciences Praetorius, Summer K. Alder, Jay R. Condron, Alan Mix, Alan C. Walczak, Maureen H. Caissie, Beth E. Erlandson, Jon M. Ice and ocean constraints on early human migrations into North America along the Pacific coast |
topic_facet |
Physical Sciences |
description |
Founding populations of the first Americans likely occupied parts of Beringia during the Last Glacial Maximum (LGM). The timing, pathways, and modes of their southward transit remain unknown, but blockage of the interior route by North American ice sheets between ~26 and 14 cal kyr BP (ka) favors a coastal route during this period. Using models and paleoceanographic data from the North Pacific, we identify climatically favorable intervals when humans could have plausibly traversed the Cordilleran coastal corridor during the terminal Pleistocene. Model simulations suggest that northward coastal currents strengthened during the LGM and at times of enhanced freshwater input, making southward transit by boat more difficult. Repeated Cordilleran glacial-calving events would have further challenged coastal transit on land and at sea. Following these events, ice-free coastal areas opened and seasonal sea ice was present along the Alaskan margin until at least 15 ka. Given evidence for humans south of the ice sheets by 16 ka and possibly earlier, we posit that early people may have taken advantage of winter sea ice that connected islands and coastal refugia. Marine ice-edge habitats offer a rich food supply and traversing coastal sea ice could have mitigated the difficulty of traveling southward in watercraft or on land over glaciers. We identify 24.5 to 22 ka and 16.4 to 14.8 ka as environmentally favorable time periods for coastal migration, when climate conditions provided both winter sea ice and ice-free summer conditions that facilitated year-round marine resource diversity and multiple modes of mobility along the North Pacific coast. |
format |
Text |
author |
Praetorius, Summer K. Alder, Jay R. Condron, Alan Mix, Alan C. Walczak, Maureen H. Caissie, Beth E. Erlandson, Jon M. |
author_facet |
Praetorius, Summer K. Alder, Jay R. Condron, Alan Mix, Alan C. Walczak, Maureen H. Caissie, Beth E. Erlandson, Jon M. |
author_sort |
Praetorius, Summer K. |
title |
Ice and ocean constraints on early human migrations into North America along the Pacific coast |
title_short |
Ice and ocean constraints on early human migrations into North America along the Pacific coast |
title_full |
Ice and ocean constraints on early human migrations into North America along the Pacific coast |
title_fullStr |
Ice and ocean constraints on early human migrations into North America along the Pacific coast |
title_full_unstemmed |
Ice and ocean constraints on early human migrations into North America along the Pacific coast |
title_sort |
ice and ocean constraints on early human migrations into north america along the pacific coast |
publisher |
National Academy of Sciences |
publishDate |
2023 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9963817/ http://www.ncbi.nlm.nih.gov/pubmed/36745804 https://doi.org/10.1073/pnas.2208738120 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Sea ice Beringia |
genre_facet |
Sea ice Beringia |
op_source |
Proc Natl Acad Sci U S A |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9963817/ http://www.ncbi.nlm.nih.gov/pubmed/36745804 http://dx.doi.org/10.1073/pnas.2208738120 |
op_rights |
Copyright © 2023 the Author(s). Published by PNAS. https://creativecommons.org/licenses/by-nc-nd/4.0/This open access article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND) (https://creativecommons.org/licenses/by-nc-nd/4.0/) . |
op_rightsnorm |
CC-BY-NC-ND |
op_doi |
https://doi.org/10.1073/pnas.2208738120 |
container_title |
Proceedings of the National Academy of Sciences |
container_volume |
120 |
container_issue |
7 |
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1766191618374762496 |