Bayesian chronological analyses consistent with synchronous age of 12,835-12,735 Cal BP for Younger Dryas boundary on four continents

The Younger Dryas impact hypothesis posits that a cosmic impact across much of the Northern Hemisphere deposited the Younger Dryas boundary (YDB) layer, containing peak abundances in a variable assemblage of proxies, including magnetic and glassy impact-related spherules, high-temperature minerals a...

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Published in:Proceedings of the National Academy of Sciences
Main Authors: Kennett, James P., Kennett, Douglas J., Culleton, Brendan J., Aura Tortosa, J. Emili, Bischoff, James L., Bunch, Ted E., Daniel, I. Randolph, Erlandson, Jon M., Ferraro, David, Firestone, Richard B., Goodyear, Albert C., Israde-Alcantara, Isabel, Johnson, John R., Jorda Pardo, Jesus F., Kimbel, David R., LeCompte, Malcolm A., Lopinot, Neal H., Mahaney, William C., Moore, Andrew M. T., Moore, Christopher R., Ray, Jack H., Stafford, Thomas W., Tankersley, Kenneth Barnett, Wittke, James H., Wolbach, Wendy S., West, Allen
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Online Access:https://pure.au.dk/portal/en/publications/672ffb3e-c454-497d-81d5-aaa467b8d6ee
https://doi.org/10.1073/pnas.1507146112
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spelling ftuniaarhuspubl:oai:pure.atira.dk:publications/672ffb3e-c454-497d-81d5-aaa467b8d6ee 2024-02-11T10:04:23+01:00 Bayesian chronological analyses consistent with synchronous age of 12,835-12,735 Cal BP for Younger Dryas boundary on four continents Kennett, James P. Kennett, Douglas J. Culleton, Brendan J. Aura Tortosa, J. Emili Bischoff, James L. Bunch, Ted E. Daniel, I. Randolph Erlandson, Jon M. Ferraro, David Firestone, Richard B. Goodyear, Albert C. Israde-Alcantara, Isabel Johnson, John R. Jorda Pardo, Jesus F. Kimbel, David R. LeCompte, Malcolm A. Lopinot, Neal H. Mahaney, William C. Moore, Andrew M. T. Moore, Christopher R. Ray, Jack H. Stafford, Thomas W. Tankersley, Kenneth Barnett Wittke, James H. Wolbach, Wendy S. West, Allen 2015-08 https://pure.au.dk/portal/en/publications/672ffb3e-c454-497d-81d5-aaa467b8d6ee https://doi.org/10.1073/pnas.1507146112 eng eng https://pure.au.dk/portal/en/publications/672ffb3e-c454-497d-81d5-aaa467b8d6ee info:eu-repo/semantics/restrictedAccess Kennett , J P , Kennett , D J , Culleton , B J , Aura Tortosa , J E , Bischoff , J L , Bunch , T E , Daniel , I R , Erlandson , J M , Ferraro , D , Firestone , R B , Goodyear , A C , Israde-Alcantara , I , Johnson , J R , Jorda Pardo , J F , Kimbel , D R , LeCompte , M A , Lopinot , N H , Mahaney , W C , Moore , A M T , Moore , C R , Ray , J H , Stafford , T W , Tankersley , K B , Wittke , J H , Wolbach , W S & West , A 2015 , ' Bayesian chronological analyses consistent with synchronous age of 12,835-12,735 Cal BP for Younger Dryas boundary on four continents ' , Proceedings of the National Academy of Sciences , vol. 112 , no. 32 , pp. E4344-E4353 . https://doi.org/10.1073/pnas.1507146112 Younger Dryas comet Bayesian radiocarbon synchroneity IMPACT HYPOTHESIS EXTRATERRESTRIAL IMPACT COSMIC IMPACT DEPTH MODELS BLACK MAT NANODIAMONDS TERMINATION CALIFORNIA SPHERULES WILDFIRE article 2015 ftuniaarhuspubl https://doi.org/10.1073/pnas.1507146112 2024-01-24T23:59:04Z The Younger Dryas impact hypothesis posits that a cosmic impact across much of the Northern Hemisphere deposited the Younger Dryas boundary (YDB) layer, containing peak abundances in a variable assemblage of proxies, including magnetic and glassy impact-related spherules, high-temperature minerals and melt glass, nanodiamonds, carbon spherules, aciniform carbon, platinum, and osmium. Bayesian chronological modeling was applied to 354 dates from 23 stratigraphic sections in 12 countries on four continents to establish a modeled YDB age range for this event of 12,835-12,735 Cal B.P. at 95% probability. This range overlaps that of a peak in extraterrestrial platinum in the Greenland Ice Sheet and of the earliest age of the Younger Dryas climate episode in six proxy records, suggesting a causal connection between the YDB impact event and the Younger Dryas. Two statistical tests indicate that both modeled and unmodeled ages in the 30 records are consistent with synchronous deposition of the YDB layer within the limits of dating uncertainty (similar to 100 y). The widespread distribution of the YDB layer suggests that it may serve as a datum layer. Article in Journal/Newspaper Greenland Ice Sheet Aarhus University: Research Greenland Proceedings of the National Academy of Sciences 112 32 E4344 E4353
institution Open Polar
collection Aarhus University: Research
op_collection_id ftuniaarhuspubl
language English
topic Younger Dryas
comet
Bayesian
radiocarbon
synchroneity
IMPACT HYPOTHESIS
EXTRATERRESTRIAL IMPACT
COSMIC IMPACT
DEPTH MODELS
BLACK MAT
NANODIAMONDS
TERMINATION
CALIFORNIA
SPHERULES
WILDFIRE
spellingShingle Younger Dryas
comet
Bayesian
radiocarbon
synchroneity
IMPACT HYPOTHESIS
EXTRATERRESTRIAL IMPACT
COSMIC IMPACT
DEPTH MODELS
BLACK MAT
NANODIAMONDS
TERMINATION
CALIFORNIA
SPHERULES
WILDFIRE
Kennett, James P.
Kennett, Douglas J.
Culleton, Brendan J.
Aura Tortosa, J. Emili
Bischoff, James L.
Bunch, Ted E.
Daniel, I. Randolph
Erlandson, Jon M.
Ferraro, David
Firestone, Richard B.
Goodyear, Albert C.
Israde-Alcantara, Isabel
Johnson, John R.
Jorda Pardo, Jesus F.
Kimbel, David R.
LeCompte, Malcolm A.
Lopinot, Neal H.
Mahaney, William C.
Moore, Andrew M. T.
Moore, Christopher R.
Ray, Jack H.
Stafford, Thomas W.
Tankersley, Kenneth Barnett
Wittke, James H.
Wolbach, Wendy S.
West, Allen
Bayesian chronological analyses consistent with synchronous age of 12,835-12,735 Cal BP for Younger Dryas boundary on four continents
topic_facet Younger Dryas
comet
Bayesian
radiocarbon
synchroneity
IMPACT HYPOTHESIS
EXTRATERRESTRIAL IMPACT
COSMIC IMPACT
DEPTH MODELS
BLACK MAT
NANODIAMONDS
TERMINATION
CALIFORNIA
SPHERULES
WILDFIRE
description The Younger Dryas impact hypothesis posits that a cosmic impact across much of the Northern Hemisphere deposited the Younger Dryas boundary (YDB) layer, containing peak abundances in a variable assemblage of proxies, including magnetic and glassy impact-related spherules, high-temperature minerals and melt glass, nanodiamonds, carbon spherules, aciniform carbon, platinum, and osmium. Bayesian chronological modeling was applied to 354 dates from 23 stratigraphic sections in 12 countries on four continents to establish a modeled YDB age range for this event of 12,835-12,735 Cal B.P. at 95% probability. This range overlaps that of a peak in extraterrestrial platinum in the Greenland Ice Sheet and of the earliest age of the Younger Dryas climate episode in six proxy records, suggesting a causal connection between the YDB impact event and the Younger Dryas. Two statistical tests indicate that both modeled and unmodeled ages in the 30 records are consistent with synchronous deposition of the YDB layer within the limits of dating uncertainty (similar to 100 y). The widespread distribution of the YDB layer suggests that it may serve as a datum layer.
format Article in Journal/Newspaper
author Kennett, James P.
Kennett, Douglas J.
Culleton, Brendan J.
Aura Tortosa, J. Emili
Bischoff, James L.
Bunch, Ted E.
Daniel, I. Randolph
Erlandson, Jon M.
Ferraro, David
Firestone, Richard B.
Goodyear, Albert C.
Israde-Alcantara, Isabel
Johnson, John R.
Jorda Pardo, Jesus F.
Kimbel, David R.
LeCompte, Malcolm A.
Lopinot, Neal H.
Mahaney, William C.
Moore, Andrew M. T.
Moore, Christopher R.
Ray, Jack H.
Stafford, Thomas W.
Tankersley, Kenneth Barnett
Wittke, James H.
Wolbach, Wendy S.
West, Allen
author_facet Kennett, James P.
Kennett, Douglas J.
Culleton, Brendan J.
Aura Tortosa, J. Emili
Bischoff, James L.
Bunch, Ted E.
Daniel, I. Randolph
Erlandson, Jon M.
Ferraro, David
Firestone, Richard B.
Goodyear, Albert C.
Israde-Alcantara, Isabel
Johnson, John R.
Jorda Pardo, Jesus F.
Kimbel, David R.
LeCompte, Malcolm A.
Lopinot, Neal H.
Mahaney, William C.
Moore, Andrew M. T.
Moore, Christopher R.
Ray, Jack H.
Stafford, Thomas W.
Tankersley, Kenneth Barnett
Wittke, James H.
Wolbach, Wendy S.
West, Allen
author_sort Kennett, James P.
title Bayesian chronological analyses consistent with synchronous age of 12,835-12,735 Cal BP for Younger Dryas boundary on four continents
title_short Bayesian chronological analyses consistent with synchronous age of 12,835-12,735 Cal BP for Younger Dryas boundary on four continents
title_full Bayesian chronological analyses consistent with synchronous age of 12,835-12,735 Cal BP for Younger Dryas boundary on four continents
title_fullStr Bayesian chronological analyses consistent with synchronous age of 12,835-12,735 Cal BP for Younger Dryas boundary on four continents
title_full_unstemmed Bayesian chronological analyses consistent with synchronous age of 12,835-12,735 Cal BP for Younger Dryas boundary on four continents
title_sort bayesian chronological analyses consistent with synchronous age of 12,835-12,735 cal bp for younger dryas boundary on four continents
publishDate 2015
url https://pure.au.dk/portal/en/publications/672ffb3e-c454-497d-81d5-aaa467b8d6ee
https://doi.org/10.1073/pnas.1507146112
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_source Kennett , J P , Kennett , D J , Culleton , B J , Aura Tortosa , J E , Bischoff , J L , Bunch , T E , Daniel , I R , Erlandson , J M , Ferraro , D , Firestone , R B , Goodyear , A C , Israde-Alcantara , I , Johnson , J R , Jorda Pardo , J F , Kimbel , D R , LeCompte , M A , Lopinot , N H , Mahaney , W C , Moore , A M T , Moore , C R , Ray , J H , Stafford , T W , Tankersley , K B , Wittke , J H , Wolbach , W S & West , A 2015 , ' Bayesian chronological analyses consistent with synchronous age of 12,835-12,735 Cal BP for Younger Dryas boundary on four continents ' , Proceedings of the National Academy of Sciences , vol. 112 , no. 32 , pp. E4344-E4353 . https://doi.org/10.1073/pnas.1507146112
op_relation https://pure.au.dk/portal/en/publications/672ffb3e-c454-497d-81d5-aaa467b8d6ee
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1073/pnas.1507146112
container_title Proceedings of the National Academy of Sciences
container_volume 112
container_issue 32
container_start_page E4344
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