Changing atmospheric Δ^(14)C and the record of deep water paleoventilation ages
We propose a new calculation method to better estimate the deep water ventilation age from benthic-planktonic foraminifera ^(14)C ages. Our study is motivated by the fact that changes in atmospheric Δ^(14)C through time can cause contemporary benthic and planktonic foraminifera to have different in...
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American Geophysical Union
1997
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Online Access: | https://doi.org/10.1029/97PA00379 |
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ftcaltechauth:oai:authors.library.caltech.edu:y46zh-8x403 2024-06-23T07:53:49+00:00 Changing atmospheric Δ^(14)C and the record of deep water paleoventilation ages Adkins, Jess F. Boyle, Edward A. 1997-06 https://doi.org/10.1029/97PA00379 unknown American Geophysical Union https://doi.org/10.1029/97PA00379 oai:authors.library.caltech.edu:y46zh-8x403 eprintid:33600 resolverid:CaltechAUTHORS:20120828-100049534 info:eu-repo/semantics/openAccess Other Paleoceanography, 12(3), 337-344, (1997-06) info:eu-repo/semantics/article 1997 ftcaltechauth https://doi.org/10.1029/97PA00379 2024-06-12T04:08:49Z We propose a new calculation method to better estimate the deep water ventilation age from benthic-planktonic foraminifera ^(14)C ages. Our study is motivated by the fact that changes in atmospheric Δ^(14)C through time can cause contemporary benthic and planktonic foraminifera to have different initial Δ^(14)C values. This effect can cause spurious ventilation age changes to be interpreted from the geologic data. Using a new calculation method, ^(14)C projection ages, we recalculate the data from the Pacific Ocean. Contrary to previous results, we find that the Pacific intermediate and deep waters were about 600 years older than today at the last glacial maximum. In addition, there are possible signals of ventilation age change prior to ice sheet melting and at the Younger Dryas. However, the data are still too sparse to constrain these ventilation transients. © 1997 American Geophysical Union. Received 19 September 1996; accepted 26 January 1997; published 1 June 1997. We would like to thank Delia Oppo, Nick Shackleton and Daniel Sigman for helpful discussions. Edouard Bard, J. R. Toggweiler and M. L. Delaney provided constructive reviews of the manuscript. J. F. A. was supported by a NASA Global Change Fellowship and a grant from the Tokyo Electric and Power Company. We gratefully acknowledge the support of NSF grant# OCE-94-02198 and NOAA grant # NA46GP0282. Published - Adkins_Paleo1997p337.pdf Article in Journal/Newspaper Ice Sheet Planktonic foraminifera Caltech Authors (California Institute of Technology) Pacific Shackleton Paleoceanography 12 3 337 344 |
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Caltech Authors (California Institute of Technology) |
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description |
We propose a new calculation method to better estimate the deep water ventilation age from benthic-planktonic foraminifera ^(14)C ages. Our study is motivated by the fact that changes in atmospheric Δ^(14)C through time can cause contemporary benthic and planktonic foraminifera to have different initial Δ^(14)C values. This effect can cause spurious ventilation age changes to be interpreted from the geologic data. Using a new calculation method, ^(14)C projection ages, we recalculate the data from the Pacific Ocean. Contrary to previous results, we find that the Pacific intermediate and deep waters were about 600 years older than today at the last glacial maximum. In addition, there are possible signals of ventilation age change prior to ice sheet melting and at the Younger Dryas. However, the data are still too sparse to constrain these ventilation transients. © 1997 American Geophysical Union. Received 19 September 1996; accepted 26 January 1997; published 1 June 1997. We would like to thank Delia Oppo, Nick Shackleton and Daniel Sigman for helpful discussions. Edouard Bard, J. R. Toggweiler and M. L. Delaney provided constructive reviews of the manuscript. J. F. A. was supported by a NASA Global Change Fellowship and a grant from the Tokyo Electric and Power Company. We gratefully acknowledge the support of NSF grant# OCE-94-02198 and NOAA grant # NA46GP0282. Published - Adkins_Paleo1997p337.pdf |
format |
Article in Journal/Newspaper |
author |
Adkins, Jess F. Boyle, Edward A. |
spellingShingle |
Adkins, Jess F. Boyle, Edward A. Changing atmospheric Δ^(14)C and the record of deep water paleoventilation ages |
author_facet |
Adkins, Jess F. Boyle, Edward A. |
author_sort |
Adkins, Jess F. |
title |
Changing atmospheric Δ^(14)C and the record of deep water paleoventilation ages |
title_short |
Changing atmospheric Δ^(14)C and the record of deep water paleoventilation ages |
title_full |
Changing atmospheric Δ^(14)C and the record of deep water paleoventilation ages |
title_fullStr |
Changing atmospheric Δ^(14)C and the record of deep water paleoventilation ages |
title_full_unstemmed |
Changing atmospheric Δ^(14)C and the record of deep water paleoventilation ages |
title_sort |
changing atmospheric î”^(14)c and the record of deep water paleoventilation ages |
publisher |
American Geophysical Union |
publishDate |
1997 |
url |
https://doi.org/10.1029/97PA00379 |
geographic |
Pacific Shackleton |
geographic_facet |
Pacific Shackleton |
genre |
Ice Sheet Planktonic foraminifera |
genre_facet |
Ice Sheet Planktonic foraminifera |
op_source |
Paleoceanography, 12(3), 337-344, (1997-06) |
op_relation |
https://doi.org/10.1029/97PA00379 oai:authors.library.caltech.edu:y46zh-8x403 eprintid:33600 resolverid:CaltechAUTHORS:20120828-100049534 |
op_rights |
info:eu-repo/semantics/openAccess Other |
op_doi |
https://doi.org/10.1029/97PA00379 |
container_title |
Paleoceanography |
container_volume |
12 |
container_issue |
3 |
container_start_page |
337 |
op_container_end_page |
344 |
_version_ |
1802645654683516928 |