Radiocarbon in annual coral rings from the eastern Tropical Pacific Ocean
Sixty radiocarbon measurements were performed on aragonite from annually banded corals collected from three sites in the Galápagos Islands. Preanthropogenic Δ14C values of coral that grew around A.D. 1930 averaged −70‰. This is substantially lower than average values previously reported (−51‰) for c...
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ftcdlib:qt4mm0f43n 2023-05-15T17:32:28+02:00 Radiocarbon in annual coral rings from the eastern Tropical Pacific Ocean Druffel, Ellen M 59 - 62 1981-01-01 application/pdf http://www.escholarship.org/uc/item/4mm0f43n english eng eScholarship, University of California qt4mm0f43n http://www.escholarship.org/uc/item/4mm0f43n Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ CC-BY Druffel, Ellen M. (1981). Radiocarbon in annual coral rings from the eastern Tropical Pacific Ocean. Geophysical Research Letters, 8(1), 59 - 62. doi:10.1029/GL008i001p00059. UC Irvine: Department of Earth System Science, UCI. Retrieved from: http://www.escholarship.org/uc/item/4mm0f43n Physical Sciences and Mathematics oceanography article 1981 ftcdlib https://doi.org/10.1029/GL008i001p00059 2016-04-02T18:18:16Z Sixty radiocarbon measurements were performed on aragonite from annually banded corals collected from three sites in the Galápagos Islands. Preanthropogenic Δ14C values of coral that grew around A.D. 1930 averaged −70‰. This is substantially lower than average values previously reported (−51‰) for corals from Florida and Belize in the western North Atlantic Ocean. A decrease of 6‰ was noticed in coral that grew from 1930 to 1954. This decrease could be interpreted as a Suess effect in surface ocean water. The 100‰ increase in Δ14C for coral that grew from 1954 to 1973 is the result of bomb-produced 14C that was introduced to the surface ocean waters. The 14C levels in corals that grew during El Niño years were considerably higher than those for normal years. These higher values are attributed to the absence of up welling at the equator during El Niño events. Article in Journal/Newspaper North Atlantic University of California: eScholarship Pacific Geophysical Research Letters 8 1 59 62 |
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Open Polar |
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University of California: eScholarship |
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ftcdlib |
language |
English |
topic |
Physical Sciences and Mathematics oceanography |
spellingShingle |
Physical Sciences and Mathematics oceanography Druffel, Ellen M Radiocarbon in annual coral rings from the eastern Tropical Pacific Ocean |
topic_facet |
Physical Sciences and Mathematics oceanography |
description |
Sixty radiocarbon measurements were performed on aragonite from annually banded corals collected from three sites in the Galápagos Islands. Preanthropogenic Δ14C values of coral that grew around A.D. 1930 averaged −70‰. This is substantially lower than average values previously reported (−51‰) for corals from Florida and Belize in the western North Atlantic Ocean. A decrease of 6‰ was noticed in coral that grew from 1930 to 1954. This decrease could be interpreted as a Suess effect in surface ocean water. The 100‰ increase in Δ14C for coral that grew from 1954 to 1973 is the result of bomb-produced 14C that was introduced to the surface ocean waters. The 14C levels in corals that grew during El Niño years were considerably higher than those for normal years. These higher values are attributed to the absence of up welling at the equator during El Niño events. |
format |
Article in Journal/Newspaper |
author |
Druffel, Ellen M |
author_facet |
Druffel, Ellen M |
author_sort |
Druffel, Ellen M |
title |
Radiocarbon in annual coral rings from the eastern Tropical Pacific Ocean |
title_short |
Radiocarbon in annual coral rings from the eastern Tropical Pacific Ocean |
title_full |
Radiocarbon in annual coral rings from the eastern Tropical Pacific Ocean |
title_fullStr |
Radiocarbon in annual coral rings from the eastern Tropical Pacific Ocean |
title_full_unstemmed |
Radiocarbon in annual coral rings from the eastern Tropical Pacific Ocean |
title_sort |
radiocarbon in annual coral rings from the eastern tropical pacific ocean |
publisher |
eScholarship, University of California |
publishDate |
1981 |
url |
http://www.escholarship.org/uc/item/4mm0f43n |
op_coverage |
59 - 62 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Druffel, Ellen M. (1981). Radiocarbon in annual coral rings from the eastern Tropical Pacific Ocean. Geophysical Research Letters, 8(1), 59 - 62. doi:10.1029/GL008i001p00059. UC Irvine: Department of Earth System Science, UCI. Retrieved from: http://www.escholarship.org/uc/item/4mm0f43n |
op_relation |
qt4mm0f43n http://www.escholarship.org/uc/item/4mm0f43n |
op_rights |
Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1029/GL008i001p00059 |
container_title |
Geophysical Research Letters |
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8 |
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1 |
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59 |
op_container_end_page |
62 |
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1766130615643537408 |