Radiocarbon age offsets between two surface dwelling planktonic foraminifera species during abrupt climate events in the SW Iberian margin ...
This study identifies temporal biases in the radiocarbon ages of the planktonic foraminifera species Globigerina bulloides and Globigerinoides ruber (white) in a sediment core from the SW Iberian margin (so‐called Shackleton site). Leaching of the outer shell and measurement of the radiocarbon conte...
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ETH Zurich
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Online Access: | https://dx.doi.org/10.3929/ethz-b-000317044 http://hdl.handle.net/20.500.11850/317044 |
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ftdatacite:10.3929/ethz-b-000317044 2024-09-30T14:41:30+00:00 Radiocarbon age offsets between two surface dwelling planktonic foraminifera species during abrupt climate events in the SW Iberian margin ... Ausin, Blanca Haghipour, Negar Wacker, Lukas Voelker, Antje H.L. Hodell, David Magill, Clayton Looser, Nathan Bernasconi, Stefano M. Eglinton, Timothy I. 2019 application/pdf https://dx.doi.org/10.3929/ethz-b-000317044 http://hdl.handle.net/20.500.11850/317044 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 radiocarbon bioturbation Globigerina bulloides Globigerinoides ruber Shackleton Sites Iberian Margin Text Journal Article ScholarlyArticle article-journal 2019 ftdatacite https://doi.org/10.3929/ethz-b-000317044 2024-09-02T07:54:09Z This study identifies temporal biases in the radiocarbon ages of the planktonic foraminifera species Globigerina bulloides and Globigerinoides ruber (white) in a sediment core from the SW Iberian margin (so‐called Shackleton site). Leaching of the outer shell and measurement of the radiocarbon content of both the leachate and leached sample enabled us to identify surface contamination of the tests and its impact on their 14C ages. Incorporation of younger radiocarbon on the outer shell affected both species and had a larger impact downcore. Interspecies comparison of the 14C ages of the leached samples reveal systematic offsets with 14C ages for G. ruber being younger than G. bulloides ages during the last deglaciation and part of the Early and mid‐Holocene. The greatest offsets (up to 1,030 years) were found during Heinrich Stadial 1, the Younger Dryas, and part of the Holocene. The potential factors differentially affecting these two planktonic species were assessed by complementary 14C, oxygen and carbon ... : Paleoceanography and Paleoclimatology, 34 (1) ... Text Planktonic foraminifera DataCite Shackleton |
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collection |
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op_collection_id |
ftdatacite |
language |
English |
topic |
radiocarbon bioturbation Globigerina bulloides Globigerinoides ruber Shackleton Sites Iberian Margin |
spellingShingle |
radiocarbon bioturbation Globigerina bulloides Globigerinoides ruber Shackleton Sites Iberian Margin Ausin, Blanca Haghipour, Negar Wacker, Lukas Voelker, Antje H.L. Hodell, David Magill, Clayton Looser, Nathan Bernasconi, Stefano M. Eglinton, Timothy I. Radiocarbon age offsets between two surface dwelling planktonic foraminifera species during abrupt climate events in the SW Iberian margin ... |
topic_facet |
radiocarbon bioturbation Globigerina bulloides Globigerinoides ruber Shackleton Sites Iberian Margin |
description |
This study identifies temporal biases in the radiocarbon ages of the planktonic foraminifera species Globigerina bulloides and Globigerinoides ruber (white) in a sediment core from the SW Iberian margin (so‐called Shackleton site). Leaching of the outer shell and measurement of the radiocarbon content of both the leachate and leached sample enabled us to identify surface contamination of the tests and its impact on their 14C ages. Incorporation of younger radiocarbon on the outer shell affected both species and had a larger impact downcore. Interspecies comparison of the 14C ages of the leached samples reveal systematic offsets with 14C ages for G. ruber being younger than G. bulloides ages during the last deglaciation and part of the Early and mid‐Holocene. The greatest offsets (up to 1,030 years) were found during Heinrich Stadial 1, the Younger Dryas, and part of the Holocene. The potential factors differentially affecting these two planktonic species were assessed by complementary 14C, oxygen and carbon ... : Paleoceanography and Paleoclimatology, 34 (1) ... |
format |
Text |
author |
Ausin, Blanca Haghipour, Negar Wacker, Lukas Voelker, Antje H.L. Hodell, David Magill, Clayton Looser, Nathan Bernasconi, Stefano M. Eglinton, Timothy I. |
author_facet |
Ausin, Blanca Haghipour, Negar Wacker, Lukas Voelker, Antje H.L. Hodell, David Magill, Clayton Looser, Nathan Bernasconi, Stefano M. Eglinton, Timothy I. |
author_sort |
Ausin, Blanca |
title |
Radiocarbon age offsets between two surface dwelling planktonic foraminifera species during abrupt climate events in the SW Iberian margin ... |
title_short |
Radiocarbon age offsets between two surface dwelling planktonic foraminifera species during abrupt climate events in the SW Iberian margin ... |
title_full |
Radiocarbon age offsets between two surface dwelling planktonic foraminifera species during abrupt climate events in the SW Iberian margin ... |
title_fullStr |
Radiocarbon age offsets between two surface dwelling planktonic foraminifera species during abrupt climate events in the SW Iberian margin ... |
title_full_unstemmed |
Radiocarbon age offsets between two surface dwelling planktonic foraminifera species during abrupt climate events in the SW Iberian margin ... |
title_sort |
radiocarbon age offsets between two surface dwelling planktonic foraminifera species during abrupt climate events in the sw iberian margin ... |
publisher |
ETH Zurich |
publishDate |
2019 |
url |
https://dx.doi.org/10.3929/ethz-b-000317044 http://hdl.handle.net/20.500.11850/317044 |
geographic |
Shackleton |
geographic_facet |
Shackleton |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 |
op_doi |
https://doi.org/10.3929/ethz-b-000317044 |
_version_ |
1811643980587204608 |