Salinity of the Eocene Arctic Ocean from oxygen isotope analysis of fish bone carbonate ...

Stable isotope analysis was performed on the structural carbonate of fish bone apatite from early and early middle Eocene samples (~55 to ~45 Ma) recently recovered from the Lomonosov Ridge by Integrated Ocean Drilling Program Expedition 302 (the Arctic Coring Expedition). The d18O values of the Eoc...

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Main Authors: Waddell, Lindsey M, Moore, Theodore C
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2008
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.733934
https://doi.pangaea.de/10.1594/PANGAEA.733934
id ftdatacite:10.1594/pangaea.733934
record_format openpolar
spelling ftdatacite:10.1594/pangaea.733934 2024-09-15T17:53:25+00:00 Salinity of the Eocene Arctic Ocean from oxygen isotope analysis of fish bone carbonate ... Waddell, Lindsey M Moore, Theodore C 2008 application/zip https://dx.doi.org/10.1594/pangaea.733934 https://doi.pangaea.de/10.1594/PANGAEA.733934 en eng PANGAEA https://dx.doi.org/10.1029/2007pa001451 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Exp302 CCGS Captain Molly Kool Vidar Viking Integrated Ocean Drilling Program / International Ocean Discovery Program IODP article Collection Supplementary Publication Series of Datasets 2008 ftdatacite https://doi.org/10.1594/pangaea.73393410.1029/2007pa001451 2024-08-01T10:54:23Z Stable isotope analysis was performed on the structural carbonate of fish bone apatite from early and early middle Eocene samples (~55 to ~45 Ma) recently recovered from the Lomonosov Ridge by Integrated Ocean Drilling Program Expedition 302 (the Arctic Coring Expedition). The d18O values of the Eocene samples ranged from -6.84 per mil to -2.96 per mil Vienna Peedee belemnite, with a mean value of -4.89 per mil, compared to 2.77 per mil for a Miocene sample in the overlying section. An average salinity of 21 to 25 per mil was calculated for the Eocene Arctic, compared to 35 per mil for the Miocene, with lower salinities during the Paleocene Eocene thermal maximum, the Azolla event at ~48.7 Ma, and a third previously unidentified event at ~47.6 Ma. At the Azolla event, where the organic carbon content of the sediment reaches a maximum, a positive d13C excursion was observed, indicating unusually high productivity in the surface waters. ... : Supplement to: Waddell, Lindsey M; Moore, Theodore C (2008): Salinity of the Eocene Arctic Ocean from oxygen isotope analysis of fish bone carbonate. Paleoceanography, 23, PA1S04 ... Article in Journal/Newspaper Arctic Ocean Lomonosov Ridge DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
Exp302
CCGS Captain Molly Kool Vidar Viking
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
spellingShingle Composite Core
Exp302
CCGS Captain Molly Kool Vidar Viking
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
Waddell, Lindsey M
Moore, Theodore C
Salinity of the Eocene Arctic Ocean from oxygen isotope analysis of fish bone carbonate ...
topic_facet Composite Core
Exp302
CCGS Captain Molly Kool Vidar Viking
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
description Stable isotope analysis was performed on the structural carbonate of fish bone apatite from early and early middle Eocene samples (~55 to ~45 Ma) recently recovered from the Lomonosov Ridge by Integrated Ocean Drilling Program Expedition 302 (the Arctic Coring Expedition). The d18O values of the Eocene samples ranged from -6.84 per mil to -2.96 per mil Vienna Peedee belemnite, with a mean value of -4.89 per mil, compared to 2.77 per mil for a Miocene sample in the overlying section. An average salinity of 21 to 25 per mil was calculated for the Eocene Arctic, compared to 35 per mil for the Miocene, with lower salinities during the Paleocene Eocene thermal maximum, the Azolla event at ~48.7 Ma, and a third previously unidentified event at ~47.6 Ma. At the Azolla event, where the organic carbon content of the sediment reaches a maximum, a positive d13C excursion was observed, indicating unusually high productivity in the surface waters. ... : Supplement to: Waddell, Lindsey M; Moore, Theodore C (2008): Salinity of the Eocene Arctic Ocean from oxygen isotope analysis of fish bone carbonate. Paleoceanography, 23, PA1S04 ...
format Article in Journal/Newspaper
author Waddell, Lindsey M
Moore, Theodore C
author_facet Waddell, Lindsey M
Moore, Theodore C
author_sort Waddell, Lindsey M
title Salinity of the Eocene Arctic Ocean from oxygen isotope analysis of fish bone carbonate ...
title_short Salinity of the Eocene Arctic Ocean from oxygen isotope analysis of fish bone carbonate ...
title_full Salinity of the Eocene Arctic Ocean from oxygen isotope analysis of fish bone carbonate ...
title_fullStr Salinity of the Eocene Arctic Ocean from oxygen isotope analysis of fish bone carbonate ...
title_full_unstemmed Salinity of the Eocene Arctic Ocean from oxygen isotope analysis of fish bone carbonate ...
title_sort salinity of the eocene arctic ocean from oxygen isotope analysis of fish bone carbonate ...
publisher PANGAEA
publishDate 2008
url https://dx.doi.org/10.1594/pangaea.733934
https://doi.pangaea.de/10.1594/PANGAEA.733934
genre Arctic Ocean
Lomonosov Ridge
genre_facet Arctic Ocean
Lomonosov Ridge
op_relation https://dx.doi.org/10.1029/2007pa001451
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.73393410.1029/2007pa001451
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