Hydrogen isotope ratios of alkenones from ODP Site 202-1234
Hydrogen isotope ratios of long-chain alkenones (δ2HC37 ratios) have been shown to correlate with salinity in several culture studies. However, it is uncertain how applicable the δ2HC37-salinity relationship is to reconstruct past salinity. δ2HC37 ratios were measured on sediments from a drill core...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.900871 2024-09-15T18:31:05+00:00 Hydrogen isotope ratios of alkenones from ODP Site 202-1234 Weiss, Gabriella M de Bar, Marijke W Stolwijk, Dave Schouten, Stefan Sinninghe Damsté, Jaap S van der Meer, Marcel T J LATITUDE: -36.219217 * LONGITUDE: -73.681700 * DATE/TIME START: 2002-04-15T00:00:00 * DATE/TIME END: 2002-04-15T00:00:00 * MINIMUM ELEVATION: -1014.7 m * MAXIMUM ELEVATION: -1014.7 m 2019 text/tab-separated-values, 648 data points https://doi.pangaea.de/10.1594/PANGAEA.900871 https://doi.org/10.1594/PANGAEA.900871 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.900871 https://doi.org/10.1594/PANGAEA.900871 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Weiss, Gabriella M; de Bar, Marijke W; Stolwjik, D J; Schouten, Stefan; Sinninghe Damsté, Jaap S; van der Meer, Marcel T J (2019): Paleosensitivity of Hydrogen Isotope Ratios of Long‐Chain Alkenones to Salinity Changes at the Chile Margin. Paleoceanography and Paleoclimatology, 34(6), 978-989, https://doi.org/10.1029/2019PA003591 202-1234 AGE Alkenone C37 per unit sediment mass Alkenone C37:2 δD standard deviation Alkenone C37:3 Alkenones Chile Margin COMPCORE Composite Core Depth composite Hydrogen isotopes Ice volume corrected Joides Resolution Leg202 NIOZ_UU NIOZ Royal Netherlands Institute for Sea Research and Utrecht University Ocean Drilling Program ODP paleosalinity South Pacific Ocean δ Deuterium C37 dataset 2019 ftpangaea https://doi.org/10.1594/PANGAEA.90087110.1029/2019PA003591 2024-07-24T02:31:34Z Hydrogen isotope ratios of long-chain alkenones (δ2HC37 ratios) have been shown to correlate with salinity in several culture studies. However, it is uncertain how applicable the δ2HC37-salinity relationship is to reconstruct past salinity. δ2HC37 ratios were measured on sediments from a drill core (ODP site 1234) at the Chilean Margin covering the last ~150 kyr. High δ2HC37 values correspond to glacial time periods and interglacial periods are characterized by lower δ2HC37 values, aligning with δ18O ratios measured on planktonic foraminifera from the same core. Effects of parameters such as species composition, the δ2H-δ18O relationship used for ice volume corrections, and nutrient or light controlled growth rate, do not appear to significantly alter δ2HC37 ratios at ODP 1234. We use linear regression equations from batch culture experiments, marine surface sediments, and suspended particulate organic matter to quantitatively characterize salinity changes over the last ~150 kyr at ODP 1234. However, most of these equations yield larger salinity shifts than previously suggested, a phenomenon also observed for other δ2HC37 records. This suggests that the paleosensitivity of δ2HC37 ratios to salinity is larger in the geologic record than has been observed in any modern environment or laboratory settings, or that glacial to interglacial salinity shifts might be larger than currently believed. Dataset Planktonic foraminifera PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-73.681700,-73.681700,-36.219217,-36.219217) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
202-1234 AGE Alkenone C37 per unit sediment mass Alkenone C37:2 δD standard deviation Alkenone C37:3 Alkenones Chile Margin COMPCORE Composite Core Depth composite Hydrogen isotopes Ice volume corrected Joides Resolution Leg202 NIOZ_UU NIOZ Royal Netherlands Institute for Sea Research and Utrecht University Ocean Drilling Program ODP paleosalinity South Pacific Ocean δ Deuterium C37 |
spellingShingle |
202-1234 AGE Alkenone C37 per unit sediment mass Alkenone C37:2 δD standard deviation Alkenone C37:3 Alkenones Chile Margin COMPCORE Composite Core Depth composite Hydrogen isotopes Ice volume corrected Joides Resolution Leg202 NIOZ_UU NIOZ Royal Netherlands Institute for Sea Research and Utrecht University Ocean Drilling Program ODP paleosalinity South Pacific Ocean δ Deuterium C37 Weiss, Gabriella M de Bar, Marijke W Stolwijk, Dave Schouten, Stefan Sinninghe Damsté, Jaap S van der Meer, Marcel T J Hydrogen isotope ratios of alkenones from ODP Site 202-1234 |
topic_facet |
202-1234 AGE Alkenone C37 per unit sediment mass Alkenone C37:2 δD standard deviation Alkenone C37:3 Alkenones Chile Margin COMPCORE Composite Core Depth composite Hydrogen isotopes Ice volume corrected Joides Resolution Leg202 NIOZ_UU NIOZ Royal Netherlands Institute for Sea Research and Utrecht University Ocean Drilling Program ODP paleosalinity South Pacific Ocean δ Deuterium C37 |
description |
Hydrogen isotope ratios of long-chain alkenones (δ2HC37 ratios) have been shown to correlate with salinity in several culture studies. However, it is uncertain how applicable the δ2HC37-salinity relationship is to reconstruct past salinity. δ2HC37 ratios were measured on sediments from a drill core (ODP site 1234) at the Chilean Margin covering the last ~150 kyr. High δ2HC37 values correspond to glacial time periods and interglacial periods are characterized by lower δ2HC37 values, aligning with δ18O ratios measured on planktonic foraminifera from the same core. Effects of parameters such as species composition, the δ2H-δ18O relationship used for ice volume corrections, and nutrient or light controlled growth rate, do not appear to significantly alter δ2HC37 ratios at ODP 1234. We use linear regression equations from batch culture experiments, marine surface sediments, and suspended particulate organic matter to quantitatively characterize salinity changes over the last ~150 kyr at ODP 1234. However, most of these equations yield larger salinity shifts than previously suggested, a phenomenon also observed for other δ2HC37 records. This suggests that the paleosensitivity of δ2HC37 ratios to salinity is larger in the geologic record than has been observed in any modern environment or laboratory settings, or that glacial to interglacial salinity shifts might be larger than currently believed. |
format |
Dataset |
author |
Weiss, Gabriella M de Bar, Marijke W Stolwijk, Dave Schouten, Stefan Sinninghe Damsté, Jaap S van der Meer, Marcel T J |
author_facet |
Weiss, Gabriella M de Bar, Marijke W Stolwijk, Dave Schouten, Stefan Sinninghe Damsté, Jaap S van der Meer, Marcel T J |
author_sort |
Weiss, Gabriella M |
title |
Hydrogen isotope ratios of alkenones from ODP Site 202-1234 |
title_short |
Hydrogen isotope ratios of alkenones from ODP Site 202-1234 |
title_full |
Hydrogen isotope ratios of alkenones from ODP Site 202-1234 |
title_fullStr |
Hydrogen isotope ratios of alkenones from ODP Site 202-1234 |
title_full_unstemmed |
Hydrogen isotope ratios of alkenones from ODP Site 202-1234 |
title_sort |
hydrogen isotope ratios of alkenones from odp site 202-1234 |
publisher |
PANGAEA |
publishDate |
2019 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.900871 https://doi.org/10.1594/PANGAEA.900871 |
op_coverage |
LATITUDE: -36.219217 * LONGITUDE: -73.681700 * DATE/TIME START: 2002-04-15T00:00:00 * DATE/TIME END: 2002-04-15T00:00:00 * MINIMUM ELEVATION: -1014.7 m * MAXIMUM ELEVATION: -1014.7 m |
long_lat |
ENVELOPE(-73.681700,-73.681700,-36.219217,-36.219217) |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
Supplement to: Weiss, Gabriella M; de Bar, Marijke W; Stolwjik, D J; Schouten, Stefan; Sinninghe Damsté, Jaap S; van der Meer, Marcel T J (2019): Paleosensitivity of Hydrogen Isotope Ratios of Long‐Chain Alkenones to Salinity Changes at the Chile Margin. Paleoceanography and Paleoclimatology, 34(6), 978-989, https://doi.org/10.1029/2019PA003591 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.900871 https://doi.org/10.1594/PANGAEA.900871 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.90087110.1029/2019PA003591 |
_version_ |
1810472697382043648 |