Late Oligocene (26.2-25.2 Ma) radiogenic isotopes (Nd and Pb) from ODP Site 113-689

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Bibliographic Details
Main Authors: Creac'h, Layla, Brzelinski, Swaantje, Gutjahr, Marcus, Lippold, Jörg
Format: Dataset Open Access
Language:en
Published: PANGAEA 2026
Subjects:
113-689D; Age; Authigenic Pb; DEPTH, sediment/rock; Detrital Nd; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Lead-206/Lead-204 ratio, authigenic; Lead-206/Lead-204 ratio, authigenic, standard error; Lead-206/Lead-204 ratio, detrital; Lead-206/Lead-204 ratio, detrital, standard error; Lead-207/Lead-204 ratio, authigenic; Lead-207/Lead-204 ratio, authigenic, standard error; Lead-207/Lead-204 ratio, detrital; Lead-207/Lead-204 ratio, detrital, standard error; Lead-207/Lead-206 ratio, authigenic; Lead-207/Lead-206 ratio, authigenic, standard error; Lead-207/Lead-206 ratio, detrital; Lead-207/Lead-206 ratio, detrital, standard error; Lead-208/Lead-204 ratio, authigenic; Lead-208/Lead-204 ratio, authigenic, standard error; Lead-208/Lead-204 ratio, detrital; Lead-208/Lead-204 ratio, detrital, standard error; Lead-208/Lead-206 ratio, authigenic; Lead-208/Lead-206 ratio, authigenic, standard error; Lead-208/Lead-206 ratio, detrital; Lead-208/Lead-206 ratio, detrital, standard error; Lead-208/Lead-207 ratio, authigenic; Lead-208/Lead-207 ratio, authigenic, standard error; Lead-208/Lead-207 ratio, detrital; Lead-208/Lead-207 ratio, detrital, standard error; Lead isotopes; Leg113; Maud Rise; Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS), ThermoFisher Scientific, Neptune Plus; Neodymium; ODP 689; Oligocene; Radiogenic isotopes; Sample code/label; South Atlantic Ocean; Southern Ocean; ε-Neodymium, detrital; ε-Neodymium, detrital, standard error; ε-Neodymium (T)
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author Creac'h, Layla
Brzelinski, Swaantje
Gutjahr, Marcus
Lippold, Jörg
author_facet Creac'h, Layla
Brzelinski, Swaantje
Gutjahr, Marcus
Lippold, Jörg
collection Datos científicos de ciencias marinas y ambientales
contents This dataset features detrital neodymium (Nd) and authigenic lead (Pb) isotopic compositions from ODP Site 689, Maud Rise (64.5°S, 3.1°E, 2080 m water depth) spanning the late Oligocene (26.2 to 25.2 Ma). The age model was established following the magnetostratigraphic constraints of Florindo and Roberts (2005, doi:10.1130/B25541.1) and tuned to the age model of IODP Site 342-U1406 (van Peer et al., 2024, doi:10.1038/s41467-024-54186-1). Nd was isolated from the detrital fraction of the sediment via column chromatography using 50W-X8 and LN-Spec resins. Nd concentrations were measured by Thermo Scientific iCAP Triple Quadrupole Inductively Coupled Mass Spectrometry (TQ-ICP-MS) at the University of Heidelberg. Isotopic compositions (eNd) were analysed on a Thermo Scientific Neptune Plus Multi-Collector-ICP-MS at GEOMAR Helmholtz Centre for Ocean Research, Kiel. Isotopic data, expressed as eNd (eNd =[(143Nd/144Nd)/0.512638–1] x 10,000), were normalised to a 143Nd/144Nd value of 0.512115 for the JNdi-1 standard. Pb was isolated from the authigenic and (selected) detrital fractions of the sediment by ion-chromatography using AG1-X8 resin. Elemental concentrations were also measured by TQ-ICP-MS at the University of Heidelberg and isotopic compositions on a Thermo Scientific Neptune Plus MC-ICP-MS at GEOMAR Kiel.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_988416
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Late Oligocene (26.2-25.2 Ma) radiogenic isotopes (Nd and Pb) from ODP Site 113-689
Creac'h, Layla
Brzelinski, Swaantje
Gutjahr, Marcus
Lippold, Jörg
113-689D; Age; Authigenic Pb; DEPTH, sediment/rock; Detrital Nd; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Lead-206/Lead-204 ratio, authigenic; Lead-206/Lead-204 ratio, authigenic, standard error; Lead-206/Lead-204 ratio, detrital; Lead-206/Lead-204 ratio, detrital, standard error; Lead-207/Lead-204 ratio, authigenic; Lead-207/Lead-204 ratio, authigenic, standard error; Lead-207/Lead-204 ratio, detrital; Lead-207/Lead-204 ratio, detrital, standard error; Lead-207/Lead-206 ratio, authigenic; Lead-207/Lead-206 ratio, authigenic, standard error; Lead-207/Lead-206 ratio, detrital; Lead-207/Lead-206 ratio, detrital, standard error; Lead-208/Lead-204 ratio, authigenic; Lead-208/Lead-204 ratio, authigenic, standard error; Lead-208/Lead-204 ratio, detrital; Lead-208/Lead-204 ratio, detrital, standard error; Lead-208/Lead-206 ratio, authigenic; Lead-208/Lead-206 ratio, authigenic, standard error; Lead-208/Lead-206 ratio, detrital; Lead-208/Lead-206 ratio, detrital, standard error; Lead-208/Lead-207 ratio, authigenic; Lead-208/Lead-207 ratio, authigenic, standard error; Lead-208/Lead-207 ratio, detrital; Lead-208/Lead-207 ratio, detrital, standard error; Lead isotopes; Leg113; Maud Rise; Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS), ThermoFisher Scientific, Neptune Plus; Neodymium; ODP 689; Oligocene; Radiogenic isotopes; Sample code/label; South Atlantic Ocean; Southern Ocean; ε-Neodymium, detrital; ε-Neodymium, detrital, standard error; ε-Neodymium (T)
This dataset features detrital neodymium (Nd) and authigenic lead (Pb) isotopic compositions from ODP Site 689, Maud Rise (64.5°S, 3.1°E, 2080 m water depth) spanning the late Oligocene (26.2 to 25.2 Ma). The age model was established following the magnetostratigraphic constraints of Florindo and Roberts (2005, doi:10.1130/B25541.1) and tuned to the age model of IODP Site 342-U1406 (van Peer et al., 2024, doi:10.1038/s41467-024-54186-1). Nd was isolated from the detrital fraction of the sediment via column chromatography using 50W-X8 and LN-Spec resins. Nd concentrations were measured by Thermo Scientific iCAP Triple Quadrupole Inductively Coupled Mass Spectrometry (TQ-ICP-MS) at the University of Heidelberg. Isotopic compositions (eNd) were analysed on a Thermo Scientific Neptune Plus Multi-Collector-ICP-MS at GEOMAR Helmholtz Centre for Ocean Research, Kiel. Isotopic data, expressed as eNd (eNd =[(143Nd/144Nd)/0.512638–1] x 10,000), were normalised to a 143Nd/144Nd value of 0.512115 for the JNdi-1 standard. Pb was isolated from the authigenic and (selected) detrital fractions of the sediment by ion-chromatography using AG1-X8 resin. Elemental concentrations were also measured by TQ-ICP-MS at the University of Heidelberg and isotopic compositions on a Thermo Scientific Neptune Plus MC-ICP-MS at GEOMAR Kiel.
title Late Oligocene (26.2-25.2 Ma) radiogenic isotopes (Nd and Pb) from ODP Site 113-689
topic 113-689D; Age; Authigenic Pb; DEPTH, sediment/rock; Detrital Nd; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Lead-206/Lead-204 ratio, authigenic; Lead-206/Lead-204 ratio, authigenic, standard error; Lead-206/Lead-204 ratio, detrital; Lead-206/Lead-204 ratio, detrital, standard error; Lead-207/Lead-204 ratio, authigenic; Lead-207/Lead-204 ratio, authigenic, standard error; Lead-207/Lead-204 ratio, detrital; Lead-207/Lead-204 ratio, detrital, standard error; Lead-207/Lead-206 ratio, authigenic; Lead-207/Lead-206 ratio, authigenic, standard error; Lead-207/Lead-206 ratio, detrital; Lead-207/Lead-206 ratio, detrital, standard error; Lead-208/Lead-204 ratio, authigenic; Lead-208/Lead-204 ratio, authigenic, standard error; Lead-208/Lead-204 ratio, detrital; Lead-208/Lead-204 ratio, detrital, standard error; Lead-208/Lead-206 ratio, authigenic; Lead-208/Lead-206 ratio, authigenic, standard error; Lead-208/Lead-206 ratio, detrital; Lead-208/Lead-206 ratio, detrital, standard error; Lead-208/Lead-207 ratio, authigenic; Lead-208/Lead-207 ratio, authigenic, standard error; Lead-208/Lead-207 ratio, detrital; Lead-208/Lead-207 ratio, detrital, standard error; Lead isotopes; Leg113; Maud Rise; Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS), ThermoFisher Scientific, Neptune Plus; Neodymium; ODP 689; Oligocene; Radiogenic isotopes; Sample code/label; South Atlantic Ocean; Southern Ocean; ε-Neodymium, detrital; ε-Neodymium, detrital, standard error; ε-Neodymium (T)
url https://doi.org/10.1594/PANGAEA.988416