_version_ 1867170451064619008
author Hallmaier, Moritz
Gutjahr, Marcus
Hemming, Sidney R
Lippold, Jörg
Weber, Michael E
Eisenhauer, Anton
author_facet Hallmaier, Moritz
Gutjahr, Marcus
Hemming, Sidney R
Lippold, Jörg
Weber, Michael E
Eisenhauer, Anton
collection Datos científicos de ciencias marinas y ambientales
contents We report radiogenic isotope records of IODP site U1537 in the Scotia Sea through the last 200,000 years. Detrital neodymium (ɛNd) varies between -3.8 and -8.6 (excluding two extremely radiogenic layers influenced by ash, which were excluded for the interpretation). Authigenic and detrital Pb isotope ratios show variations in line with detrital ɛNd. The data shows excursions towards older sediment and water mass sources during terminations, indicating a deglacial Weddell Sea Deep Water Pulse. All isotope measurements were conducted on a Multi-Collector Inductively Coupled Mass Spectrometer (MC-ICP-MS, Thermo Scientific Neptune Plus) at GEOMAR Helmholtz Center for Ocean Research. Smoothed records were fitted to the data with a Loess Bootstrap Model (see dataset in Further Details). For details on sample preparation and measurements consult the main manuscript. The radiogenic isotope datasets are complemented by the > 63 µm sediment weight fraction. For the last 170 ka the reported ages are based on the age model from Lu et al. 2022, older ages follow Weber et al. 2022.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_993170
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Detrital neodymium isotope composition of IODP Site U1537
Hallmaier, Moritz
Gutjahr, Marcus
Hemming, Sidney R
Lippold, Jörg
Weber, Michael E
Eisenhauer, Anton
382-U1537; AGE; Antarctica; Comment; COMPCORE; Composite Core; Depth, composite; detrital; Exp382; Fraction, description; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; isotopes; Joides Resolution; Lead isotopes; Neodymium-143/Neodymium-144 ratio; Neodymium-144/Neodymium-143 ratio, standard error; Neodymium isotopes; Number; Sample code/label; Scotia Sea; Southern Ocean; Weddell Sea; ε-Neodymium; ε-Neodymium, standard error
We report radiogenic isotope records of IODP site U1537 in the Scotia Sea through the last 200,000 years. Detrital neodymium (ɛNd) varies between -3.8 and -8.6 (excluding two extremely radiogenic layers influenced by ash, which were excluded for the interpretation). Authigenic and detrital Pb isotope ratios show variations in line with detrital ɛNd. The data shows excursions towards older sediment and water mass sources during terminations, indicating a deglacial Weddell Sea Deep Water Pulse. All isotope measurements were conducted on a Multi-Collector Inductively Coupled Mass Spectrometer (MC-ICP-MS, Thermo Scientific Neptune Plus) at GEOMAR Helmholtz Center for Ocean Research. Smoothed records were fitted to the data with a Loess Bootstrap Model (see dataset in Further Details). For details on sample preparation and measurements consult the main manuscript. The radiogenic isotope datasets are complemented by the > 63 µm sediment weight fraction. For the last 170 ka the reported ages are based on the age model from Lu et al. 2022, older ages follow Weber et al. 2022.
title Detrital neodymium isotope composition of IODP Site U1537
topic 382-U1537; AGE; Antarctica; Comment; COMPCORE; Composite Core; Depth, composite; detrital; Exp382; Fraction, description; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; isotopes; Joides Resolution; Lead isotopes; Neodymium-143/Neodymium-144 ratio; Neodymium-144/Neodymium-143 ratio, standard error; Neodymium isotopes; Number; Sample code/label; Scotia Sea; Southern Ocean; Weddell Sea; ε-Neodymium; ε-Neodymium, standard error
url https://doi.org/10.1594/PANGAEA.993170