Authigenic neodymium records from sediment core GL1090 for the penultimate glacial termination and Last Interglacial

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Auteurs principaux: Dias, Bruna Borba, Chiessi, Cristiano Mazur, Piotrowski, Alexander M, Campos, Marília C, Jena, Partha Sarathi, Ballalai, João M, Nascimento, Rodrigo Azevedo, Santos, Thiago Pereira dos, Venancio, Igor Martins, Mashayek, Ali, Albuquerque, Ana Luiza Spadano
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Langue:en
Publié: PANGAEA 2025
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author Dias, Bruna Borba
Chiessi, Cristiano Mazur
Piotrowski, Alexander M
Campos, Marília C
Jena, Partha Sarathi
Ballalai, João M
Nascimento, Rodrigo Azevedo
Santos, Thiago Pereira dos
Venancio, Igor Martins
Mashayek, Ali
Albuquerque, Ana Luiza Spadano
author_facet Dias, Bruna Borba
Chiessi, Cristiano Mazur
Piotrowski, Alexander M
Campos, Marília C
Jena, Partha Sarathi
Ballalai, João M
Nascimento, Rodrigo Azevedo
Santos, Thiago Pereira dos
Venancio, Igor Martins
Mashayek, Ali
Albuquerque, Ana Luiza Spadano
collection Datos científicos de ciencias marinas y ambientales
contents We present authigenic neodymium isotopes (ℇNd) values from a mid-depth core in the western South Atlantic to assess changes in deep ocean circulation during the penultimate glacial termination and the Last Interglacial (LIG). Authigenic ℇNd were analyzed on uncleaned mixed planktonic foraminifera from the intervals of the penultimate glacial termination and the LIG. These data were compared to the authigenic ℇNd dataset from the last glacial termination and the Holocene published by Howe et al. (2018, doi:10.1016/j.epsl.2018.03.006). The samples were dissolved, and rare earth elements (REE) were separated from other elements using Eichrom TRUspec™ resin. Neodymium was then extracted from the other REE using Eichrom Lnspec™ resin. Samples were analyzed using a Neptune Plus multi-collector mass spectrometer (MC-ICP-MS). The reported error corresponds to 2 standard deviations of reproducibility of the bracketing standards.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_971660
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle Authigenic neodymium records from sediment core GL1090 for the penultimate glacial termination and Last Interglacial
Dias, Bruna Borba
Chiessi, Cristiano Mazur
Piotrowski, Alexander M
Campos, Marília C
Jena, Partha Sarathi
Ballalai, João M
Nascimento, Rodrigo Azevedo
Santos, Thiago Pereira dos
Venancio, Igor Martins
Mashayek, Ali
Albuquerque, Ana Luiza Spadano
AGE; Deep ocean circulation; DEPTH, sediment/rock; Foraminifera; GL1090; GL-1090; glacial terminations; grain-size; Interglacials; MC-ICP-MS ThermoFisher Scientific Neptune Plus; western South Atlantic; ε-Neodymium, authigenic; ε-Neodymium, authigenic, standard deviation
We present authigenic neodymium isotopes (ℇNd) values from a mid-depth core in the western South Atlantic to assess changes in deep ocean circulation during the penultimate glacial termination and the Last Interglacial (LIG). Authigenic ℇNd were analyzed on uncleaned mixed planktonic foraminifera from the intervals of the penultimate glacial termination and the LIG. These data were compared to the authigenic ℇNd dataset from the last glacial termination and the Holocene published by Howe et al. (2018, doi:10.1016/j.epsl.2018.03.006). The samples were dissolved, and rare earth elements (REE) were separated from other elements using Eichrom TRUspec™ resin. Neodymium was then extracted from the other REE using Eichrom Lnspec™ resin. Samples were analyzed using a Neptune Plus multi-collector mass spectrometer (MC-ICP-MS). The reported error corresponds to 2 standard deviations of reproducibility of the bracketing standards.
title Authigenic neodymium records from sediment core GL1090 for the penultimate glacial termination and Last Interglacial
topic AGE; Deep ocean circulation; DEPTH, sediment/rock; Foraminifera; GL1090; GL-1090; glacial terminations; grain-size; Interglacials; MC-ICP-MS ThermoFisher Scientific Neptune Plus; western South Atlantic; ε-Neodymium, authigenic; ε-Neodymium, authigenic, standard deviation
url https://doi.org/10.1594/PANGAEA.971660