Stable isotopes (δ13C and δ18O) and Mg/Ca-based temperatures of Globorotalia truncatulinoides from a Holocene sediment core southwest off the Cabo Verde archipelago (MUC5)

Pérez-Rodríguez, Irene; Nürnberg, Dirk; Schindlbeck-Belo, Julie; Wharton, Jack; Hansteen, Thor H; Huvenne, Veerle A I; Thornalley, David J R; Mosquera Giménez, Ángela; Kutterolf, Steffen; Barnhill, Kelsey Archer; Orejas, Covadonga

Stable isotopes (δ13C and δ18O) and Mg/Ca-based temperatures of Globorotalia truncatulinoides from a Holocene sediment core southwest off the Cabo Verde archipelago (MUC5)

2024

This dataset presents combined stable isotopes (δ13C and δ18O) and Mg/Ca ratios for the sub-thermocline dwelling planktonic foraminifer Globorotalia truncatulinoides. Al/Ca, Fe/Ca, and Mn/Ca ratios are also included to assess potential contamination of the foraminiferal tests. The microfossils were obtained from the 315-400 μm sediment fraction of a core collected at a water depth of 4394 m off the Cabo Verde archipelago, which covers most of the Holocene Epoch.

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Palabras clave de AGROVOC

age depth holocene

Información bibliográfica

Editorial

PANGAEA

Otras materias

Bottom/max; Strontium/calcium ratio; Iron/calcium ratio; Multicorer; Top/min; Δ13c; Aluminium/calcium ratio; Integrated assessment of atlantic marine ecosystems in space and time; Microfossils; Muc; Foraminiferal stable isotopes; Sarmiento de gamboa; Sediment/rock; Cabo verde archipelago; Planktonic foraminifera mg/ca; Imirabilis2_leg1_muc5; Δ18o; Event label; Iatlantic; Manganese/calcium ratio; Sub-surface temperature; Sample code/label; Imirabilis2_leg1; Magnesium/calcium ratio; Muc5

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Formato

text/tab-separated-values, 385 data points

Licencia

CC-BY-4.0: Creative Commons Attribution 4.0 International (License comes into effect after moratorium ends), Access constraints: access rights needed, info:eu-repo/semantics/restrictedAccess

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Dataset

En AGRIS desde: 2025-01-28

Fecha de modificación: 2025-02-24

Formato: Dublin Core

Proveedor de Datos

Este registro bibliográfico ha sido proporcionado por Alfred Wegener Institute for Polar and Marine Research

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