δ18O and Mg/Ca thermometry in planktonic foraminifera: a multi-proxy approach towards tracing coastal upwelling dynamics

Planktonic foraminifera δ18O and Mg/Ca ratios are widely considered as a powerful proxy to reconstruct past seawater-column temperature in coastal upwelling regions. Due to the complexity in the interpretation of planktonic foraminifera δ18O data with respect to past seawater temperatures, temperatu...

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Bibliographic Details
Main Authors: Salgueiro, Emilia, Voelker, Antje H L, Martin, Pamela A, Rodrigues, Teresa, Zúñiga, D, Froján, María, de la Granda, Francisco, Villacieros-Robineau, Nicolás, Alonso-Perez, F, Alberto, Ana, Rebotim, Andreia, González-Álvarez, Raquel, Castro, Carmen G, Abrantes, Fatima F
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2019
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.910309
https://doi.org/10.1594/PANGAEA.910309