Single chamber Mg/Ca analyses of Globigerinoides ruber for paleo-proxy calibration using femtosecond LA-ICP-MS

Abstract Mg/Ca is an independent proxy in paleoceanography to reconstruct past seawater temperature. Femtosecond Laser Ablation Inductively Coupled Plasma Mass Spectrometry (fs-LA-ICP-MS) was employed to determine the Mg/Ca composition of tests (shells) of the planktic foraminifer species Globigerin...

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Bibliographic Details
Published in:Scientific Data
Main Authors: Alexa Fischer, Ralf Schiebel, Klaus Peter Jochum, Lena Heins, Anthea I. Arns, Hedy M. Aardema, Hans Slagter, Maria Ll. Calleja, Noy Levy, Brigitte Stoll, David Walter, Ulrike Weis, Janne Repschläger, Gerald H. Haug
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2024
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Online Access:https://doi.org/10.1038/s41597-024-03402-0
https://doaj.org/article/4c6b58232b734c939d0be7c18172c782
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Summary:Abstract Mg/Ca is an independent proxy in paleoceanography to reconstruct past seawater temperature. Femtosecond Laser Ablation Inductively Coupled Plasma Mass Spectrometry (fs-LA-ICP-MS) was employed to determine the Mg/Ca composition of tests (shells) of the planktic foraminifer species Globigerinoides ruber albus (white chromotype) and G. ruber ruber (red/pink chromotype) sampled alive from the temperate to subtropical eastern North Atlantic with the research sailing yacht Eugen Seibold. Mg/Ca data are compared to (i) the measured in-situ temperature of ambient seawater, (ii) average mixed layer temperature, and (iii) sea surface temperature (SST). The pooled mean chamber Mg/Ca from each plankton tow site exhibits a positive relationship with SST. Two chamber-specific calibrations are derived, which are consistent with previous calibration equations for comparable paleo-archives. The results confirm fs-LA-ICP-MS as reliable method for determining Mg/Ca in G. ruber, and both the penultimate and antepenultimate chambers of adult specimens may provide comprehensible Mg/Ca temperatures of the surface ocean.