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  Six Ca-Mg-Fe Carbonate Reference Materials for In-Situ Analysis of Oxygen and Carbon Isotope Ratios

Scicchitano, M. R., Harris, C., Luyt, J., Pack, A., die Rocco, T., Vennemann, T., Wilke, F., Schleicher, A. M., Glodny, J., Tait, K. T., Philippo, S., Wiedenbeck, M. (2025): Six Ca-Mg-Fe Carbonate Reference Materials for In-Situ Analysis of Oxygen and Carbon Isotope Ratios - Book of Abstracts, Geo4Göttingen 2025 (Göttingen, Germany 2025).
https://doi.org/10.48380/b811-j803

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 Creators:
Scicchitano, Maria Rosa1, 2, Author                 
Harris, Chris2, 3, Author
Luyt, Julie2, 3, Author
Pack, Andreas2, 3, Author
die Rocco, Tommaso2, 3, Author
Vennemann, Torsten2, 3, Author
Wilke, Franziska1, 2, Author
Schleicher, Anja Maria1, 2, Author
Glodny, J.1, 2, Author                 
Tait, Kimberly T.2, 3, Author
Philippo, Simon2, 3, Author
Wiedenbeck, Michael1, 2, Author           
Affiliations:
13.1 Inorganic and Isotope Geochemistry, 3.0 Geochemistry, Departments, GFZ Publication Database, GFZ Helmholtz Centre for Geosciences, ou_146040              
2GFZ SIMS Publications, GFZ Helmholtz Centre for Geosciences, Potsdam, ou_1692888              
3External Organizations, ou_persistent22              

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 Abstract:

Six Ca-Mg-Fe carbonate reference materials (RMs) were characterized for oxygen and carbon isotope ratios analyses by Secondary Ion Mass Spectrometry (SIMS). This new suite includes four dolomites with Fe# ranging from 0.0004 to 0.3429, one magnesite with Fe# = 0.0099 and one siderite with Fe# = 0.6152. The six samples were split into between 128 to 2048 metrologically identical aliquots, each containing roughly 100 mg of material. We performed a detailed characterization on split materials for their major and minor chemical element composition using EPMA and their mineralogical composition using XRD. The oxygen and carbon isotope reference values were also determined in multiple gas-source isotope ratio mass spectrometry laboratories while the homogeneity of the oxygen and carbon isotope ratios at the sub-nanogram test portion mass were assessed using SIMS. The repeatability of our SIMS measurements varied from ± 0.15 to ± 0.31‰ (1s) for δ18O and from ± 0.29 to ± 0.71‰ (1s) for δ13C. Significant compositional SIMS matrix effects were observed across the dolomite-ankerite and magnesite-siderite solid-solution series in the investigated compositional range. This confirms the need of multiple matrix-matched RMs spanning a wide chemical range in order to get accurate SIMS isotope ratios in minerals that form theses solid-solutions.

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Language(s): eng - English
 Dates: 20252025
 Publication Status: Finally published
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 Identifiers: DOI: 10.48380/b811-j803
GFZPOF: p4 MESI
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Title: Geo4Göttingen 2025
Place of Event: Göttingen, Germany
Start-/End Date: 2025-09-14 - 2025-09-18

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Title: Book of Abstracts
Source Genre: Proceedings
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