Improving the routine analysis of siderite for δ(13)C and δ(18)O in environmental change research

RATIONALE: The carbon (δ(13)C) and oxygen (δ(18)O) isotope composition of siderite (FeCO(3)) is used widely to understand and quantify geochemical processes to reconstruct past climate and environmental change. However, few laboratories follow precisely the same protocol for the preparation and anal...

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Detalles Bibliográficos
Autores principales: Lacey, Jack H., Sloane, Hilary J., Leng, Melanie J., Crowley, Stephen F.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2023
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10078271/
https://www.ncbi.nlm.nih.gov/pubmed/36515622
http://dx.doi.org/10.1002/rcm.9456

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10078271/
https://www.ncbi.nlm.nih.gov/pubmed/36515622
http://dx.doi.org/10.1002/rcm.9456

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