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Chert oxygen isotope ratios are driven by Earth's thermal evolution

The (18)O/(16)O ratio of cherts (δ(18)O(chert)) increases nearly monotonically by ~15‰ from the Archean to present. Two end-member explanations have emerged: cooling seawater temperature (T(SW)) and increasing seawater δ(18)O (δ(18)O(sw)). Yet despite decades of work, there is no consensus, leading...

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Detalles Bibliográficos
Autores principales:	Tatzel, M., Frings, P. J., Oelze, M., Herwartz, D., Lünsdorf, N. K., Wiedenbeck, M.
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	National Academy of Sciences 2022
Materias:	Physical Sciences
Acceso en línea:	https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9907065/ https://www.ncbi.nlm.nih.gov/pubmed/36516068 http://dx.doi.org/10.1073/pnas.2213076119

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