Early Cretaceous sea surface temperature evolution in subtropical shallow seas

Late Cretaceous sea surface temperatures (SST) are, amongst others, traditionally reconstructed by compiling oxygen isotope records of planktonic foraminifera obtained from globally distributed pelagic IODP drill cores. In contrast, the evolution of Early Cretaceous SSTs is essentially based on the...

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Detalles Bibliográficos
Autores principales: Huck, Stefan, Heimhofer, Ulrich
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8492702/
https://www.ncbi.nlm.nih.gov/pubmed/34611212
http://dx.doi.org/10.1038/s41598-021-99094-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8492702/
https://www.ncbi.nlm.nih.gov/pubmed/34611212
http://dx.doi.org/10.1038/s41598-021-99094-2

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