Early Cretaceous sea surface temperature evolution in subtropical shallow seas

Abstract 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 base...

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Autores principales: Stefan Huck, Ulrich Heimhofer
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/b8011f6bd425472491fc677f841d9c3f
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