Cretaceous sea-surface temperature evolution: Constraints from TEX86 and planktonic foraminiferal oxygen isotopes
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DOI: 10.1016/j.earscirev.2017.07.012
Abstract: It is well established that greenhouse conditions prevailed during the Cretaceous Period (~ 145–66 Ma). Determining the exact nature of the greenhouse-gas forcing, climatic warming and climate sensitivity remains, however, an active topic of research.… read more here.
Keywords: tex86; temperature; surface; cretaceous sea ... See more keywords