Cretaceous sea-surface temperature evolution: Constraints from TEX86 and planktonic foraminiferal oxygen isotopes

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. Quantitative and qualitative geochemical and pal...

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Bibliographic Details
Main Authors:	O'Brien, C, Robinson, S, Pancost, R, Sinninghe Damsté, J, Schouten, S, Lunt, D, Alsenz, H, Bornemann, A, Bottinni, C, Brassell, S, Farnsworth, A, Forster, A, Huber, B, Inglis, G, Jenkyns, H, Linnert, C, Littler, K, Markwick, P, McAnena, A, Mutterlose, J, Naafs, B, Puttmann, W, Sluijs, A, van Helmond, N, Vellekoop, J, Wagner, T, Wrobel, N
Format:	Journal article
Published:	Elsevier 2017

Cretaceous sea-surface temperature evolution: Constraints from TEX86 and planktonic foraminiferal oxygen isotopes

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