Geochemical data, paleo-sea surface temperatures reconstructed by TEX86 paleothermometry and time intervals differentiated based thereon at ODP Sites 207-1258 and 207-1259

Paleoclimate records of geologic time periods characterized by extreme global warmth such as the mid-Cretaceous are important for a better understanding of the Earth's climate system operating in an exceptionally warm mode. Here we applied an organic geochemical proxy (TEX86) on organic matter-...

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Bibliographic Details
Main Authors: Forster, Astrid, Schouten, Stefan, Baas, Marianne, Sinninghe Damsté, Jaap S
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2007
Subjects:
207-1258
207-1259
COMPCORE
Composite Core
Joides Resolution
Leg207
North Atlantic Ocean
Ocean Drilling Program
ODP
North Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.721812
https://doi.org/10.1594/PANGAEA.721812
Description
Summary:Paleoclimate records of geologic time periods characterized by extreme global warmth such as the mid-Cretaceous are important for a better understanding of the Earth's climate system operating in an exceptionally warm mode. Here we applied an organic geochemical proxy (TEX86) on organic matter-rich Albian-Santonian sediments, recovered from Ocean Drilling Program Leg 207 Sites 1258 and 1259 on Demerara Rise, to reconstruct sea surface temperatures (SSTs) in the western equatorial Atlantic. Preceded by a stepwise Cenomanian warming trend (~31-35°C), the onset of the Cretaceous thermal maximum coincided here with the Cenomanian-Turonian boundary event. Once established, this extreme warm climate regime, characterized by averaged tropical SSTs close to 35°C, lasted up to the Turonian-Coniacian transition. Two pronounced cooler intervals (~2-3°C) interrupt this otherwise remarkably stable record, providing the first d18O independent evidence for middle Turonian cooling that previously has been attributed to glacioeustatic sea-level lowering. Coniacian SSTs decline stepwise, reaching a minimum in the Santonian (~32-33°C), where cooling is most pronounced, presumably concomitant with the first progressive opening of a deep-water passage through the equatorial Atlantic gateway.

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