Astronomical tuning for the upper Messinian Spanish Atlantic margin: Disentangling basin evolution, climate cyclicity and MOW
文摘

Astronomically tuned age model for the Messinian Spanish Atlantic margin

Precession cycles forced by climatically driven fluctuations of sediment input

The nature of the cycles changes due to changing depositional environment.

δ18O patterns correspond well with open ocean records suggesting Atlantic waters.

No direct influence of MOW on the late Messinian sediments in this core.

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