Orbital tuning dating who is ice cube dating
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This model allows for abrupt changes of sedimentation rate (eg., at the boundaries of the Selli) and for hiatuses (eg., at the base of the Selli).
A thin nodular interval (about 2 cm) immediately below the base of the Selli suggests condensed sedimentation or a hiatus.
The goal of our study is to date by orbital tuning the duration of the Selli Level and of the hiatus/condensation at is base.
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Responses in austral regions are also influenced by a fast response to summer insolation forcing at high southern latitudes.