We provide age constraints to the aggradational successions of the Tiber River.
We demonstrate the glacio-eustatic forcing on sediment aggradation in the last 450 ka.
We use a conceptual sedimentary model as a proxy for glacial terminations.
We provide radioisotopic independent ages for the last five glacial terminations.
We discuss a possible misfit with astrochronological calibration of T-4 at 330 ka.
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