Extensive sedimentary deposits in, for example, the marine and terrestrial for earc basins associated with subduction zones, and sedimentary fans and deltas fed by large fluvial or glaciofluvial systems, preserve high-resolution time series allowing us to unravel feedbacks between deep Earth and surface processes, such as the coupling between subsidence and uplift associated with or ogens, subsequent erosion and sediment deliver and the resulting changes in Earth's climate factory.