The dynamic processes that shape the surface of our planet are governed by climate and tectonics, with temperature and precipitation dictating rates of weathering and rock uplift controlling erosion rates (e.g., DiBiase & Whipple, 2011;Perron, 2017). However, the influence of climate variability on denudation rates and erosion over geological timescales has been the subject of an ongoing debate. On one side, weathering rates in mountainous source regions show acceleration with variations in climatic conditions (e.g., Carretier et al., 2013;Ferrier et al., 2013;Tofelde et al., 2017). Conversely, records from sedimentary basins indicate that rates of sediment input into the oceans have remained stable throughout the Late-Cenozoic (von Blanckenburg et al., 2015;Willenbring & von Blanckenburg, 2010). In this work, we examine sediment transport of the sand-sized fraction in four large rivers worldwide. We apply a stochastic numerical model that quantifies sediment residence times within fluvial systems based on sediment transport dynamics and constrained by measured and published cosmogenic nuclide data. These calculated residence times are key in understanding how transport through sedimentary systems can affect how changes to rates of erosion at the source preserved in the sedimentary record (Castelltort & Van Den Driessche, 2003).