“…1), the lunar impact record and its crater size-frequency distribution are commonly used as a proxy for the impact crater production rate on Earth (e.g., Neukum and Ivanov, 1994;Neukum et al, 2001;Werner et al, 2002;Ivanov et al, 2003). Additional constraints come from the size-frequency distribution of near-Earth asteroids (e.g., Shoemaker et al, 1979;Durda et al, 1998;Morbidelli, 1999;Bottke et al, 2000;Werner et al, 2002;Stuart and Binzel, 2004;Michel and Morbidelli, 2007;Le Feuvre and Wieczorek, 2011;Johnson and Bowling, 2014;Wheeler and Mathias, 2019), the population of Earth-crossing comets, the Sun's position in the galactic plane (e.g., Shoemaker, 1998b;Ye, 2018), as well as the distribution of extraterrestrial 3 He (Farley, 1995(Farley, , 1998(Farley, , 2001), platinum-group metals (Peucker-Ehrenbrink, 2001), and fossil meteorites and extraterrestrial chromite grains (e.g., Schmitz et al, 1996Schmitz et al, , 2001Schmitz et al, , 2015Heck et al, 2004;Alwmark and Schmitz, 2009;Schmitz, 2013) in marine sediments. While some authors proposed that the impact flux in the Earth-Moon system has continuously declined over the past 3 Gyr (Minton and Malhotra, 2010), others suggested that the impact flux has remained more or less stable over the last 2 Gyr (e.g., Neukum and Ivanov, 1994;Hörz, 2000;Hughes, 2000).…”