Impact cratering rate consistency test from ages of layered ejecta on Mars Lagain, A. Bouley, S. /Baratoux, David Costard, F. Wieczorek, M. Impact craters Mars Impact rate Layered ejecta craters Ages of geological units of planetary bodies are determined from impact crater counts on their surface. These ages are model-dependent, and several models largely used in the community assume a constant production function and a constant cratering rate over the last 3 Ga. We have mapped the population of small impact craters (>200 m in diameter) formed over a population of large impact craters (>5 km in diameter) with layered ejecta on Acidalia Planitia, Mars. We have deduced the age of each large impact crater under the assumption of a constant impact rate and constant production function. The impact rate inferred from this set of ages is, however, not constant and show a significant increasing during the last similar to 1 Ga compared to chronology models commonly used. We interpret this inconsistency as an evidence for temporal variations in the size-frequency distribution (SFD) of impactors in the main belt, consistent with recent studies argued for a late increasing of the large impactor flux on Earth and the Moon. 2020 text https://www.documentation.ird.fr/hor/fdi:010077879 fdi:010077879 Lagain A., Bouley S., Baratoux David, Costard F., Wieczorek M.. Impact cratering rate consistency test from ages of layered ejecta on Mars. 2020, 180, art. 104755 [11 p.] EN