“…A subgroup of phyllosilicates particularly interesting in the prebiotic context is clay minerals due to their large surface area and optimal interlayer sites for the concentration and preservation of organic compounds when rapidly deposited under reducing chemical conditions [73]. These minerals have been detected at several locations on Mars [4,74,75,76,77,78,79,80,81,82], including Echus Chasma, Mawrth Vallis, Eridania basin, the Memnonia quadrangle, the Elysium quadrangle, Nili Fossae, and the large Argyre Planitia area.…”