“…In CGS, structural CO 2 trapping is the principal storage mechanism whereby shale (in its classical caprock role), if strongly water‐wet, provides an efficient seal to the reservoir disallowing upward CO 2 migration [ Arif et al ., ; Armitage et al ., ; Chaudhary et al ., ; Iglauer et al ., ]. However, rock material can be even strongly CO 2 ‐wet [ Arif et al ., ; Iglauer et al ., ; Iglauer , ]—which would massively reduce storage capacity [ Al‐Menhali et al ., ; Chaudhary et al ., ; Iglauer et al , , ]—and shale wettability has so far only been reported for low‐total organic content (TOC) shales [ Chaudhary et al ., ; Iglauer et al ., ; Roshan et al ., ; Shojai Kaveh et al ., ] despite the fact that shales can be very rich in organic carbon, i.e., high TOC [ Vernik and Milovac , ].…”