RT Journal Article SR Electronic(1) A1 Mitchell, Neil C. A1 Shi, Wen A1 Izzeldin, A.Y. A1 Stewart, Ian C. F.YR 2021 T1 Reconstructing the level of the central Red Sea evaporites at the end of the Miocene JF Basin Research, VO 33 IS 2 SP 1266 OP 1292 DO https://doi.org/10.1111/bre.12513 PB European Association of Geoscientists & Engineers, SN 1365-2117, AB [Abstract Reconstructing the original depositional level of the Mesozoic and older c‘salt giants’ can reveal if their basins became filled to global sea level, but is complicated by dissolution, diapirism and because the time elapsed is so great. This is less of a problem in the Red Sea, a young rift basin that is transitioning to an ocean basin and where the evaporites away from coastal fringes are less affected by diapirism. In this study, we explore vertical movements of the evaporite surface of the central Red Sea imaged with deep seismic profiling, for the period of time after most evaporite deposition ended at 5.3 Ma (the Miocene‐Pliocene boundary). This boundary is readily mapped across the basin as a prominent reflection in seismic data correlated with stratigraphy at three DSDP sites. We quantify changes in the average elevation of the evaporite surface due to (a) thermal lithospheric subsidence, (b) isostatic loading by Plio‐Pleistocene sediments and water, (c) deflation needed to balance the volume of evaporites overflowing oceanic crust of 5.3 Ma age, (d) loss of halite by dissolution and (e) dynamic topography. Our best estimate of the evaporite level (−132 m air‐loaded or −192 m water‐loaded) lies below the range of estimated global sea level towards the end of the Miocene, suggesting that the basin remained under‐filled. If geological interpretations of shallow water conditions existing at the end of the Miocene (Zeit Formation) are correct, this implies that the water level of the Red Sea declined and was unstable. These calculations illustrate how spreading of evaporites can enhance thermal subsidence to cause rapid development of accommodation space above major evaporite bodies, which in the Red Sea case has remained largely unfilled., A series of five corrections are made to the present level of the Miocene evaporites in the central Red Seat, suggesting that the basin remained under‐filled at the Miocene‐Pliocene boundary (i, ii). ], UL https://www.earthdoc.org/content/journals/10.1111/bre.12513