~40 ppt (global avg: 35 ppt). Caused by: high evaporation (3 m/yr), minimal rainfall, no river inflow, restricted connection to Indian Ocean (Bab el-Mandeb). Result: dense, buoyant water; unique stratification.
Surface: 30°C (86°F) avg; up to 40°C (104°F) summer. Deep water: 21.5°C (constant below 300 m)—unlike other seas where deep water is near 4°C. Heat from below (tectonic) + insulation.
Rift valley opening (30 Ma); still spreading (~1 cm/yr). Hydrothermal vents, brine pools (Atlantis II Deep: 68°C, 260 ppt).
A natural laboratory for extreme marine adaptation.