Over two thousand feet beneath the surface of the North Atlantic, on the seamount Atlantis Massif, at the intersection between the Mid-Atlantic Ridge and the Atlantis Transform Fault, a jagged landscape of towers rises from the deep ocean gloom. Discovered in 2000, the Lost City Hydrothermal Field, often referred to simply as the Lost City, is an area of marine alkaline hydrothermal vents. It is the longest-lived venting environment known in the ocean. Nothing else like it has ever been found.
ScienceAlert.com notes that for at least 120,000 years and maybe longer, the upthrusting mantle in this part of the world has reacted with seawater to puff hydrogen, methane, and other dissolved gases out into the ocean. In the cracks and crevices of the field’s vents, hydrocarbons feed novel microbial communities even without the presence of oxygen.