Abstract
The abyssal ocean covers more than half of the Earth’s surface, yet remains understudied and underappreciated. In this Perspectives article, we mark the occasion of the Deep Submergence Vehicle Alvin’s increased depth range (from 4500 to 6500 m) to highlight the scientific potential of the abyssal seafloor. From a geologic perspective, ultra-slow spreading mid-ocean ridges, Petit Spot volcanism, transform faults, and subduction zones put the full life cycle of oceanic crust on display in the abyss, revealing constructive and destructive forces over wide ranges in time and space. Geochemically, the abyssal pressure regime influences the solubility of constituents such as silica and carbonate, and extremely high-temperature fluid-rock reactions in the shallow subsurface lead to distinctive and potentially unique geochemical profiles. Microbial residents range from low-abundance, low-energy communities on the abyssal plains to fast growing thermophiles at hydrothermal vents. Given its spatial extent and position as an intermediate zone between coastal and deep hadal settings, the abyss represents a lynchpin in global-scale processes such as nutrient and energy flux, population structure, and biogeographic diversity. Taken together, the abyssal ocean contributes critical ecosystem services while facing acute and diffuse anthropogenic threats from deep-sea mining, pollution, and climate change.
Highlights
The abyssal ocean, which includes the water column and seafloor between 3000 and 6000 m depth (Vinogradova, 1997), constitutes 54% of Earth’s surface (Gage and Tyler, 1991)
The uniqueness of the abyssal ocean is shaped both by features found dominantly or exclusively at these depths, as well as features typically encountered in other zones but overprinted by 30–60 MPa of hydrostatic pressure
The abyssal ocean likely holds critical clues to longstanding scientific questions pertaining to the flow of mantlederived energy, the mobilization of chemicals into ocean waters, and the origin, evolution, and distribution of life
Summary
The abyssal ocean, which includes the water column and seafloor between 3000 and 6000 m depth (Vinogradova, 1997), constitutes 54% of Earth’s surface (Gage and Tyler, 1991). Abyssal environments are largely unexplored and poorly understood, but given its volumetric importance and unique geological, geochemical, and biological attributes, we feel that increased scientific attention to the abyssal ocean has the potential to alter our understanding of the global ocean processes in fundamental ways.
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