Labrador Sea a key player in providing oxygen for deep North Atlantic life
Researchers from Cornell University have pinpointed the source of oxygen that sustains deep-sea life in the North Atlantic Ocean: the churning waters in the Labrador Sea.
Benthic ecosystems are ecological systems associated with the bottom substrates of aquatic environments, including marine, estuarine, and freshwater habitats, where organisms inhabit or interact with sediments, hardgrounds, or biogenic structures. They encompass diverse communities such as infauna, epifauna, demersal fishes, microphytobenthos, and benthic microbial assemblages that mediate key biogeochemical processes, including organic matter remineralization, nutrient regeneration, and sediment–water fluxes. Benthic ecosystems are structured by gradients in depth, hydrodynamics, sedimentology, oxygen availability, and resource inputs, and they play critical roles in carbon cycling, secondary production, habitat provision, and the coupling of pelagic and sedimentary processes within broader aquatic food webs and ecosystem functioning.
Researchers from Cornell University have pinpointed the source of oxygen that sustains deep-sea life in the North Atlantic Ocean: the churning waters in the Labrador Sea.
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