Ocean currents determine the structure of the deep-sea ocean floor and the transport of sediments, organic carbon, nutrients and pollutants. In flume-tank experiments, researchers from MARUM – Center for Marine Environmental Sciences at the University of Bremen have simulated how currents shape the seafloor and control sediment deposition. This will help in reconstructions of past marine conditions. They have now published their results in the Nature journal Communications Earth & Environment.
Details of past climate conditions are revealed to researchers not only by sediment samples from the ocean floor, but also by the surface of the seafloor, which is exposed to currents that are constantly altering it. Deposits shaped by near-bottom currents are called contourites. These sediment deposits contain information about past ocean conditions as well as clues to climate. Contourites are often found on continental slopes or around deep-sea mountains. But they can be found in any environment where strong currents occur near the seafloor. The mechanisms that control them are not yet well understood. Experiments in flume tanks will help to change this through the depiction of deposition in future models.
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