Abstract:Seafloor currents, including episodic sediment-laden turbidity flows and more sustained thermohaline-driven bottom currents, control the ultimate fate of sediment, carbon and pollutants in the deep-sea. Collectively, these currents form the largest sediment accumulations on Earth, from which past climate records are reconstructed. A long-standing view has been that thermohaline-driven bottom currents are persistent and stable; however, a paucity of direct near-seabed monitoring means this remains untested at f… Show more
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