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Free-floating sediment traps were suspended at 200 and 900 m in the northern North Pacific Ocean during 20-21 May, 1974. A considerable amount of large, dark-green particles, larger than 1 mm in diameter, was collected at both depths. These large particles corresponded morphologically with fecal pellets of salps. Vertical carbon flux was estimated to be 10.5 and 6.7 mg C m 2 d ' at 200 and 900 m, respectively. This suggests that vertical transport of salp fecal pellets could play a n important role in meeting the energy requirements of bathypelagic organisms in the open ocean.

Particulate Organic Matter Transport to the Deep Sea by Salp Fecal Pellets