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SUMMARY: The investigations carried out make it possible to conclude that filamentous- cluster organisms (Krassilnikoviae) rather form accumulations-layers at certain depths than get diffusely distributed in the sea and ocean water column. Possibly these layers occur at the junctions of water masses of different densities. The filamentous-cluster organisms have been found in all geographic zones of the world ocean, from Polar latitudes down to the equator.
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