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Based on figures available, role of upwelling in some fine sediment patches on China Sea shelves is examined from the viewpoints of physical process and biological process, respectively. It is further vertified with more data wherever upwelling exists on continental shelf mud must occur coincidence of upwelling areas with mud patches. Marine rain is named for physical process and marine snow is used as usual. It is pointed out that marine rain and marine snow are usually coexistent and interact each other. It is concluded that the mud patch southeast of Cheju Is. is formed by marine rain rather than marine snow since terrigenous elements are high and biogenic elements are not and that judging from sediment trap data the mud in the Okinawa Trough is accumulated by horizontal transport via wind driven transverse circulation from inner shelf in winter and by vertical flux through biological activities (marine snow) and aeolian deposit in spring. A number of controversies on fine sediment issues on China Sea shelves need to be further deliberated. Interaction between marine rain and snow also needs to be experimentally and theoretically studied.
Based on figures available, role of upwelling in some fine sediment patches on China sea shelves is examined from the viewpoints of physical process and biological process, respectively. It is further vertified with more data wherever upwelling exists on continental shelf mud must occur coincidence of upwelling areas with mud patches. Marine rain is named for physical process and marine snow is used as usual. It is pointed that that marine rain and marine snow are usually coexistent and interact each other. It is noted that the mud patch southeast of Cheju Is. is formed by marine rain rather than marine snow since terrigenous elements are high and biogenic elements are not and that judging from sediment trap data the mud in the Okinawa Trough is accumulated by horizontal transport via wind driven transverse circulation from inner shelf in winter and by vertical flux through biological activities (marine snow) and aeolian deposit in spring. A number of controversies on fine sedim ent issues on China Sea shelves need to be further deliberated. Interaction between marine rain and snow also needs to be experimentally and theoretically studied.