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- W2016033679 abstract "Sinking material was collected every week with sediment traps for a 13-month period in a subtropical inlet, Kaneohe Bay, Hawaii. A ratio method was applied to distinguish sedimentation from resuspension. No seasonality was observed in the sedimentation rate. An annual average of 73±6% of the total material trapped had been resuspended. The resuspension rate appeared to be controlled by wind speed (P<0·001). The annual average sedimentation of particulate organic carbon produced in the water column was estimated to be 0·49±0·22 g C m−2 day−1, which was about 42% of the primaryproduction by phytoplankton in the water column. Comparison of this estimate with an independent long-term geological estimate suggests significant accumulation of organic matter in the bottom sediments from non-sedimentation processes. Annual sedimentation rate excluding terrestrial material was 155 g C m−2 year−1, which was about 43% of organic carbon supply. About 51% of organic carbon supply was respired in the water column and about 6% was exported out of the bay." @default.
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- W2016033679 date "1982-05-01" @default.
- W2016033679 modified "2023-09-30" @default.
- W2016033679 title "Sedimentation of newly produced particulate organic matter in a subtropical inlet, Kaneohe Bay, Hawaii" @default.
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- W2016033679 doi "https://doi.org/10.1016/s0302-3524(82)80075-3" @default.
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