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- W2004648107 abstract "Abstract The δ 13 C-values of organic material in the marine sediments off Hinchinbrook Island, Australia, indicate a widespread (> 230 km 2 ) influence of terrestrial organic carbon, C T . Extensive mangrove forests on the island are known to export T day −1 of leaf litter and 7.5 Mg C T day −1 of micro-particulate organic carbon (POC) (1 Mg = 10 6 g). 210 Ph sedimentation rates, organic-carbon contents and the stable-isotope ratios of organic matter in the sediment were used to calculate an accumulation rate of 13–29 Mg C T day −1 for these marine sediments. This preliminary balance indicates that terrestrial organic carbon in this marine environment can be accounted for by terrestrial export although significant losses do occur. Shoreline redeposition of floating leaves, etc., and organic matter degradation to CO 2 and/or CH 4 followed by bubble ebullition are likely to be major loss terms. Considered with the work of Hedges and Parker (1976) , this work suggests that leaf litter may be the most important single source of terrestrial organic carbon in the marine environment, although it is realized that mangroves represent an extreme example of terrestrial productivity." @default.
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- W2004648107 date "1985-08-01" @default.
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- W2004648107 title "Terrestrial organic carbon in marine sediment: A preliminary balance for a mangrove environment derived from 13C" @default.
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- W2004648107 doi "https://doi.org/10.1016/0168-9622(85)90048-x" @default.
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