Carbon isotope ratios of organic compound fractions in oceanic suspended particles

نویسندگان

  • Jeomshik Hwang
  • Ellen R. M. Druffel
چکیده

[1] To study cycling of organic fractions in the ocean, relative abundances and radioand stable-carbon isotope measurements of total lipid extract, acid-soluble, and acidinsoluble fractions of suspended particulate organic carbon (POC) were made. Changes in relative abundances occurred mostly in the upper 1000 m of the water column, with a decrease in total lipid extract and the acid-soluble fraction and an increase in the acid-insoluble fraction with increasing depth. We found lower DC values for total lipid extract and the acid-insoluble fraction than for the acid-soluble fraction, which is consistent with the previous suggestion of incorporation of dissolved organic carbon and/or resuspended sediment to POC (Druffel and Williams, 1990; Sherrell et al., 1998). The DC values of these fractions in a given organic carbon pool must be understood in terms of acquisition of C-depleted carbon from other carbon pools in addition to aging within the reservoir. Citation: Hwang, J., and E. R. M. Druffel (2006), Carbon isotope ratios of organic compound fractions in oceanic suspended particles, Geophys. Res. Lett., 33, L23610, doi:10.1029/2006GL027928.

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تاریخ انتشار 2006