Bioavailability and remineralization rates of sediment-derived dissolved organic carbon from a Baltic Sea depositional area

This pilot study investigated the bioavailability and remineralization kinetics of the sediment-derived dissolved organic carbon (DOC) from the Gdańsk Deep, a depositional area in the Baltic Sea. This was assessed in the long-lasting (126 d) incubation experiment, in which the mixture of DOC from sediment pore water and bottom water was exposed to oxic microbial respiration with incubation of bottom water as a control run. The obtained decay curves allowed us to distinguish three DOC fractions: labile (DOC L ), semi-labile (DOC SL ), and refractory (DOC R ). In bottom water, the refractory fraction was predominant and amounted to almost 85% of total DOC, whereas about 15% of DOC was bioavailable: 6% labile and 9% semi-labile. In contrast, DOC from pore water was much more bioavailable DOC (~55% of total DOC) and contained 11% DOC L and 44% DOC SL . The remineralization rate constants recalculated to the in situ temperature of 6°C for labile and semi-labile DOC in pore water were 0.025 d −1 and 0.002 d −1 , respectively, whereas, in bottom water, 0.026 d −1 and 0.004 d −1 . The half-life times for DOC L were comparable for both bottom water and pore water and amounted to 26.2 d and 27.6 d, respectively. For DOC SL , the half-life time was shorter for bottom water (165.5 d) than for pore water (322.9 d).