Time-series data on the freshwater inflow of total organic car
bon (TOC) to the Stockholm Archipelago, Baltic Sea, covering four full years, showed a distinct seasonal pattern with six times higher monthly flow in winter–spring than in the summer with an annual freshwater TOC input of 28 Gg year
−1. Estimation of
burial flux and source apportionment of sedimentary OC in the Inner Archipelago (IA) was
based on extensive sediment sampling of seismically surveyed accumulation
bottom areas. The resulting IA-averaged OC content was 56
b1;16 mg g dw
−1 sediment, yielding an IA-wide
bottom sediment deposition for the 1992–1995 period of 3.1 Gg year
−1.
The sediments in the eastern Lake Mxe4;laren (LM), IA, and Outer Archipelago (OA) were geochemically distinguishable based on their stable carbon isotope signatures (b4;13C). The b4;13C values were −28.2b1;0.6, −25.4b1;1.0, and −23.6b1;0.3, respectively, for LM (n