The burial pattern of carbon, nitrogen and phosphorus in soft bottom sedime
nts from all sub-basins of the Baltic Sea has been investigated. The highes
t total concentrations of carbon and nitrogen are found in the central deep
part of the Baltic proper. The inorganic concentration of carbon is normal
ly far below 1% in the entire Baltic Sea except for some localities with an
oxic conditions where authigenic precipitation of mixed manganese carbonate
s occurs, for example, the eastern Gotland deep. Manganese seems to be of e
ssential importance for such precipitation. As in the case for carbon, a do
minant proportion of the nitrogen found in the sediments is organically bou
nd. For phosphorus, on the other hand, a dominant proportion is inorganical
ly bound. The highest total concentrations are found in the eastern part of
Gulf of Finland and in the well-oxidized sediments of the Bothnian Bay and
Bothnia Sea. The organic C/N ratio is very stable vertically through the s
ediment very stable at each location indicating that the degradation of the
organic matter in the sediment proceeds in a C/N proportion. The organic C
/P ratio within the sediment departs considerably from the Redfield ratio,
mainly due to more or less instantaneous releases of easily hydrolyzable or
ganic phosphorus molecules.