An. Dzyuban et al., Microbiological processes of organic matter destruction in the bottom sediments of the Baltic Sea, OCEANOLOGY, 41(2), 2001, pp. 204-210
Microbiological processes of organic matter (OM) destruction in the bottom
sediments of the Baltic Sea in the winter period were investigated. The dai
ly rates of some processes reached are as follows: total destruction of OM
was 10-130 mg C/m(2) absorption of O-2 was 0-59 mg/m(2), release of CO2 was
18-120 me C/m(2), assimilation of CO2 was 2.6-36 mg C/m(2), sulfate reduct
ion was 2.7-90 mg S/m(2), methanogenesis was 0.06-5.4 ml CH4/m(2) and aerob
ic methane oxidation was 0-4.3 mi CH4/m(2). It was found that the major par
t of OM in the sediments is destroyed anaerobically. As this occurs, the re
duced products of decay are incorporated into bacterial metabolism. In the
winter, the products of chemosynthesis and methane compensate for the short
age of OM photosynthesis in the ecosystem.