Titlebook: Biological, Physical and Geochemical Features of Enclosed and Semi-enclosed Marine Systems; Proceedings of the J Ea Maria Blomqvist,Erik Bo

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Signature of branched fibrations,re dependence of the growth rate of phytoplankton, and the remineralization rate of detritus, as well as the variable sinking velocity of phytoplankton. Model simulations from spring to autumn of the years 1994 and 1995 were performed to investigate the effect of external forcing to the chemical-bio

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https://doi.org/10.1007/978-3-642-99823-2Also, nitrification activity was highest in these areas. The water above the sediment was well oxygenated (7.2–9.2 mg 1.) in all stations. In some areas dissimilatory NO.. reduction to NH.. seemed to be the main pathway in sediment nitrogen dynamics. These results are in agreement with existing mass

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Knotengruppe und Homologieinvariantenprokaryotes and eukaryotes group were predominant in spring, whereas in autumn, the Gram-positive bacteria group was predominant. Monounsaturated PLFA/branched PLFA ratio was high in spring and low in autumn, indicating the relative dominance of these biomarker fatty acids. Significant seasonal diff

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https://doi.org/10.1007/978-3-642-65616-3ity may also have been important. The change in the share of bacterial production in the primary production along the gradient (40% in Pojo Bay, 20% in the archipelago, and 16% in the open sea area) indicates the decreasing input of the other sources than phytoplankton in the bacterial carbon need.

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https://doi.org/10.1007/978-3-322-80287-3west in autumn/winter summer (1.1×10. cells m1.), being on the whole among the highest reported from marine sediments. The HNF abundances were significantly different between seasons, whereas spatial differences between stations were not.

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https://doi.org/10.1007/978-3-322-80287-3sumed that physical and dynamical factors dominate in the formation of small-scale spatial heterogeneity of the studied fields. Biological factors, such as diet vertical migrations, trophic interactions etc. will also contribute to the formation of patches at night.

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Water exchange as the main physical process in semi-enclosed marine systems: the Gulf of Riga case

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