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Geochemical changes in organic matter of bottom sediments from the Mozambique Basin at the river-sea barrier from the mouths of the Zambezi and Limpopo rivers toward the pelagic zone are discussed. Changes in bitumen, hydrolyzable material, humic acids, amino acids, n-alkanes, and polycyclic aromatic compounds resulting from genetic and diagenetic factors are described. This information is significant for paleoceanology reconstructions and for knowing ways of organic matter transformation into fossil forms.

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6 resultados para Ticks as carriers of disease -- Mozambique.

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(Table 2) Biomass of seston at distances of 2 m and 30 m above the bottom in different areas of the Mozambique Channel, Indian Ocean

Results of thermal stress on the evolutionary trajectories of disease resistance in three marine populations of three-spined sticklebacks (Gasterosteus aculeatus) from the North Sea

(Table 6.3.3) Sulfate reduction rate in bottom sediments of the Mozambique Channel, Indian Ocean

(Table 6.3.2) Abundance of different groups of microorganisms in bottom sediments of the Mozambique Channel, Indian Ocean

(Table 6.3.1) Contains of organic carbon and total reduced sulfur in reduced bottom sediments from the Mozambique Channel, Indian Ocean

(Table 1) Lithological and organic-geochemical compositions of bottom sediments from the Southwestern Indian Ocean (Mozambique Basin)