Titlebook: Chemical Structure of Pelagic Redox Interfaces; Observation and Mode Evgeniy V. Yakushev Book 2013 Springer-Verlag Berlin Heidelberg 2013 B

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PACT

大沟

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Definitive

Manganese and Iron at the Redox Interfaces in the Black Sea, the Baltic Sea, and the Oslo Fjord,e Fe and Mn) obtained in the Black Sea, the Baltic Sea, and the Oslo Fjord allowed to reveal the common features that testify the similarity of the mechanism of the redox layer biogeochemical structure formation in these regions. Our investigations demonstrated that Mn bound in stable complexes with

Atrium

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Cacophonous

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Biogeochemical Characteristics in the Elefsis Bay (Aegean Sea, Eastern Mediterranean) in Relation tnamics in a semi-enclosed area of the Mediterranean Sea, Elefsis Bay, in phase with the development of intermittently hypoxic and anoxic conditions. Sediment records covering most of the Holocene showed that the area was affected by hypoxia and/or anoxia in the past. However, the occurrence of hypox

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