The manganese and iron shuttle in a modern euxinic basin and implications for molybdenum cycling at euxinic ocean margins

Chemical Geology

Volumn 355, Issue , 2013, Pages 56-68

  Scholz, Florian ^a   McManus, James ^a   Sommer, Stefan ^b  

^a OREGON STATE UNIVERSITY   (United States)

^b GEOMAR HELMHOLTZ CENTRE FOR OCEAN RESEARCH KIEL   (Germany)

Author keywords

Baltic Sea; Iron; Manganese; Molybdenum; Paleo redox; Shuttle

Indexed keywords

BALTIC SEA; CONTINENTAL SHELVES; ISOTOPE COMPOSITIONS; ISOTOPE FRACTIONATION; OXYGEN MINIMUM ZONE; PALEO-REDOX; REDUCING ENVIRONMENT; SHUTTLE;

ADSORPTION; IRON; ISOTOPES; MANGANESE; MOLYBDENUM OXIDE; SEAWATER; SEDIMENTS;

MOLYBDENUM;

ADSORPTION; ANOXIC CONDITIONS; BASIN; EUXINIC ENVIRONMENT; INFLOW; IRON; ISOTOPIC COMPOSITION; ISOTOPIC FRACTIONATION; MANGANESE; MOLYBDENUM; ORGANIC MATTER; OXIC CONDITIONS; REDOX CONDITIONS; RESIDENCE TIME; SEAWATER; SOLUBILITY; SULFIDE; URANIUM; WATER COLUMN; WATER MASS;

ATLANTIC OCEAN; BALTIC SEA; BLACK SEA; GOTLAND BASIN; GOTLAND DEEP;

EID: 84881537251     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2013.07.006     Document Type: Article

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