Shelf-derived iron inputs drive biological productivity in the southern Drake Passage

Global Biogeochemical Cycles

Volumn 23, Issue 4, 2009, Pages

  Dulaiova, H ^c   Ardelan, M V ^a   Henderson, P B ^b   Charette, M A ^b  

^a NORWEGIAN UNIVERSITY OF SCIENCE AND TECHNOLOGY   (Norway)

^b WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

^c UNIVERSITY OF HAWAII   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ANTARCTIC CIRCUMPOLAR CURRENT; ANTARCTIC PENINSULA; BIOLOGICAL PRODUCTIVITY; DISSOLVED IRON; DRAKE PASSAGE; EXPORT FLUX; IRON FLUXES; IRON RICH; LATERAL MIXING; LATERAL TRANSPORT; MIXED LAYER; NATURALLY OCCURRING; PHYTOPLANKTON BLOOM; RADIUM ISOTOPES; RAPID MIXING; SHELF WATERS; SOUTHERN OCEAN; WATER COLUMNS;

BLOOMS (METAL); ISOTOPES; OCEAN CURRENTS; RADIUM;

DISSOLUTION;

ALGAL BLOOM; ANTARCTIC CIRCUMPOLAR WAVE; BIOLOGICAL PRODUCTION; IRON; NUTRIENT DYNAMICS; PHYTOPLANKTON; RADIUM ISOTOPE; SHELF SEDIMENT; VERTICAL MIXING; WATER COLUMN;

ANTARCTIC CIRCUMPOLAR CURRENT; ANTARCTIC PENINSULA; ANTARCTICA; DRAKE PASSAGE; SOUTHERN OCEAN; WEST ANTARCTICA;

ALGAE;

EID: 74049093772     PISSN: 08866236     EISSN: None     Source Type: Journal    
DOI: 10.1029/2008GB003406     Document Type: Article

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