Physiological acclimation by phytoplankton explains observed changes in Si and N uptake rates during the SERIES iron-enrichment experiment

Deep-Sea Research Part I: Oceanographic Research Papers

Volumn 57, Issue 3, 2010, Pages 394-408

  Lan Smith, S ^a   Yoshie, Naoki ^b   Yamanaka, Yasuhiro ^a,c  

^a JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

^b EHIME UNIVERSITY   (Japan)

^c JAPAN SCIENCE AND TECHNOLOGY AGENCY   (Japan)

Author keywords

Ecosystem; Iron; Model; Nutrients; Uptake kinetics

Indexed keywords

AMBIENT CONCENTRATIONS; BIOGENIC SILICA; COMPOSITION MODEL; CONCENTRATION OF; DRAW-DOWN RATIO; ELEMENTAL COMPOSITIONS; FIELD EXPERIMENT; GROWTH-LIMITING NUTRIENTS; IRON-ENRICHMENT; IRON-FERTILIZATION; IRON-LIMITATION; LABORATORY STUDIES; MONTE CARLO MARKOV CHAIN; MULTI-ELEMENT; NUTRIENT CONCENTRATIONS; NUTRIENT UPTAKE; NUTRIENT UPTAKE KINETICS; PARTICULATE ORGANIC CARBON; SILICIC ACIDS; SPECIFIC GROWTH RATE; UPTAKE KINETICS; UPTAKE RATE;

ALGAE CONTROL; CELL CULTURE; CHLOROPHYLL; CONCENTRATION (PROCESS); ECOLOGY; EXPERIMENTS; KINETICS; MARKOV PROCESSES; ORGANIC CARBON; PHYTOPLANKTON; PORPHYRINS; SILICA; SILICON;

NUTRIENTS;

ACCLIMATION; BIOGENIC MATERIAL; CHEMOSTAT; CHLOROPHYLL; CONCENTRATION (COMPOSITION); DIATOM; ENRICHMENT; IRON; LABORATORY METHOD; LIMITING FACTOR; MARKOV CHAIN; NITROGEN; NUTRIENT UPTAKE; PHYSIOLOGICAL RESPONSE; PHYTOPLANKTON; SILICIC ACID; SILICON; SPONGE; TRACE ELEMENT;

BACILLARIOPHYTA;

EID: 77649186956     PISSN: 09670637     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.dsr.2009.09.009     Document Type: Article

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