Disassembling Iron Availability to Phytoplankton

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Disassembling Iron Availability to Phytoplankton

The bioavailability of iron to microorganisms and its underlying mechanisms have far reaching repercussions to many natural systems and diverse fields of research, including ocean biogeochemistry, carbon cycling and climate, harmful algal blooms, soil and plant research, bioremediation, pathogenesis, and medicine. Within the framework of ocean sciences, short supply and restricted bioavailabili...

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Effect of ocean acidification on iron availability to marine phytoplankton.

The acidification caused by the dissolution of anthropogenic carbon dioxide (CO2) in the ocean changes the chemistry and hence the bioavailability of iron (Fe), a limiting nutrient in large oceanic regions. Here, we show that the bioavailability of dissolved Fe may decline because of ocean acidification. Acidification of media containing various Fe compounds decreases the Fe uptake rate of diat...

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Comparative metatranscriptomics identifies molecular bases for the physiological responses of phytoplankton to varying iron availability.

In vast expanses of the oceans, growth of large phytoplankton such as diatoms is limited by iron availability. Diatoms respond almost immediately to the delivery of iron and rapidly compose the majority of phytoplankton biomass. The molecular bases underlying the subsistence of diatoms in iron-poor waters and the plankton community dynamics that follow iron resupply remain largely unknown. Here...

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Availability of iron and major nutrients for phytoplankton in the northeast Atlantic Ocean

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ژورنال

عنوان ژورنال: Frontiers in Microbiology

سال: 2012

ISSN: 1664-302X

DOI: 10.3389/fmicb.2012.00123