论文信息 - Section 2. The Iron Cycle: Biogeochemistry and Mineralogy

Section 2. The Iron Cycle: Biogeochemistry and Mineralogy

Iron is delivered to the open ocean mainly by rivers, aeolian dust, icebergs (and subglacial runoff), hydrothermal activity and by recycling from shelf sediments ([Fig. 1.5][1]). It is believed that only rivers and hydrothermal activity supply iron in a dissolved form but neither source is effective

D. Canfield | R. Raiswell

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