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The iron cycle (Fe) is the biogeochemical cycle of iron through the atmosphere, hydrosphere, biosphere and lithosphere. While Fe is highly abundant in the Earth's crust, it is less common in oxygenated surface waters. Iron is a key micronutrient in primary productivity, and a limiting nutrient in the Southern ocean, eastern equatorial Pacific, and the…
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iron cycle bacteria fe electron ocean regions phytoplankton oxygen ii form dust iii iron-oxidizing important fe2 extracellular biological nitrogen transport
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Iron cycle | is a | important component of the terrestrial ecosystems | 0.90 | text |
| Shewanella spp. | instance of | Examples of bacteria | 0.80 | text |
| Geobacter spp. | instance of | Examples of bacteria | 0.80 | text |
| and some Enterococcus spp. use this form of metabolism | instance of | Examples of bacteria | 0.80 | text |
| Iron cycle | related to Anthropogenic influences | Human | 0.60 | section |
| Iron cycle | related to Anthropogenic influences | Today | 0.60 | section |
| Iron cycle | related to Anthropogenic influences | Changes | 0.60 | section |
| Iron cycle | related to Anthropogenic influences | Other | 0.60 | section |
| Iron cycle | related to Anthropogenic influences | Highest | 0.60 | section |
| Iron cycle | related to Anthropogenic influences | East Asia | 0.60 | section |
| Iron cycle | related to Bacterial influences | Bacteria | 0.60 | section |
| Iron cycle | related to Bacterial influences | These | 0.60 | section |
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