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. 2016 Aug 18;7:1223. doi: 10.3389/fpls.2016.01223

Table 1.

Tradeoffs and co-limitation scenarios for iron-nitrogen, manganese, copper, and light interactions.

Resource Description of interaction Type of interaction/s with iron Trade offs Adaptations to low [Fe] Co-limitation scenarios
Nitrogen Photochemically produced reductive energy (NADPH) requires Fe based electron carriers.
Fe dependent enzymes: Nitrate and nitrite reductases (NO3) Nitrogenase (N2)
Biochemical dependence Ambient Fe concentrations constrain biogeographic distribution of diazotrophic/non-diazotrophic phytoplankton in accordance with their partitioning strategy. Temporal partitioning of N2 fixations allows for smaller cells and Fe recycling. While iron limitation lowers the efficiency of NO3 uptake, nitrogen demands of Fe-limited cells can still be fully met.
Nitrogen fixation may be Fe limited.
Manganese Mn-SOD may replace Fe-SOD Transporter promiscuity – Mn may enter cell via specific Fe transporters. Substitution
Indirect
Mn-SOD compensates for decreased levels of Fe-SOD under limitation. Mn concentrations in most natural waters are above limiting levels (see Brand et al., 1983 and Hecky and Kilham, 1988).
Copper Plastocyanin is a Cu based electron carrier which may substitute for the Fe containing cytochrome c6.
Cu dependent high affinity Fe transporters.
Substitution Biochemical dependence Fe demands decreased but greater Cu demands of open ocean diatoms leave them more prone to Cu limitation. Plastocyanin is constitutively expressed in open ocean diatoms in lieu of cytochrome c6. Ambient Cu concentrations are mostly sufficient (see Peers et al., 2005 and Peers and Price, 2006).
Light Iron is essential to photosynthesis, the greatest cellular Fe sink. Biochemical dependence Species with lowered PSI:PSII and Cytochrome b6f:PSII ratios have lower Fe demands but smaller dynamic range for handling fluctuating light intensities. Open ocean strains have less PSI and Cytochrome b6f.
Southern Ocean diatoms increase PSU size rather than number, increasing light capture without inflating Fe costs.
Low iron waters at high latitudes.