Mechanisms of increased Trichodesmium fitness under iron and phosphorus co-limitation in the present and future ocean
Nitrogen fixation by cyanobacteria supplies critical bioavailable nitrogen to marine ecosystems worldwide; however, field and lab data have demonstrated it to be limited by iron, phosphorus and/or CO 2 . To address unknown future interactions among these factors, we grew the nitrogen-fixing cyanobac...
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Published in: | Nature communications Vol. 7; no. 1; p. 12081 |
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Abstract | Nitrogen fixation by cyanobacteria supplies critical bioavailable nitrogen to marine ecosystems worldwide; however, field and lab data have demonstrated it to be limited by iron, phosphorus and/or CO
2
. To address unknown future interactions among these factors, we grew the nitrogen-fixing cyanobacterium
Trichodesmium
for 1 year under Fe/P co-limitation following 7 years of both low and high CO
2
selection. Fe/P co-limited cell lines demonstrated a complex cellular response including increased growth rates, broad proteome restructuring and cell size reductions relative to steady-state growth limited by either Fe or P alone. Fe/P co-limitation increased abundance of a protein containing a conserved domain previously implicated in cell size regulation, suggesting a similar role in
Trichodesmium.
Increased CO
2
further induced nutrient-limited proteome shifts in widespread core metabolisms. Our results thus suggest that N
2
-fixing microbes may be significantly impacted by interactions between elevated CO
2
and nutrient limitation, with broad implications for global biogeochemical cycles in the future ocean.
Cyanobacterial nitrogen fixation supplies bioavailable nitrogen to marine ecosystems, but the mechanisms governing iron and phosphorus co-limitation in elevated CO
2
remain unknown. Here, the authors show a complex cellular response to co-limitation characterized by changes in growth, cell size, and the proteome. |
---|---|
AbstractList | Nitrogen fixation by cyanobacteria supplies critical bioavailable nitrogen to marine ecosystems worldwide; however, field and lab data have demonstrated it to be limited by iron, phosphorus and/or CO2. To address unknown future interactions among these factors, we grew the nitrogen-fixing cyanobacterium Trichodesmium for 1 year under Fe/P co-limitation following 7 years of both low and high CO2 selection. Fe/P co-limited cell lines demonstrated a complex cellular response including increased growth rates, broad proteome restructuring and cell size reductions relative to steady-state growth limited by either Fe or P alone. Fe/P co-limitation increased abundance of a protein containing a conserved domain previously implicated in cell size regulation, suggesting a similar role in Trichodesmium. Increased CO2 further induced nutrient-limited proteome shifts in widespread core metabolisms. Our results thus suggest that N2-fixing microbes may be significantly impacted by interactions between elevated CO2 and nutrient limitation, with broad implications for global biogeochemical cycles in the future ocean. Abstract Nitrogen fixation by cyanobacteria supplies critical bioavailable nitrogen to marine ecosystems worldwide; however, field and lab data have demonstrated it to be limited by iron, phosphorus and/or CO 2 . To address unknown future interactions among these factors, we grew the nitrogen-fixing cyanobacterium Trichodesmium for 1 year under Fe/P co-limitation following 7 years of both low and high CO 2 selection. Fe/P co-limited cell lines demonstrated a complex cellular response including increased growth rates, broad proteome restructuring and cell size reductions relative to steady-state growth limited by either Fe or P alone. Fe/P co-limitation increased abundance of a protein containing a conserved domain previously implicated in cell size regulation, suggesting a similar role in Trichodesmium. Increased CO 2 further induced nutrient-limited proteome shifts in widespread core metabolisms. Our results thus suggest that N 2 -fixing microbes may be significantly impacted by interactions between elevated CO 2 and nutrient limitation, with broad implications for global biogeochemical cycles in the future ocean. Nitrogen fixation by cyanobacteria supplies critical bioavailable nitrogen to marine ecosystems worldwide; however, field and lab data have demonstrated it to be limited by iron, phosphorus and/or CO 2 . To address unknown future interactions among these factors, we grew the nitrogen-fixing cyanobacterium Trichodesmium for 1 year under Fe/P co-limitation following 7 years of both low and high CO 2 selection. Fe/P co-limited cell lines demonstrated a complex cellular response including increased growth rates, broad proteome restructuring and cell size reductions relative to steady-state growth limited by either Fe or P alone. Fe/P co-limitation increased abundance of a protein containing a conserved domain previously implicated in cell size regulation, suggesting a similar role in Trichodesmium. Increased CO 2 further induced nutrient-limited proteome shifts in widespread core metabolisms. Our results thus suggest that N 2 -fixing microbes may be significantly impacted by interactions between elevated CO 2 and nutrient limitation, with broad implications for global biogeochemical cycles in the future ocean. Cyanobacterial nitrogen fixation supplies bioavailable nitrogen to marine ecosystems, but the mechanisms governing iron and phosphorus co-limitation in elevated CO 2 remain unknown. Here, the authors show a complex cellular response to co-limitation characterized by changes in growth, cell size, and the proteome. Cyanobacterial nitrogen fixation supplies bioavailable nitrogen to marine ecosystems, but the mechanisms governing iron and phosphorus co-limitation in elevated CO2remain unknown. Here, the authors show a complex cellular response to co-limitation characterized by changes in growth, cell size, and the proteome. |
ArticleNumber | 12081 |
Author | Walworth, Nathan G. Saito, Mak A. Lee, Michael D. Moran, Dawn Mcllvin, Matthew R. Fu, Fei-Xue Webb, Eric A. Hutchins, David A. |
Author_xml | – sequence: 1 givenname: Nathan G. surname: Walworth fullname: Walworth, Nathan G. organization: Department of Biological Sciences, Marine and Environmental Biology, University of Southern California – sequence: 2 givenname: Fei-Xue surname: Fu fullname: Fu, Fei-Xue organization: Department of Biological Sciences, Marine and Environmental Biology, University of Southern California – sequence: 3 givenname: Eric A. surname: Webb fullname: Webb, Eric A. organization: Department of Biological Sciences, Marine and Environmental Biology, University of Southern California – sequence: 4 givenname: Mak A. surname: Saito fullname: Saito, Mak A. organization: Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution – sequence: 5 givenname: Dawn surname: Moran fullname: Moran, Dawn organization: Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution – sequence: 6 givenname: Matthew R. surname: Mcllvin fullname: Mcllvin, Matthew R. organization: Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution – sequence: 7 givenname: Michael D. surname: Lee fullname: Lee, Michael D. organization: Department of Biological Sciences, Marine and Environmental Biology, University of Southern California – sequence: 8 givenname: David A. surname: Hutchins fullname: Hutchins, David A. email: dahutch@usc.edu organization: Department of Biological Sciences, Marine and Environmental Biology, University of Southern California |
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Snippet | Nitrogen fixation by cyanobacteria supplies critical bioavailable nitrogen to marine ecosystems worldwide; however, field and lab data have demonstrated it to... Abstract Nitrogen fixation by cyanobacteria supplies critical bioavailable nitrogen to marine ecosystems worldwide; however, field and lab data have... Cyanobacterial nitrogen fixation supplies bioavailable nitrogen to marine ecosystems, but the mechanisms governing iron and phosphorus co-limitation in... |
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Title | Mechanisms of increased Trichodesmium fitness under iron and phosphorus co-limitation in the present and future ocean |
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