Magnitude of oceanic nitrogen fixation influenced by the nutrient uptake ratio of phytoplankton (original) (raw)

References

  1. Redfield, A. C. in James Johnstone Memorial Volume (ed. Daniel, R. J.) 177–192 (Univ. Press Liverpool, 1934).
    Google Scholar
  2. Anderson, L. A. & Sarmiento, J. L. Redfield ratios of remineralization determined by nutrient data-Analysis. Glob. Biogeochem. Cycles 8, 65–80 (1994).
    Article Google Scholar
  3. Gruber, N. & Sarmiento, J. L. Global patterns of marine nitrogen fixation and denitrification. Glob. Biogeochem. Cycles 11, 235–266 (1997).
    Article Google Scholar
  4. Moore, J. K., Doney, S. C., Kleypas, J. A., Glover, D. M. & Fung, I. Y. An intermediate complexity marine ecosystem model for the global domain. Deep-Sea Res. II 49, 403–462 (2002).
    Article Google Scholar
  5. Quigg, A. et al. The evolutionary inheritance of elemental stoichiometry in marine phytoplankton. Nature 425, 291–294 (2003).
    Article Google Scholar
  6. Arrigo, K. R. et al. Phytoplankton community structure and the drawdown of nutrients and CO2 in the Southern Ocean. Science 283, 365–367 (1999).
    Article Google Scholar
  7. Geider, R. J. & La Roche, J. Redfield revisited: Variability of C:N:P in marine microalgae and its biochemical basis. Eur. J. Phycol. 37, 1–17 (2002).
    Article Google Scholar
  8. Bertilsson, S., Berglund, O., Karl, D. M. & Chisholm, S. W. Elemental composition of marine Prochlorococcus and Synechococcus : Implications for the ecological stoichiometry of the sea. Limnol. Oceanogr. 48, 1721–1731 (2003).
    Article Google Scholar
  9. Klausmeier, C. A., Litchman, E., Daufresne, T. & Levin, S. A. Optimal nitrogen-to-phosphorus stoichiometry of phytoplankton. Nature 429, 171–174 (2004).
    Article Google Scholar
  10. Deutsch, C., Sarmiento, J. L., Sigman, D. M., Gruber, N. & Dunne, J. P. Spatial coupling of nitrogen inputs and losses in the ocean. Nature 445, 163–167 (2007).
    Article Google Scholar
  11. Anderson, T. R. & Pondaven, P. Non-Redfield carbon and nitrogen cycling in the Sargasso Sea: Pelagic imbalances and export flux. Deep-Sea Res. I 50, 573–591 (2003).
    Article Google Scholar
  12. Christian, J. R. Biogeochemical cycling in the oligotrophic ocean: Redfield and non-Redfield models. Limnol. Oceanogr. 50, 646–657 (2005).
    Article Google Scholar
  13. Chavez, F. P., Buck, K. R., Service, S. K., Newton, J. & Barber, R. T. Phytoplankton variability in the central and eastern tropical Pacific. Deep-Sea Res. II 43, 835–870 (1996).
    Article Google Scholar
  14. Bruland, K. W., Rue, E. L., Smith, G. J. & DiTullio, G. R. Iron, macronutrients and diatom blooms in the Peru upwelling regime: Brown and blue waters of Peru. Mar. Chem. 93, 81–103 (2005).
    Article Google Scholar
  15. Dandonneau, Y. et al. Seasonal and interannual variability of ocean colour and composition of phytoplankton communities in the North Atlantic, equatorial Pacific and South Pacific. Deep-Sea Res. II 51, 303–318 (2004).
    Article Google Scholar
  16. Garcia, H. E., Locarnini, R. A., Boyer, T. P. & Anotov, J. I. in NOAA Atlas NESDIS 64 (ed. Levitus, S.) (US Government Printing Office, 2006).
    Google Scholar
  17. Voss, M., Bombar, D., Loick, N. & Dippner, J. W. Riverine influence on nitrogen fixation in the upwelling region off Vietnam, South China Sea. Geophys. Res. Lett. 33, L07604 (2006).
    Article Google Scholar
  18. Capone, D. G. et al. An extensive bloom of the N2-fixing cyanobacterium Trichodesmium erythraeum in the central Arabian Sea. Mar. Ecol. Prog. Ser. 172, 281–292 (1998).
    Article Google Scholar
  19. Canfield, D. E. Models of oxic respiration, denitrification and sulfate reduction in zones of coastal upwelling. Geochim. Cosmochim. Acta 70, 5753–5765 (2006).
    Article Google Scholar
  20. Moore, J. K. & Doney, S. C. Iron availability limits the ocean nitrogen inventory stabilizing feedbacks between marine denitrification and nitrogen fixation. Glob. Biogeochem. Cycles 21 (2007).
  21. Tagliabue, A., Bopp, L. & Aumont, O. Ocean biogeochemistry exhibits contrasting responses to a large scale reduction in dust deposition. Biogeosciences 5, 11–24 (2008).
    Article Google Scholar
  22. Glibert, P. M. & Bronk, D. A. Release of dissolved organic nitrogen by marine diazotrophic cyanobacteria, Trichodesmium spp. Appl. Environ. Microbiol. 60, 3996–4000 (1994).
    Google Scholar
  23. Yamamoto-Kawai, M., Carmack, E. & McLaughlin, F. Nitrogen balance and Arctic throughflow. Nature 443, 43–43 (2006).
    Article Google Scholar
  24. Lochte, K., Ducklow, H. W., Fasham, M. J. R. & Stienen, C. Plankton succession and carbon cycling at 47° N 20° W during the JGOFS North-Atlantic bloom experiment. Deep-Sea Res. II 40, 91–114 (1993).
    Article Google Scholar
  25. Staal, M. et al. Nitrogen fixation along a north–south transect in the eastern Atlantic Ocean. Limnol. Oceanogr. 52, 1305–1316 (2007).
    Article Google Scholar
  26. Richardson, T. L. & Jackson, G. A. Small phytoplankton and carbon export from the surface ocean. Science 315, 838–840 (2007).
    Article Google Scholar
  27. Schmittner, A. Decline of the marine ecosystem caused by a reduction in the Atlantic overturning circulation. Nature 434, 628–633 (2005).
    Article Google Scholar
  28. Irwin, A. J. & Oliver, M. J. Are ocean deserts getting larger? Geophys. Res. Lett. 36, L18609 (2009).
    Article Google Scholar
  29. Codispoti, L. A. et al. The oceanic fixed nitrogen and nitrous oxide budgets: Moving targets as we enter the anthropocene? Sci. Marina 65, 85–105 (2001).
    Article Google Scholar
  30. Paulmier, A., Kriest, I. & Oschlies, A. Stoichiometries of remineralisation and denitrification in global biogeochemical ocean models. Biogeosciences 6, 2539–2566 (2009).
    Article Google Scholar

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