Marine phytoplankton and the changing ocean iron cycle
Author:
Publisher
Springer Science and Business Media LLC
Subject
Social Sciences (miscellaneous),Environmental Science (miscellaneous)
Link
http://www.nature.com/articles/nclimate3147.pdf
Reference97 articles.
1. Moore, J. K., Lindsay, K., Doney, S. C., Long, M. C. & Misumi, K. Marine ecosystem dynamics and biogeochemical cycling in the Community Earth System Model CESM1(BGC). J. Clim. 26, 9291–9321 (2013).
2. Tagliabue, A. et al. How well do global ocean biogeochemistry models simulate dissolved iron distributions? Glob. Biogeochem. Cycles 30, 149–174 (2016). Compares 13 global ocean iron biogeochemistry models to iron measurement data sets from cross-basin transects, and finds that most do not match well, with suggestions for improvements.
3. Lis, H., Shaked, Y., Kranzler, C., Keren, N. & Morel, F. M. M. Iron bioavailability to phytoplankton: an empirical approach. ISME J. 9, 1003–1013 (2015).
4. Twining, B. S. & Baines, S. B. The trace metal composition of marine phytoplankton. Annu. Rev. Mar. Sci. 5, 191–215 (2013).
5. Boyd, P. W. & Ellwood, M. J. The biogeochemical cycle of iron in the ocean. Nat. Geosci. 3, 675–682 (2010).
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