User:Hemst010/Redfield ratio/Bibliography

example:

Sigman, D. M., & Hain, M. P. (2012). The Biological Productivity of the Ocean. http://bats.bios.edu


 * Has a good graphic for explaining the relationship between why ocean N and P form a ratio of 16:1

Martiny, A.C., C.T.A. Pham, F.W. Primeau, J.A. Vrugt, J.K. Moore, S.A. Levin, and M.W. Lomas. 2013. Strong latitudinal patterns in the elemental ratios of marine plankton and organic matter. Nature Geoscience 6(4):279–283


 * Discusses 4 methods that explain why there is variable phytoplankton stoich.

Katsumi Matsumoto, B., Tanioka, T., & Rickaby, R. (n.d.). Linkages Between Dynamic Phytoplankton C:N:P and the Ocean Carbon Cycle Under Climate Change (Vol. 33, Issue 2).


 * Provides C:N:P ratios calculated by the model as well as info on Redfield

Moore, C. M., Mills, M. M., Arrigo, K. R., Berman-Frank, I., Bopp, L., Boyd, P. W., Galbraith, E. D., Geider, R. J., Guieu, C., Jaccard, S. L., Jickells, T. D., la Roche, J., Lenton, T. M., Mahowald, N. M., Marañón, E., Marinov, I., Moore, J. K., Nakatsuka, T., Oschlies, A., … Ulloa, O. (2013). Processes and patterns of oceanic nutrient limitation. In Nature Geoscience (Vol. 6, Issue 9, pp. 701–710). https://doi.org/10.1038/ngeo1765


 * Good info on how iron can also be a limiting nutrient and is an important addition to the Redfield ratio

Tanioka, T., Matsumoto, K., & Lomas, M. W. (2021). Drawdown of Atmospheric pCO2 Via Variable Particle Flux Stoichiometry in the Ocean Twilight Zone. Geophysical Research Letters, 48(22). https://doi.org/10.1029/2021GL094924


 * A good example of how the Redfield ratio can be used in applied settings

Auguères, A. S., & Loreau, M. (2015). Regulation of Redfield ratios in the deep ocean. Global Biogeochemical Cycles, 29(2), 254–266. https://doi.org/10.1002/2014GB005066



Frigstad, H., Andersen, T., Hessen, D. O., Naustvoll, L. J., Johnsen, T. M., & Bellerby, R. G. J. (2011). Seasonal variation in marine C:N:P stoichiometry: Can the composition of seston explain stable Redfield ratios? Biogeosciences, 8(10), 2917–2933. https://doi.org/10.5194/bg-8-2917-2011



Emerson, S., Mecking, S., & Abell, J. (2001). The biological pump in subtropical North Pacific Ocean: Nutrient sources, Redfield ratios, and recent changes. Global Biogeochemical Cycles, 15(3), 535–554. https://doi.org/10.1029/2000GB001320



Körtzinger, A., Hedges, J. I., & Quay, P. D. (2001). Redfield ratios revisited: Removing the biasing effect of anthropogenic CO2. Limnology and Oceanography, 46(4), 964–970. https://doi.org/10.4319/lo.2001.46.4.0964