1. A new, mechanistic model for organic carbon fluxes in the ocean based on the quantitative association of POC with ballast minerals;Armstrong;Deep-Sea Research Part II,2002
2. Baines, S.B., Twining, B.S., Brzezinski, M.A., Nelson, D.M., Fisher, N.S. The causes and biogeochemical implications of regional differences in silicification of marine diatoms. Global Biogeochemical Cycles, accepted for publication.
3. Balch, W.M., Poulton, A.J., Drapeau, D.T., Bowler, B.C., Windecker, L.A., Booth, E.S., 2011. Zonal and meridional patterns of phytoplankton biomass and carbon fixation in the equatorial Pacific Ocean between 110°W and 140°W. Deep-Sea Research II 58, 400–416.
4. Spatial and temporal variability of phytoplankton pigment distributions in the central equatorial Pacific Ocean;Bidigare;Deep-Sea Research Part II,1996
5. The Si–C–N ratio of marine diatoms—interspecific variability and the effect of some environmental variables;Brzezinski;Journal of Phycology,1985