Platt's early research was framed by the overarching goals originally envisioned by the founders of the Atlantic Oceanographic Group of the Fisheries Research Board of Canada at the Bedford Institute of Oceanography, namely: “to describe pathways and to measure amounts and rates of energy transfer in marine biological communities; and to study the structure and degree of organization of biological systems in the sea”. One such early collaborative work concerning energy flow and species diversity in marine phytoplankton blooms was motivated by the ideas of Ramon Margalef, who evidently was nominated by Platt in a later year to receive one of three inaugural medals of the A.G. Huntsman Award for Excellence in the Marine Sciences. In the ensuing years, Platt, with collaborators, undertook a research program that progressed from investigations of the spatial inhomogeneity of plankton distribution in response to the power spectrum of turbulence,[9] through the physiological responses of the growth of cells in response to light and nutrients, to dimensional analysis and the size structure of pelagic food chains, further to theoretical considerations of the limits of biological production in the ocean, and eventually to the effects of climate change and variability on the biological cycle in the ocean By the late 1980s, Platt's research program at the Bedford Institute of Oceanography had reached a stage where the solid foundations built from a close relationship between theoretical developments and observations at sea provided the ready capabilities to embrace the possibilities offered by satellite remote sensing of the ocean. With his close collaborator Shubha Sathyendranath, Platt successfully implemented the analytical solutions and measurement-driven algorithms at regional and ocean basin scales to compute integrated primary production through the water column. In 1995, the long-sought calculation of annual global production by marine phytoplankton was made possible for the first time, after Alan Longhurst successfully partitioned the global ocean into a set of biogeochemical provinces within which the phytoplankton are likely subject to common physical forcing. In later years after the estimation of marine primary production at large geographical scale was made operational, Platt increasingly turned his attention to the use of remotely-sensed ocean colour as indicators of ecosystem performance towards the management of fisheries and stewardship of the ocean.