The Biogeochemical Cycles of Trace Metals in the Oceans

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Spinning the “Ferrous Wheel”: The importance of the microbial community in an iron budget during the FeCycle experiment (2005, background): “[3] A large number of lab (reviewed by Morel and Price [2003] ), shipboard (reviewed by de Baar and Boyd [1999]) and mesoscale Fe-enrichment [Boyd, 2004] experiments have highlighted the importance of Fe in a myriad of oceanic processes.”
The role of grazing in structuring Southern Ocean pelagic ecosystems and biogeochemical cycles (2004, background): “Although only trace amounts of iron are required by plankton, its involvement and indispensibility in many key enzyme systems (chlorophyll synthesis, nitrate utilisation, redox systems, etc.) results in its playing as much a "building block" role as the macronutrients (Morel & Price 2003).”
Biogeochemical signatures through time as inferred from whole microbial genomes (2005, background): “…oxygenation of the oceans, based on assumptions made by Saito and others (2003), except molybdenum concentrations, which were derived from other sources (Bertine and Turekian, 1973; Collier, 1985; Lewis and Landing, 1992; Stumm and Morgan, 1996; Morford and Emerson, 1999; Anbar and Knoll, 2002).”
An Introduction to the Application and Future Use of 234Th in Aquatic Systems (2006, background): “Recent evidence suggests many trace elements, in addition to iron, have an active role in regulating primary production and species composition (Morel and Price, 2003).”