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Trace Metals & Phytoplankton. Gert Vlaming. 24-01-2003. Contents. Introduction Trace metals Importance of phytoplankton Conclusion. Gaia theory. Environment. Life. Trace metals. Fe 3+ Mn 2+ Co 2+ Cu 2+. Ni 2+ Cd 2+ Zn 2+. Trace metals of importance. Complexation field diagram.
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Trace Metals & Phytoplankton Gert Vlaming 24-01-2003
Contents • Introduction • Trace metals • Importance of phytoplankton • Conclusion
Gaia theory Environment Life
Fe3+ Mn2+ Co2+ Cu2+ Ni2+ Cd2+ Zn2+ Trace metals of importance
Complexation field diagram Whitfield, 1997
Recycled elements • Low concentrations in the surface layer • Enhanced concentrations in the deeper water • Residence time: intermediate (103 – 105 yrs) • Concentrations: 10-12 – 10-5 M
Concentrations mol/l
Concentrations II • Atlantic ocean receives a greater flux of windborne dust and atmospheric contaminants than the Pacific • Accumulated elements released from the decaying particulate matter • Mn and Co: adsorption onto particles
Biochemical functions And many enzymatic reactions
Availability • > 97% of the total metal in solution is held in strong organic complexes • These complexes are not available for phytoplanktonic uptake The essential trace metals have very low concentrations
Fractionation Broecker & Peng, 1982
Recycling ratio flux circulating within the ecosystem R = flux circulating through the environment R R
Recycling ratio Whitfield, 1997
Recycling ratio II • The inability of phytoplankton to exercise absolute discrimination • Phytoplankton are capable of actively regulating their internal economy • For most essential trace metals the cells are at, or close to, their nutrient limitation levels
Adaptations • Internal • External • Interspecific • Collective There’s a “chemical war” going on ...
Uptake • Diffusion • Transfer of complexes • Capture • Uptake by Michaelis-Menten kinetics
Organic complexation • Cells release organic complexing agents • Beneficial for Fe, Cu en Mn • Enabling large pool of Fe to be maintained • Maintaining concentrations below toxic levels
Conclusions • Availability of trace metals is a significant factor regulating primary production • Phytoplankton is strongly effecting the concentrations of trace metals
Evolution of life • Prokaryotic life: 3.5 Ga • Eukaryotic life: 1.5 Ga • Multicellular life: 600 Ma
Start of multicellular life Possibly because: • Lowering of the alkalinity of the oceans • The attainment of an appropriately low global mean temperature • The maintenance of a critical level of dissolved oxygen in the sea • The establishment of the required cocktail of available trace metals