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equator to pole, from the continental shelf to the deep ocean and from the past to the present. The ocean is Earth’s largest reservoir of CO2 and heat; circulation, mixing, biogeochemistry and other marine
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the composition and functioning of microbial communities in environments ranging from the deep sea to large lake systems. Within this department a subgroup of organic geochemists is developing novel (analytical
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. Upwelling events bring nutrient rich deep-water to the surface, promoting phytoplankton production through communities dominated by known producers of omega-3. As such, these areas could represent hot-spots
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