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      Processes and patterns of oceanic nutrient limitation

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          An Earth-system perspective of the global nitrogen cycle.

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            Global iron connections between desert dust, ocean biogeochemistry, and climate.

            The environmental conditions of Earth, including the climate, are determined by physical, chemical, biological, and human interactions that transform and transport materials and energy. This is the "Earth system": a highly complex entity characterized by multiple nonlinear responses and thresholds, with linkages between disparate components. One important part of this system is the iron cycle, in which iron-containing soil dust is transported from land through the atmosphere to the oceans, affecting ocean biogeochemistry and hence having feedback effects on climate and dust production. Here we review the key components of this cycle, identifying critical uncertainties and priorities for future research.
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              Iron deficiency limits phytoplankton growth in the north-east Pacific subarctic

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                Author and article information

                Journal
                Nature Geoscience
                Nature Geosci
                Springer Nature America, Inc
                1752-0894
                1752-0908
                September 2013
                March 31 2013
                September 2013
                : 6
                : 9
                : 701-710
                Article
                10.1038/ngeo1765
                c4eb41ed-a451-4adf-877d-1551b542f915
                © 2013

                http://www.springer.com/tdm

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