Global Iron Connections Between Desert Dust, Ocean Biogeochemistry, and Climate

  title={Global Iron Connections Between Desert Dust, Ocean Biogeochemistry, and Climate},
  author={Tim D. Jickells and Zhi-shan An and K. K. Andersen and Alex R. Baker and Gilles Bergametti and N. Brooks and J. J. Cao and Philip W. Boyd and Robert A. Duce and K. A. Hunter and Hodaka Kawahata and Nilg{\"u}n Kubilay and Julie LaRoche and Peter S. Liss and Nathaniel Mahowald and Joseph M. Prospero and Andy Ridgwell and Ina Tegen and Raquel Torres},
  pages={67 - 71}
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… 

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