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      Monitoring Australian Monsoon variability over the past four glacial cycles

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          A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records

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            Distribution of the Elements in Some Major Units of the Earth's Crust

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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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                Author and article information

                Journal
                Palaeogeography, Palaeoclimatology, Palaeoecology
                Palaeogeography, Palaeoclimatology, Palaeoecology
                Elsevier BV
                00310182
                April 2021
                April 2021
                : 568
                : 110280
                Article
                10.1016/j.palaeo.2021.110280
                b8366685-f302-401b-91ee-02eddb5ede69
                © 2021

                https://www.elsevier.com/tdm/userlicense/1.0/

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