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Human activities perturb the atmosphere and thereby influence the global climate. Prominent examples are greenhouse trace gases and sulfate aerosols which both affect the radiative balance at the surface of the Earth. This is also true for black carbon and organic carbon aerosols emitted by burning of biomass and fossil fuel, as well as eolian mineral dust originating from changes in land use and land cover.

The Late Quaternary History of Atmospheric Trace Gases and Aerosols: Interactions Between Climate and Biogeochemical Cycles