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            <funder>grant 2011/01/D/ST10/02579 from the Polish National Centre of Science (NCN) (PI:Barbara Fiałkiewicz-Kozieł). We acknowledge the support of the International Network for Terrestrial Researchand Monitoring in the Arctic (INTERACT) that funded the project: “Functioning of Siberian mire ecosystemsand their response to climate changes” (CliMireSiber) (PI: Fatima Laggoun-Defarge) and Grant PSPB-013/2010through the Swiss Contribution to the enlarged European Union (CLIMPEAT, www.climpeat.pl) (PI: MariuszLamentowicz). This study is a contribution to the Virtual Institute of Integrated Climate and Landscape Evolution(ICLEA) of the Helmholtz Association and Science and Research Funds for 2015–2016, allocated to a co-financedinternational project (No. 3500/ICLEA/15/2016/0).</funder>
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              <p>As human impact have been increasing strongly over the last decades, it is crucial to distinguish human-induced dust sources from natural ones in order to define the boundary of a newly proposed epoch-the Anthropocene. Here, we track anthropogenic signatures and natural geochemical anomalies in the Mukhrino peatland, Western Siberia. Human activity was recorded there from cal AD 1958 (±6). Anthropogenic spheroidal aluminosilicates clearly identify the beginning of industrial development and are proposed as a new indicator of the Anthropocene. In cal AD 1963 (±5), greatly elevated dust deposition and an increase in REE serve to show that the geochemistry of elements in the peat can be evidence of nuclear weapon testing; such constituted an enormous force blowing soil dust into the atmosphere. Among the natural dust sources, minor signals of dryness and of the Tunguska cosmic body (TCB) impact were noted. The TCB impact was indirectly confirmed by an unusual occurrence of mullite in the peat.</p>
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