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Regional Environmental Change

, Volume 16, Issue 4, pp 1089–1096 | Cite as

Remobilization of trace elements by forest fire in Patagonia, Chile

  • Kingsley O. OdigieEmail author
  • Ethel Khanis
  • Sharon A. Hibdon
  • Patricia Jana
  • Alberto Araneda
  • Roberto Urrutia
  • A. Russell Flegal
Original Article

Abstract

Temporal changes in the amounts of trace elements (As, Co, Cu, Mn, Ni, Pb, and Zn) and their correlations with temporal changes in charcoal abundance in age-dated sediments collected from Lake Thompson in Patagonia, Chile, attest to the substantial pyrogenic remobilization of contaminants that occurred in Patagonia during the mid-1900s. This remobilization was concurrent with the extensive slash and burn period in the region during that period. The changes in concentrations of Co, Cu, and Ni in relation to charcoal abundance in the lacustrine sediments over time were small compared to those of As, Mn, Pb, and Zn. However, the relatively low enrichment factors of all those trace elements, normalized to Fe, indicate that they were predominantly derived from local, natural sources impacted by fires rather than industrial sources. The primarily local source of Pb in the sediments was corroborated by the temporal consistency of its isotopic ratios (206Pb/207Pb:208Pb/206Pb), which were similar to previously reported values for natural lead in Central and Southern Chile. However, the pyrogenic remobilization of both natural and industrial trace elements by forest fires in Chile and elsewhere is expected to rise as a consequence of climate change, which is projected to increase both the frequency and intensity of forest fires on a global scale.

Keywords

Pyrogenic remobilization Trace elements Lead isotopic composition Wildfire 

Notes

Acknowledgments

The authors are grateful to Rob Franks of UCSC for analytical support and all members of the WIGS Laboratory for their support with this project. This work was partly supported by the US Department of Energy (DOE) Office of Science Graduate Fellowship Program, University of California Cota Robles Fellowship, Chilean government through the Fondecyt projects 1120765 and 1120807, and the Fulbright U.S. Scholar Program. All opinions expressed in this work are the authors’ and do not necessarily reflect the policies and views of the DOE Office of Science. Data for this study are provided in the supporting information file.

Supplementary material

10113_2015_825_MOESM1_ESM.docx (1.5 mb)
Supplementary material 1 (DOCX 1585 kb)

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Copyright information

© Springer-Verlag Berlin Heidelberg 2015

Authors and Affiliations

  • Kingsley O. Odigie
    • 1
    Email author
  • Ethel Khanis
    • 1
  • Sharon A. Hibdon
    • 1
  • Patricia Jana
    • 2
  • Alberto Araneda
    • 2
  • Roberto Urrutia
    • 2
  • A. Russell Flegal
    • 1
    • 2
  1. 1.WIGS Laboratory, Environmental ToxicologyUniversity of California at Santa CruzSanta CruzUSA
  2. 2.Group of Paleolimnological Studies (GEP), Aquatic Systems Research Unit, Environmental Sciences Center EULA-ChileUniversity of ConcepcionConcepciónChile

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