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Geochemistry of terricolous lichens in the White Sea catchment area

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DOKLADY EARTH SCIENCES
卷 450, 期 1, 页码 514-520

出版社

MAIK NAUKA/INTERPERIODICA/SPRINGER
DOI: 10.1134/S1028334X13050073

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资金

  1. Institution of Scientific-Technical Work of Youth (Moscow)
  2. Program of Fundamental Research of the Presidium of the Russian Academy of Sciences [23]
  3. Russian Foundation for Basic Research [11-05-00300-a]
  4. ANR Arctic Metals [ANR-09-JCJC-0035 MERCY]
  5. Otto Schmidt Russian-German Laboratory

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This paper presents new data on the multielemental composition of terricolous lichens in the White Sea catchment area. The content of 51 chemical elements was determined in 31 samples using modern analytical methods. It was shown that the chemical composition of terricolous lichens varies widely and depends on many factors. The lithogenic dust plays the main role in accumulation of Ti, Cr, Co, Ga, Fe, Zr, Nb, Ga, Th, U, and REE. Long-range transport from remote pollution sources is important for Pb, Zn, Cd, Bi, Hg, and Se. The Kostomuksha ore dressing mill provides the local enrichment of the lichens in Fe, whereas the Monchegorsk copper-nickel enterprise affects large distances and additionally enriches the lichens in Cu, Ni, Co, Pb, and Cd in comparison with the background regions. The marine impact is reflected in elevated contents and enrichment factors in Na, Mg, and the Na/K ratio.

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