Trace elements deposition in the Tierra del Fuego region (south Patagonia) by using lichen transplants after the Puyehue-Cordón Caulle (north Patagonia) volcanic eruption in 2011

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• 作者：Marcelo Enrique Conti ; Raquel Jasan…
• 关键词：Lichen transplants ; Usnea barbata ; Trace elements ; Atmospheric deposition ; Tierra del Fuego ; Puyehue ; Cordón Caulle volcano
• 刊名：Environmental Science and Pollution Research
• 出版年：2016
• 出版时间：April 2016
• 年：2016
• 卷：23
• 期：7
• 页码：6574-6583
• 全文大小：469 KB
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• 作者单位：Marcelo Enrique Conti (1)
  Raquel Jasan (2)
  Maria Grazia Finoia (3)
  Ivo Iavicoli (4)
  Rita Plá (2)
  
  1. Department of Management, University of Rome, Sapienza, Via del Castro Laurenziano 9, 00161, Rome, Italy
  2. Departamento Química Nuclear, GAATEN, Comisión Nacional de Energía Atómica, Av. del Libertador 8250, Buenos Aires, 1429, Argentina
  3. Institute for Environmental Protection and Research (ISPRA), Via di Casalotti 300, 00166, Rome, Italy
  4. Department of Public Health, Division of Occupational Medicine, University of Naples Federico II, Naples, Italy
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：Environment
  Environment
  Atmospheric Protection, Air Quality Control and Air Pollution
  Waste Water Technology, Water Pollution Control, Water Management and Aquatic Pollution
  Industrial Pollution Prevention
  
• 出版者：Springer Berlin / Heidelberg
• ISSN：1614-7499

文摘

Lichen Usnea barbata transplants were tested as a biomonitor of atmospheric deposition in an apparently pristine environment that is Tierra del Fuego region (Patagonia, Argentina). The present survey is connected with the volcanic eruption that started in north Patagonia on June 4, 2011 from the Puyehue-Cordón Caulle volcano, Chile (north Patagonia, at 1700 km of distance of our sampling sites). Lichens were collected in September 2011 (one month of exposure) and September 2012 (1 year of exposure) in 27 sites covering the northern region of the province where trees are not present. The atmospheric deposition of 27 elements by using Neutron Activation Analysis (NAA) was determined in the collected samples. The first aim of the study was to evaluate the influence of the volcanic eruption on the regional atmospheric deposition comparing our results with baseline data we determined in U. barbata in 2006 in the same sites. The second aim was to test possible patterns of bioaccumulation between the two sampling campaigns after the volcanic eruption. With respect to 2006 baseline levels, we found significant higher levels for As, Ba, Co, Cr, Cs, Na, Sb and U in lichens collected after 1 month of exposure (first sampling campaign—2011). Between the two sampling campaigns (2011–2012) after the eruption, lichens reflected the natural contamination by volcanic ashes with significantly higher median levels of Br, Cr, Fe, K, Na, Sc, and Se. Results confirmed the very good aptitude of U. barbata to reflect the levels of elements in the environment at global scale and to reflect the volcanic emissions at distant places. Volcanic eruptions cause the emission in the atmosphere of elevated levels of particulate matter. In this regard, our findings demonstrate the importance to evaluate the metal composition of the particles to avoid possible health effects.