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The Role of Climate: 71 ka of Atmospheric Mercury Deposition in the Southern Hemisphere Recorded by Rano Aroi Mire, Easter Island (Chile)

Institut für Geoökologie, Abt. Umweltgeochemie, Technische Universität Braunschweig, Langer Kamp, 38106 Braunschweig, Germany
Departamento de Edafoloxía e Química Agrícola, Universidade de Santiago de Compostela, 15782 Santiago de Compostela, Spain
Spanish National Research Council (CSIC), Global Ecology Unit CREAF-CEAB-UAB, Cerdanyola del Vallès, 08193 Catalonia, Spain
Ecological Research Center and Forestry Applications (CREAF), Campus de Bellaterra (UAB), Cerdanyola del Vallès, 08193 Barcelona, Spain
Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Rocasolano, Spanish National Research Council (CSIC), Serrano 119, 28006 Madrid, Spain
Institute of Earth Sciences Jaume Almera (ICTJA-CSIC), Lluis Sole i Sabaris s/n, 08028 Barcelona, Spain
Author to whom correspondence should be addressed.
Geosciences 2018, 8(10), 374;
Received: 27 August 2018 / Revised: 28 September 2018 / Accepted: 7 October 2018 / Published: 11 October 2018
(This article belongs to the Special Issue Mercury Biogeochemical Cycle in A Changing World)
The study of mercury accumulation in peat cores provides an excellent opportunity to improve the knowledge on mercury cycling and depositional processes at remote locations far from pollution sources. We analyzed mercury concentrations in 150 peat samples from two cores from Rano Aroi (Easter Island, 27° S) and in selected vegetation samples of present-day flora of the island, in order to characterize the mercury cycling for the last ~71 ka BP. The mercury concentrations showed values ranging between 35 and 200 ng g−1, except for a large maxima (~1000 ng g−1) which occurred at the end of the Last Glacial Maximum (LGM, ~20 ka cal BP) in both peat cores. Low temperatures during the LGM would accelerate the atmospheric oxidation of Hg(0) to divalent mercury that, coupled with higher rainfall during this period, most likely resulted in a very efficient surface deposition of atmospheric mercury. Two exceptional short-lived Hg peaks occurred during the Holocene at 8.5 (350 ng g−1) and 4.7 (1000 ng g−1) ka cal BP. These values are higher than those recorded in most peat records belonging to the industrial period, highlighting that natural factors played a significant role in Hg accumulation—sometimes even more so than anthropogenic sources. Our results suggest that wet deposition, linked to atmospheric oxidation, was the main process controlling the short-lived Hg events, both in the mire and in the catchment soils. View Full-Text
Keywords: mercury cycle; Easter Island; Pleistocene; Holocene; climate; peatland mercury cycle; Easter Island; Pleistocene; Holocene; climate; peatland
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Pérez-Rodríguez, M.; Margalef, O.; Corella, J.P.; Saiz-Lopez, A.; Pla-Rabes, S.; Giralt, S.; Martínez Cortizas, A. The Role of Climate: 71 ka of Atmospheric Mercury Deposition in the Southern Hemisphere Recorded by Rano Aroi Mire, Easter Island (Chile). Geosciences 2018, 8, 374.

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