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    Chronology of the Atmospheric Mercury in Lagoa da Pata Basin, Upper Rio Negro Region of Brazilian Amazon

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    Author
    Santos, G. M.
    Cordeiro, R. C.
    Silva Filho, E. V.
    Turcq, B.
    Lacerda, L. D.
    Fifield, L. K.
    Gomes, P. R. S.
    Hausladen, P. A.
    Sifeddine, A.
    Albuquerque, A. L. S.
    Issue Date
    2001-01-01
    Keywords
    drainage basins
    Lagoa da Pata
    mercury
    Rio Negro
    Sao Gabriel da Cachoeira Brazil
    lacustrine sedimentation
    human ecology
    lake sediments
    Amazon Basin
    depositional environment
    cores
    sedimentation
    sedimentation rates
    pollution
    human activity
    atmosphere
    Brazil
    South America
    correlation
    chronology
    metals
    paleoclimatology
    Pleistocene
    upper Pleistocene
    sediments
    Cenozoic
    Quaternary
    C 14
    carbon
    dates
    isotopes
    radioactive isotopes
    absolute age
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    Citation
    Santos, G. M., Cordeiro, R. C., Silva Filho, E. V., Turcq, B., Lacerda, L. D., Fifield, L. K., ... & Albuquerque, A. L. S. (2001). Chronology of the atmospheric mercury in Lagoa da Pata basin, Upper Rio Negro region of Brazilian Amazon. Radiocarbon, 43(2B), 801-808.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    Description
    From the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000.
    URI
    http://hdl.handle.net/10150/654466
    DOI
    10.1017/S0033822200041473
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    We present prehistoric mercury accumulation rates in a dated sediment core from Lagoa da Pata, a remote lake in Sao Gabriel da Cachoeira, northern Amazon. The sediment samples were subdivided for mercury and radiocarbon analyses. A group of 18 samples have been prepared at ANU for 14C dating by accelerator mass spectrometry (AMS). The dating results show a good correlation with depth in the core, down to 41,500 BP. Three distinct sections are clearly identified in the core. They consist of upper and lower organic-rich layer, separated by an inorganic layer which represents a short period of rapid accumulation around 18 ka BP. The mercury accumulation rate is found to be larger in the upper layer (18 ka to present) than in the lower one (41 ka to 25 ka), by a factor of three. The larger accumulation rate of mercury is probably associated with warmer temperatures and a higher frequency of forest fires during the Holocene.
    Type
    Proceedings
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200041473
    Scopus Count
    Collections
    Radiocarbon, Volume 43, Number 2B (2001)

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