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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Elevated mercury accumulation in a peat bog of the Magellanic Moorlands, Chile (53°S)-an anthropogenic signal from the Southern Hemisphere
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Elevated mercury accumulation in a peat bog of the Magellanic Moorlands, Chile (53°S)-an anthropogenic signal from the Southern Hemisphere

机译:智利麦哲伦沼泽地的泥炭沼泽中汞的积累增加(53°S)-来自南半球的人为信号

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Increasing mercury deposition rates in the Northern Hemisphere recorded in natural archives such as peat bogs of lake sediments have been documented in numerous studies. However, data on atmospheric Hg deposition in the Southern Hemisphere dating back to pre-industrial time are rare. Here, we provide a continuous record of atmospheric Hg deposition in the Southern Hemisphere recorded by an ombrotrophic peat bog of the Magellanic Moorlands, Chile (53°S), extending back 3000 yr. Pre-industrial mercury accumulation rates range between 2.5 and 3.9 μg/m~2/yr. In the past 100 yr, Hg accumulation rates increased 18-fold from about 3 μg/m~2/yr to a maximum of 62.5 μg/m~2/yr. If Hg accumulation rates were normalized to peat accumulation rates, maximum rates were 7.9 μg/m~2/yr, which is only 2.5 times the pre-industrial rates. Thus, Hg accumulation rates normalized to peat accumulation rates are more comparable to the three-fold net increase in atmospheric Hg concentrations estimated for the same period. We suggest that the increase in Hg accumulation rates in the Magellanic Moorlands within the past 100 yr is at least partly attributed to global dispersion of Hg derived from anthropogenic sources in the Northern Hemisphere. The finding that no increase of atmospheric deposition of Pb could be observed in the bog indicates the extraordinary long-range transport and ubiquitous dispersion of anthropogenic derived gaseous Hg compared to other metals.
机译:在自然档案中记录的北半球汞沉积速率不断提高,例如湖泊沉积物的泥炭沼泽已被许多研究记录。然而,有关南半球大气汞沉积的数据可追溯到工业化之前。在这里,我们提供了南半球大气汞沉积的连续记录,该记录由智利麦哲伦高沼地的营养营养泥炭沼泽(53°S)记录,可追溯到3000年。工业化前的汞累积率介于2.5和3.9μg/ m〜2 / yr之间。在过去的100年中,Hg的累积速率从约3μg/ m〜2 / yr增加到最高的62.5μg/ m〜2 / yr,增长了18倍。如果将汞的积累速率标准化为泥炭的积累速率,则最大速率为7.9μg/ m〜2 / yr,仅是工业化前速率的2.5倍。因此,归一化为泥炭积累率的汞积累率与同期估计的大气中汞浓度的三倍净增加具有可比性。我们认为,过去100年来麦哲伦高地中汞的累积速率增加,至少部分归因于北半球人为来源产生的汞的全球扩散。沼泽中未观察到Pb在大气中的沉积增加的发现表明,与其他金属相比,人为衍生的气态Hg具有非凡的远距离迁移和普遍分布性。

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