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Hemispheric black carbon increase after the 13th-century Maori arrival in New Zealand

机译:13世纪的毛利人抵达新西兰后半球黑碳增加

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摘要

New Zealand was among the last habitable places on earth to be colonized by humans~(1). Charcoal records indicate that wildfires were rare prior to colonization and widespread following the 13th- to 14th-century Māori settlement~(2), but the precise timing and magnitude of associated biomass-burning emissions are unknown~(1,3), as are effects on light-absorbing black carbon aerosol concentrations over the pristine Southern Ocean and Antarctica~(4). Here we used an array of well-dated Antarctic ice-core records to show that while black carbon deposition rates were stable over continental Antarctica during the past two millennia, they were approximately threefold higher over the northern Antarctic Peninsula during the past 700 years. Aerosol modelling~(5)demonstrates that the observed deposition could result only from increased emissions poleward of 40° S-implicating fires in Tasmania, New Zealand and Patagonia-but only New Zealand palaeofire records indicate coincident increases. Rapid deposition increases started in 1297 (±30 s.d.) in the northern Antarctic Peninsula, consistent with the late 13th-century Māori settlement and New Zealand black carbon emissions of 36 (±21 2 s.d.) Gg y~(-1)during peak deposition in the 16th century. While charcoal and pollen records suggest earlier, climate-modulated burning in Tasmania and southern Patagonia~(6,7), deposition in Antarctica shows that black carbon emissions from burning in New Zealand dwarfed other preindustrial emissions in these regions during the past 2,000 years, providing clear evidence of large-scale environmental effects associated with early human activities across the remote Southern Hemisphere.
机译:新西兰被人类殖民殖民地殖民地的最后一个可居住的地方〜(1)。木炭记录表明,在13日至14世纪的毛利沉降之后殖民化之前野火罕见,但相关的生物质燃烧排放的精确时间和大小是未知的〜(1,3)。对原始南海海洋和抗野菌〜(4)进行光吸收黑色碳气溶胶浓度的影响。在这里,我们使用了一系列富裕的南极冰核记录,表明,在过去的两千年内,虽然黑碳沉积率在大陆南极洲稳定,但在过去的700年里,它们在北南极半岛上大约高出三倍。气溶胶造型〜(5)表明观察到的沉积可能只能从塔斯马尼亚,新西兰和巴塔哥尼亚州的40°S屏蔽火灾的增加的排放量增加到40°S暗示的火灾 - 但只有新西兰古地区记录表明重合增加。在北南极半岛1297(±30 SD)中开始的快速沉积增加,与峰值沉积期间的13世纪毛利沉降和新西兰黑碳排放为36(±21 2 SD)GG Y〜(-1)在16世纪。虽然木炭和花粉记录提出,但塔斯马尼亚和南塔哥代岛的气候调制燃烧〜(6,7),南极洲沉积表明,在新西兰燃烧的黑色碳排放在过去的2000年里,这些地区的其他预工业排放量越来越多,提供明确的证据表明与远程南半球的早期人类活动相关的大规模环境影响。

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  • 来源
    《Nature》 |2021年第7879期|82-85|共4页
  • 作者单位

    Division of Hydrologic Sciences Desert Research Institute;

    Division of Hydrologic Sciences Desert Research Institute;

    British Antarctic Survey Natural Environment Research Council;

    Department of Atmospheric and Climate Research Norwegian Institute for Air Research Kjeller;

    Department of Meteorology and Geophysics University of Vienna;

    School of Natural and Built Environment Queen's University Belfast;

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung;

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung;

    Norwegian Polar Institute Fram Centre;

    Department of Environmental Science and Management Portland State University;

    Division of Hydrologic Sciences Desert Research Institute;

    Department of Earth Sciences Montana State University;

    Research School of Earth Sciences Australian National University|ARC Centre of Excellence for Climate Extremes Australian National University|Australian Centre for Excellence in Antarctic Science Australian National University;

    School of Earth and Atmospheric Sciences Georgia Institute of Technology|School of Engineering and Applied Sciences Harvard University;

    Instituto Antártico Argentino Centro Regional de Investigaciones Cientifícas y Teconológicas;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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