首页> 外文期刊>The Journal of Foraminiferal Research >POLLUTION MONITORING IN TWO NORTH AMERICAN ESTUARIES: HISTORICAL RECONSTRUCTIONS USING BENTHIC FORAMINIFERA
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POLLUTION MONITORING IN TWO NORTH AMERICAN ESTUARIES: HISTORICAL RECONSTRUCTIONS USING BENTHIC FORAMINIFERA

机译:两种北美河口的污染监测:使用有孔有孔菌的历史重建

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摘要

Both surface and core studies from two highly impacted estuaries (New Bedford Harbor, Massachusetts, USA and Halifax Harbour, Nova Scotia, Canada) were carried out to determine if benthic foraminifera could be used to detect changes through time in these areas. New Bedford Harbor is in a highly industrialized area that has undergone severe environmental stresses from a variety of sources for almost 400 years, and has been declared an U.S. Environmental Protection Agency (EPA) Superfund site (i.e., a site so impacted that a special EPA fund is set up to clean it up in designated time frame). Halifax Harbour has been subjected mostly to domestic pollution (i.e., organic carbon produced by human wastes), rather than industrial (chemical) pollution since the founding of the city in 1749. Although many geochemical studies have been done in both estuaries, there are few baseline data on the biota. In this paper we use benthic foraminiferal assemblages retrieved from sediment cores to reconstruct biotic changes of the recent past. It is then possible to correlate faunal changes with already known geochemical parameters. The character of the pollution has changed in New Bedford Harbor as remediation efforts have taken hold. This change was detected with the foraminifera. One outcome is that deformities among one species, Haynesina orbiculare, appear to occur simultaneously with high polychlorinated biphenyls (PCB’s) in the sediments. In Halifax Harbour, where the largest impact is due to high organic input from domestic sources, species tolerant of low-oxygen conditions are most prominent at present. Core studies show that prior to the rapid growth of Halifax (in the 1960s) the organic input was much lower than at present. The higher input of organic carbon (OC) at present is indicated by foraminiferal species tolerant of high OC in cores since 1960, generally those with agglutinated as opposed to calcareous tests. We define industrial vs. OC pollution in sediments using foraminifera as proxies, and further, the environmental history is accurately depicted without original baseline data. Data from these two estuaries can be compared to other sites where degradation may be in different stages, which can be assessed by looking at foraminiferal faunas in those areas.
机译:对两个受到严重影响的河口(美国马萨诸塞州新贝德福德港和加拿大新斯科舍省哈利法克斯港)进行了表面和核心研究,以确定底栖生物 > 有孔虫可以用来检测这些地区随时间的变化。新贝德福德港位于高度工业化的地区,由于各种来源遭受了严重的环境压力,已有近400年的历史,并且已被宣布为 美国环境保护署(EPA)超级基金网站 (即,受到如此影响以至于在指定的时间范围内设立了EPA特殊基金 的网站)。自哈利法克斯港(Halifax Harbour)以来,主要受到家庭污染(例如,人类废物产生的有机碳)的污染,而不是工业(化学)污染。该城市于1749年成立。尽管在两个河口都进行了许多 地球化学研究,但 有关该生物群的基线数据却很少。在本文中,我们使用从沉积物核心获取的底栖有孔虫组合重建最近的生物变化。然后可以将 的动物变化与已知的地球化学参数相关联。由于采取了整治措施,新贝德福德港的污染 发生了变化。使用有孔虫 检测到此变化。一个结果是, 物种之一的Haynesina orbiculare中的畸变似乎与沉积物中的高多氯联苯(PCB's)同时发生。 在哈利法克斯在港口中,最大的影响是来自国内的高有机输入量,目前,耐低氧条件下的物种耐受性最为突出。核心研究表明 在哈利法克斯(Halifax)快速增长之前(在1960年代), 的有机物投入远低于目前。自1960年以来,有孔虫对有机碳中高OC的耐受性表明,目前有机碳(OC)的输入 较高,通常这些 而不是钙质测试。我们使用有孔虫 作为代理来定义沉积物中的工业污染与OC污染,此外,没有原始基准数据即可准确地描述环境历史。可以将这两个 河口的数据与其他可能在不同阶段退化的站点进行比较,可以通过查看该县有孔虫类动物来对其进行评估。这些区域。

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  • 来源
    《The Journal of Foraminiferal Research》 |2005年第1期|00000065-00000082|共18页
  • 作者单位

    Centre for Environmental and Marine Geology, Dalhousie University, Halifax, Nova Scotia B3H3J5, CANADA.;

    Centre for Environmental and Marine Geology, Dalhousie University, Halifax, Nova Scotia B3H3J5, CANADA.;

    Centre for Environmental and Marine Geology, Dalhousie University, Halifax, Nova Scotia B3H3J5, CANADA.;

    Centre for Environmental and Marine Geology, Dalhousie University, Halifax, Nova Scotia B3H3J5, CANADA.;

    U.S. Environmental Protection Agency, 27 Tarzwell Drive, Narragansett, RI 02882, USA.;

    U.S. Environmental Protection Agency, 27 Tarzwell Drive, Narragansett, RI 02882, USA.;

    Centro Studio Geodinamica Alpina del C.N.R., Dipartimento di Mineralogia e Petrologia, Universita’ di Padova, C.so Garibaldi 37, 35137, Padova, ITALY.;

    Department of Geology, Erlangen University, Erlangen, GERMANY.;

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