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Elemental composition and bacterial occurrence in sediment samples on two sides of Broggerhalvoya, Svalbard

机译:斯瓦尔巴特群岛Broggerhalvoya两侧的沉积物样品中的元素组成和细菌发生

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摘要

The present study was conducted to determine the elemental concentration and bacterial presence in the ocean on the two sides of Broggerhalvoya, a peninsula in Svalbard. Sediments from 25 different locations were collected and subjected to elemental analysis using inductively coupled plasma mass spectrometry (ICPMS). In total, 21 elements were analysed. The elements in their decreasing order of concentrations on the Kongsfjorden side of Broggerhalvoya were Fe> Mn> Ba > V > Zn > Sr > Rb > Cr > Li > Ni > As > Pb > Cu > Co > Cs > Ag > Be > U> Bi > Tl > Cd while that for Forlandsendet side of Broggerhalvoya they were Fe > Ba > Mn > V> Sr > Zn > Rb > Cr > Li > Ni > Pb > Cu > As > Co > Cs > Be > U> Tl > Bi > Cd. On the other hand, at a coastal outcrop, elements in their decreasing order of concentration were Fe > Mn > Cr > Sr > Ba > Rb > Cr > Zn > V > Rb > Ni > Li > Co > Cu > As > Pb > Cs > Be > Cd > Tl > U > Bi. AMS dates confirmed the age of outcrop sediment to be 12,496 to 42,500 BP. The crustal enrichment factor calculated for all the elements with reference to Fe values, demonstrates that the elements have derived from a crustal source. Total bacterial counts ranged from 3.30 x 10(5) to 3.02 x 10(6) per gm soil sediment. Culturable bacterial counts in these sediments were between 2.00 x 10(2) to 2.09 x 10(5) CFU's per gm. Overall comparison showed high Fe and Mn concentrations around Broggerhalvoya, due to the presence of specific bacteria which play key roles in metal cycling and carry out biogeochemical transformations.
机译:进行本研究是为了确定斯瓦尔巴群岛的半岛Broggerhalvoya两侧海洋中的元素浓度和细菌的存在。收集来自25个不同位置的沉积物,并使用感应耦合等离子体质谱(ICPMS)进行元素分析。总共分析了21个元素。在Broggerhalvoya的Kongsfjorden侧,浓度从高到低依次为Fe> Mn> Ba> V> Zn> Sr> Rb> Cr> Li> Ni> As> Pb> Cu> Co> Cs> Ag> Be> U > Bi> Tl> Cd,而对于Broggerhalvoya的Forlandendet侧则为Fe> Ba> Mn> V> Sr> Zn> Rb> Cr> Li> Ni> Pb> Cu> As> Co> Cs> Be> U> Tl > Bi> Cd。另一方面,在沿海露头,元素浓度从高到低依次为:Fe> Mn> Cr> Sr> Ba> Rb> Cr> Zn> V> Rb> Ni> Li> Co> Cu> As> Pb> Cs> Be> Cd> Tl> U> Bi。 AMS日期证实露头沉积物的年龄为12,496至42,500 BP。参照Fe值计算出的所有元素的地壳富集系数,表明这些元素均来自地壳来源。每克土壤沉积物中细菌总数为3.30 x 10(5)至3.02 x 10(6)。这些沉积物中可培养的细菌数为每克2.00 x 10(2)至2.09 x 10(5)CFU。总体比较显示,由于特定细菌的存在,其在Broggerhalvoya附近的Fe和Mn浓度较高,这些细菌在金属循环和进行生物地球化学转化中起关键作用。

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  • 来源
    《Polar Record》 |2015年第6期|680-691|共12页
  • 作者单位

    Natl Ctr Antarctic & Ocean Res, Vasco 403804, Goa, India;

    Natl Ctr Antarctic & Ocean Res, Vasco 403804, Goa, India;

    Natl Res Ctr Grapes, Pune 412307, Maharashtra, India;

    Natl Res Ctr Grapes, Pune 412307, Maharashtra, India;

    Natl Res Ctr Grapes, Pune 412307, Maharashtra, India;

  • 收录信息 美国《科学引文索引》(SCI);
  • 原文格式 PDF
  • 正文语种 eng
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