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首页> 外文期刊>Antarctic science >Aspects of the biogeochemistry of sulphur in glacial melt water ponds on the McMurdo Ice Shelf, Antarctica
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Aspects of the biogeochemistry of sulphur in glacial melt water ponds on the McMurdo Ice Shelf, Antarctica

机译:南极麦克默多冰架上冰川融化水池中硫的生物地球化学特征

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The distribution of dimethylsulphide (DMS), together with the precursor dimethylsulphonio-propionate (DMSP) and the oxidation product dimethylsulphoxide (DMSO), was measured in melt waters on the McMurdo Ice Shelf in the immediate vicinity of Bratina Island. Conductivity in these sulphate dominated ponds was extremely variable, ranging from 0.106–52.3 mS cm?1. Similarly, chlorophyll a concentrations in the pond waters (1–150 μg 1?1) and mats (1.4–33 μg cm?2) differed considerably. The biomass was dominated by benthic felts of phototrophic cyanobacteria, which might act as a source of biogenic sulphur compounds in the ponds. The mean (and ranges) of concentrations of dissolved sulphur compounds (nmol 1?1) were: CS2 0.16 (
机译:在Bratina岛附近的McMurdo冰架上的熔融水中测量了二甲基亚砜(DMS)的分布,以及前体丙二酸二甲基亚砜酯(DMSP)和氧化产物二甲基亚砜(DMSO)的分布。这些以硫酸盐为主的池塘的电导率变化很大,范围为0.106-52.3 mS cm?1。同样,池塘水域(1-150μg1?1)和垫子(1.4-33μgcm?2)中叶绿素a的浓度也有很大差异。生物量主要由光养性蓝细菌的底栖毛毡主导,这些毛毡可能是池塘中生物硫化合物的来源。溶解的硫化合物的浓度(nmol 1?1)的平均值(和范围)为:CS2 0.16(

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