首页> 外文学位 >Biogeochemical cycling of arsenic in the marine shallow-water hydrothermal system of Tutum Bay, Ambitle Island, Papua New Guinea.
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Biogeochemical cycling of arsenic in the marine shallow-water hydrothermal system of Tutum Bay, Ambitle Island, Papua New Guinea.

机译:巴布亚新几内亚安特比尔岛图坦湾海洋浅水热液系统中砷的生物地球化学循环。

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摘要

The marine shallow-water hydrothermal vent system of Tutum Bay, Ambitle Island, PNG discharges hot, acidic, arsenic-rich, chemically reduced fluid into cool, alkaline, oxygenated seawater. Gradients in temperature, pH, total arsenic (TAs) and arsenic species, among others, are established as the two aqueous phases mix.;Hydrous ferric oxides (HFO) are precipitated around focused venting, and coat the surrounding sediments visibly to 150 m away. HFO coatings, mechanical transport and weathering of volcanoclastic sediments, as well as dissolution of carbonate sediments nearer to venting, combine to alter sediment chemistry substantially.;Tutum Bay surface sediments have a mean As concentration of 527 mg/kg. Arsenic at concentrations up to 50 mg/kg (mean = 19.7 mg/kg) was extracted from the easily extractable fraction of surface sediments. Arsenic is elevated in surface seawaters (8 mug/L) directly over hydrothermal vents, and As(III) is substantially enriched in both surface and bottom seawater throughout Tutum Bay. Surprisingly, aqueous As(V) far exceeded aqueous As(III) at almost all distances and depths investigated for Tutum Bay pore waters. These data indicate that throughout Tutum Bay, chemical disequilibria among As species provides potential metabolic energy for arsenite oxidizing and arsenate reducing microorganisms, and that As is bioavailable from two major environments: (1) easily-exchangeable As from surface sediments, and (2) in surface seawaters, which may allow for biological uptake and trophic transfer through plankton.;The soft coral Clavularia sp., the calcareous algae Halimeda sp., and the tunicate Polycarpa sp. were collected and analyzed to assess bioaccumulation and biotransformation patterns. All organisms collected from the hydrothermal area displayed higher (2 to 20 times) TAs. Concentrations of arsenic species in their tissues were also elevated compared to the control site. Increased concentrations were observed near focused venting. Distinct arsenic speciation patterns in Clavularia and Polycarpa collected from near hydrothermal venting suggest rapid methylation/detoxification of arsenic, with enhanced bioaccumulation of dimethylarsenate and arsenobetaine as products of the organisms metabolic pathways. Elevated concentrations of As(III) in Halimeda suggest that this organism is not as efficient at methylating inorganic arsenic. The presence of arsenobetaine in Halimeda suggests the biomethylation pathway for calcareous algae is different from commonly studied seaweeds.
机译:PNG Ambitle岛Tutum湾的海洋浅水热液排放系统将热的,酸性的,富含砷的,化学还原的流体排入冷的碱性氧化的海水中。在两个水相的混合中建立温度,pH,总砷(TAs)和砷种类等的梯度。;集中排气口附近沉淀出三水氧化铁(HFO),并在150 m处明显覆盖周围的沉积物。 HFO涂层,火山碎屑沉积物的机械输送和风化以及更接近排放的碳酸盐沉积物的溶解,大大改变了沉积物的化学性质。图特姆湾表面沉积物的平均As浓度为527 mg / kg。从表面沉积物中易于提取的部分中提取了最高浓度为50 mg / kg(平均值= 19.7 mg / kg)的砷。直接在热液喷口上方的表层海水(8杯/升)中砷含量升高,整个图腾湾的表层和底层海水中砷(III)都大量富集。出乎意料的是,在图坦湾孔隙水研究的几乎所有距离和深度下,As(V)水溶液都远远超过了As(III)水溶液。这些数据表明,在整个图坦湾,As物种之间的化学不平衡为砷氧化和还原砷的微生物提供了潜在的代谢能量,并且As在两个主要环境中都可生物利用:(1)易于从表面沉积物中交换的As,以及(2)地表海水中的磷,可能允许通过浮游生物进行生物吸收和营养转移;软珊瑚Clavularia sp。,钙质藻类Halimeda sp。和被覆膜Polycarpa sp.。收集并分析以评估生物积累和生物转化模式。从热液区收集的所有生物均显示出较高的TA(2至20倍)。与对照部位相比,其组织中砷物质的浓度也升高。在集中通风处附近观察到浓度增加。从近水热通风中收集的锁骨和Poly果中不同的砷形态模式表明,砷快速甲基化/解毒,并增加了砷酸二甲酯和砷甜菜碱作为生物体代谢途径的产物的生物积累。 Halimeda中As(III)浓度升高表明该生物体不能有效地甲基化无机砷。 Halimeda中存在砷代甜菜碱,这表明钙质藻类的生物甲基化途径不同于通常研究的海藻。

著录项

  • 作者

    Price, Roy E.;

  • 作者单位

    University of South Florida.;

  • 授予单位 University of South Florida.;
  • 学科 Geochemistry.
  • 学位 Ph.D.
  • 年度 2008
  • 页码 159 p.
  • 总页数 159
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;
  • 关键词

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