Abstract Arsenic bioaccumulation and biotransformation in deep-sea hydrothermal vent organisms from the PACMANUS hydrothermal field, Manus Basin, Papua New Guinea
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Arsenic bioaccumulation and biotransformation in deep-sea hydrothermal vent organisms from the PACMANUS hydrothermal field, Manus Basin, Papua New Guinea

机译:巴布亚新几内亚马努斯盆地PACMANUS热液场中深海热液喷口生物中的砷生物富集和生物转化

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Abstract Hydrothermal vents are often enriched in arsenic, and organisms living in these environments may accumulate high concentrations of this and other trace elements. However, very little research to date has focused on understanding arsenic bioaccumulation and biotransformation in marine organisms at deep-sea vent areas; none to date have focused organisms from back-arc spreading centers. We present for the first time concentration and speciation data for As in vent biota from several hydrothermal vent fields in the eastern Manus basin, a back-arc basin vent field located in the Bismark Sea, western Pacific Ocean. The gastropods Alviniconcha hessleri and Ifremeria nautilei, and the mussel Bathymodiolus manusensis were collected from diffuse venting areas where pH was slightly lower (6.2–6.8), and temperature (26.8–10.5°C) and arsenic concentrations (169.5–44.0nM) were higher than seawater. In the tissues of these organisms, the highest total measured As concentrations were in the gills of A. hessleri (5580mgkg−1), with 721mgkg−1 and 43mgkg−1 in digestive gland and muscle, respectively. I. nautilei contained 118mgkg−1 in the gill, 108mgkg−1 in the digestive gland and 22mgkg−1 in the muscle. B. manusensis contained 15.7mgkg−1 in the digestive gland, followed by 9.8mgkg-1 and 4.5mgkg-1 in its gill and muscle tissue, respectively. We interpret the decreasing overall total concentrations in each organism as a function of distance from the source of hydrothermally derived As. The high concentration of arsenic in A. hessleri gills may be associated with elemental sulfur known to occur in this organism as a result of symbiotic microorganisms. Arsenic extracted from freeze-dried A. hessleri tissue was dominated by AsIII and AsV in the digestive gland (82% and 16%, respectively) and gills (97% AsIII, 2.3% AsV), with only 1.8% and 0.2% arsenobetaine (As-Bet) in the digestive gland and gills, respectively. However, the muscle contained substantial amounts of As-Bet (42% As-Bet compared to 48% AsIII and 10% AsV), suggesting As-Bet is a metabolite. Trace arsenosugar (SO4-sug) was observed in digestive gland and gills only. The other snail, I. nautilei, was also dominated by AsIII and AsV in digestive glands (82, 10%) and gills (80, 10%), with 6–9% As-Bet, but its muscle contained 62% As-Bet and 32% AsIII, with 7% trimethylarsoniopropionate (TMAP). Trace dimethylarsinic acid (DMAV) was observed in its gills, and trace TMAP and arsenocholine (AC) was observed in digestive glands. The mussel B. manusensis was dominated by As-Bet in all three tissue types. Digestive gland and gills contained ~22% AsIII, 5–10% AsV, 20–25% DMAV, along with some TMAP and tetramethylarsonium ion (TETRA). However, the muscle contained significantly more As-Bet (91.6%), with the only other species being AsIII (8.4%). Unfortunately, as is often the case in bioaccumulation and biotransformation studies, extraction efficiencies were low, limiting any rigorous interpretation of arsenic biotransformation patterns. Through process of elimination, we suggest that arsenosugars may be synthesized by H2S-oxidizing chemotrophic microbial mats, ultimately leading to the syntheses of As-Bet within vent organisms. However, because As-sugs rarely occur in deep-sea vent organisms, As-Bet, as well as TMAP, AC, and TETRA could also potentially be synthesized directly by the “Edmonds” pathway, the proposed arseno-analog to amino acid formation, without the necessity for arsenosugar formation as an intermediate. Future research should endeavor for more comprehensive extraction of organoarsenicals. Highlights The deep-sea vent gastropods A. hessleri and I. nautilie and the mussel B. manusensis contained up to 6344, 248, and 30mgkg−1 As, respectively. Inogranic As and arsenobetain (As-Bet) were the dominant species, with trace SO4-sug only found in A. hessleri. Trace TMAP, AC, and Tetra were found in the other organisms. Several hypotheses are proposed for biosynthesis of As-sug and As-Bet in deep-sea vent organisms. Future research on As bioaccumulation in deep-sea vent biota must consider improved method for total extraction.
机译: 摘要 水热喷口通常富含砷,生活在这些环境中的生物可能会富集这种和其他微量元素。但是,迄今为止,很少有研究集中在了解深海通风区海洋生物中砷的生物富集和生物转化。迄今为止,还没有人将重点放在弧后扩散中心。我们首次展示了来自东部Manus盆地几个热液喷口区域的喷口生物区中As的浓度和形态数据,该区域位于西太平洋比斯马克海的后弧盆地喷口区域。从弥散体中收集腹足纲动物 Alviniconcha hessleri Nautilei ,贻贝 Bathymodiolus manusensis 。 pH值稍低(6.2–6.8),温度(26.8–10.5 °C)和砷浓度(169.5–44.0 nM)高于海水。在这些生物的组织中,测得的最高总砷浓度在 A the中。 hessleri (5580 mg kg − 1 ),其中包含721 mg kg − 1 和43 < ce:hsp sp =“ 0.25” /> mg kg -1 分别在消化腺和肌肉中。 I。鹦鹉螺包含118 mg kg − 1 在the中的108 mg kg -1 消化腺和肌肉中的22 mg kg -1 B。 manusensis 包含15.7 mg kg − 1 在消化腺中,然后是9.8 mg kg - 1和4.5 mg kg - 1组织。我们将每个生物体中总体总浓度的下降解释为距水热衍生砷源的距离的函数。 A中高浓度的砷。 s可能与共生微生物在该生物体中存在的元素硫有关。从冷冻干燥的 A中提取的砷。 hessleri 组织中,As III 和As V 消化腺(分别为82%和16%)和g(97%As III ,2.3%As V < / ce:sup>),在消化腺和g中分别只有1.8%和0.2%的砷甜菜碱(As-Bet)。但是,肌肉中含有大量的As-Bet(42%的As-Bet与48%的As III 和10%的As V ),表明As-Bet是一种代谢产物。仅在消化腺和g中观察到微量砷糖(SO4-sug)。另一只蜗牛 I。鹦鹉螺也被As III 和As V 所控制消化腺(82%,10%)和g(80%,10%),As-Bet占6-9%,但其肌肉中As-Bet占62%,As-ce占32% III ,并添加7%的三甲基ar丙酸(TMAP)。在其g中观察到痕量的二甲基砷酸(DMA V ),在消化腺中观察到痕量的TMAP和砷胆碱(AC)。贻贝 B。三种组织类型中,Manusensis 均以As-Bet为主。消化腺和g含〜22%As III ,5-10%As V , 20-25%的DMA V ,以及一些TMAP和四甲基ar离子(TETRA)。但是,肌肉中的As-Bet含量明显更高(91.6%),唯一的其他物种是As III (8.4%)。不幸的是,正如生物富集和生物转化研究中经常发生的那样,提取效率很低,限制了对砷生物转化模式的任何严格解释。通过消除过程,我们建议可以通过H 2 S-氧化化营养微生物垫合成砷糖,最终导致发泄生物体内As-Bet的合成。 。但是,由于在深海喷口生物中很少出现As-sug,因此也可能通过“ Edmonds”途径直接合成As-Bet以及TMAP,AC和TETRA。,拟议的arseno-analog氨基酸形成,而没有需要arseno糖形成作为中间体。未来的研究应努力更全面地提取有机砷。 突出显示 The深海腹足纲动物 hessleri I。鹦鹉螺和贻贝 B 。 manusensis最多包含6344、248和30 mg kg -1 分别为。 A中发现了痕量SO4-糖。 hessleri 。在其他生物中也发现了痕量的TMAP,AC和Tetra。 在深海喷口生物中,有人提出了关于As-sug和As-Bet生物合成的假说。 深海砷生物富集的未来研究发泄生物群必须考虑改进总提取方法。

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