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Geochemistry of reduced fluids from shallow cold vents hosting chemosynthetic communities (Comau Fjord, Chilean Patagonia 42 degrees S)

机译:来自拥有化学合成群落的浅冷通风口的还原液的地球化学特征(智利巴塔哥尼亚42度,科马峡湾)

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Reduced fluids from shallow-marine vents sustain chemosynthetic bacterial mats located at the base of the volcano Barranco Colorado in Comau Fjord (X-Huinay; 42 23.279'S, 72 27.635'W). We characterized the chemical environment in which these bacteria thrive. To this end, we analyzed CH4, Eii2s, 02, DIC, and stable isotopes (813C, 52H and 8180) and compared them with readings taken at a control station (which lacks evidence of fluid venting and mat-forming bacteria). In addition, CI'D measurements, chlorophyll-a, and nutrient analyses were performed. At depths of approximately 5-7 m, the water column exhibited a pycnocline that formed under the influence of fresh water discharges, especially during the summer season, which also affected the surface temperature. Bacterial mats and elemental sulfur flocs were observed in the vicinity of the vents (X-Huinay station), and higher concentrations of reduced compounds (CH4 and H2S) were found in the vent fluids, in particular at a depth of 36 m. No significant differences in the temperatures of vent and ambient waters were detected. The bottom water close to the vents possessed notably low concentrations of reduced compounds, indicating a rapid and large-quantity dilution of the chemicals from vents. The surface water featured light isotopic values of 82H and 180 due to the freshwater input from melting ice and precipitation. A linear mixing trend was observed between the freshwater (negative isotopic values) and the fjord bottom water (positive values) that was not influenced by vent fluid. This trend suggests that the venting water corresponds to the mixing among local meteoric water, spring water, and seawater. This result is relevant to understanding how freshwater and meteoric water influence the chemical composition of seawater and how this mixing could impact the marine biota in the vicinities of the vents. (C) 2014 Elsevier Ltd. All rights reserved.
机译:来自浅海排放口的减少的流体维持着位于科马峡湾Barranco Colorado火山底部的化学合成细菌垫(X-Huinay; 42 23.279'S,72 27.635'W)。我们表征了这些细菌在其中生长的化学环境。为此,我们分析了CH4,Eii2s,02,DIC和稳定同位素(813C,52H和8180),并将它们与在控制站(缺乏流体排放和形成垫层细菌的证据)的读数进行了比较。此外,还进行了CI'D测量,叶绿素-a和营养成分分析。在大约5-7 m的深度处,水柱显示出一条比浓可可碱,该比浓可可碱是在淡水排放的影响下形成的,尤其是在夏季,这也影响了地表温度。在排气孔附近(X-Huinay站)观察到细菌垫和元素硫絮状物,并且在排气液中发现了较高浓度的还原化合物(CH4和H2S),特别是在36 m的深度处。未检测到排放口和周围水温的显着差异。靠近排气孔的底部水具有极低的还原化合物浓度,这表明来自排气孔的化学物质迅速大量稀释。由于来自融冰和降水的淡水输入,地表水的轻同位素值为82H和180。在淡水(负同位素值)和峡湾底水(正值)之间观察到了线性混合趋势,不受排放流体的影响。这种趋势表明,排出的水对应于当地的大气,泉水和海水之间的混合。该结果与了解淡水和大气水如何影响海水的化学组成以及这种混合如何影响通风口附近的海洋生物群有关。 (C)2014 Elsevier Ltd.保留所有权利。

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  • 来源
    《Progress in Oceanography》 |2014年第decaptaa期|159-169|共11页
  • 作者单位

    Univ Catolica Norte, Dept Biol Marina, Coquimbo, Chile|CEAZA, La Serena, Chile;

    Univ Catolica Norte, Dept Biol Marina, Coquimbo, Chile|CEAZA, La Serena, Chile;

    Univ Catolica Norte, Dept Biol Marina, Coquimbo, Chile;

    Univ Catolica Norte, Dept Biol Marina, Coquimbo, Chile;

    Univ Erlangen Nurnberg, Inst Geog, D-91054 Erlangen, Germany|Univ Munich, GeoBio Ctr, Munich, Germany|Univ Munich, Dept Geo & Umweltwissensch, Munich, Germany;

    Univ Catolica Norte, Dept Biol Marina, Coquimbo, Chile;

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