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Energetics of potential heterotrophic metabolisms in the marine hydrothermal system of Vulcano Island, Italy

机译:意大利武尔卡诺岛海洋热液系统中潜在异养代谢的能量学

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摘要

Values of overall Gibbs free energy of 144 organic oxidation (respiration) and disproportionation (fermentation) reactions are calculated at the temperatures and chemical compositions that exist in nine submarine vents, sediment seeps and geothermal wells in the hydrothermal system of Vulcano Island, Italy. The organic compounds considered here include four carboxylic acids (formic, acetic, propanoic and lactic), two C-5 aldoses (arabinose and xylose), three C-6 aldoses (galactose, glucose and mannose), and 15 protein-forming amino acids (Ala, Arg, Asp, Glu, Gly, His, Ile, Leu, Lys, Met, Phe, Ser, Thr, Tyr, and Val). Oxidation of these compounds is coupled to five redox pairs: O-2/H2O, SO42-/H2S, S-0/H2S, NO3-/NH4+ and Fe3O4/Fe2+. Energy yields from potential respiration reactions range from 6 to 118 kJ/mol of electrons transferred and show systematic behavior with respect to the terminal electron acceptor. Overall, respiration with O-2 yields the most energy (98-118 kJ/mol e(-)), followed by reactions with NO3- (53-86 kJ/mol e(-)), magnetite (29-91 kJ/mol e-), S-0 (11-33 kJ/mol e(-)) and SO42- (6-34 kJ/mol e(-)). Energy yields show little correlation with organic compound family, but are correlated with fluid pH. Variability in energy yields across the nine sites is greatest for Fe(III) reduction and is primarily influenced by pH and the activity of Fe2+. In addition to the potential respiration reactions, the energetics of 24 potential fermentation reactions are also calculated. As expected, fermentation reactions generally yield much less energy than respiration. Normalized to the number of moles of carbon transferred, fermentation yields-8 to 71 kJ/mol C, compared with 16 to 531 kJ/mol C for respiration reactions. All respiration and fermentation reactions, except for methionine (Met) fermentation, are exergonic under the in situ hydrothermal conditions and represent a plethora of potential metabolisms for Vulcano's diverse thermophilic heterotrophs. (c) 2006 Elsevier Inc. All rights reserved.
机译:在意大利Vulcano岛热液系统中9个海底通风口,沉积物渗漏和地热井中存在的温度和化学组成下,计算了144次有机氧化(呼吸)和歧化(发酵)反应的吉布斯总自由能值。这里考虑的有机化合物包括四种羧酸(甲酸,乙酸,丙酸和乳酸),两种C-5醛糖(阿拉伯糖和木糖),三种C-6醛糖(半乳糖,葡萄糖和甘露糖)和15种蛋白质形成氨基酸(Ala,Arg,Asp,Glu,Gly,His,Ile,Leu,Lys,Met,Phe,Ser,Thr,Tyr和Val)。这些化合物的氧化与五个氧化还原对耦合:O-2 / H2O,SO42- / H2S,S-0 / H2S,NO3- / NH4 +和Fe3O4 / Fe2 +。潜在的呼吸反应产生的能量为6至118 kJ / mol转移的电子,相对于末端电子受体显示出系统的行为。总体而言,以O-2进行的呼吸能产生的能量最多(98-118 kJ / mol e(-)),其次是与NO3-(53-86 kJ / mol e(-)),磁铁矿(29-91 kJ / mol e-),S-0(11-33 kJ / mol e(-))和SO42-(6-34 kJ / mol e(-))。能量产量与有机化合物家族关系不大,但与流体pH值相关。对于Fe(III)还原而言,这9个位点的能量产量变化最大,并且主要受pH和Fe2 +活性的影响。除潜在的呼吸反应外,还计算了24个潜在的发酵反应的能量。不出所料,发酵反应产生的能量通常比呼吸少得多。归一化为转移的碳的摩尔数,发酵的产量为8至71 kJ / mol C,而呼吸反应的产率为16至531 kJ / molC。除蛋氨酸(Met)发酵外,所有呼吸和发酵反应在原位水热条件下都是能动的,并且代表了Vulcano各种嗜热异养菌的大量潜在代谢。 (c)2006 Elsevier Inc.保留所有权利。

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