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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Carbon isotopic fractionation by Archaeans and other thermophilic prokaryotes
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Carbon isotopic fractionation by Archaeans and other thermophilic prokaryotes

机译:古细菌和其他嗜热原核生物的碳同位素分馏

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This study of carbon isotopic fractionation in a wide array of 21 phylogenetically diverse microbial species provides an opportunity to correlate carbon isotopic fractionations with a biochemical pathway. These carbon isotopic fractionation experiments included two members of the Aquificales and two members of the Thermoproteales using the reductive TCA cycle, three members of the Sulfolobales using the 3-hydroxypropionate cycle, as well as three Archaeoglobales and seven methanogens using the acetyl-CoA pathway. In these experiments, microorganisms using the reductive tricarboxylic acid cycle (with 6 values between 2.0 and 5.5parts per thousand) and the 3-hydroxypropionate cycle (with epsilon values between 0.2 and 3.6parts per thousand) demonstrated significantly less carbon isotopic fractionation than methanogens using the acetyl-CoA pathway. The results reported here for the acetyl-CoA pathway-utilizing microbes, however, vary over a remarkably wide range with epsilon values of 2.7 to 8.0parts per thousand for the Archaeoglobales and epsilon values of 4.8 to 26.7parts per thousand for the methanogens. The magnitude of carbon isotopic fractionation observed in species of Methanococcus were related to the particular growth status that had been attained by the various cultures, with increasing isotopic fractionation as growth proceeded. (C) 2002 Elsevier Science Ltd. All rights reserved. [References: 40]
机译:这项对21种系统发育多样的微生物物种中碳同位素分馏的研究为将碳同位素分馏与生化途径相关提供了机会。这些碳同位素分馏实验包括使用还原性TCA循环的两个Aquificales成员和两个热蛋白酶的成员,使用3-羟基丙酸酯循环的三个Sulfolobales成员,以及使用乙酰辅酶AA途径的三个Archaeoglobales和七个产甲烷菌。在这些实验中,使用还原性三羧酸循环(6个值在千分之二至5.5之间)和3-羟基丙酸酯循环(ε值在千分之0.2至3.6之间)的微生物表现出的碳同位素分馏比使用甲烷化的产甲烷菌明显少。乙酰辅酶A途径。然而,此处报道的利用乙酰辅酶A途径的微生物的结果变化范围非常大,古生细菌的ε值为2.7至8.0千分之几,产甲烷菌的ε值为4.8至26.7千分之几。在甲烷球菌物种中观察到的碳同位素分馏的幅度与各种培养物所达到的特定生长状况有关,随着同位素的分馏随着生长的进行而增加。 (C)2002 Elsevier ScienceLtd。保留所有权利。 [参考:40]

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