Suppr超能文献

产甲烷古菌中由呋喃甲醇和二氧化碳形成N-羧甲基呋喃(氨基甲酸盐)的过程。自发反应的热力学和动力学

N-carboxymethanofuran (carbamate) formation from methanofuran and CO2 in methanogenic archaea. Thermodynamics and kinetics of the spontaneous reaction.

作者信息

Bartoschek S, Vorholt J A, Thauer R K, Geierstanger B H, Griesinger C

机构信息

Max-Planck-Institut für terrestrische Mikrobiologie and Laboratorium für Mikrobiologie, Fachbereich Biologie, Philipps-Universität, Marburg, Germany.

出版信息

Eur J Biochem. 2000 Jun;267(11):3130-8. doi: 10.1046/j.1432-1327.2000.01331.x.

Abstract

N-carboxymethanofuran (carbamate) formation from unprotonated methanofuran (MFR) and CO2 is the first reaction in the reduction of CO2 to methane in methanogenic archaea. The reaction proceeds spontaneously. We address here the question whether the rate of spontaneous carbamate formation is high enough to account for the observed rate of methanogenesis from CO2. The rates of carbamate formation (v1) and cleavage (v2) were determined under equilibrium conditions via 2D proton exchange NMR spectroscopy (EXSY). At pH 7.0 and 300 K the second order rate constant k1* of carbamate formation from 'MFR'(MFR + MFRH+) and 'CO2' (CO2 + H2CO3 + HCO3-+ CO32-) was found to be 7 M-1.s-1 (v1 = k1* ['MFR'] ['CO2']) while the pseudo first order rate constant k2* of carbamate cleavage was 12 s-1 (v2 = k2* [carbamate]). The equilibrium constant K* = k1*/k2* = [carbamate]/['MFR']['CO2'] was 0.6 M-1 at pH 7.0 corresponding to a free energy change DeltaG degrees ' of + 1.3 kJ.mol-1. The pH and temperature dependence of k1*, of k2* and of K* were determined. From the second order rate constant k1* it was calculated that under physiological conditions the rate of spontaneous carbamate formation is of the same order as the maximal rate of methane formation and as the rate of spontaneous CO2 formation from HCO3- in methanogenic archaea, the latter being important as CO2 is mainly present as HCO3- which has to be converted to CO2 before it can react with MFR. An enzyme catalyzed carbamate formation thus appears not to be required for methanogenesis from CO2. Consistent with this conclusion is our finding that the rate of carbamate formation was not enhanced by cell extracts of Methanosarcina barkeri and Methanobacterium thermoautotrophicum or by purified formylmethanofuran dehydrogenase which catalyzes the reduction of N-carboxymethanofuran to N-formylmethanofuran. From the concentrations of 'CO2' and of 'MFR' determined by 1D-NMR spectroscopy and the pKa of H2CO3 and of MFRH+ the concentrations of CO2 and of MFR were obtained, allowing to calculate k1 (v1 = k1 [MFR] [CO2]). The second order rate constant k1 was found to be approximately 1000 M-1 x s-1 at 300 K and pH values between 7.0 and 8. 0 which is in the order of k1 values determined for other carbamate forming reactions by stopped flow.

摘要

在产甲烷古菌中将二氧化碳还原为甲烷的过程中,未质子化的呋喃甲醇(MFR)与二氧化碳反应生成N - 羧甲基呋喃(氨基甲酸盐)是第一步反应。该反应自发进行。我们在此探讨自发形成氨基甲酸盐的速率是否足以解释观察到的由二氧化碳生成甲烷的速率。通过二维质子交换核磁共振光谱(EXSY)在平衡条件下测定了氨基甲酸盐形成(v1)和解离(v2)的速率。在pH 7.0和300 K时,由“MFR”(MFR + MFRH⁺)和“CO₂”(CO₂ + H₂CO₃ + HCO₃⁻ + CO₃²⁻)形成氨基甲酸盐的二级速率常数k1为7 M⁻¹·s⁻¹(v1 = k1[“MFR”][“CO₂”]),而氨基甲酸盐解离的准一级速率常数k2为12 s⁻¹(v2 = k2[氨基甲酸盐])。在pH 7.0时平衡常数K* = k1*/k2* = [氨基甲酸盐]/[“MFR”][“CO₂”]为0.6 M⁻¹,对应自由能变化ΔG°’为 + 1.3 kJ·mol⁻¹。测定了k1*、k2和K对pH和温度的依赖性。根据二级速率常数k1*计算得出,在生理条件下,自发形成氨基甲酸盐的速率与甲烷形成的最大速率以及产甲烷古菌中由HCO₃⁻自发形成CO₂的速率处于同一数量级,后者很重要,因为CO₂主要以HCO₃⁻形式存在,在与MFR反应之前必须转化为CO₂。因此,由二氧化碳生成甲烷似乎不需要酶催化形成氨基甲酸盐。与该结论一致的是我们的发现,巴氏甲烷八叠球菌和嗜热自养甲烷杆菌的细胞提取物或纯化的甲酰呋喃甲醇脱氢酶(催化N - 羧甲基呋喃还原为N - 甲酰呋喃甲醇)并未提高氨基甲酸盐的形成速率。通过一维核磁共振光谱测定的“CO₂”和“MFR”的浓度以及H₂CO₃和MFRH⁺的pKa,得到了CO₂和MFR的浓度,从而可以计算k1(v1 = k1[MFR][CO₂])。在300 K和pH值介于7.0和8.0之间时,二级速率常数k1约为1000 M⁻¹·s⁻¹,这与通过停流法测定的其他形成氨基甲酸盐反应的k1值处于同一数量级。

文献AI研究员

20分钟写一篇综述,助力文献阅读效率提升50倍。

立即体验

用中文搜PubMed

大模型驱动的PubMed中文搜索引擎

马上搜索

文档翻译

学术文献翻译模型,支持多种主流文档格式。

立即体验