Voordouw Gerrit
Max Planck Institute for Marine Microbiology, D-28359 Bremen, Germany.
J Bacteriol. 2002 Nov;184(21):5903-11. doi: 10.1128/JB.184.21.5903-5911.2002.
Sulfate-reducing bacteria, like Desulfovibrio vulgaris Hildenborough, use the reduction of sulfate as a sink for electrons liberated in oxidation reactions of organic substrates. The rate of the latter exceeds that of sulfate reduction at the onset of growth, causing a temporary accumulation of hydrogen and other fermentation products (the hydrogen or fermentation burst). In addition to hydrogen, D. vulgaris was found to produce significant amounts of carbon monoxide during the fermentation burst. With excess sulfate, the hyd mutant (lacking periplasmic Fe-only hydrogenase) and hmc mutant (lacking the membrane-bound, electron-transporting Hmc complex) strains produced increased amounts of hydrogen from lactate and formate compared to wild-type D. vulgaris during the fermentation burst. Both hydrogen and CO were produced from pyruvate, with the hyd mutant producing the largest transient amounts of CO. When grown with lactate and excess sulfate, the hyd mutant also exhibited a temporary pause in sulfate reduction at the start of stationary phase, resulting in production of 600 ppm of headspace hydrogen and 6,000 ppm of CO, which disappeared when sulfate reduction resumed. Cultures with an excess of the organic electron donor showed production of large amounts of hydrogen, but no CO, from lactate. Pyruvate fermentation was diverse, with the hmc mutant producing 75,000 ppm of hydrogen, the hyd mutant producing 4,000 ppm of CO, and the wild-type strain producing no significant amount of either as a fermentation end product. The wild type was most active in transient production of an organic acid intermediate, tentatively identified as fumarate, indicating increased formation of organic fermentation end products in the wild-type strain. These results suggest that alternative routes for pyruvate fermentation resulting in production of hydrogen or CO exist in D. vulgaris. The CO produced can be reoxidized through a CO dehydrogenase, the presence of which is indicated in the genome sequence.
硫酸盐还原菌,如希登伯勒脱硫弧菌,利用硫酸盐的还原作为有机底物氧化反应中释放电子的归宿。在生长开始时,有机底物氧化反应的速率超过硫酸盐还原的速率,导致氢气和其他发酵产物暂时积累(氢气或发酵爆发)。除了氢气,还发现希登伯勒脱硫弧菌在发酵爆发期间会产生大量一氧化碳。在有过量硫酸盐的情况下,与野生型希登伯勒脱硫弧菌相比,hyd突变体(缺乏周质仅含铁氢化酶)和hmc突变体(缺乏膜结合的电子传递Hmc复合物)菌株在发酵爆发期间从乳酸盐和甲酸盐中产生的氢气量增加。氢气和一氧化碳都由丙酮酸产生,hyd突变体产生的一氧化碳瞬时量最大。当以乳酸盐和过量硫酸盐培养时,hyd突变体在稳定期开始时也表现出硫酸盐还原的暂时停顿,导致产生600 ppm的顶空氢气和6000 ppm的一氧化碳,当硫酸盐还原恢复时这些气体消失。含有过量有机电子供体的培养物从乳酸盐中产生大量氢气,但不产生一氧化碳。丙酮酸发酵情况多样,hmc突变体产生75000 ppm的氢气,hyd突变体产生4000 ppm的一氧化碳,野生型菌株作为发酵终产物均未产生大量的这两种气体。野生型在一种暂定为富马酸的有机酸中间体的瞬时产生中最为活跃,这表明野生型菌株中有机发酵终产物的形成增加。这些结果表明,希登伯勒脱硫弧菌中存在导致产生氢气或一氧化碳的丙酮酸发酵替代途径。产生的一氧化碳可以通过一氧化碳脱氢酶重新氧化,基因组序列中显示了该酶的存在。