Visscher P T, Gritzer R F, Leadbetter E R
Department of Marine Sciences, and Department of Molecular and Cell Biology, University of Connecticut, Groton, Connecticut 06340, USA.
Appl Environ Microbiol. 1999 Aug;65(8):3272-8. doi: 10.1128/AEM.65.8.3272-3278.1999.
Several low-molecular-weight sulfonates were added to microbial mat slurries to investigate their effects on sulfate reduction. Instantaneous production of sulfide occurred after taurine and cysteate were added to all of the microbial mats tested. The rates of production in the presence of taurine and cysteate were 35 and 24 microM HS(-) h(-1) in a stromatolite mat, 38 and 36 microM HS(-) h(-1) in a salt pond mat, and 27 and 18 microM HS(-) h(-1) in a salt marsh mat, respectively. The traditionally used substrates lactate and acetate stimulated the rate of sulfide production 3 to 10 times more than taurine and cysteate stimulated the rate of sulfide production in all mats, but when ethanol, glycolate, and glutamate were added to stromatolite mat slurries, the resulting increases were similar to the increases observed with taurine and cysteate. Isethionate, sulfosuccinate, and sulfobenzoate were tested only with the stromatolite mat slurry, and these compounds had much smaller effects on sulfide production. Addition of molybdate resulted in a greater inhibitory effect on acetate and lactate utilization than on sulfonate use, suggesting that different metabolic pathways were involved. In all of the mats tested taurine and cysteate were present in the pore water at nanomolar to micromolar concentrations. An enrichment culture from the stromatolite mat was obtained on cysteate in a medium lacking sulfate and incubated anaerobically. The rate of cysteate consumption by this enrichment culture was 1.6 pmol cell(-1) h(-1). Compared to the results of slurry studies, this rate suggests that organisms with properties similar to the properties of this enrichment culture are a major constituent of the sulfidogenic population. In addition, taurine was consumed at some of highest dilutions obtained from most-probable-number enrichment cultures obtained from stromatolite samples. Based on our comparison of the sulfide production rates found in various mats, low-molecular-weight sulfonates are important sources of C and S in these ecosystems.
向微生物席浆液中添加了几种低分子量磺酸盐,以研究它们对硫酸盐还原的影响。在向所有测试的微生物席中添加牛磺酸和半胱氨酸盐后,立即产生了硫化物。在叠层石席中,存在牛磺酸和半胱氨酸盐时的产生速率分别为35和24 μM HS⁻ h⁻¹;在盐池席中为38和36 μM HS⁻ h⁻¹;在盐沼席中为27和18 μM HS⁻ h⁻¹。传统使用的底物乳酸盐和乙酸盐刺激硫化物产生的速率比牛磺酸和半胱氨酸盐在所有席中刺激硫化物产生的速率高3至10倍,但是当向叠层石席浆液中添加乙醇、乙醇酸盐和谷氨酸盐时,产生的增加与用牛磺酸和半胱氨酸盐观察到的增加相似。羟乙磺酸盐、磺基琥珀酸盐和磺基苯甲酸盐仅用叠层石席浆液进行了测试,这些化合物对硫化物产生的影响要小得多。添加钼酸盐对乙酸盐和乳酸盐利用的抑制作用比对磺酸盐利用的抑制作用更大,这表明涉及不同的代谢途径。在所有测试的席中,孔隙水中牛磺酸和半胱氨酸盐的浓度为纳摩尔至微摩尔。在缺乏硫酸盐的培养基中,从叠层石席获得了一种以半胱氨酸盐为基础的富集培养物,并进行厌氧培养。这种富集培养物消耗半胱氨酸盐的速率为1.6 pmol cell⁻¹ h⁻¹。与浆液研究结果相比,该速率表明具有与这种富集培养物性质相似性质的生物体是产硫化物种群的主要组成部分。此外,在从叠层石样品获得的最可能数富集培养物中,在一些最高稀释度下牛磺酸被消耗。基于我们对各种席中发现的硫化物产生速率的比较,低分子量磺酸盐是这些生态系统中碳和硫的重要来源。