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Nitrogen Fixation in Thermophilic Chemosynthetic Microbial Communities Depending on Hydrogen Sulfate and Carbon Dioxide

机译:取决于氢气硫酸盐和二氧化碳的嗜热性化学合成微生物群落中的固氮作用

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摘要

The activity of nitrogen fixation measured by acetylene reduction was examined in chemosynthetic microbial mats at 72–75°C in slightly-alkaline sulfidic hot springs in Nakabusa, Japan. Nitrogenase activity markedly varied from sampling to sampling. Nitrogenase activity did not correlate with methane production, but was detected in samples showing methane production levels less than the maximum amount, indicating a possible redox dependency of nitrogenase activity. Nitrogenase activity was not affected by 2-bromo-ethane sulfonate, an inhibitor of methanogenesis. However, it was inhibited by the addition of molybdate, an inhibitor of sulfate reduction and sulfur disproportionation, suggesting the involvement of sulfate-reducing or sulfur-disproportionating organisms. Nitrogenase activity was affected by different O2 concentrations in the gas phase, again supporting the hypothesis of a redox potential dependency, and was decreased by the dispersion of mats with a homogenizer. The loss of activity that occurred from dispersion was partially recovered by the addition of H2, sulfate, and carbon dioxide. These results suggested that the observed activity of nitrogen fixation was related to chemoautotrophic sulfate reducers, and fixation may be active in a limited range of ambient redox potential. Since thermophilic chemosynthetic communities may resemble ancient microbial communities before the appearance of photosynthesis, the present results may be useful when considering the ancient nitrogen cycle on earth.
机译:在日本中部的弱碱性硫化温泉中,在72–75°C的化学合成微生物垫中检测了通过乙炔还原测量的固氮活性。每次采样之间的固氮酶活性明显不同。固氮酶的活性与甲烷的产生无关,但是在样品中检测到甲烷的产生水平低于最大量,表明固氮酶活性可能与氧化还原有关。硝化酶的活性不受2-溴乙烷磺酸盐的影响。然而,它通过添加钼酸盐(一种硫酸盐还原和硫歧化抑制剂)而被抑制,这表明硫酸盐还原或硫歧化生物参与其中。固氮酶活性受气相中不同O2浓度的影响,再次支持氧化还原电势依赖性的假设,并且由于用均质器分散垫而降低了。通过添加氢气,硫酸盐和二氧化碳可以部分弥补分散引起的活性下降。这些结果表明观察到的固氮活性与化学自养硫酸盐还原剂有关,并且固氮可能在有限的环境氧化还原电位范围内具有活性。由于嗜热的化学合成群落在光合作用出现之前可能类似于古代的微生物群落,因此当考虑地球上古代的氮循环时,本结果可能是有用的。

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