对细菌发酵中的碳同位素分离的代谢控制
Elliott P Mueller1,2, Verena B Heuer3, Jared R Leadbetter1
1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125.
概括
微生物发酵产生了不同的碳同位素分离,挑战了以前的假设. 这种酸丰富的特征为研究古代和现代生物地球化学过程提供了一个新的生物标志物.
科学领域:
- 生物地质化学生物地质化学
- 微生物生态学 微生物生态学
- 同位素地球化学 同位素地球化学
背景情况:
- 微生物发酵对于有机物分解至关重要,但缺乏环境生物标志物.
- 发酵被认为具有最小的碳同位素分离,阻碍了它的研究.
- 了解发酵的同位素特征是重建过去生物地球化学循环的关键.
研究的目的:
- 为了研究微生物发酵过程中的碳同位素分离.
- 在地质记录中识别潜在的发酵生物标志物.
- 挑战现有的碳同位素循环模型.
主要方法:
- 在葡萄糖上培养四种发酵细菌.
- 测量有机酸和醇的碳同位素组成.
- 使用生物同位素模型来识别分离酶.
主要成果:
- 发酵过程显示出显著的碳同位素分离 (6‰至16‰).
- 酸13C-丰富被确定为一个广泛的发酵签名.
- 生物同位素模型成功地重现了观察到的同位素值.
结论:
- 发酵强加于热带碳同位素分离,影响二次降解剂.
- 酸盐丰富可以作为古代发酵的生物标志物.
- 这一发现修订了我们对地球历史上碳循环和脂质同位素组成的理解.
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