深海的石油羽毛丰富了本土的石油降解细菌
Terry C Hazen1, Eric A Dubinsky, Todd Z DeSantis
1MS 70A-3317, One Cyclotron Road, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA. tchazen@lbl.gov
概括
深海细菌迅速降解了来自深水地平线泄漏的石油. 这种自然生物修复发生在深海,没有显著的氧气耗尽,为生态系统恢复提供了希望.
科学领域:
- 海洋生物学 海洋生物学
- 环境科学环境科学
- 微生物学 微生物学
背景情况:
- 深水地平线爆炸释放了大量的石油进入墨西哥湾.
- 这个深海油柱的命运和生物效应在很大程度上是未知的.
- 了解微生物对这种前所未有的事件的反应对于评估环境影响至关重要.
研究的目的:
- 为了研究深海油柱的生物效应.
- 为了确定分散的石油碳化合物的命运.
- 评估深海自然生物修复的潜力.
主要方法:
- 分析深海海中的碳化合物度和微生物群落组成.
- 在本土细菌中识别碳化合物降解基因.
- 在5°C环境中与环境分离物进行化实验,以测量生物降解率.
主要成果:
- 分散的石油羽毛刺激了土著γ-蛋白质细菌的生长,与已知的石油降解剂密切相关.
- 发现碳化合物降解基因是丰富的,并且与油污染物度相关.
- 碳化合物在5°C的生物降解速度比预期的更快,即使在深海条件下也是如此.
- 没有观察到显著的氧气消耗,这表明对深海氧气水平的影响很小.
结论:
- 本土深海微生物,特别是γ-蛋白质细菌,具有降解石油碳化合物的能力.
- 深海油柱以惊人的快速速度受到内在生物修复.
- 深水石油泄漏可能容易发生自然生物降解,但不会导致水柱中严重的氧气耗尽.
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