Botanisches Institut, Christian-Albrechts-Universität, Kiel, Germany.
PLoS One. 2010 Nov 5;5(11):e13846. doi: 10.1371/journal.pone.0013846.
Surface waters of aquatic environments have been shown to both evolve and consume hydrogen and the ocean is estimated to be the principal natural source. In some marine habitats, H(2) evolution and uptake are clearly due to biological activity, while contributions of abiotic sources must be considered in others. Until now the only known biological process involved in H(2) metabolism in marine environments is nitrogen fixation.
We analyzed marine and freshwater environments for the presence and distribution of genes of all known hydrogenases, the enzymes involved in biological hydrogen turnover. The total genomes and the available marine metagenome datasets were searched for hydrogenase sequences. Furthermore, we isolated DNA from samples from the North Atlantic, Mediterranean Sea, North Sea, Baltic Sea, and two fresh water lakes and amplified and sequenced part of the gene encoding the bidirectional NAD(P)-linked hydrogenase. In 21% of all marine heterotrophic bacterial genomes from surface waters, one or several hydrogenase genes were found, with the membrane-bound H(2) uptake hydrogenase being the most widespread. A clear bias of hydrogenases to environments with terrestrial influence was found. This is exemplified by the cyanobacterial bidirectional NAD(P)-linked hydrogenase that was found in freshwater and coastal areas but not in the open ocean.
This study shows that hydrogenases are surprisingly abundant in marine environments. Due to its ecological distribution the primary function of the bidirectional NAD(P)-linked hydrogenase seems to be fermentative hydrogen evolution. Moreover, our data suggests that marine surface waters could be an interesting source of oxygen-resistant uptake hydrogenases. The respective genes occur in coastal as well as open ocean habitats and we presume that they are used as additional energy scavenging devices in otherwise nutrient limited environments. The membrane-bound H(2)-evolving hydrogenases might be useful as marker for bacteria living inside of marine snow particles.
水生环境的地表水已经被证明既能产生又能消耗氢气,而海洋则被估计为主要的天然来源。在一些海洋栖息地中,H2 的产生和吸收显然是由于生物活动,而在其他一些地方则必须考虑非生物来源的贡献。到目前为止,唯一已知的参与海洋环境中 H2 代谢的生物过程是固氮作用。
我们分析了海洋和淡水环境中所有已知氢化酶(参与生物氢转化的酶)的存在和分布。对总基因组和现有的海洋宏基因组数据集进行了搜索,以寻找氢化酶序列。此外,我们从北大西洋、地中海、北海、波罗的海以及两个淡水湖的样本中分离出 DNA,并扩增和测序了编码双向 NAD(P)-连接氢化酶的部分基因。在海洋异养细菌表面水中的所有基因组中,有 21%的基因组中发现了一个或多个氢化酶基因,其中膜结合的 H2 摄取氢化酶最为广泛。氢化酶明显偏向于受陆地影响的环境。这可以通过在淡水和沿海地区发现但在开阔海域不存在的蓝细菌双向 NAD(P)-连接氢化酶来说明。
这项研究表明,氢化酶在海洋环境中非常丰富。由于其生态分布,双向 NAD(P)-连接氢化酶的主要功能似乎是发酵性的 H2 产生。此外,我们的数据表明,海洋地表水可能是一种有趣的耐氧摄取氢化酶的来源。相应的基因存在于沿海和开阔海域的栖息地,我们推测它们在其他营养有限的环境中被用作额外的能量捕获装置。膜结合的 H2 产生氢化酶可能是一种有用的标记物,用于标记生活在海洋雪颗粒内部的细菌。