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海洋异戊二烯降解群落的特征。

Characterization of marine isoprene-degrading communities.

机构信息

Department of Biological Sciences, University of Essex, Wivenhoe Park, Colchester, CO4 3SQ, UK.

出版信息

Environ Microbiol. 2009 Dec;11(12):3280-91. doi: 10.1111/j.1462-2920.2009.02069.x. Epub 2009 Oct 5.

DOI:10.1111/j.1462-2920.2009.02069.x
PMID:19807779
Abstract

Isoprene is a volatile and climate-altering hydrocarbon with an atmospheric concentration similar to that of methane. It is well established that marine algae produce isoprene; however, until now there was no specific information about marine isoprene sinks. Here we demonstrate isoprene consumption in samples from temperate and tropical marine and coastal environments, and furthermore show that the most rapid degradation of isoprene coincides with the highest rates of isoprene production in estuarine sediments. Isoprene-degrading enrichment cultures, analysed by denaturing gradient gel electrophoresis and 454 pyrosequencing of the 16S rRNA gene and by culturing, were generally dominated by Actinobacteria, but included other groups such as Alphaproteobacteria and Bacteroidetes, previously not known to degrade isoprene. In contrast to specialist methane-oxidizing bacteria, cultivated isoprene degraders were nutritionally versatile, and nearly all of them were able to use n-alkanes as a source of carbon and energy. We therefore tested and showed that the ubiquitous marine hydrocarbon-degrader, Alcanivorax borkumensis, could also degrade isoprene. A mixture of the isolates consumed isoprene emitted from algal cultures, confirming that isoprene can be metabolized at low, environmentally relevant concentrations, and suggesting that, in the absence of spilled petroleum hydrocarbons, algal production of isoprene could maintain viable populations of hydrocarbon-degrading microbes. This discovery of a missing marine sink for isoprene is the first step in obtaining more robust predictions of its flux, and suggests that algal-derived isoprene provides an additional source of carbon for diverse microbes in the oceans.

摘要

异戊二烯是一种挥发性的、改变气候的碳氢化合物,其大气浓度与甲烷相似。人们已经证实海洋藻类会产生异戊二烯;然而,到目前为止,对于海洋异戊二烯汇还没有具体的信息。在这里,我们展示了来自温带和热带海洋及沿海环境的样本中异戊二烯的消耗情况,并且进一步表明,异戊二烯的最快降解速度与河口沉积物中异戊二烯产生的最高速率相吻合。通过变性梯度凝胶电泳和 16S rRNA 基因的 454 焦磷酸测序以及培养物分析,异戊二烯降解富集培养物通常由放线菌主导,但也包括其他群体,如以前不知道能降解异戊二烯的α变形菌和拟杆菌门。与专门的甲烷氧化细菌不同,培养的异戊二烯降解菌具有广泛的营养适应性,并且几乎所有的菌都能够将正烷烃作为碳和能源的来源。因此,我们进行了测试并表明,普遍存在的海洋烃类降解菌 Alcanivorax borkumensis 也能够降解异戊二烯。混合分离物消耗了从藻类培养物中排放的异戊二烯,这证实了异戊二烯可以在低浓度下被代谢,这表明在没有溢油烃类的情况下,藻类产生的异戊二烯可以维持烃类降解微生物的存活种群。这一发现填补了海洋中异戊二烯汇的空白,是更准确预测其通量的第一步,并且表明藻类衍生的异戊二烯为海洋中的各种微生物提供了额外的碳源。

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