Hewson Ian, Moisander Pia H, Morrison Amanda E, Zehr Jonathan P
Department of Ocean Sciences, University of California Santa Cruz, Santa Cruz, CA 95064, USA.
ISME J. 2007 May;1(1):78-91. doi: 10.1038/ismej.2007.5.
We investigated diazotrophic bacterioplankton assemblage composition in the Heron Reef lagoon (Great Barrier Reef, Australia) using culture-independent techniques targeting the nifH fragment of the nitrogenase gene. Seawater was collected at 3 h intervals over a period of 72 h (i.e. over diel as well as tidal cycles). An incubation experiment was also conducted to assess the impact of phosphate (PO(4)3*) availability on nifH expression patterns. DNA-based nifH libraries contained primarily sequences that were most similar to nifH from sediment, microbial mat and surface-associated microorganisms, with a few sequences that clustered with typical open ocean phylotypes. In contrast to genomic DNA sequences, libraries prepared from gene transcripts (mRNA amplified by reverse transcription-polymerase chain reaction) were entirely cyanobacterial and contained phylotypes similar to those observed in open ocean plankton. The abundance of Trichodesmium and two uncultured cyanobacterial phylotypes from previous studies (group A and group B) were studied by quantitative-polymerase chain reaction in the lagoon samples. These were detected as transcripts, but were not detected in genomic DNA. The gene transcript abundance of these phylotypes demonstrated variability over several diel cycles. The PO(4)3* enrichment experiment had a clearer pattern of gene expression over diel cycles than the lagoon sampling, however PO(4)3* additions did not result in enhanced transcript abundance relative to control incubations. The results suggest that a number of diazotrophs in bacterioplankton of the reef lagoon may originate from sediment, coral or beachrock surfaces, sloughing into plankton with the flooding tide. The presence of typical open ocean phylotype transcripts in lagoon bacterioplankton may indicate that they are an important component of the N cycle of the coral reef.
我们采用针对固氮酶基因nifH片段的非培养技术,对澳大利亚大堡礁苍鹭礁泻湖中的固氮细菌浮游生物群落组成进行了调查。在72小时内每隔3小时采集一次海水样本(即涵盖昼夜以及潮汐周期)。还进行了一项培养实验,以评估磷酸盐(PO₄³⁻)有效性对nifH表达模式的影响。基于DNA的nifH文库主要包含与沉积物、微生物垫及表面相关微生物的nifH最为相似的序列,还有一些序列与典型的开阔海洋系统发育型聚类。与基因组DNA序列不同,从基因转录本(通过逆转录 - 聚合酶链反应扩增的mRNA)制备的文库完全是蓝细菌的,并且包含与开阔海洋浮游生物中观察到的相似的系统发育型。通过定量聚合酶链反应研究了泻湖样本中来自先前研究的束毛藻以及两种未培养蓝细菌系统发育型(A组和B组)的丰度。这些在转录本中被检测到,但在基因组DNA中未被检测到。这些系统发育型的基因转录本丰度在几个昼夜周期中表现出变异性。PO₄³⁻富集实验在昼夜周期中的基因表达模式比泻湖采样更清晰,然而相对于对照培养,添加PO₄³⁻并未导致转录本丰度增加。结果表明,礁湖细菌浮游生物中的许多固氮菌可能源自沉积物、珊瑚或滨岩表面,随着涨潮进入浮游生物。泻湖细菌浮游生物中典型开阔海洋系统发育型转录本的存在可能表明它们是珊瑚礁氮循环的重要组成部分。