Max Planck Institute for Marine Microbiology, Celciusstraße 1, Bremen, Germany.
1] Department of Biological Oceanography, NIOZ - Royal Netherlands Institute for Sea Research, Texel, The Netherlands [2] Aquatic Microbiology, Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, Amsterdam, The Netherlands.
ISME J. 2014 Jan;8(1):212-25. doi: 10.1038/ismej.2013.135. Epub 2013 Aug 15.
The release of organic material upon algal cell lyses has a key role in structuring bacterial communities and affects the cycling of biolimiting elements in the marine environment. Here we show that already before cell lysis the leakage or excretion of organic matter by infected yet intact algal cells shaped North Sea bacterial community composition and enhanced bacterial substrate assimilation. Infected algal cultures of Phaeocystis globosa grown in coastal North Sea water contained gamma- and alphaproteobacterial phylotypes that were distinct from those in the non-infected control cultures 5 h after infection. The gammaproteobacterial population at this time mainly consisted of Alteromonas sp. cells that were attached to the infected but still intact host cells. Nano-scale secondary-ion mass spectrometry (nanoSIMS) showed ∼20% transfer of organic matter derived from the infected (13)C- and (15)N-labelled P. globosa cells to Alteromonas sp. cells. Subsequent, viral lysis of P. globosa resulted in the formation of aggregates that were densely colonised by bacteria. Aggregate dissolution was observed after 2 days, which we attribute to bacteriophage-induced lysis of the attached bacteria. Isotope mass spectrometry analysis showed that 40% of the particulate (13)C-organic carbon from the infected P. globosa culture was remineralized to dissolved inorganic carbon after 7 days. These findings reveal a novel role of viruses in the leakage or excretion of algal biomass upon infection, which provides an additional ecological niche for specific bacterial populations and potentially redirects carbon availability.
藻类细胞裂解时释放的有机物质在构建细菌群落方面起着关键作用,并影响海洋环境中生物限制元素的循环。在这里,我们表明,在细胞裂解之前,受感染但完整的藻类细胞渗漏或排泄有机物就已经影响了北海细菌群落的组成,并增强了细菌对基质的同化作用。在北海近岸海水培养的聚球藻中,感染后的藻类培养物中含有不同于未感染对照培养物的γ-和α-变形菌门的生物型 5 小时后。此时,γ-变形菌种群主要由附着在受感染但仍完整的宿主细胞上的交替单胞菌细胞组成。纳米级二次离子质谱(nanoSIMS)表明,约 20%源自感染(13)C 和(15)N 标记的聚球藻细胞的有机物转移到交替单胞菌细胞。随后,聚球藻的病毒裂解导致形成了被细菌密集定植的聚集体。在 2 天后观察到聚集体溶解,我们认为这归因于附着细菌的噬菌体诱导裂解。同位素质量光谱分析表明,在感染后 7 天,来自感染的聚球藻培养物的 40%颗粒态(13)C-有机碳被再矿化为溶解无机碳。这些发现揭示了病毒在感染时藻类生物量渗漏或排泄中的新作用,这为特定细菌种群提供了一个额外的生态位,并可能改变碳的可用性。