CNRS, Sorbonne Université, Laboratoire d'Océanographie Microbienne, LOMIC, Banyuls-sur-Mer, France.
Marine Biology Research Division and Climate, Atmospheric Science & Physical Oceanography Department, Scripps Institution of Oceanography, San Diego, California, USA.
Environ Microbiol Rep. 2022 Dec;14(6):907-916. doi: 10.1111/1758-2229.13117. Epub 2022 Aug 26.
The ecology of the SAR11 clade, the most abundant bacterial group in the ocean, has been intensively studied in temperate and tropical regions, but its distribution remains largely unexplored in the Southern Ocean. Through amplicon sequencing of the 16S rRNA gene, we assessed the contribution of the SAR11 clade to bacterial community composition in the naturally iron fertilized region off Kerguelen Island. We investigated the upper 300 m at seven sites located in early spring phytoplankton blooms and at one high-nutrient low-chlorophyll site. Despite pronounced vertical patterns of the bacterioplankton assemblages, the SAR11 clade had high relative abundances at all depths and sites, averaging 40% (±15%) of the total community relative abundance. Micro-autoradiography combined with CARD-FISH further revealed that the clade had an overall stable contribution (45%-60% in surface waters) to bacterial biomass production (determined by H-leucine incorporation) during different early bloom stages. The spatio-temporal partitioning of some of the SAR11 subclades suggests a niche specificity and periodic selection of different subclades in response to the fluctuating extreme conditions of the Southern Ocean. These observations improve our understanding of the ecology of the SAR11 clade and its implications in biogeochemical cycles in the rapidly changing Southern Ocean.
SAR11 丛的生态学在温带和热带地区得到了深入研究,SAR11 丛是海洋中最丰富的细菌群之一,但在南大洋的分布仍然很大程度上未被探索。通过对 16S rRNA 基因的扩增子测序,我们评估了 SAR11 丛对克尔格伦岛附近自然铁施肥区细菌群落组成的贡献。我们在七个地点调查了上 300m 的水层,这些地点位于早春浮游植物大量繁殖期间,以及一个高营养低叶绿素的地点。尽管浮游细菌组合存在明显的垂直模式,但 SAR11 丛在所有深度和地点的相对丰度都很高,平均占总群落相对丰度的 40%(±15%)。微放射性自显影结合 CARD-FISH 进一步表明,在不同的早期繁殖阶段,该丛对细菌生物量的产生(通过 H-亮氨酸掺入来确定)有一个总体稳定的贡献(在表层水中占 45%-60%)。一些 SAR11 亚群的时空分区表明,它们具有特定的生态位特异性,并对南大洋不断变化的极端条件做出周期性选择不同的亚群。这些观察结果提高了我们对 SAR11 丛生态学及其在快速变化的南大洋生物地球化学循环中的意义的理解。