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Characterization of bacterioplankton communities and quantification of organic carbon pools off the Galapagos Archipelago under contrasting environmental conditions

机译:在不同环境条件下加拉帕戈斯群岛外浮游细菌群落的特征和有机碳库的定量

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摘要

Bacteria play a crucial role in the marine carbon cycle, contributing to the production and degradation of organic carbon. Here, we investigated organic carbon pools, aggregate formation, and bacterioplankton communities in three contrasting oceanographic settings in the Galapagos Archipelago. We studied a submarine CO2 vent at Roca Redonda (RoR), an upwelling site at Bolivar Channel (BoC) subjected to a weak El Niño event at the time of sampling in October 2014, as well as a site without volcanic or upwelling influence at Cowley Islet (CoI). We recorded physico-chemical parameters, and quantified particulate and dissolved organic carbon, transparent exopolymeric particles, and the potential of the water to form larger marine aggregates. Free-living and particle-attached bacterial communities were assessed via 16S rRNA gene sequencing. Both RoR and BoC exhibited temperatures elevated by 1–1.5 °C compared to CoI. RoR further experienced reduced pH between 6.8 and 7.4. We observed pronounced differences in organic carbon pools at each of the three sites, with highest dissolved organic carbon concentrations at BoC and RoR, and highest particulate organic carbon concentrations and aggregate formation at BoC. Bacterioplankton communities at BoC were dominated by opportunistic copiotrophic taxa, such as Alteromonas and Roseobacter, known to thrive in phytoplankton blooms, as opposed to oligotrophic taxa dominating at CoI, such as members of the SAR11 clade. Therefore, we propose that bacterial communities were mainly influenced by the availability of organic carbon at the investigated sites. Our study provides a comprehensive characterization of organic carbon pools and bacterioplankton communities, highlighting the high heterogeneity of various components of the marine carbon cycle around the Galapagos Archipelago.
机译:细菌在海洋碳循环中起着至关重要的作用,有助于有机碳的生产和降解。在这里,我们研究了加拉帕戈斯群岛三种不同海洋环境中的有机碳库,聚集体形成和浮游细菌群落。我们研究了Roca Redonda(RoR)的海底二氧化碳排放口,Roca Redonda是玻利瓦尔海峡(BoC)的上升流场,在2014年10月采样时遭受了弱的厄尔尼诺事件,并且在Cowley没有火山或上升流的影响胰岛(CoI)。我们记录了理化参数,并对颗粒和溶解的有机碳,透明的外聚合颗粒以及水形成更大的海洋聚集体的潜力进行了量化。通过16S rRNA基因测序评估了自由生活和附着颗粒的细菌群落。与CoI相比,RoR和BoC都显示出温度升高了1–1.5°C。 RoR进一步将pH降低到6.8和7.4之间。我们观察到三个站点中每个站点的有机碳库存在明显差异,其中BoC和RoR处的溶解有机碳浓度最高,而BoC处的颗粒有机碳浓度和聚集体形成最高。 BoC的浮游细菌群落以机会性嗜营养类群为主导,例如已知在浮游植物绽放中繁盛的嗜盐单生菌和玫瑰细菌,而不是在SAR11进化枝中以寡养类群为主的CoI。因此,我们建议细菌群落主要受调查地点有机碳的可用性影响。我们的研究提供了有机碳库和浮游细菌群落的全面特征,突出了加拉帕戈斯群岛周围海洋碳循环各组成部分的高度异质性。

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