Cordone Angelina, Selci Matteo, Barosa Bernardo, Bastianoni Alessia, Bastoni Deborah, Bolinesi Francesco, Capuozzo Rosaria, Cascone Martina, Correggia Monica, Corso Davide, Di Iorio Luciano, Misic Cristina, Montemagno Francesco, Ricciardelli Annarita, Saggiomo Maria, Tonietti Luca, Mangoni Olga, Giovannelli Donato
Department of Biology, University of Naples Federico II, 80126 Naples, Italy.
Dipartimento di Scienze della Terra, Dell'Ambiente e della Vita, Universitá di Genova, 16132 Genova, Italy.
Microorganisms. 2023 Mar 9;11(3):702. doi: 10.3390/microorganisms11030702.
The Antarctic Circumpolar Current (ACC) is the major current in the Southern Ocean, isolating the warm stratified subtropical waters from the more homogeneous cold polar waters. The ACC flows from west to east around Antarctica and generates an overturning circulation by fostering deep-cold water upwelling and the formation of new water masses, thus affecting the Earth's heat balance and the global distribution of carbon. The ACC is characterized by several water mass boundaries or fronts, known as the Subtropical Front (STF), Subantarctic Front (SAF), Polar Front (PF), and South Antarctic Circumpolar Current Front (SACCF), identified by typical physical and chemical properties. While the physical characteristics of these fronts have been characterized, there is still poor information regarding the microbial diversity of this area. Here we present the surface water bacterioplankton community structure based on 16S rRNA sequencing from 13 stations sampled in 2017 between New Zealand to the Ross Sea crossing the ACC Fronts. Our results show a distinct succession in the dominant bacterial phylotypes present in the different water masses and suggest a strong role of sea surface temperatures and the availability of Carbon and Nitrogen in controlling community composition. This work represents an important baseline for future studies on the response of Southern Ocean epipelagic microbial communities to climate change.
南极绕极流(ACC)是南大洋的主要洋流,将温暖的分层亚热带水域与更为均匀的寒冷极地水域隔离开来。ACC围绕南极洲自西向东流动,通过促进深层冷水上涌和新水体的形成产生翻转环流,从而影响地球的热量平衡和碳的全球分布。ACC的特征是有几个水体边界或锋面,称为亚热带锋(STF)、亚南极锋(SAF)、极地锋(PF)和南极绕极流锋(SACCF),可通过典型的物理和化学性质来识别。虽然这些锋面的物理特征已得到描述,但关于该区域微生物多样性的信息仍然匮乏。在此,我们基于2017年在新西兰至罗斯海之间跨越ACC锋面的13个站点采集的样本,通过16S rRNA测序展示了表层水细菌浮游生物群落结构。我们的结果显示,不同水体中存在的优势细菌系统型呈现出明显的演替,并表明海表温度以及碳和氮的可利用性在控制群落组成方面发挥着重要作用。这项工作为未来关于南大洋上层海洋微生物群落对气候变化响应的研究提供了重要的基线。