Max Planck Institute for Marine Microbiology, Bremen, 28359, Germany.
Physical Oceanography of the Polar Seas, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, 27570, Germany.
ISME J. 2023 Oct;17(10):1612-1625. doi: 10.1038/s41396-023-01461-6. Epub 2023 Jul 8.
The Arctic Ocean is experiencing unprecedented changes because of climate warming, necessitating detailed analyses on the ecology and dynamics of biological communities to understand current and future ecosystem shifts. Here, we generated a four-year, high-resolution amplicon dataset along with one annual cycle of PacBio HiFi read metagenomes from the East Greenland Current (EGC), and combined this with datasets spanning different spatiotemporal scales (Tara Arctic and MOSAiC) to assess the impact of Atlantic water influx and sea-ice cover on bacterial communities in the Arctic Ocean. Densely ice-covered polar waters harboured a temporally stable, resident microbiome. Atlantic water influx and reduced sea-ice cover resulted in the dominance of seasonally fluctuating populations, resembling a process of "replacement" through advection, mixing and environmental sorting. We identified bacterial signature populations of distinct environmental regimes, including polar night and high-ice cover, and assessed their ecological roles. Dynamics of signature populations were consistent across the wider Arctic; e.g. those associated with dense ice cover and winter in the EGC were abundant in the central Arctic Ocean in winter. Population- and community-level analyses revealed metabolic distinctions between bacteria affiliated with Arctic and Atlantic conditions; the former with increased potential to use bacterial- and terrestrial-derived substrates or inorganic compounds. Our evidence on bacterial dynamics over spatiotemporal scales provides novel insights into Arctic ecology and indicates a progressing Biological Atlantification of the warming Arctic Ocean, with consequences for food webs and biogeochemical cycles.
由于气候变暖,北极海洋正在经历前所未有的变化,这需要对生态系统和生物群落的动态进行详细分析,以了解当前和未来的生态系统变化。在这里,我们生成了一个为期四年的高分辨率扩增子数据集,以及来自东格陵兰流(EGC)的一个年度 Pacific Biosciences 长读长宏基因组数据集,并将其与跨越不同时空尺度的数据集(Tara 北极和 MOSAiC)相结合,以评估大西洋水入侵和海冰覆盖对北极海洋细菌群落的影响。密集冰覆盖的极地水域拥有一个时间上稳定的常驻微生物组。大西洋水的涌入和海冰覆盖的减少导致季节性波动的种群占主导地位,这类似于通过平流、混合和环境分选进行的“替代”过程。我们确定了不同环境条件下的细菌特征种群,包括极夜和高冰覆盖,并评估了它们的生态作用。特征种群的动态在更广泛的北极地区是一致的;例如,在 EGC 中与密集冰覆盖和冬季相关的种群在北极中部海洋的冬季非常丰富。种群和群落水平的分析揭示了与北极和大西洋条件相关的细菌之间的代谢差异;前者具有增加利用细菌和陆地衍生底物或无机化合物的潜力。我们在时空尺度上对细菌动态的证据提供了对北极生态的新见解,并表明变暖的北极海洋正在经历生物大西洋化,这对食物网和生物地球化学循环有影响。