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海冰覆盖对南极大陆架沉积物中微生物群落的影响。

The Impact of Sea Ice Cover on Microbial Communities in Antarctic Shelf Sediments.

作者信息

Baloza Marwa, Henkel Susann, Kasten Sabine, Holtappels Moritz, Molari Massimiliano

机构信息

Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany.

Faculty 2 Biology/Chemistry, University of Bremen, Leobener Str., 28359 Bremen, Germany.

出版信息

Microorganisms. 2023 Jun 14;11(6):1572. doi: 10.3390/microorganisms11061572.

Abstract

The area around the Antarctic Peninsula (AP) is facing rapid climatic and environmental changes, with so far unknown impacts on the benthic microbial communities of the continental shelves. In this study, we investigated the impact of contrasting sea ice cover on microbial community compositions in surface sediments from five stations along the eastern shelf of the AP using 16S ribosomal RNA (rRNA) gene sequencing. Redox conditions in sediments with long ice-free periods are characterized by a prevailing ferruginous zone, whereas a comparatively broad upper oxic zone is present at the heavily ice-covered station. Low ice cover stations were highly dominated by microbial communities of (mostly , , and ), , and , whereas , , , and prevail at the heavy ice cover station. In the ferruginous zone, was the dominant member of Desulfuromonadales for all stations and, along with eleven other taxa, showed significant positive correlations with dissolved Fe concentrations, suggesting a significant role in iron reduction or an ecological relationship with iron reducers. Our results indicate that sea ice cover and its effect on organic carbon fluxes are the major drivers for changes in benthic microbial communities, favoring potential iron reducers at stations with increased organic matter fluxes.

摘要

南极半岛(AP)周边地区正面临快速的气候和环境变化,对大陆架底栖微生物群落的影响迄今尚不清楚。在本研究中,我们利用16S核糖体RNA(rRNA)基因测序,调查了不同海冰覆盖情况对AP东部陆架五个站点表层沉积物中微生物群落组成的影响。无冰期较长的沉积物中的氧化还原条件以普遍存在的铁质区为特征,而在海冰覆盖严重的站点存在相对较宽的上部有氧区。低冰覆盖站点主要由(主要是、和)、、和的微生物群落主导,而在高冰覆盖站点占主导地位。在铁质区,是所有站点脱硫单胞菌目的主要成员,并且与其他11个分类群一起,与溶解铁浓度呈显著正相关,表明在铁还原中起重要作用或与铁还原菌存在生态关系。我们的结果表明,海冰覆盖及其对有机碳通量的影响是底栖微生物群落变化的主要驱动因素,有利于有机质通量增加的站点中的潜在铁还原菌。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a4ca/10305693/d5f728a1b3e3/microorganisms-11-01572-g001.jpg

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