Malard Lucie A, Šabacká Marie, Magiopoulos Iordanis, Mowlem Matt, Hodson Andy, Tranter Martyn, Siegert Martin J, Pearce David A
Department of Applied Sciences, Faculty of Health and Life Sciences, Northumbria University at Newcastle, Newcastle upon Tyne, United Kingdom.
Centre for Polar Ecology, University of South Bohemia in České Budějovice, České Budějovice, Czechia.
Front Microbiol. 2019 Mar 26;10:461. doi: 10.3389/fmicb.2019.00461. eCollection 2019.
It was once a long-held view that the Antarctic was a pristine environment with low biomass, low biodiversity and low rates of microbial activity. However, as the intensity of scientific investigation has increased, so these views have started to change. In particular, the role and impact of human activity toward indigenous microbial communities has started to come under more intense scrutiny. During the Subglacial Lake Ellsworth exploration campaign in December 2012, a microbiological survey was conducted to determine the extent and likelihood of exogenous input into the subglacial lake system during the hot-water drilling process. Snow was collected from the surface to represent that used for melt water production for hot-water drilling. The results of this study showed that snow used to provide melt water differed in its microbiological composition from that of the surrounding area and raised the question of how the biogeography of snow-borne microorganisms might influence the potential outcome of scientific analyses. In this study, we investigated the biogeography of microorganisms in snow around a series of Antarctic logistic hubs, where human activity was clearly apparent, and from which scientific investigations have been undertaken. A change in microbial community structure with geographical location was apparent and, notably, a decrease in alpha diversity at more remote southern latitudes. Soil-related microorganisms dominated microbial assemblages suggesting terrestrial input, most likely from long-range aeolian transport into continental Antarctica. We also observed that relic DNA was not a major issue when assessing snow samples. Overall, our observations might have profound implications for future scientific activities in Antarctica, such as the need to establish "no-go" protected areas, the need for better characterization of field sites and improved protocols for sterilization and verification of ice drilling equipment.
曾经有一个长期持有的观点,即南极是一个生物量低、生物多样性低且微生物活动速率低的原始环境。然而,随着科学调查强度的增加,这些观点开始发生变化。特别是,人类活动对当地微生物群落的作用和影响已开始受到更严格的审查。在2012年12月的埃尔斯沃思湖冰下探索活动中,进行了一项微生物学调查,以确定在热水钻探过程中外源输入冰下湖泊系统的程度和可能性。从表面收集雪样,以代表用于热水钻探融水生产的雪。这项研究的结果表明,用于提供融水的雪在微生物组成上与周围地区不同,并引发了一个问题,即雪载微生物的生物地理学如何可能影响科学分析的潜在结果。在这项研究中,我们调查了一系列南极后勤枢纽周围微生物的生物地理学,这些枢纽人类活动明显,并且已经开展了科学调查。微生物群落结构随地理位置的变化很明显,值得注意的是,在更偏远的南纬地区,α多样性有所下降。与土壤相关 的微生物主导了微生物群落,表明有陆地输入,很可能是通过远距离风成输送进入南极大陆。我们还观察到,在评估雪样时,残留DNA不是一个主要问题。总体而言,我们的观察结果可能对未来南极的科学活动产生深远影响,例如需要建立“禁区”保护区,需要更好地描述野外场地,以及改进冰钻设备的灭菌和验证方案。