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原核细胞从格陵兰冰盖的融水输出。

Meltwater export of prokaryotic cells from the Greenland ice sheet.

作者信息

Cameron Karen A, Stibal Marek, Hawkings Jon R, Mikkelsen Andreas B, Telling Jon, Kohler Tyler J, Gözdereliler Erkin, Zarsky Jakub D, Wadham Jemma L, Jacobsen Carsten S

机构信息

Department of Geochemistry, Geological Survey of Denmark and Greenland (GEUS), Øster Voldgade 10, DK-1350, Copenhagen, Denmark.

Center for Permafrost (CENPERM), University of Copenhagen, Øster Voldgade 10, DK-1350, Copenhagen, Denmark.

出版信息

Environ Microbiol. 2017 Feb;19(2):524-534. doi: 10.1111/1462-2920.13483. Epub 2016 Aug 30.

DOI:10.1111/1462-2920.13483
PMID:27489963
Abstract

Microorganisms are flushed from the Greenland Ice Sheet (GrIS) where they may contribute towards the nutrient cycling and community compositions of downstream ecosystems. We investigate meltwater microbial assemblages as they exit the GrIS from a large outlet glacier, and as they enter a downstream river delta during the record melt year of 2012. Prokaryotic abundance, flux and community composition was studied, and factors affecting community structures were statistically considered. The mean concentration of cells exiting the ice sheet was 8.30 × 10 cells mL and we estimate that ∼1.02 × 10 cells were transported to the downstream fjord in 2012, equivalent to 30.95 Mg of carbon. Prokaryotic microbial assemblages were dominated by Proteobacteria, Bacteroidetes, and Actinobacteria. Cell concentrations and community compositions were stable throughout the sample period, and were statistically similar at both sample sites. Based on our observations, we argue that the subglacial environment is the primary source of the river-transported microbiota, and that cell export from the GrIS is dependent on discharge. We hypothesise that the release of subglacial microbiota to downstream ecosystems will increase as freshwater flux from the GrIS rises in a warming world.

摘要

微生物从格陵兰冰盖(GrIS)被冲刷出来,在那里它们可能对下游生态系统的养分循环和群落组成有所贡献。我们研究了融水微生物群落,它们从一条大型出口冰川流出格陵兰冰盖时,以及在2012年创纪录的融化年份进入下游河口三角洲时的情况。研究了原核生物的丰度、通量和群落组成,并对影响群落结构的因素进行了统计分析。从冰盖流出的细胞平均浓度为8.30×10个细胞/毫升,我们估计在2012年约有1.02×10个细胞被输送到下游峡湾,相当于30.95吨碳。原核微生物群落以变形菌门、拟杆菌门和放线菌门为主。在整个采样期间,细胞浓度和群落组成保持稳定,且在两个采样点在统计学上相似。基于我们的观察,我们认为冰下环境是河流输送微生物群的主要来源,并且从格陵兰冰盖输出的细胞取决于流量。我们推测,在气候变暖的世界里,随着来自格陵兰冰盖的淡水通量增加,冰下微生物群向下游生态系统的释放将会增加。

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