不断变化的北冰洋中细菌和古细菌群落动态的多年时间序列(2004-2012 年

IF 5.1 Q1 ECOLOGY
Susanne A Kraemer, A. Ramachandran, Vera E. Onana, William K W Li, David A Walsh
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引用次数: 0

摘要

气候变化正在对北极产生深远影响,导致多年海冰消失,北冰洋上层变得更温暖、更清新。微生物群落对这些由气候引起的变化的反应在很大程度上是未知的。在这里,我们记录了加拿大海盆 9 年时间序列中细菌和古细菌群落的年际变化,其中包括两次历史上的海冰最小值(2007 年和 2012 年)。我们报告了细菌和古生物群落丰富度的总体下降以及群落组成的显著变化。分层水层的变化幅度和最快速变化的时期各不相同。在时间序列中,上层水(表层混合层和北极上层水)的变化最明显,而下层水(太平洋源水)的变化较晚。分类组成在不同时间段的变化是微妙的,但最明显的变化特征是类细菌群(Bacteroidota)分类群的减少和潮海生物群(Thaumarchaeota)与极海生物群(Euryarchaeota)分类群的增加。这一时间序列为了解气候变化对北极微生物群落的潜在影响提供了难得的一瞥;将这一时间序列扩展到今天,将有助于更深入地了解北极海洋生态系统对气候变暖和清新的响应轨迹。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A multiyear time series (2004–2012) of bacterial and archaeal community dynamics in a changing Arctic Ocean
Climate change is profoundly impacting the Arctic, leading to a loss of multiyear sea ice and a warmer, fresher upper Arctic Ocean. The response of microbial communities to these climate-mediated changes is largely unknown. Here, we document the interannual variation in bacterial and archaeal communities across a 9-year time series of the Canada Basin that includes two historic sea ice minima (2007 and 2012). We report an overall loss of bacterial and archaeal community richness and significant shifts in community composition. The magnitude and period of most rapid change differed between the stratified water layers. The most pronounced changes in the upper water layers (surface mixed layer and upper Arctic water) occurred earlier in the time series, while changes in the lower layer (Pacific-origin water) occurred later. Shifts in taxonomic composition across time were subtle, but a decrease in Bacteroidota taxa and increase in Thaumarchaeota and Euryarchaeota taxa were the clearest signatures of change. This time series provides a rare glimpse into the potential influence of climate change on Arctic microbial communities; extension to the present day should contribute to deeper insights into the trajectory of Arctic marine ecosystems in response to warming and freshening.
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