Research and Innovation Centre, Fondazione Edmund Mach, S. Michele all'Adige, Italy; National Biodiversity Future Center (NBFC), Università di Palermo, Palermo, Italy.
Competence Centre for Mountain Innovation Ecosystems, Free University of Bolzano, Bolzano/Bozen, Italy.
Sci Total Environ. 2024 Sep 20;944:173826. doi: 10.1016/j.scitotenv.2024.173826. Epub 2024 Jun 10.
In glacier-fed streams, the Windows of Opportunity (WOs) are periods of mild environmental conditions supporting the seasonal development of benthic microorganisms. WOs have been defined based on changes in biofilm biomass, but the responses of microbial diversity to WOs in Alpine streams have been overlooked. A two year (2017-2018) metabarcoding of epilithic and epipsammic biofilm prokaryotes was conducted in Alpine streams fed by glaciers (kryal), rock glaciers (rock glacial), or groundwater/precipitation (krenal) in two catchments of the Central-Eastern European Alps (Italy), aiming at testing the hypothesis that: 1) environmental WOs enhance not only the biomass but also the α-diversity of the prokaryotic biofilm in all stream types, 2) diversity and phenology of prokaryotic biofilm are mainly influenced by the physical habitat in glacial streams, and by water chemistry in the other two stream types. The study confirmed kryal and krenal streams as endmembers of epilithic and sediment prokaryotic α- and β-diversity, with rock glacial streams sharing a large proportion of taxa with the two other stream types. Alpha-diversity appeared to respond to ecological WOs, but, contrary to expectations, seasonality was less pronounced in the turbid kryal than in the clear streams. This was attributed to the small size of the glaciers feeding the studied kryal streams, whose discharge dynamics were those typical of the late phase of deglaciation. Prokaryotic α-diversity of non-glacial streams tended to be higher in early summer than in early autumn. Our findings, while confirming that high altitude streams are heavily threatened by climate change, underscore the still neglected role of rock glacier runoffs as climate refugia for the most stenothermic benthic aquatic microorganism. This advocates the need to define and test strategies for protecting these ecosystems for preserving, restoring, and connecting cold Alpine aquatic biodiversity in the context of the progressing global warming.
在冰川补给的溪流中,机会之窗(Windows of Opportunity,WO)是指环境条件较为温和的时期,有利于底栖微生物的季节性发育。WO 是根据生物膜生物量的变化来定义的,但微生物多样性对高山溪流 WO 的响应却被忽视了。本研究采用两年(2017-2018 年)宏条形码技术,对阿尔卑斯山两个流域(意大利)中由冰川(kryal)、岩石冰川(rock glacial)或地下水/降水(krenal)补给的高山溪流中的表生和表土生物膜原核生物进行了研究,旨在检验以下假设:1)环境 WO 不仅能增加所有溪流类型中生物膜的生物量,还能增加原核生物的 α-多样性;2)原核生物生物膜的多样性和物候主要受冰川溪流的物理生境以及其他两种溪流类型的水化学影响。研究结果证实,kryal 和 krenal 溪流是表生和沉积物中原核生物 α-和 β-多样性的端元,而岩石冰川溪流与其他两种溪流类型共享大量的分类群。α-多样性似乎对生态 WO 有响应,但与预期相反,混浊的 kryal 溪流的季节性不如清澈溪流明显。这归因于为研究 kryal 溪流提供水源的冰川较小,其流量动态与冰川消退后期的典型特征相似。非冰川溪流的原核生物 α-多样性在初夏时往往高于初秋。我们的研究结果虽然证实了高海拔溪流受到气候变化的严重威胁,但强调了岩石冰川径流作为最耐寒的底栖水生微生物的气候避难所的作用仍被忽视。这表明需要定义和测试保护这些生态系统的策略,以保护寒冷的阿尔卑斯山水生生物多样性,在全球变暖的背景下,恢复和连接这些生态系统。