Diatom diversity in headwaters influenced by permafrost thawing: First evidence from the Central Italian Alps

Q3 Earth and Planetary Sciences Advances in Oceanography and Limnology Pub Date : 2018-12-20 DOI:10.4081/AIOL.2018.7929
Federica Rotta, L. Cerasino, A. Occhipinti‐Ambrogi, M. Rogora, R. Seppi, M. Tolotti
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引用次数: 8

Abstract

Glacier melting and permafrost thawing are the most evident effects of the current climate change that is strongly affecting high mountain areas, including the European Alps. As the thawing rate of subsurface ice is lower than for glacier ice, it is expected that, while glaciers retreat, an increasing number of Alpine headwaters will become more influenced by permafrost degradation during the 21st century. Despite the expected change in the relative importance of glacier and permafrost in determining Alpine hydrology, studies addressing effects of permafrost thawing on chemical and, especially, biological features of adjacent surface waters are still scarce. The present study contributes to characterise the epilithic and epiphytic diatom diversity in a set of permafrost-fed headwaters in three sub-catchments differing in bedrock lithology of the Italian Central Alps (Trentino Alto-Adige) in relation to water chemistry and habitat features. In addition, it explores chemical and biological differences between permafrost-fed streams and headwaters with no direct contact to permafrost, namely glacier-fed (kryal) and precipitation-/groundwater-fed (rhithral) streams. Permafrost-fed waters showed higher electrical conductivity and enhanced ion concentrations than glacier- and precipitation-fed waters, while concentration of trace elements (e.g. Sr, Ni, Zn, As) were more irregularly distributed among waters of different origin, though they showed a tendency to reach higher levels in permafrost-fed waters. Diatom species richness and diversity were lower in permafrost-fed headwaters, and were principally related to water pH and trace metal concentrations. Epiphytic diatom assemblages were more diverse than epilithic ones, independently from the water origin, while differences in species composition were not sufficient to unequivocally identify a typical diatom composition for the different water types considered in this study.
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受永久冻土融化影响的源头硅藻多样性:来自意大利中部阿尔卑斯山的首次证据
冰川融化和永久冻土融化是当前气候变化最明显的影响,它正在强烈影响包括欧洲阿尔卑斯山在内的高山地区。由于地下冰的融化速度低于冰川冰,预计在冰川退缩的同时,越来越多的高山源头将在21世纪受到多年冻土退化的更大影响。尽管冰川和永久冻土在决定高山水文方面的相对重要性有望发生变化,但研究永久冻土融化对邻近地表水的化学、特别是生物特征的影响仍然很少。本研究对意大利中部阿尔卑斯(Trentino Alto-Adige)基岩岩性不同的三个子集水区的一组永久冻土区水源中附着硅藻和附生硅藻的多样性与水化学和栖息地特征的关系进行了研究。此外,它还探讨了以永久冻土为水源的河流和与永久冻土没有直接接触的水源之间的化学和生物学差异,即冰川为水源(kryal)和降水/地下水为水源(rhithral)的河流。与冰川和降水补给水相比,冻土补给水的电导率和离子浓度更高,而微量元素(如Sr、Ni、Zn、As)的浓度在不同来源的水之间分布更为不规则,但在冻土补给水中呈现出较高的趋势。土壤源区硅藻物种丰富度和多样性较低,主要与水体pH和微量金属浓度有关。附生硅藻组合比附生硅藻更多样化,独立于水源,而物种组成的差异不足以明确确定本研究中考虑的不同水类型的典型硅藻组成。
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来源期刊
Advances in Oceanography and Limnology
Advances in Oceanography and Limnology Agricultural and Biological Sciences-Aquatic Science
CiteScore
2.00
自引率
0.00%
发文量
2
审稿时长
12 weeks
期刊介绍: Advances in Oceanography and Limnology was born in 2010 from the 35 years old Proceedings of the national congress of the Italian Association of Oceanology and Limnology. The AIOL Journal was funded as an interdisciplinary journal embracing both fundamental and applied Oceanographic and Limnological research, with focus on both single and multiple disciplines. Currently, two regular issues of the journal are published each year. In addition, Special Issues that focus on topics that are timely and of interest to a significant number of Limnologists and Oceanographers are also published. The journal, which is intended as an official publication of the AIOL, is also published in association with the EFFS (European Federation for Freshwater Sciences), which aims and objectives are directed towards the promotion of freshwater sciences throughout Europe. Starting from the 2015 issue, the AIOL Journal is published as an Open Access, peer-reviewed journal. Space is given to regular articles, review, short notes and opinion paper
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