4.7 Article

Moss and Liverwort Covers Structure Soil Bacterial and Fungal Communities Differently in the Icelandic Highlands

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MICROBIAL ECOLOGY
卷 86, 期 3, 页码 1893-1908

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SPRINGER
DOI: 10.1007/s00248-023-02194-x

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Cryptogamic cover; Bryophyte; Iceland; Metabarcoding; Microbial ecology; Polar areas

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Cryptogamic covers, such as bryophytes and lichens, are the first visible colonizers of deglaciated areas in polar tundra regions. In this study, we analyzed the influence of bryophyte covers dominated by different lineages on the diversity and composition of bacterial and fungal communities, as well as the abiotic attributes of soils in the southern part of the Highlands of Iceland. Our findings indicate that the composition of cryptogamic covers affects soil microbial communities and abiotic attributes, which is valuable for predicting the biotic responses of polar ecosystems to future climate change.
Cryptogamic covers extend over vast polar tundra regions and their main components, e.g., bryophytes and lichens, are frequently the first visible colonizers of deglaciated areas. To understand their role in polar soil development, we analyzed how cryptogamic covers dominated by different bryophyte lineages (mosses and liverworts) influence the diversity and composition of edaphic bacterial and fungal communities as well as the abiotic attributes of underlying soils in the southern part of the Highlands of Iceland. For comparison, the same traits were examined in soils devoid of bryophyte covers. We measured an increase in soil C, N, and organic matter contents coupled with a lower pH in association with bryophyte cover establishment. However, liverwort covers showed noticeably higher C and N contents than moss covers. Significant changes in diversity and composition of bacterial and fungal communities were revealed between (a) bare and bryophyte-covered soils, (b) bryophyte covers and the underlying soils, and (c) moss and liverworts covers. These differences were more obvious for fungi than bacteria, and involved different lineages of saprotrophic and symbiotic fungi, which suggests a certain specificity of microbial taxa to particular bryophyte groups. In addition, differences observed in the spatial structure of the two bryophyte covers may be also responsible for the detected differences in microbial community diversity and composition. Altogether, our findings indicate that soil microbial communities and abiotic attributes are ultimately affected by the composition of the most conspicuous elements of cryptogamic covers in polar regions, which is of great value to predict the biotic responses of these ecosystems to future climate change.

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