4.3 Article

Myco- and photobiont associations in crustose lichens in the McMurdo Dry Valleys (Antarctica) reveal high differentiation along an elevational gradient

Journal

POLAR BIOLOGY
Volume 43, Issue 12, Pages 1967-1983

Publisher

SPRINGER
DOI: 10.1007/s00300-020-02754-8

Keywords

Crustose lichens; Specificity; Spatial patterns; Polar desert; Foehn winds; Humidity

Funding

  1. Paris Lodron University of Salzburg

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Climatically extreme regions such as the polar deserts of the McMurdo Dry Valleys (78 degrees S) in Continental Antarctica are key areas for a better understanding of changes in ecosystems. Therefore, it is particularly important to analyze and communicate current patterns of biodiversity in these sensitive areas, where precipitation mostly occurs in form of snow and liquid water is rare. Humidity provided by dew, clouds, and fog are the main water sources, especially for rock-dwelling crustose lichens as one of the most common vegetation-forming organisms. We investigated the diversity and interaction specificity of myco-/photobiont associations of 232 crustose lichen specimens, collected along an elevational gradient (171-959 m a.s.l.) within the McMurdo Dry Valleys. The mycobiont species and photobiont OTUs were identified by using three markers each (nrITS, mtSSU,RPB1,and nrITS, psbJ-L, COX2). Elevation, positively associated with water availability, turned out to be the key factor explaining most of the distribution patterns of the mycobionts. Pairwise comparisons showedLecidea cancriformisandRhizoplaca macleaniito be significantly more common at higher elevations andCarbonea vorticosaandLecidea polypycnidophoraat lower elevations. Lichen photobionts were dominated by the globally distributedTrebouxiaOTU,Tr_A02 which occurred at all habitats. Network specialization resulting from myco-/photobiont bipartite network structure varied with elevation and associated abiotic factors. Along an elevational gradient, the spatial distribution, diversity, and genetic variability of the lichen symbionts appear to be mainly influenced by improved water relations at higher altitudes.

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