Abstract
We examined the variations in microfungal communities from different surface types (cyanobacterial crusts, lichen-dominated crusts, and noncrusted bare surface) at two different positions—north-oriented slope and sun-exposed plain in the Tabernas Desert, Spain. A total of 77 species from 46 genera was isolated using the soil dilution plate method. The studied mycobiota, similar to the majority of desert mycobiotas, was dominated by melanin-containing species. However, in the Tabernas crusts, unlike the studied crusts of the Negev Desert (Israel) and the Tengger Desert (China), melanized fungi with large multicellular spores were much less abundantly represented, while the thermotolerant group, Aspergillus spp., remarkably contributed to the communities’ structure. Density of microfungal isolates positively correlated with chlorophyll content indicating possible significant influence of organic matter content on fungal biomass. The variations in crust composition, biomass, and the position of habitats were accompanied by the variations in microfungal community structure, diversity level, and isolate densities, with the communities at the plain sun-exposed position being much less variable than the communities at the north-oriented position. The study shows that microclimatic and edaphic factors play an essential role in the development of crust and noncrust microfungal communities, and their structure can be a sensitive indicator of changing environmental conditions at a microscale.
Highlights
Biological soil crusts (BSCs, biocrusts) are widely distributed components of arid and semiarid ecosystems, which make a significant contribution to soil surface stabilization, hydrological processes, and nutrient cycling, e.g., References [1,2,3,4]
The chlorophyll content in the most xeric lichen crusts dominated by P. decipiens was significantly lower than that in the mesic lichens crusts dominated by
PH was higher at the north-oriented positon, while in the crusts, higher pH values were recorded at the plain south-exposed position
Summary
Biological soil crusts (BSCs, biocrusts) are widely distributed components of arid and semiarid ecosystems, which make a significant contribution to soil surface stabilization, hydrological processes, and nutrient cycling, e.g., References [1,2,3,4]. Free-living microfungi, together with cyanobacteria, heterotrophic bacteria, green algae, lichens, and mosses play an important role in the composition and functioning of the BSCs. Several studies conducted in the deserts and semiarid grasslands, based both on culture-dependent methods [9,10]. On culture-independent molecular approaches [11,12,13,14,15,16,17], revealed a rich diversity of crust-inhabiting fungi mainly belonging to the phylum Ascomycota.
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