Relationship between Species Richness, Biomass and Structure of Vegetation and Mycobiota along an Altitudinal Transect in the Polar Urals
Aboveground species richness patterns of vascular plants, aphyllophoroid macrofungi, bryophytes and lichens were compared along an altitudinal gradient (80–310 m a.s.l.) on the Slantsevaya mountain at the eastern macroslope of the Polar Urals (Russia). Five altitudinal levels were included in the st...
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2020-12-01
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author | Anton G. Shiryaev Ursula Peintner Vladimir V. Elsakov Svetlana Yu. Sokovnina Denis A. Kosolapov Olga S. Shiryaeva Nadezhda M. Devi Andrei A. Grigoriev |
author_facet | Anton G. Shiryaev Ursula Peintner Vladimir V. Elsakov Svetlana Yu. Sokovnina Denis A. Kosolapov Olga S. Shiryaeva Nadezhda M. Devi Andrei A. Grigoriev |
author_sort | Anton G. Shiryaev |
collection | DOAJ |
description | Aboveground species richness patterns of vascular plants, aphyllophoroid macrofungi, bryophytes and lichens were compared along an altitudinal gradient (80–310 m a.s.l.) on the Slantsevaya mountain at the eastern macroslope of the Polar Urals (Russia). Five altitudinal levels were included in the study: (1) Northern boreal forest with larch-spruce in the Sob’ river valley habitats; (2–3) two levels of closed, northern boreal, larch-dominated forests on the slopes; (4) crook-stemmed forest; (5) tundra habitats above the timberline. Vascular plant or bryophyte species richness was not affected by altitudinal levels, but lichen species richness significantly increased from the river valley to the tundra. For aphyllophoroid macrofungi, species richness was highest at intermediate and low altitudes, and poorest in the tundra. These results indicate a positive ecotone effect on aphyllophoroid fungal species richness. The species richness of aphyllophoroid fungi as a whole was neither correlated to mortmass stocks, nor to species richness of vascular plants, but individual ecological or morphological groups depended on these parameters. Poroid fungal species richness was positively correlated to tree age, wood biomass and crown density, and therefore peaked in the middle of the slope and at the foot of the mountain. In contrast, clavarioid fungal species richness was negatively related to woody bio- and mortmass, and therefore peaked in the tundra. This altitudinal level was characterized by high biomass proportions of lichens and mosses, and by high litter mortmass. The proportion of corticoid fungi increased with altitude, reaching its maximum at the timberline. Results from the different methods used in this work were concordant, and showed significant patterns. Tundra communities differ significantly from the forest communities, as is also confirmed by nonmetric multidimensional scaling (NMDS) analyses based on the spectrum of morphological and ecological groups of aphyllophoroid fungi. |
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spelling | doaj.art-015aa31e16f34b0ba76242627959be372023-11-21T00:03:06ZengMDPI AGJournal of Fungi2309-608X2020-12-016435310.3390/jof6040353Relationship between Species Richness, Biomass and Structure of Vegetation and Mycobiota along an Altitudinal Transect in the Polar UralsAnton G. Shiryaev0Ursula Peintner1Vladimir V. Elsakov2Svetlana Yu. Sokovnina3Denis A. Kosolapov4Olga S. Shiryaeva5Nadezhda M. Devi6Andrei A. Grigoriev7Vegetation and Mycobiota Biodiversity Department, Institute of Plant and Animal Ecology, Ural Branch of the Russian Academy of Sciences, 8 March Str., 202, 620144 Ekaterinburg, RussiaInstitute of Microbiology, Innsbruck University, Technikerstr. 25, 6020 Innsbruck, AustriaKomi Scientific Centre, Northern Flora and Vegetation Department, Institute of Biology, Ural Branch of the Russian Academy of Sciences, Kommunisticheskaya Str., 28, 167982 Syktyvkar, RussiaArctic Research Station, Institute of Plant and Animal Ecology, Ural Branch of the Russian Academy of Sciences, Zelenaya Gorka Str., 21, 629400 Labytnangi, RussiaKomi Scientific Centre, Northern Flora and Vegetation Department, Institute of Biology, Ural Branch of the Russian Academy of Sciences, Kommunisticheskaya Str., 28, 167982 Syktyvkar, RussiaVegetation and Mycobiota Biodiversity Department, Institute of Plant and Animal Ecology, Ural Branch of the Russian Academy of Sciences, 8 March Str., 202, 620144 Ekaterinburg, RussiaDendrochronology Department, Institute of Plant and Animal Ecology, Ural Branch of the Russian Academy of Sciences, 8 March Str., 202, 620144 Ekaterinburg, RussiaGeoinformation Technologies Department, Institute of Plant and Animal Ecology, Ural Branch of the Russian Academy of Sciences, 8 March Str., 202, 620144 Ekaterinburg, RussiaAboveground species richness patterns of vascular plants, aphyllophoroid macrofungi, bryophytes and lichens were compared along an altitudinal gradient (80–310 m a.s.l.) on the Slantsevaya mountain at the eastern macroslope of the Polar Urals (Russia). Five altitudinal levels were included in the study: (1) Northern boreal forest with larch-spruce in the Sob’ river valley habitats; (2–3) two levels of closed, northern boreal, larch-dominated forests on the slopes; (4) crook-stemmed forest; (5) tundra habitats above the timberline. Vascular plant or bryophyte species richness was not affected by altitudinal levels, but lichen species richness significantly increased from the river valley to the tundra. For aphyllophoroid macrofungi, species richness was highest at intermediate and low altitudes, and poorest in the tundra. These results indicate a positive ecotone effect on aphyllophoroid fungal species richness. The species richness of aphyllophoroid fungi as a whole was neither correlated to mortmass stocks, nor to species richness of vascular plants, but individual ecological or morphological groups depended on these parameters. Poroid fungal species richness was positively correlated to tree age, wood biomass and crown density, and therefore peaked in the middle of the slope and at the foot of the mountain. In contrast, clavarioid fungal species richness was negatively related to woody bio- and mortmass, and therefore peaked in the tundra. This altitudinal level was characterized by high biomass proportions of lichens and mosses, and by high litter mortmass. The proportion of corticoid fungi increased with altitude, reaching its maximum at the timberline. Results from the different methods used in this work were concordant, and showed significant patterns. Tundra communities differ significantly from the forest communities, as is also confirmed by nonmetric multidimensional scaling (NMDS) analyses based on the spectrum of morphological and ecological groups of aphyllophoroid fungi.https://www.mdpi.com/2309-608X/6/4/353biodiversityfungal ecologyclimatic gradientproductivityfloralichen |
spellingShingle | Anton G. Shiryaev Ursula Peintner Vladimir V. Elsakov Svetlana Yu. Sokovnina Denis A. Kosolapov Olga S. Shiryaeva Nadezhda M. Devi Andrei A. Grigoriev Relationship between Species Richness, Biomass and Structure of Vegetation and Mycobiota along an Altitudinal Transect in the Polar Urals Journal of Fungi biodiversity fungal ecology climatic gradient productivity flora lichen |
title | Relationship between Species Richness, Biomass and Structure of Vegetation and Mycobiota along an Altitudinal Transect in the Polar Urals |
title_full | Relationship between Species Richness, Biomass and Structure of Vegetation and Mycobiota along an Altitudinal Transect in the Polar Urals |
title_fullStr | Relationship between Species Richness, Biomass and Structure of Vegetation and Mycobiota along an Altitudinal Transect in the Polar Urals |
title_full_unstemmed | Relationship between Species Richness, Biomass and Structure of Vegetation and Mycobiota along an Altitudinal Transect in the Polar Urals |
title_short | Relationship between Species Richness, Biomass and Structure of Vegetation and Mycobiota along an Altitudinal Transect in the Polar Urals |
title_sort | relationship between species richness biomass and structure of vegetation and mycobiota along an altitudinal transect in the polar urals |
topic | biodiversity fungal ecology climatic gradient productivity flora lichen |
url | https://www.mdpi.com/2309-608X/6/4/353 |
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