Longitudinal changes of clavarioid funga (Basidiomycota) diversity in the tundra zone of Eurasia

The study deals with certain variations of the diversity level of clavarioid funga in the 33 localities (100 km2 each) inside seven longitudinal sectors (100,000 km2) situated along the gradient of the climatic continentality of the Eurasian tundra zone. As continentality increases, from the maritim...

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Published in:Mycology
Main Author: Anton G. Shiryaev
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2017
Subjects:
Online Access:https://doi.org/10.1080/21501203.2017.1345801
https://doaj.org/article/3ab720cde1c14a468cd2481f446ef9e2
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spelling ftdoajarticles:oai:doaj.org/article:3ab720cde1c14a468cd2481f446ef9e2 2023-05-15T14:57:53+02:00 Longitudinal changes of clavarioid funga (Basidiomycota) diversity in the tundra zone of Eurasia Anton G. Shiryaev 2017-07-01T00:00:00Z https://doi.org/10.1080/21501203.2017.1345801 https://doaj.org/article/3ab720cde1c14a468cd2481f446ef9e2 EN eng Taylor & Francis Group http://dx.doi.org/10.1080/21501203.2017.1345801 https://doaj.org/toc/2150-1203 https://doaj.org/toc/2150-1211 2150-1203 2150-1211 doi:10.1080/21501203.2017.1345801 https://doaj.org/article/3ab720cde1c14a468cd2481f446ef9e2 Mycology, Vol 8, Iss 3, Pp 135-146 (2017) Arctic biogeography climate change distribution spatial turnover permafrost Biology (General) QH301-705.5 Microbiology QR1-502 article 2017 ftdoajarticles https://doi.org/10.1080/21501203.2017.1345801 2022-12-31T03:24:05Z The study deals with certain variations of the diversity level of clavarioid funga in the 33 localities (100 km2 each) inside seven longitudinal sectors (100,000 km2) situated along the gradient of the climatic continentality of the Eurasian tundra zone. As continentality increases, from the maritime climate of Fennoscandia to the continental climate of Yakutia, α-diversity and γ-diversity decrease considerably. On the other side, spatial turnover of species, or β-diversity, grows in the direction of continental areas. This paper uses the following methods to assess the spatial turnover: Whittaker’s index and mean Jaccard similarity index, as well as by several other parameters. In addition, our data show that the genus Typhula is richest in the tundra, and its share in the structure of the clavarioid funga grows as the studied area decreases, as well as when the environmental conditions become more severe (continentality of the climate). Also, the paper discusses the issue of newly emerging taiga fungi species in the European Arctic, which is connected with climatic warming followed by ″greening″ of the tundra. Note that in the cryo-semiarid continental climate of Yakutia, where climatic changes are just as pronounced, no new taxons have been discovered so far. Article in Journal/Newspaper Arctic Climate change Fennoscandia permafrost taiga Tundra Yakutia Directory of Open Access Journals: DOAJ Articles Arctic Mycology 8 3 135 146
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Arctic
biogeography
climate change
distribution
spatial turnover
permafrost
Biology (General)
QH301-705.5
Microbiology
QR1-502
spellingShingle Arctic
biogeography
climate change
distribution
spatial turnover
permafrost
Biology (General)
QH301-705.5
Microbiology
QR1-502
Anton G. Shiryaev
Longitudinal changes of clavarioid funga (Basidiomycota) diversity in the tundra zone of Eurasia
topic_facet Arctic
biogeography
climate change
distribution
spatial turnover
permafrost
Biology (General)
QH301-705.5
Microbiology
QR1-502
description The study deals with certain variations of the diversity level of clavarioid funga in the 33 localities (100 km2 each) inside seven longitudinal sectors (100,000 km2) situated along the gradient of the climatic continentality of the Eurasian tundra zone. As continentality increases, from the maritime climate of Fennoscandia to the continental climate of Yakutia, α-diversity and γ-diversity decrease considerably. On the other side, spatial turnover of species, or β-diversity, grows in the direction of continental areas. This paper uses the following methods to assess the spatial turnover: Whittaker’s index and mean Jaccard similarity index, as well as by several other parameters. In addition, our data show that the genus Typhula is richest in the tundra, and its share in the structure of the clavarioid funga grows as the studied area decreases, as well as when the environmental conditions become more severe (continentality of the climate). Also, the paper discusses the issue of newly emerging taiga fungi species in the European Arctic, which is connected with climatic warming followed by ″greening″ of the tundra. Note that in the cryo-semiarid continental climate of Yakutia, where climatic changes are just as pronounced, no new taxons have been discovered so far.
format Article in Journal/Newspaper
author Anton G. Shiryaev
author_facet Anton G. Shiryaev
author_sort Anton G. Shiryaev
title Longitudinal changes of clavarioid funga (Basidiomycota) diversity in the tundra zone of Eurasia
title_short Longitudinal changes of clavarioid funga (Basidiomycota) diversity in the tundra zone of Eurasia
title_full Longitudinal changes of clavarioid funga (Basidiomycota) diversity in the tundra zone of Eurasia
title_fullStr Longitudinal changes of clavarioid funga (Basidiomycota) diversity in the tundra zone of Eurasia
title_full_unstemmed Longitudinal changes of clavarioid funga (Basidiomycota) diversity in the tundra zone of Eurasia
title_sort longitudinal changes of clavarioid funga (basidiomycota) diversity in the tundra zone of eurasia
publisher Taylor & Francis Group
publishDate 2017
url https://doi.org/10.1080/21501203.2017.1345801
https://doaj.org/article/3ab720cde1c14a468cd2481f446ef9e2
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Fennoscandia
permafrost
taiga
Tundra
Yakutia
genre_facet Arctic
Climate change
Fennoscandia
permafrost
taiga
Tundra
Yakutia
op_source Mycology, Vol 8, Iss 3, Pp 135-146 (2017)
op_relation http://dx.doi.org/10.1080/21501203.2017.1345801
https://doaj.org/toc/2150-1203
https://doaj.org/toc/2150-1211
2150-1203
2150-1211
doi:10.1080/21501203.2017.1345801
https://doaj.org/article/3ab720cde1c14a468cd2481f446ef9e2
op_doi https://doi.org/10.1080/21501203.2017.1345801
container_title Mycology
container_volume 8
container_issue 3
container_start_page 135
op_container_end_page 146
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