Tardigrade distribution in soils of high Arctic habitats

Abstract Tardigrades are omnipresent microfauna with scarce record on their ecology in soils. Here, we investigated soil inhabiting tardigrade communities in five contrasting polar habitats, evaluating their abundance, diversity, species richness, and species composition. Moreover, we measured selec...

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Published in:Ecology and Evolution
Main Authors: Michala Tůmová, Veronika Jílková, Petr Macek, Miloslav Devetter
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
Online Access:https://doi.org/10.1002/ece3.11386
https://doaj.org/article/0cf654d197834a76b102c2d4ac1b1df7
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spelling ftdoajarticles:oai:doaj.org/article:0cf654d197834a76b102c2d4ac1b1df7 2024-09-15T18:39:42+00:00 Tardigrade distribution in soils of high Arctic habitats Michala Tůmová Veronika Jílková Petr Macek Miloslav Devetter 2024-07-01T00:00:00Z https://doi.org/10.1002/ece3.11386 https://doaj.org/article/0cf654d197834a76b102c2d4ac1b1df7 EN eng Wiley https://doi.org/10.1002/ece3.11386 https://doaj.org/toc/2045-7758 2045-7758 doi:10.1002/ece3.11386 https://doaj.org/article/0cf654d197834a76b102c2d4ac1b1df7 Ecology and Evolution, Vol 14, Iss 7, Pp n/a-n/a (2024) bird cliff soil microfauna soil structure water bears Ecology QH540-549.5 article 2024 ftdoajarticles https://doi.org/10.1002/ece3.11386 2024-08-26T15:21:18Z Abstract Tardigrades are omnipresent microfauna with scarce record on their ecology in soils. Here, we investigated soil inhabiting tardigrade communities in five contrasting polar habitats, evaluating their abundance, diversity, species richness, and species composition. Moreover, we measured selected soil physico‐chemical properties to find the drivers of tardigrade distribution among these habitats. In spite of reported tardigrade viability in extreme conditions, glacier forelands represented a habitat almost devoid of tardigrades. Even dry and wet tundra with soil developing for over more than 10 000 years held low abundances compared to usual numbers of tardigrades in temperate habitats. Polar habitats also differ in species composition, with Diaforobiotus islandicus being typical species for dry and Hypsibius exemplaris for wet tundra. Overall, tardigrade abundance was affected by the content of nutrients as well as physical properties of soil, i.e. content of total nitrogen (TN), total organic carbon (TOC), stoniness, soil texture and the water holding capacity (WHC). While diversity and species composition were significantly related to soil physical properties such as the bulk density (BD), soil texture, stoniness, and WHC. Physical structure of environment was, therefore, an important predictor of tardigrade distribution in polar habitats. Since many studies failed to identify significant determinants of tardigrade distribution, we encourage scientists to include physical properties of tardigrade habitats as explanatory variables in their studies. Article in Journal/Newspaper Tundra Tardigrade Directory of Open Access Journals: DOAJ Articles Ecology and Evolution 14 7
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic bird cliff
soil microfauna
soil structure
water bears
Ecology
QH540-549.5
spellingShingle bird cliff
soil microfauna
soil structure
water bears
Ecology
QH540-549.5
Michala Tůmová
Veronika Jílková
Petr Macek
Miloslav Devetter
Tardigrade distribution in soils of high Arctic habitats
topic_facet bird cliff
soil microfauna
soil structure
water bears
Ecology
QH540-549.5
description Abstract Tardigrades are omnipresent microfauna with scarce record on their ecology in soils. Here, we investigated soil inhabiting tardigrade communities in five contrasting polar habitats, evaluating their abundance, diversity, species richness, and species composition. Moreover, we measured selected soil physico‐chemical properties to find the drivers of tardigrade distribution among these habitats. In spite of reported tardigrade viability in extreme conditions, glacier forelands represented a habitat almost devoid of tardigrades. Even dry and wet tundra with soil developing for over more than 10 000 years held low abundances compared to usual numbers of tardigrades in temperate habitats. Polar habitats also differ in species composition, with Diaforobiotus islandicus being typical species for dry and Hypsibius exemplaris for wet tundra. Overall, tardigrade abundance was affected by the content of nutrients as well as physical properties of soil, i.e. content of total nitrogen (TN), total organic carbon (TOC), stoniness, soil texture and the water holding capacity (WHC). While diversity and species composition were significantly related to soil physical properties such as the bulk density (BD), soil texture, stoniness, and WHC. Physical structure of environment was, therefore, an important predictor of tardigrade distribution in polar habitats. Since many studies failed to identify significant determinants of tardigrade distribution, we encourage scientists to include physical properties of tardigrade habitats as explanatory variables in their studies.
format Article in Journal/Newspaper
author Michala Tůmová
Veronika Jílková
Petr Macek
Miloslav Devetter
author_facet Michala Tůmová
Veronika Jílková
Petr Macek
Miloslav Devetter
author_sort Michala Tůmová
title Tardigrade distribution in soils of high Arctic habitats
title_short Tardigrade distribution in soils of high Arctic habitats
title_full Tardigrade distribution in soils of high Arctic habitats
title_fullStr Tardigrade distribution in soils of high Arctic habitats
title_full_unstemmed Tardigrade distribution in soils of high Arctic habitats
title_sort tardigrade distribution in soils of high arctic habitats
publisher Wiley
publishDate 2024
url https://doi.org/10.1002/ece3.11386
https://doaj.org/article/0cf654d197834a76b102c2d4ac1b1df7
genre Tundra
Tardigrade
genre_facet Tundra
Tardigrade
op_source Ecology and Evolution, Vol 14, Iss 7, Pp n/a-n/a (2024)
op_relation https://doi.org/10.1002/ece3.11386
https://doaj.org/toc/2045-7758
2045-7758
doi:10.1002/ece3.11386
https://doaj.org/article/0cf654d197834a76b102c2d4ac1b1df7
op_doi https://doi.org/10.1002/ece3.11386
container_title Ecology and Evolution
container_volume 14
container_issue 7
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