Area, depth and elevation of cryoconite holes in the Arctic do not influence Tardigrada densities

Water bears (Tardigrada) are known as one of the most extremophile animals in the world. They inhabit environments from the deepest parts of the oceans up to the highest mountains. One of the most extreme and still poorly studied habitats which tardigrades inhabit are cryoconite holes. We analysed t...

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Published in:Polish Polar Research
Main Authors: Zawierucha Krzysztof, Vonnahme Tobias R., Devetter Miloslav, Kolicka Małgorzata, Ostrowska Marta, Chmielewski Sebastian, Kosicki Jakub Z.
Format: Article in Journal/Newspaper
Language:English
Published: Polish Academy of Sciences 2016
Subjects:
Online Access:https://doi.org/10.1515/popore-2016-0009
https://doaj.org/article/e845485964744a60ab76fef5c15d219a
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spelling ftdoajarticles:oai:doaj.org/article:e845485964744a60ab76fef5c15d219a 2023-05-15T14:50:22+02:00 Area, depth and elevation of cryoconite holes in the Arctic do not influence Tardigrada densities Zawierucha Krzysztof Vonnahme Tobias R. Devetter Miloslav Kolicka Małgorzata Ostrowska Marta Chmielewski Sebastian Kosicki Jakub Z. 2016-06-01T00:00:00Z https://doi.org/10.1515/popore-2016-0009 https://doaj.org/article/e845485964744a60ab76fef5c15d219a EN eng Polish Academy of Sciences http://www.degruyter.com/view/j/popore.2016.37.issue-2/popore-2016-0009/popore-2016-0009.xml?format=INT https://doaj.org/toc/2081-8262 2081-8262 doi:10.1515/popore-2016-0009 https://doaj.org/article/e845485964744a60ab76fef5c15d219a Polish Polar Research, Vol 37, Iss 2, Pp 325-334 (2016) Arctic Svalbard Tardigrada cryoconite holes ecology glaciers Geology QE1-996.5 article 2016 ftdoajarticles https://doi.org/10.1515/popore-2016-0009 2022-12-31T04:38:41Z Water bears (Tardigrada) are known as one of the most extremophile animals in the world. They inhabit environments from the deepest parts of the oceans up to the highest mountains. One of the most extreme and still poorly studied habitats which tardigrades inhabit are cryoconite holes. We analysed the relation between area, depth, elevation and tardigrades densities in cryoconite holes on four glaciers on Spitsbergen. The mean (±SD) of cryoconite area was 1287.21±2400.8 cm2, while the depth was on average 10.8±11.2 cm, the elevation 172.6±109.66 m a.s.l., and tardigrade density 24.9±33.0 individuals per gram of wet material (n = 38). The densities of tardigrades on Hans Glacier reached values of up to 168 ind. cm3, 104 ind. g−1 wet weight, and 275 ind. g−1 dry weight. The densities of tardigrades of the three glaciers in Billefjorden were up to 82 ind. cm2, 326 ind. g−1 wet weight and 624 ind. g−1 dry weight. Surprisingly, although the model included area, depth and elevation as independent variables, it cannot explain Tardigrada density in cryoconite holes. We propose that due to the rapid melting of the glacier surface in the Arctic, the constant flushing of cryoconite sediments, and inter-hole water-sediment mixing, the functioning of these ecosystems is disrupted. We conclude that cryoconite holes are dynamic ecosystems for microinvertebrates in the Arctic. Article in Journal/Newspaper Arctic Billefjorden glacier Polar Research Svalbard Spitsbergen Tardigrade Directory of Open Access Journals: DOAJ Articles Arctic Billefjorden ENVELOPE(16.417,16.417,78.563,78.563) Svalbard Water Bears ENVELOPE(-54.431,-54.431,49.600,49.600) Polish Polar Research 37 2 325 334
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Arctic
Svalbard
Tardigrada
cryoconite holes
ecology
glaciers
Geology
QE1-996.5
spellingShingle Arctic
Svalbard
Tardigrada
cryoconite holes
ecology
glaciers
Geology
QE1-996.5
Zawierucha Krzysztof
Vonnahme Tobias R.
Devetter Miloslav
Kolicka Małgorzata
Ostrowska Marta
Chmielewski Sebastian
Kosicki Jakub Z.
Area, depth and elevation of cryoconite holes in the Arctic do not influence Tardigrada densities
topic_facet Arctic
Svalbard
Tardigrada
cryoconite holes
ecology
glaciers
Geology
QE1-996.5
description Water bears (Tardigrada) are known as one of the most extremophile animals in the world. They inhabit environments from the deepest parts of the oceans up to the highest mountains. One of the most extreme and still poorly studied habitats which tardigrades inhabit are cryoconite holes. We analysed the relation between area, depth, elevation and tardigrades densities in cryoconite holes on four glaciers on Spitsbergen. The mean (±SD) of cryoconite area was 1287.21±2400.8 cm2, while the depth was on average 10.8±11.2 cm, the elevation 172.6±109.66 m a.s.l., and tardigrade density 24.9±33.0 individuals per gram of wet material (n = 38). The densities of tardigrades on Hans Glacier reached values of up to 168 ind. cm3, 104 ind. g−1 wet weight, and 275 ind. g−1 dry weight. The densities of tardigrades of the three glaciers in Billefjorden were up to 82 ind. cm2, 326 ind. g−1 wet weight and 624 ind. g−1 dry weight. Surprisingly, although the model included area, depth and elevation as independent variables, it cannot explain Tardigrada density in cryoconite holes. We propose that due to the rapid melting of the glacier surface in the Arctic, the constant flushing of cryoconite sediments, and inter-hole water-sediment mixing, the functioning of these ecosystems is disrupted. We conclude that cryoconite holes are dynamic ecosystems for microinvertebrates in the Arctic.
format Article in Journal/Newspaper
author Zawierucha Krzysztof
Vonnahme Tobias R.
Devetter Miloslav
Kolicka Małgorzata
Ostrowska Marta
Chmielewski Sebastian
Kosicki Jakub Z.
author_facet Zawierucha Krzysztof
Vonnahme Tobias R.
Devetter Miloslav
Kolicka Małgorzata
Ostrowska Marta
Chmielewski Sebastian
Kosicki Jakub Z.
author_sort Zawierucha Krzysztof
title Area, depth and elevation of cryoconite holes in the Arctic do not influence Tardigrada densities
title_short Area, depth and elevation of cryoconite holes in the Arctic do not influence Tardigrada densities
title_full Area, depth and elevation of cryoconite holes in the Arctic do not influence Tardigrada densities
title_fullStr Area, depth and elevation of cryoconite holes in the Arctic do not influence Tardigrada densities
title_full_unstemmed Area, depth and elevation of cryoconite holes in the Arctic do not influence Tardigrada densities
title_sort area, depth and elevation of cryoconite holes in the arctic do not influence tardigrada densities
publisher Polish Academy of Sciences
publishDate 2016
url https://doi.org/10.1515/popore-2016-0009
https://doaj.org/article/e845485964744a60ab76fef5c15d219a
long_lat ENVELOPE(16.417,16.417,78.563,78.563)
ENVELOPE(-54.431,-54.431,49.600,49.600)
geographic Arctic
Billefjorden
Svalbard
Water Bears
geographic_facet Arctic
Billefjorden
Svalbard
Water Bears
genre Arctic
Billefjorden
glacier
Polar Research
Svalbard
Spitsbergen
Tardigrade
genre_facet Arctic
Billefjorden
glacier
Polar Research
Svalbard
Spitsbergen
Tardigrade
op_source Polish Polar Research, Vol 37, Iss 2, Pp 325-334 (2016)
op_relation http://www.degruyter.com/view/j/popore.2016.37.issue-2/popore-2016-0009/popore-2016-0009.xml?format=INT
https://doaj.org/toc/2081-8262
2081-8262
doi:10.1515/popore-2016-0009
https://doaj.org/article/e845485964744a60ab76fef5c15d219a
op_doi https://doi.org/10.1515/popore-2016-0009
container_title Polish Polar Research
container_volume 37
container_issue 2
container_start_page 325
op_container_end_page 334
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