Research on cryosestic communities in Svalbard: the snow algae of temporary snowfields in Petuniabukta, Central Svalbard

Although the observations of the colored snow in Svalbard are dated from 17th century, the research in cryosestic algae during last 50 years was focused to NW part of Svalbard, Hornsund and Sveagruva areas. No observations have been reported for the Central or East Svalbard yet, with exception of Lo...

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Main Author: Kvíderová, Jana
Format: Article in Journal/Newspaper
Language:English
Published: Masaryk Univerzity 2012
Subjects:
Online Access:http://journals.muni.cz/CPR/article/view/12811
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spelling ftmasarykunivojs:oai:ojs.journals.muni.cz:article/12811 2023-05-15T16:22:10+02:00 Research on cryosestic communities in Svalbard: the snow algae of temporary snowfields in Petuniabukta, Central Svalbard Kvíderová, Jana 2012-01-01 application/pdf http://journals.muni.cz/CPR/article/view/12811 eng eng Masaryk Univerzity http://journals.muni.cz/CPR/article/view/12811/11127 http://journals.muni.cz/CPR/article/view/12811 Copyright (c) 2020 Czech Polar Reports https://creativecommons.org/licenses/by-nc-nd/4.0 CC-BY-NC-ND Czech Polar Reports; Vol 2 No 1 (2012); 8-19 Czech Polar Reports; Vol. 2 No. 1 (2012); 8-19 1805-0697 1805-0689 Snow fields cryoseston info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2012 ftmasarykunivojs 2022-06-26T10:16:32Z Although the observations of the colored snow in Svalbard are dated from 17th century, the research in cryosestic algae during last 50 years was focused to NW part of Svalbard, Hornsund and Sveagruva areas. No observations have been reported for the Central or East Svalbard yet, with exception of Longyearbyen and Sveagruva areas. In Petuniabukta, two types of possible cryoseston habitats were recognized: 1) temporal snow fields that melt-away in summer completely, and 2) perennial glacier surfaces. During summer seasons 2009 - 2011, ten temporary snow field samples were sampled in the Petuniabukta area. The cryosestic communities did not cause visible snow coloration, however the presence of snow algae was revealed by light microscope. In samples, zygospores of Chlamydomonas cf. nivalis, were dominant. Other found species included Chlamydomonas nivalis, Chloromonas nivalis, Cryodactylon glaciale, and cf. Chainomonas sp. No motile stages of snow algae were observed. Due to low cell concentration and association of the cells with dust grains, wind transport of snow algae to the snow fields seems to be more possible than presence of a stable cryosestic community growing in situ. Article in Journal/Newspaper glacier Hornsund Longyearbyen Svalbard Sveagruva Masaryk University Journals Svalbard Longyearbyen Hornsund ENVELOPE(15.865,15.865,76.979,76.979) Petuniabukta ENVELOPE(16.532,16.532,78.687,78.687) Sveagruva ENVELOPE(16.720,16.720,77.900,77.900)
institution Open Polar
collection Masaryk University Journals
op_collection_id ftmasarykunivojs
language English
topic Snow fields
cryoseston
spellingShingle Snow fields
cryoseston
Kvíderová, Jana
Research on cryosestic communities in Svalbard: the snow algae of temporary snowfields in Petuniabukta, Central Svalbard
topic_facet Snow fields
cryoseston
description Although the observations of the colored snow in Svalbard are dated from 17th century, the research in cryosestic algae during last 50 years was focused to NW part of Svalbard, Hornsund and Sveagruva areas. No observations have been reported for the Central or East Svalbard yet, with exception of Longyearbyen and Sveagruva areas. In Petuniabukta, two types of possible cryoseston habitats were recognized: 1) temporal snow fields that melt-away in summer completely, and 2) perennial glacier surfaces. During summer seasons 2009 - 2011, ten temporary snow field samples were sampled in the Petuniabukta area. The cryosestic communities did not cause visible snow coloration, however the presence of snow algae was revealed by light microscope. In samples, zygospores of Chlamydomonas cf. nivalis, were dominant. Other found species included Chlamydomonas nivalis, Chloromonas nivalis, Cryodactylon glaciale, and cf. Chainomonas sp. No motile stages of snow algae were observed. Due to low cell concentration and association of the cells with dust grains, wind transport of snow algae to the snow fields seems to be more possible than presence of a stable cryosestic community growing in situ.
format Article in Journal/Newspaper
author Kvíderová, Jana
author_facet Kvíderová, Jana
author_sort Kvíderová, Jana
title Research on cryosestic communities in Svalbard: the snow algae of temporary snowfields in Petuniabukta, Central Svalbard
title_short Research on cryosestic communities in Svalbard: the snow algae of temporary snowfields in Petuniabukta, Central Svalbard
title_full Research on cryosestic communities in Svalbard: the snow algae of temporary snowfields in Petuniabukta, Central Svalbard
title_fullStr Research on cryosestic communities in Svalbard: the snow algae of temporary snowfields in Petuniabukta, Central Svalbard
title_full_unstemmed Research on cryosestic communities in Svalbard: the snow algae of temporary snowfields in Petuniabukta, Central Svalbard
title_sort research on cryosestic communities in svalbard: the snow algae of temporary snowfields in petuniabukta, central svalbard
publisher Masaryk Univerzity
publishDate 2012
url http://journals.muni.cz/CPR/article/view/12811
long_lat ENVELOPE(15.865,15.865,76.979,76.979)
ENVELOPE(16.532,16.532,78.687,78.687)
ENVELOPE(16.720,16.720,77.900,77.900)
geographic Svalbard
Longyearbyen
Hornsund
Petuniabukta
Sveagruva
geographic_facet Svalbard
Longyearbyen
Hornsund
Petuniabukta
Sveagruva
genre glacier
Hornsund
Longyearbyen
Svalbard
Sveagruva
genre_facet glacier
Hornsund
Longyearbyen
Svalbard
Sveagruva
op_source Czech Polar Reports; Vol 2 No 1 (2012); 8-19
Czech Polar Reports; Vol. 2 No. 1 (2012); 8-19
1805-0697
1805-0689
op_relation http://journals.muni.cz/CPR/article/view/12811/11127
http://journals.muni.cz/CPR/article/view/12811
op_rights Copyright (c) 2020 Czech Polar Reports
https://creativecommons.org/licenses/by-nc-nd/4.0
op_rightsnorm CC-BY-NC-ND
_version_ 1766010148041523200