Cryoconite Hole Location in East-Antarctic Untersee Oasis Shapes Physical and Biological Diversity
Antarctic cryoconite holes (CHs) are mostly perennially ice-lidded and sediment-filled depressions that constitute important features on glaciers and ice sheets. Once being hydrologically connected, these microbially dominated mini-ecosystems provide nutrients and biota for downstream environments....
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2020
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Online Access: | https://doi.org/10.3389/fmicb.2020.01165 https://doaj.org/article/a148d11178cb4f9eb5153065d8b561d4 |
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ftdoajarticles:oai:doaj.org/article:a148d11178cb4f9eb5153065d8b561d4 2023-05-15T13:35:24+02:00 Cryoconite Hole Location in East-Antarctic Untersee Oasis Shapes Physical and Biological Diversity Klemens Weisleitner Alexandra Kristin Perras Seraphin Hubert Unterberger Christine Moissl-Eichinger Dale T. Andersen Birgit Sattler 2020-06-01T00:00:00Z https://doi.org/10.3389/fmicb.2020.01165 https://doaj.org/article/a148d11178cb4f9eb5153065d8b561d4 EN eng Frontiers Media S.A. https://www.frontiersin.org/article/10.3389/fmicb.2020.01165/full https://doaj.org/toc/1664-302X 1664-302X doi:10.3389/fmicb.2020.01165 https://doaj.org/article/a148d11178cb4f9eb5153065d8b561d4 Frontiers in Microbiology, Vol 11 (2020) Anuchin Glacier 16S rRNA cryoconite holes mineralogy archaea bacterial activity Microbiology QR1-502 article 2020 ftdoajarticles https://doi.org/10.3389/fmicb.2020.01165 2022-12-31T02:13:58Z Antarctic cryoconite holes (CHs) are mostly perennially ice-lidded and sediment-filled depressions that constitute important features on glaciers and ice sheets. Once being hydrologically connected, these microbially dominated mini-ecosystems provide nutrients and biota for downstream environments. For example, the East Antarctic Anuchin Glacier gradually melts into the adjacent perennially ice-covered Lake Untersee, and CH biota from this glacier contribute up to one third of the community composition in benthic microbial mats within the lake. However, biogeochemical features of these CHs and associated spatial patterns across the glacier are still unknown. Here we hypothesized about the CH minerogenic composition between the different sources such as the medial moraine and other zones. Further, we intended to investigate if the depth of the CH mirrors the CH community composition, organic matter (OM) content and would support productivity. In this study we show that both microbial communities and biogeochemical parameters in CHs were significantly different between the zones medial moraine and the glacier terminus. Variations in microbial community composition are the result of factors such as depth, diameter, organic matter, total carbon, particle size, and mineral diversity. More than 90% of all ribosomal sequence variants (RSV) reads were classified as Proteobacteria, Cyanobacteria, Bacteroidetes, Actinobacteria, and Acidobacteria. Archaea were detected in 85% of all samples and exclusively belonged to the classes Halobacteria, Methanomicrobia, and Thermoplasmata. The most abundant genus was Halorubrum (Halobacteria) and was identified in nine RSVs. The core microbiome for bacteria comprised 30 RSVs that were affiliated with Cyanobacteria, Bacteroidetes, Actinobacteria, and Proteobacteria. The archaeal fraction of the core microbiome consisted of three RSVs belonging to unknown genera of Methanomicrobiales and Thermoplasmatales and the genus Rice_Cluster_I (Methanocellales). Further, mean bacterial carbon ... Article in Journal/Newspaper Antarc* Antarctic Anuchin Glacier Directory of Open Access Journals: DOAJ Articles Antarctic Anuchin Glacier ENVELOPE(13.517,13.517,-71.283,-71.283) Untersee ENVELOPE(13.467,13.467,-71.350,-71.350) Frontiers in Microbiology 11 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Anuchin Glacier 16S rRNA cryoconite holes mineralogy archaea bacterial activity Microbiology QR1-502 |
spellingShingle |
Anuchin Glacier 16S rRNA cryoconite holes mineralogy archaea bacterial activity Microbiology QR1-502 Klemens Weisleitner Alexandra Kristin Perras Seraphin Hubert Unterberger Christine Moissl-Eichinger Dale T. Andersen Birgit Sattler Cryoconite Hole Location in East-Antarctic Untersee Oasis Shapes Physical and Biological Diversity |
topic_facet |
Anuchin Glacier 16S rRNA cryoconite holes mineralogy archaea bacterial activity Microbiology QR1-502 |
description |
Antarctic cryoconite holes (CHs) are mostly perennially ice-lidded and sediment-filled depressions that constitute important features on glaciers and ice sheets. Once being hydrologically connected, these microbially dominated mini-ecosystems provide nutrients and biota for downstream environments. For example, the East Antarctic Anuchin Glacier gradually melts into the adjacent perennially ice-covered Lake Untersee, and CH biota from this glacier contribute up to one third of the community composition in benthic microbial mats within the lake. However, biogeochemical features of these CHs and associated spatial patterns across the glacier are still unknown. Here we hypothesized about the CH minerogenic composition between the different sources such as the medial moraine and other zones. Further, we intended to investigate if the depth of the CH mirrors the CH community composition, organic matter (OM) content and would support productivity. In this study we show that both microbial communities and biogeochemical parameters in CHs were significantly different between the zones medial moraine and the glacier terminus. Variations in microbial community composition are the result of factors such as depth, diameter, organic matter, total carbon, particle size, and mineral diversity. More than 90% of all ribosomal sequence variants (RSV) reads were classified as Proteobacteria, Cyanobacteria, Bacteroidetes, Actinobacteria, and Acidobacteria. Archaea were detected in 85% of all samples and exclusively belonged to the classes Halobacteria, Methanomicrobia, and Thermoplasmata. The most abundant genus was Halorubrum (Halobacteria) and was identified in nine RSVs. The core microbiome for bacteria comprised 30 RSVs that were affiliated with Cyanobacteria, Bacteroidetes, Actinobacteria, and Proteobacteria. The archaeal fraction of the core microbiome consisted of three RSVs belonging to unknown genera of Methanomicrobiales and Thermoplasmatales and the genus Rice_Cluster_I (Methanocellales). Further, mean bacterial carbon ... |
format |
Article in Journal/Newspaper |
author |
Klemens Weisleitner Alexandra Kristin Perras Seraphin Hubert Unterberger Christine Moissl-Eichinger Dale T. Andersen Birgit Sattler |
author_facet |
Klemens Weisleitner Alexandra Kristin Perras Seraphin Hubert Unterberger Christine Moissl-Eichinger Dale T. Andersen Birgit Sattler |
author_sort |
Klemens Weisleitner |
title |
Cryoconite Hole Location in East-Antarctic Untersee Oasis Shapes Physical and Biological Diversity |
title_short |
Cryoconite Hole Location in East-Antarctic Untersee Oasis Shapes Physical and Biological Diversity |
title_full |
Cryoconite Hole Location in East-Antarctic Untersee Oasis Shapes Physical and Biological Diversity |
title_fullStr |
Cryoconite Hole Location in East-Antarctic Untersee Oasis Shapes Physical and Biological Diversity |
title_full_unstemmed |
Cryoconite Hole Location in East-Antarctic Untersee Oasis Shapes Physical and Biological Diversity |
title_sort |
cryoconite hole location in east-antarctic untersee oasis shapes physical and biological diversity |
publisher |
Frontiers Media S.A. |
publishDate |
2020 |
url |
https://doi.org/10.3389/fmicb.2020.01165 https://doaj.org/article/a148d11178cb4f9eb5153065d8b561d4 |
long_lat |
ENVELOPE(13.517,13.517,-71.283,-71.283) ENVELOPE(13.467,13.467,-71.350,-71.350) |
geographic |
Antarctic Anuchin Glacier Untersee |
geographic_facet |
Antarctic Anuchin Glacier Untersee |
genre |
Antarc* Antarctic Anuchin Glacier |
genre_facet |
Antarc* Antarctic Anuchin Glacier |
op_source |
Frontiers in Microbiology, Vol 11 (2020) |
op_relation |
https://www.frontiersin.org/article/10.3389/fmicb.2020.01165/full https://doaj.org/toc/1664-302X 1664-302X doi:10.3389/fmicb.2020.01165 https://doaj.org/article/a148d11178cb4f9eb5153065d8b561d4 |
op_doi |
https://doi.org/10.3389/fmicb.2020.01165 |
container_title |
Frontiers in Microbiology |
container_volume |
11 |
_version_ |
1766065221744459776 |