Bacterial community structure in a sympagic habitat expanding with global warming: brackish ice brine at 85–90 °N
© 2018, International Society for Microbial Ecology.Larger volumes of sea ice have been thawing in the Central Arctic Ocean (CAO) during the last decades than during the past 800,000 years. Brackish brine (fed by meltwater inside the ice) is an expanding sympagic habitat in summer all over the CAO....
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ftunivchile:oai:repositorio.uchile.cl:2250/171328 2023-05-15T14:01:29+02:00 Bacterial community structure in a sympagic habitat expanding with global warming: brackish ice brine at 85–90 °N Fernández-Gómez, Beatriz Díez, Beatriz Polz, Martin F. Arroyo, José Ignacio Alfaro, Fernando D. Marchandon, Germán Sanhueza, Cynthia Farías, Laura Trefault, Nicole Marquet, Pablo A. Molina-Montenegro, Marco A. Sylvander, Peter Snoeijs-Leijonmalm, Pauline 2019 application/pdf https://doi.org/10.1038/s41396-018-0268-9 https://repositorio.uchile.cl/handle/2250/171328 en eng Nature Publishing Group ISME Journal, Volumen 13, Issue 2, 2019, Pages 316-333 17517370 17517362 doi:10.1038/s41396-018-0268-9 https://repositorio.uchile.cl/handle/2250/171328 Attribution-NonCommercial-NoDerivs 3.0 Chile http://creativecommons.org/licenses/by-nc-nd/3.0/cl/ CC-BY-NC-ND ISME Journal Microbiology Ecology Evolution Behavior and Systematics Artículo de revista 2019 ftunivchile https://doi.org/10.1038/s41396-018-0268-9 2022-09-24T23:51:14Z © 2018, International Society for Microbial Ecology.Larger volumes of sea ice have been thawing in the Central Arctic Ocean (CAO) during the last decades than during the past 800,000 years. Brackish brine (fed by meltwater inside the ice) is an expanding sympagic habitat in summer all over the CAO. We report for the first time the structure of bacterial communities in this brine. They are composed of psychrophilic extremophiles, many of them related to phylotypes known from Arctic and Antarctic regions. Community structure displayed strong habitat segregation between brackish ice brine (IB; salinity 2.4–9.6) and immediate sub-ice seawater (SW; salinity 33.3–34.9), expressed at all taxonomic levels (class to genus), by dominant phylotypes as well as by the rare biosphere, and with specialists dominating IB and generalists SW. The dominant phylotypes in IB were related to Candidatus Aquiluna and Flavobacterium, those in SW to Balneatrix and ZD0405, and those shared between the habitats t Article in Journal/Newspaper Antarc* Antarctic Arctic Arctic Ocean Global warming Sea ice Universidad de Chile: Repositorio académico Antarctic Arctic Arctic Ocean The ISME Journal 13 2 316 333 |
institution |
Open Polar |
collection |
Universidad de Chile: Repositorio académico |
op_collection_id |
ftunivchile |
language |
English |
topic |
Microbiology Ecology Evolution Behavior and Systematics |
spellingShingle |
Microbiology Ecology Evolution Behavior and Systematics Fernández-Gómez, Beatriz Díez, Beatriz Polz, Martin F. Arroyo, José Ignacio Alfaro, Fernando D. Marchandon, Germán Sanhueza, Cynthia Farías, Laura Trefault, Nicole Marquet, Pablo A. Molina-Montenegro, Marco A. Sylvander, Peter Snoeijs-Leijonmalm, Pauline Bacterial community structure in a sympagic habitat expanding with global warming: brackish ice brine at 85–90 °N |
topic_facet |
Microbiology Ecology Evolution Behavior and Systematics |
description |
© 2018, International Society for Microbial Ecology.Larger volumes of sea ice have been thawing in the Central Arctic Ocean (CAO) during the last decades than during the past 800,000 years. Brackish brine (fed by meltwater inside the ice) is an expanding sympagic habitat in summer all over the CAO. We report for the first time the structure of bacterial communities in this brine. They are composed of psychrophilic extremophiles, many of them related to phylotypes known from Arctic and Antarctic regions. Community structure displayed strong habitat segregation between brackish ice brine (IB; salinity 2.4–9.6) and immediate sub-ice seawater (SW; salinity 33.3–34.9), expressed at all taxonomic levels (class to genus), by dominant phylotypes as well as by the rare biosphere, and with specialists dominating IB and generalists SW. The dominant phylotypes in IB were related to Candidatus Aquiluna and Flavobacterium, those in SW to Balneatrix and ZD0405, and those shared between the habitats t |
format |
Article in Journal/Newspaper |
author |
Fernández-Gómez, Beatriz Díez, Beatriz Polz, Martin F. Arroyo, José Ignacio Alfaro, Fernando D. Marchandon, Germán Sanhueza, Cynthia Farías, Laura Trefault, Nicole Marquet, Pablo A. Molina-Montenegro, Marco A. Sylvander, Peter Snoeijs-Leijonmalm, Pauline |
author_facet |
Fernández-Gómez, Beatriz Díez, Beatriz Polz, Martin F. Arroyo, José Ignacio Alfaro, Fernando D. Marchandon, Germán Sanhueza, Cynthia Farías, Laura Trefault, Nicole Marquet, Pablo A. Molina-Montenegro, Marco A. Sylvander, Peter Snoeijs-Leijonmalm, Pauline |
author_sort |
Fernández-Gómez, Beatriz |
title |
Bacterial community structure in a sympagic habitat expanding with global warming: brackish ice brine at 85–90 °N |
title_short |
Bacterial community structure in a sympagic habitat expanding with global warming: brackish ice brine at 85–90 °N |
title_full |
Bacterial community structure in a sympagic habitat expanding with global warming: brackish ice brine at 85–90 °N |
title_fullStr |
Bacterial community structure in a sympagic habitat expanding with global warming: brackish ice brine at 85–90 °N |
title_full_unstemmed |
Bacterial community structure in a sympagic habitat expanding with global warming: brackish ice brine at 85–90 °N |
title_sort |
bacterial community structure in a sympagic habitat expanding with global warming: brackish ice brine at 85–90 °n |
publisher |
Nature Publishing Group |
publishDate |
2019 |
url |
https://doi.org/10.1038/s41396-018-0268-9 https://repositorio.uchile.cl/handle/2250/171328 |
geographic |
Antarctic Arctic Arctic Ocean |
geographic_facet |
Antarctic Arctic Arctic Ocean |
genre |
Antarc* Antarctic Arctic Arctic Ocean Global warming Sea ice |
genre_facet |
Antarc* Antarctic Arctic Arctic Ocean Global warming Sea ice |
op_source |
ISME Journal |
op_relation |
ISME Journal, Volumen 13, Issue 2, 2019, Pages 316-333 17517370 17517362 doi:10.1038/s41396-018-0268-9 https://repositorio.uchile.cl/handle/2250/171328 |
op_rights |
Attribution-NonCommercial-NoDerivs 3.0 Chile http://creativecommons.org/licenses/by-nc-nd/3.0/cl/ |
op_rightsnorm |
CC-BY-NC-ND |
op_doi |
https://doi.org/10.1038/s41396-018-0268-9 |
container_title |
The ISME Journal |
container_volume |
13 |
container_issue |
2 |
container_start_page |
316 |
op_container_end_page |
333 |
_version_ |
1766271330482651136 |