Quantification of basal ice microbial cell delivery to the glacier margin

We present the first assessment of microbial cell discharge from sediment-laden glacier basal ice. At Svínafellsjökull, a temperate valley glacier in Iceland, approximately 10 17 cells a −1 are transferred through basal ice to the proglacial environment, and between 10 1 and 10 6 cells g −1 basal ic...

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Main Authors: Toubes-Rodrigo, Mario, Cook, Simon J., Elliott, David, Sen, Robin
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/bg-2016-471
https://www.biogeosciences-discuss.net/bg-2016-471/
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spelling ftcopernicus:oai:publications.copernicus.org:bgd55648 2023-05-15T16:21:37+02:00 Quantification of basal ice microbial cell delivery to the glacier margin Toubes-Rodrigo, Mario Cook, Simon J. Elliott, David Sen, Robin 2018-09-26 application/pdf https://doi.org/10.5194/bg-2016-471 https://www.biogeosciences-discuss.net/bg-2016-471/ eng eng doi:10.5194/bg-2016-471 https://www.biogeosciences-discuss.net/bg-2016-471/ eISSN: 1726-4189 Text 2018 ftcopernicus https://doi.org/10.5194/bg-2016-471 2019-12-24T09:51:51Z We present the first assessment of microbial cell discharge from sediment-laden glacier basal ice. At Svínafellsjökull, a temperate valley glacier in Iceland, approximately 10 17 cells a −1 are transferred through basal ice to the proglacial environment, and between 10 1 and 10 6 cells g −1 basal ice were cultured from our samples under laboratory conditions. We suggest that the delivery of viable cells and dead microbial matter to proglacial ecosystems could be playing a crucial role in soil formation and primary succession during deglaciation, but further quantification of cell transfer from a range of glacier contexts is required. Text glacier Iceland Copernicus Publications: E-Journals Svínafellsjökull ENVELOPE(-16.823,-16.823,64.021,64.021)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description We present the first assessment of microbial cell discharge from sediment-laden glacier basal ice. At Svínafellsjökull, a temperate valley glacier in Iceland, approximately 10 17 cells a −1 are transferred through basal ice to the proglacial environment, and between 10 1 and 10 6 cells g −1 basal ice were cultured from our samples under laboratory conditions. We suggest that the delivery of viable cells and dead microbial matter to proglacial ecosystems could be playing a crucial role in soil formation and primary succession during deglaciation, but further quantification of cell transfer from a range of glacier contexts is required.
format Text
author Toubes-Rodrigo, Mario
Cook, Simon J.
Elliott, David
Sen, Robin
spellingShingle Toubes-Rodrigo, Mario
Cook, Simon J.
Elliott, David
Sen, Robin
Quantification of basal ice microbial cell delivery to the glacier margin
author_facet Toubes-Rodrigo, Mario
Cook, Simon J.
Elliott, David
Sen, Robin
author_sort Toubes-Rodrigo, Mario
title Quantification of basal ice microbial cell delivery to the glacier margin
title_short Quantification of basal ice microbial cell delivery to the glacier margin
title_full Quantification of basal ice microbial cell delivery to the glacier margin
title_fullStr Quantification of basal ice microbial cell delivery to the glacier margin
title_full_unstemmed Quantification of basal ice microbial cell delivery to the glacier margin
title_sort quantification of basal ice microbial cell delivery to the glacier margin
publishDate 2018
url https://doi.org/10.5194/bg-2016-471
https://www.biogeosciences-discuss.net/bg-2016-471/
long_lat ENVELOPE(-16.823,-16.823,64.021,64.021)
geographic Svínafellsjökull
geographic_facet Svínafellsjökull
genre glacier
Iceland
genre_facet glacier
Iceland
op_source eISSN: 1726-4189
op_relation doi:10.5194/bg-2016-471
https://www.biogeosciences-discuss.net/bg-2016-471/
op_doi https://doi.org/10.5194/bg-2016-471
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