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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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 |
_version_ |
1766009626463043584 |