Identification and analysis of low-molecular-weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography
Determining the concentration and composition of dissolved organic carbon (DOC) in glacial ecosystems is important for assessments of in situ microbial activity and contributions to wider biogeochemical cycles. Nonetheless, there is limited knowledge of the abundance and character of DOC in basal ic...
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Format: | Article in Journal/Newspaper |
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European Geosciences Union
2016
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Online Access: | https://doi.org/10.5194/bg-13-3833-2016 https://nottingham-repository.worktribe.com/file/792293/1/O%27Donnell%20et%20al.,%202016.pdf https://nottingham-repository.worktribe.com/output/792293 |
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ftunnottinghamrr:oai:nottingham-repository.worktribe.com:792293 2023-05-15T13:42:39+02:00 Identification and analysis of low-molecular-weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography O'Donnell, Emily C. Wadham, Jemma L. Lis, Grzegorz P. Tranter, Martyn Pickard, Amy E. Stibal, Marek Dewsbury, Paul Fitzsimons, Sean 2016-07-01 https://doi.org/10.5194/bg-13-3833-2016 https://nottingham-repository.worktribe.com/file/792293/1/O%27Donnell%20et%20al.,%202016.pdf https://nottingham-repository.worktribe.com/output/792293 unknown European Geosciences Union https://nottingham-repository.worktribe.com/output/792293 Biogeosciences Volume 13 doi:https://doi.org/10.5194/bg-13-3833-2016 https://nottingham-repository.worktribe.com/file/792293/1/O%27Donnell%20et%20al.,%202016.pdf 1726-4170 doi:10.5194/bg-13-3833-2016 openAccess Glacier Dissolved organic carbon Greenland Ion chromatography Basal ice ecosystems Journal Article 2016 ftunnottinghamrr https://doi.org/10.5194/bg-13-3833-2016 2022-10-13T22:09:02Z Determining the concentration and composition of dissolved organic carbon (DOC) in glacial ecosystems is important for assessments of in situ microbial activity and contributions to wider biogeochemical cycles. Nonetheless, there is limited knowledge of the abundance and character of DOC in basal ice and the subglacial environment and a lack of quantitative data on low-molecular-weight (LMW) DOC components, which are believed to be highly bioavailable to microorganisms. We investigated the abundance and composition of DOC in basal ice via a molecular-level DOC analysis. Spectrofluorometry and a novel ion chromatographic method, which has been little utilized in glacial science for LMW-DOC determinations, were employed to identify and quantify the major LMW fractions (free amino acids, carbohydrates, and carboxylic acids) in basal ice from four glaciers, each with a different type of overridden material (i.e. the pre-entrainment sedimentary type such as lacustrine material or palaeosols). Basal ice from Joyce Glacier (Antarctica) was unique in that 98% of the LMW-DOC was derived from the extremely diverse free amino acid (FAA) pool, comprising 14 FAAs. LMW-DOC concentrations in basal ice were dependent on the bioavailability of the overridden organic carbon (OC), which in turn was influenced by the type of overridden material. Mean LMW-DOC concentrations in basal ice from Russell Glacier (Greenland), Finsterwalderbreen (Svalbard), and Engabreen (Norway) were low (0–417nMC), attributed to the relatively refractory nature of the OC in the overridden palaeosols and bedrock. In contrast, mean LMW-DOC concentrations were an order of magnitude higher (4430nMC) in basal ice from Joyce Glacier, a reflection of the high bioavailability of the overridden lacustrine material (> 17% of the sediment OC comprised extractable carbohydrates, a proxy for bioavailable OC). We find that the overridden material may act as a direct (via abiotic leaching) and indirect (via microbial cycling) source of DOC to the subglacial ... Article in Journal/Newspaper Antarc* Antarctica glacier glacier glacier Greenland Svalbard University of Nottingham: Repository@Nottingham Svalbard Greenland Norway Engabreen ENVELOPE(13.771,13.771,66.682,66.682) Finsterwalderbreen ENVELOPE(15.273,15.273,77.489,77.489) Joyce Glacier ENVELOPE(163.700,163.700,-78.017,-78.017) Biogeosciences 13 12 3833 3846 |
institution |
Open Polar |
collection |
University of Nottingham: Repository@Nottingham |
op_collection_id |
ftunnottinghamrr |
language |
unknown |
topic |
Glacier Dissolved organic carbon Greenland Ion chromatography Basal ice ecosystems |
spellingShingle |
Glacier Dissolved organic carbon Greenland Ion chromatography Basal ice ecosystems O'Donnell, Emily C. Wadham, Jemma L. Lis, Grzegorz P. Tranter, Martyn Pickard, Amy E. Stibal, Marek Dewsbury, Paul Fitzsimons, Sean Identification and analysis of low-molecular-weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography |
topic_facet |
Glacier Dissolved organic carbon Greenland Ion chromatography Basal ice ecosystems |
description |
Determining the concentration and composition of dissolved organic carbon (DOC) in glacial ecosystems is important for assessments of in situ microbial activity and contributions to wider biogeochemical cycles. Nonetheless, there is limited knowledge of the abundance and character of DOC in basal ice and the subglacial environment and a lack of quantitative data on low-molecular-weight (LMW) DOC components, which are believed to be highly bioavailable to microorganisms. We investigated the abundance and composition of DOC in basal ice via a molecular-level DOC analysis. Spectrofluorometry and a novel ion chromatographic method, which has been little utilized in glacial science for LMW-DOC determinations, were employed to identify and quantify the major LMW fractions (free amino acids, carbohydrates, and carboxylic acids) in basal ice from four glaciers, each with a different type of overridden material (i.e. the pre-entrainment sedimentary type such as lacustrine material or palaeosols). Basal ice from Joyce Glacier (Antarctica) was unique in that 98% of the LMW-DOC was derived from the extremely diverse free amino acid (FAA) pool, comprising 14 FAAs. LMW-DOC concentrations in basal ice were dependent on the bioavailability of the overridden organic carbon (OC), which in turn was influenced by the type of overridden material. Mean LMW-DOC concentrations in basal ice from Russell Glacier (Greenland), Finsterwalderbreen (Svalbard), and Engabreen (Norway) were low (0–417nMC), attributed to the relatively refractory nature of the OC in the overridden palaeosols and bedrock. In contrast, mean LMW-DOC concentrations were an order of magnitude higher (4430nMC) in basal ice from Joyce Glacier, a reflection of the high bioavailability of the overridden lacustrine material (> 17% of the sediment OC comprised extractable carbohydrates, a proxy for bioavailable OC). We find that the overridden material may act as a direct (via abiotic leaching) and indirect (via microbial cycling) source of DOC to the subglacial ... |
format |
Article in Journal/Newspaper |
author |
O'Donnell, Emily C. Wadham, Jemma L. Lis, Grzegorz P. Tranter, Martyn Pickard, Amy E. Stibal, Marek Dewsbury, Paul Fitzsimons, Sean |
author_facet |
O'Donnell, Emily C. Wadham, Jemma L. Lis, Grzegorz P. Tranter, Martyn Pickard, Amy E. Stibal, Marek Dewsbury, Paul Fitzsimons, Sean |
author_sort |
O'Donnell, Emily C. |
title |
Identification and analysis of low-molecular-weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography |
title_short |
Identification and analysis of low-molecular-weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography |
title_full |
Identification and analysis of low-molecular-weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography |
title_fullStr |
Identification and analysis of low-molecular-weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography |
title_full_unstemmed |
Identification and analysis of low-molecular-weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography |
title_sort |
identification and analysis of low-molecular-weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography |
publisher |
European Geosciences Union |
publishDate |
2016 |
url |
https://doi.org/10.5194/bg-13-3833-2016 https://nottingham-repository.worktribe.com/file/792293/1/O%27Donnell%20et%20al.,%202016.pdf https://nottingham-repository.worktribe.com/output/792293 |
long_lat |
ENVELOPE(13.771,13.771,66.682,66.682) ENVELOPE(15.273,15.273,77.489,77.489) ENVELOPE(163.700,163.700,-78.017,-78.017) |
geographic |
Svalbard Greenland Norway Engabreen Finsterwalderbreen Joyce Glacier |
geographic_facet |
Svalbard Greenland Norway Engabreen Finsterwalderbreen Joyce Glacier |
genre |
Antarc* Antarctica glacier glacier glacier Greenland Svalbard |
genre_facet |
Antarc* Antarctica glacier glacier glacier Greenland Svalbard |
op_relation |
https://nottingham-repository.worktribe.com/output/792293 Biogeosciences Volume 13 doi:https://doi.org/10.5194/bg-13-3833-2016 https://nottingham-repository.worktribe.com/file/792293/1/O%27Donnell%20et%20al.,%202016.pdf 1726-4170 doi:10.5194/bg-13-3833-2016 |
op_rights |
openAccess |
op_doi |
https://doi.org/10.5194/bg-13-3833-2016 |
container_title |
Biogeosciences |
container_volume |
13 |
container_issue |
12 |
container_start_page |
3833 |
op_container_end_page |
3846 |
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1766170434980544512 |