Modelled composition of cryogenically produced subglacial brines, Antarctica
Polar subglacial hydrologic systems have garnered much interest since the recognition of Lake Vostok in 1996. In Antarctica, these environments are hydrologically diverse, including isolated lakes of different sizes, river–lake flow-through systems, “swamps” and groundwater (Siegert 2016). The refre...
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Online Access: | http://dx.doi.org/10.1017/s095410201900004x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410201900004X |
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crcambridgeupr:10.1017/s095410201900004x 2024-03-03T08:38:32+00:00 Modelled composition of cryogenically produced subglacial brines, Antarctica Gardner, Christopher B. Lyons, W. Berry 2019 http://dx.doi.org/10.1017/s095410201900004x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410201900004X en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms https://www.cambridge.org/core/terms Antarctic Science volume 31, issue 3, page 165-166 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 2019 crcambridgeupr https://doi.org/10.1017/s095410201900004x 2024-02-08T08:38:27Z Polar subglacial hydrologic systems have garnered much interest since the recognition of Lake Vostok in 1996. In Antarctica, these environments are hydrologically diverse, including isolated lakes of different sizes, river–lake flow-through systems, “swamps” and groundwater (Siegert 2016). The refreezing of subglacial meltwater is also an important process beneath a large portion of the East Antarctic Ice Sheet (Bell et al. 2011). As subglacial water refreezes it exsolves salts, potentially leaving behind saline and hypersaline brines. Brines thought to derive from this cryoconcentration process have been observed in the northern polar permafrost regions and in the McMurdo Dry Valleys (MDVs) region of Antarctica. Additionally, sediments in the Victoria Land Basin have diagenetic signatures produced by brine movement dating from 3–11 m.y.a, suggesting hypersaline brines have existed in the McMurdo region since at least this time (Staudigel et al. 2018). Article in Journal/Newspaper Antarc* Antarctic Antarctic Science Antarctica Ice Ice Sheet McMurdo Dry Valleys permafrost Victoria Land Cambridge University Press Antarctic Victoria Land McMurdo Dry Valleys East Antarctic Ice Sheet Lake Vostok ENVELOPE(106.000,106.000,-77.500,-77.500) Antarctic Science 31 3 165 166 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology Ecology, Evolution, Behavior and Systematics Oceanography |
spellingShingle |
Geology Ecology, Evolution, Behavior and Systematics Oceanography Gardner, Christopher B. Lyons, W. Berry Modelled composition of cryogenically produced subglacial brines, Antarctica |
topic_facet |
Geology Ecology, Evolution, Behavior and Systematics Oceanography |
description |
Polar subglacial hydrologic systems have garnered much interest since the recognition of Lake Vostok in 1996. In Antarctica, these environments are hydrologically diverse, including isolated lakes of different sizes, river–lake flow-through systems, “swamps” and groundwater (Siegert 2016). The refreezing of subglacial meltwater is also an important process beneath a large portion of the East Antarctic Ice Sheet (Bell et al. 2011). As subglacial water refreezes it exsolves salts, potentially leaving behind saline and hypersaline brines. Brines thought to derive from this cryoconcentration process have been observed in the northern polar permafrost regions and in the McMurdo Dry Valleys (MDVs) region of Antarctica. Additionally, sediments in the Victoria Land Basin have diagenetic signatures produced by brine movement dating from 3–11 m.y.a, suggesting hypersaline brines have existed in the McMurdo region since at least this time (Staudigel et al. 2018). |
format |
Article in Journal/Newspaper |
author |
Gardner, Christopher B. Lyons, W. Berry |
author_facet |
Gardner, Christopher B. Lyons, W. Berry |
author_sort |
Gardner, Christopher B. |
title |
Modelled composition of cryogenically produced subglacial brines, Antarctica |
title_short |
Modelled composition of cryogenically produced subglacial brines, Antarctica |
title_full |
Modelled composition of cryogenically produced subglacial brines, Antarctica |
title_fullStr |
Modelled composition of cryogenically produced subglacial brines, Antarctica |
title_full_unstemmed |
Modelled composition of cryogenically produced subglacial brines, Antarctica |
title_sort |
modelled composition of cryogenically produced subglacial brines, antarctica |
publisher |
Cambridge University Press (CUP) |
publishDate |
2019 |
url |
http://dx.doi.org/10.1017/s095410201900004x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410201900004X |
long_lat |
ENVELOPE(106.000,106.000,-77.500,-77.500) |
geographic |
Antarctic Victoria Land McMurdo Dry Valleys East Antarctic Ice Sheet Lake Vostok |
geographic_facet |
Antarctic Victoria Land McMurdo Dry Valleys East Antarctic Ice Sheet Lake Vostok |
genre |
Antarc* Antarctic Antarctic Science Antarctica Ice Ice Sheet McMurdo Dry Valleys permafrost Victoria Land |
genre_facet |
Antarc* Antarctic Antarctic Science Antarctica Ice Ice Sheet McMurdo Dry Valleys permafrost Victoria Land |
op_source |
Antarctic Science volume 31, issue 3, page 165-166 ISSN 0954-1020 1365-2079 |
op_rights |
https://www.cambridge.org/core/terms https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s095410201900004x |
container_title |
Antarctic Science |
container_volume |
31 |
container_issue |
3 |
container_start_page |
165 |
op_container_end_page |
166 |
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1792506922505601024 |