The biogeochemistry of meltwater habitats in the Darwin Glacier region (80 degrees S), Victoria Land, Antarctica
Meltwater habitats in the Darwin Glacier region, Victoria Land (808S), were sampled in December 2007 and January 2009 to characterize their microbial and metazoan ecology, nutrient status and geochemistry. Targeted areas included terrestrial ponds of the Grant Valley, Lake Wellman, Tentacle Ridgeand...
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ftunivtasecite:oai:ecite.utas.edu.au:66531 2023-05-15T13:35:38+02:00 The biogeochemistry of meltwater habitats in the Darwin Glacier region (80 degrees S), Victoria Land, Antarctica Webster-Brown, J Gall, M Gibson, J Wood, S Hawes, I 2010 application/pdf https://doi.org/10.1017/S0954102010000787 http://ecite.utas.edu.au/66531 en eng Cambridge Univ Press http://ecite.utas.edu.au/66531/1/Darwin.J Gibson.pdf http://dx.doi.org/10.1017/S0954102010000787 Webster-Brown, J and Gall, M and Gibson, J and Wood, S and Hawes, I, The biogeochemistry of meltwater habitats in the Darwin Glacier region (80 degrees S), Victoria Land, Antarctica, Antarctic Science, 22, (6) pp. 646-661. ISSN 0954-1020 (2010) [Refereed Article] http://ecite.utas.edu.au/66531 Environmental Sciences Ecological Applications Landscape Ecology Refereed Article PeerReviewed 2010 ftunivtasecite https://doi.org/10.1017/S0954102010000787 2019-12-13T21:35:26Z Meltwater habitats in the Darwin Glacier region, Victoria Land (808S), were sampled in December 2007 and January 2009 to characterize their microbial and metazoan ecology, nutrient status and geochemistry. Targeted areas included terrestrial ponds of the Grant Valley, Lake Wellman, Tentacle Ridgeand Diamond Hill, and supraglacial ponds and cryoconite holes of the lower Darwin Glacier. Geochemistry ranged from Na-Cl dominated terrestrial ponds to Na-HCO3 dominated, dilute supraglacial ponds and cryoconites. All showed the nitrate enrichment typical of inland ponds of Victoria Land (up to 13 g.l-1NO3-N), with some precipitating nitratine (NaNO3) salt. Elevated pH indicated ongoing photosynthetic processes. Benthic microbial mats were thin and poorly developed, dominated by oscillatoriacean cyanobacteria. Nitrogen-fixing genera were generally absent and diatoms were rare. A large (20 mm long)Cyanothece species was the most abundant cyanobacterium in the water and in sediments of the cryoconites. DNA finger-printing identified distinct differences in cyanobacterial and bacterial communitystructure between the cryoconites, terrestrial ponds and ponds on glacial margins. Eleven metazoan species were identified, with rotifers being the most abundant. Pond substrate (terrestrial rock, ice-cored moraine orsupraglacial ice) proved to be a more significant influence on biogeochemistry than other aspects of geography or climatic conditions. Article in Journal/Newspaper Antarc* Antarctic Science Antarctica Darwin Glacier Victoria Land eCite UTAS (University of Tasmania) Darwin Glacier ENVELOPE(159.000,159.000,-79.883,-79.883) Diamond Hill ENVELOPE(159.083,159.083,-79.867,-79.867) Grant Valley ENVELOPE(156.417,156.417,-79.967,-79.967) Victoria Land Wellman ENVELOPE(-61.400,-61.400,-64.483,-64.483) Antarctic Science 22 6 646 661 |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Environmental Sciences Ecological Applications Landscape Ecology |
spellingShingle |
Environmental Sciences Ecological Applications Landscape Ecology Webster-Brown, J Gall, M Gibson, J Wood, S Hawes, I The biogeochemistry of meltwater habitats in the Darwin Glacier region (80 degrees S), Victoria Land, Antarctica |
topic_facet |
Environmental Sciences Ecological Applications Landscape Ecology |
description |
Meltwater habitats in the Darwin Glacier region, Victoria Land (808S), were sampled in December 2007 and January 2009 to characterize their microbial and metazoan ecology, nutrient status and geochemistry. Targeted areas included terrestrial ponds of the Grant Valley, Lake Wellman, Tentacle Ridgeand Diamond Hill, and supraglacial ponds and cryoconite holes of the lower Darwin Glacier. Geochemistry ranged from Na-Cl dominated terrestrial ponds to Na-HCO3 dominated, dilute supraglacial ponds and cryoconites. All showed the nitrate enrichment typical of inland ponds of Victoria Land (up to 13 g.l-1NO3-N), with some precipitating nitratine (NaNO3) salt. Elevated pH indicated ongoing photosynthetic processes. Benthic microbial mats were thin and poorly developed, dominated by oscillatoriacean cyanobacteria. Nitrogen-fixing genera were generally absent and diatoms were rare. A large (20 mm long)Cyanothece species was the most abundant cyanobacterium in the water and in sediments of the cryoconites. DNA finger-printing identified distinct differences in cyanobacterial and bacterial communitystructure between the cryoconites, terrestrial ponds and ponds on glacial margins. Eleven metazoan species were identified, with rotifers being the most abundant. Pond substrate (terrestrial rock, ice-cored moraine orsupraglacial ice) proved to be a more significant influence on biogeochemistry than other aspects of geography or climatic conditions. |
format |
Article in Journal/Newspaper |
author |
Webster-Brown, J Gall, M Gibson, J Wood, S Hawes, I |
author_facet |
Webster-Brown, J Gall, M Gibson, J Wood, S Hawes, I |
author_sort |
Webster-Brown, J |
title |
The biogeochemistry of meltwater habitats in the Darwin Glacier region (80 degrees S), Victoria Land, Antarctica |
title_short |
The biogeochemistry of meltwater habitats in the Darwin Glacier region (80 degrees S), Victoria Land, Antarctica |
title_full |
The biogeochemistry of meltwater habitats in the Darwin Glacier region (80 degrees S), Victoria Land, Antarctica |
title_fullStr |
The biogeochemistry of meltwater habitats in the Darwin Glacier region (80 degrees S), Victoria Land, Antarctica |
title_full_unstemmed |
The biogeochemistry of meltwater habitats in the Darwin Glacier region (80 degrees S), Victoria Land, Antarctica |
title_sort |
biogeochemistry of meltwater habitats in the darwin glacier region (80 degrees s), victoria land, antarctica |
publisher |
Cambridge Univ Press |
publishDate |
2010 |
url |
https://doi.org/10.1017/S0954102010000787 http://ecite.utas.edu.au/66531 |
long_lat |
ENVELOPE(159.000,159.000,-79.883,-79.883) ENVELOPE(159.083,159.083,-79.867,-79.867) ENVELOPE(156.417,156.417,-79.967,-79.967) ENVELOPE(-61.400,-61.400,-64.483,-64.483) |
geographic |
Darwin Glacier Diamond Hill Grant Valley Victoria Land Wellman |
geographic_facet |
Darwin Glacier Diamond Hill Grant Valley Victoria Land Wellman |
genre |
Antarc* Antarctic Science Antarctica Darwin Glacier Victoria Land |
genre_facet |
Antarc* Antarctic Science Antarctica Darwin Glacier Victoria Land |
op_relation |
http://ecite.utas.edu.au/66531/1/Darwin.J Gibson.pdf http://dx.doi.org/10.1017/S0954102010000787 Webster-Brown, J and Gall, M and Gibson, J and Wood, S and Hawes, I, The biogeochemistry of meltwater habitats in the Darwin Glacier region (80 degrees S), Victoria Land, Antarctica, Antarctic Science, 22, (6) pp. 646-661. ISSN 0954-1020 (2010) [Refereed Article] http://ecite.utas.edu.au/66531 |
op_doi |
https://doi.org/10.1017/S0954102010000787 |
container_title |
Antarctic Science |
container_volume |
22 |
container_issue |
6 |
container_start_page |
646 |
op_container_end_page |
661 |
_version_ |
1766068325949898752 |