Limnological features of the saline lakes of the Bunger Hills (Wilkes Land, Antarctica)
Twelve saline lakes 5-35m above sea level in Bunger Hills (66°10'S, 101°00'E) were investigated from January to April in 1987-89. Some lakes may be relict and all were subject to wind-borne marine salts with present salinities between 3.4-79.0°/‰ and δ 18 O values mostly between -10 to -14...
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Cambridge University Press (CUP)
1993
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Online Access: | http://dx.doi.org/10.1017/s0954102093000070 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102093000070 |
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crcambridgeupr:10.1017/s0954102093000070 2024-03-03T08:37:31+00:00 Limnological features of the saline lakes of the Bunger Hills (Wilkes Land, Antarctica) Kaup, E. Haendel, D. Vaikmäe, R. 1993 http://dx.doi.org/10.1017/s0954102093000070 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102093000070 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 5, issue 1, page 41-50 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 1993 crcambridgeupr https://doi.org/10.1017/s0954102093000070 2024-02-08T08:36:03Z Twelve saline lakes 5-35m above sea level in Bunger Hills (66°10'S, 101°00'E) were investigated from January to April in 1987-89. Some lakes may be relict and all were subject to wind-borne marine salts with present salinities between 3.4-79.0°/‰ and δ 18 O values mostly between -10 to -14%. Temperatures up to 17.7°C were measured at the bottom of Lake Polest where a sharp thermohalocline was observed during the period of open water. Mg 2+ dominated over Ca 2+ in all the lakes. Phosphates concentration was 3-10 μgP I -1 and total phosphorus 8-16 μgP I -1 . The concentrations of nitrates and nitrites were often equal, ranging between 1-4 μgN I -1 . Dissolved O 2 was usually near saturation levels but peaked at more than 230% of saturation in the hypolimnion of Lake Polest as a result of temperature-enhanced photosynthesis with an assimilation rate of 23.9 mgC (mg Chl a ) -1 h -1 . The values for chlorophyll a were 0.26-1.93 mg m -3 and for primary production 0.013-0.171 gCm -3 d -1 , the latter being an order of magnitude higher than in the fresh water lakes of the Bunger Hills. Article in Journal/Newspaper Antarc* Antarctic Science Antarctica Wilkes Land Cambridge University Press Bunger Hills ENVELOPE(100.883,100.883,-66.167,-66.167) Wilkes Land ENVELOPE(120.000,120.000,-69.000,-69.000) Antarctic Science 5 1 41 50 |
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Open Polar |
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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 Kaup, E. Haendel, D. Vaikmäe, R. Limnological features of the saline lakes of the Bunger Hills (Wilkes Land, Antarctica) |
topic_facet |
Geology Ecology, Evolution, Behavior and Systematics Oceanography |
description |
Twelve saline lakes 5-35m above sea level in Bunger Hills (66°10'S, 101°00'E) were investigated from January to April in 1987-89. Some lakes may be relict and all were subject to wind-borne marine salts with present salinities between 3.4-79.0°/‰ and δ 18 O values mostly between -10 to -14%. Temperatures up to 17.7°C were measured at the bottom of Lake Polest where a sharp thermohalocline was observed during the period of open water. Mg 2+ dominated over Ca 2+ in all the lakes. Phosphates concentration was 3-10 μgP I -1 and total phosphorus 8-16 μgP I -1 . The concentrations of nitrates and nitrites were often equal, ranging between 1-4 μgN I -1 . Dissolved O 2 was usually near saturation levels but peaked at more than 230% of saturation in the hypolimnion of Lake Polest as a result of temperature-enhanced photosynthesis with an assimilation rate of 23.9 mgC (mg Chl a ) -1 h -1 . The values for chlorophyll a were 0.26-1.93 mg m -3 and for primary production 0.013-0.171 gCm -3 d -1 , the latter being an order of magnitude higher than in the fresh water lakes of the Bunger Hills. |
format |
Article in Journal/Newspaper |
author |
Kaup, E. Haendel, D. Vaikmäe, R. |
author_facet |
Kaup, E. Haendel, D. Vaikmäe, R. |
author_sort |
Kaup, E. |
title |
Limnological features of the saline lakes of the Bunger Hills (Wilkes Land, Antarctica) |
title_short |
Limnological features of the saline lakes of the Bunger Hills (Wilkes Land, Antarctica) |
title_full |
Limnological features of the saline lakes of the Bunger Hills (Wilkes Land, Antarctica) |
title_fullStr |
Limnological features of the saline lakes of the Bunger Hills (Wilkes Land, Antarctica) |
title_full_unstemmed |
Limnological features of the saline lakes of the Bunger Hills (Wilkes Land, Antarctica) |
title_sort |
limnological features of the saline lakes of the bunger hills (wilkes land, antarctica) |
publisher |
Cambridge University Press (CUP) |
publishDate |
1993 |
url |
http://dx.doi.org/10.1017/s0954102093000070 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102093000070 |
long_lat |
ENVELOPE(100.883,100.883,-66.167,-66.167) ENVELOPE(120.000,120.000,-69.000,-69.000) |
geographic |
Bunger Hills Wilkes Land |
geographic_facet |
Bunger Hills Wilkes Land |
genre |
Antarc* Antarctic Science Antarctica Wilkes Land |
genre_facet |
Antarc* Antarctic Science Antarctica Wilkes Land |
op_source |
Antarctic Science volume 5, issue 1, page 41-50 ISSN 0954-1020 1365-2079 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0954102093000070 |
container_title |
Antarctic Science |
container_volume |
5 |
container_issue |
1 |
container_start_page |
41 |
op_container_end_page |
50 |
_version_ |
1792499418669252608 |