Estimates of sulphate reduction rates in Lake Vanda, Antarctica support the proposed recent history of the lake
Lake Vanda, a perennially ice-covered Antarctic lake has a highly stratified structure with a pronounced density gradient from 45 m and is anoxic from 68 m down. In order to gain a greater understanding of the carbon cycling in the lake we attempted to measure sulphate reduction in the summer of 199...
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crcambridgeupr:10.1017/s0954102001000554 2024-04-28T07:59:25+00:00 Estimates of sulphate reduction rates in Lake Vanda, Antarctica support the proposed recent history of the lake Purdy, K.J. Hawes, I. Bryant, C.L. Fallick, A.E. Nedwell, D.B. 2001 http://dx.doi.org/10.1017/s0954102001000554 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102001000554 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 13, issue 4, page 393-399 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 2001 crcambridgeupr https://doi.org/10.1017/s0954102001000554 2024-04-09T06:55:00Z Lake Vanda, a perennially ice-covered Antarctic lake has a highly stratified structure with a pronounced density gradient from 45 m and is anoxic from 68 m down. In order to gain a greater understanding of the carbon cycling in the lake we attempted to measure sulphate reduction in the summer of 1994, but rates were below detectable limits of 1.2 × 10 6 mol sulphate yr −1 . Therefore sulphate reduction was estimated by calculating the rate of sulphide diffusion from the anoxic zone. Sulphate reduction rates were estimated to be 17.7 × 10 3 mol sulphate yr −1 , accounting for 30% of planktonic primary production over the whole lake, but over 100% of primary productivity in the deep chlorophyll maximum. Radiocarbon dating of organic matter in the sediment (565 ± 50 yr bp ), suggests that little new organic carbon reaches the sediment from the upper water column. Oxygen diffusion into the anoxic zone could account for only 44% of sulphide reoxidation; therefore, alternative oxidizing potential presumably accounted for the remainder. Sulphate concentration may be controlled by the solubility limit for a mineral phase, perhaps gypsum, as it shows a positive correlation with conductivity. The sulphur species in the anoxic zone are highly enriched in 34 S (sulphate δ 34 S = + 42 to + 46% 0 , sulphide δ 34 S = + 13.9% 0 ) which may be explained by either selective removal of sulphide at the oxic/anoxic interface by precipitation of metal sulphides or previous loss ofH 2 S to the atmosphere. While sulphate reduction is an important part of the carbon cycle within the lake, the oligotrophic nature of Lake Vanda means that all microbiological process rates are very low. The data presented suggest a dynamic and complex history for Lake Vanda and are entirely consistent with present theories of the lake's history. Article in Journal/Newspaper Antarc* Antarctic Antarctic Science Antarctica Cambridge University Press Antarctic Science 13 4 393 399 |
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Cambridge University Press |
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English |
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Geology Ecology, Evolution, Behavior and Systematics Oceanography |
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Geology Ecology, Evolution, Behavior and Systematics Oceanography Purdy, K.J. Hawes, I. Bryant, C.L. Fallick, A.E. Nedwell, D.B. Estimates of sulphate reduction rates in Lake Vanda, Antarctica support the proposed recent history of the lake |
topic_facet |
Geology Ecology, Evolution, Behavior and Systematics Oceanography |
description |
Lake Vanda, a perennially ice-covered Antarctic lake has a highly stratified structure with a pronounced density gradient from 45 m and is anoxic from 68 m down. In order to gain a greater understanding of the carbon cycling in the lake we attempted to measure sulphate reduction in the summer of 1994, but rates were below detectable limits of 1.2 × 10 6 mol sulphate yr −1 . Therefore sulphate reduction was estimated by calculating the rate of sulphide diffusion from the anoxic zone. Sulphate reduction rates were estimated to be 17.7 × 10 3 mol sulphate yr −1 , accounting for 30% of planktonic primary production over the whole lake, but over 100% of primary productivity in the deep chlorophyll maximum. Radiocarbon dating of organic matter in the sediment (565 ± 50 yr bp ), suggests that little new organic carbon reaches the sediment from the upper water column. Oxygen diffusion into the anoxic zone could account for only 44% of sulphide reoxidation; therefore, alternative oxidizing potential presumably accounted for the remainder. Sulphate concentration may be controlled by the solubility limit for a mineral phase, perhaps gypsum, as it shows a positive correlation with conductivity. The sulphur species in the anoxic zone are highly enriched in 34 S (sulphate δ 34 S = + 42 to + 46% 0 , sulphide δ 34 S = + 13.9% 0 ) which may be explained by either selective removal of sulphide at the oxic/anoxic interface by precipitation of metal sulphides or previous loss ofH 2 S to the atmosphere. While sulphate reduction is an important part of the carbon cycle within the lake, the oligotrophic nature of Lake Vanda means that all microbiological process rates are very low. The data presented suggest a dynamic and complex history for Lake Vanda and are entirely consistent with present theories of the lake's history. |
format |
Article in Journal/Newspaper |
author |
Purdy, K.J. Hawes, I. Bryant, C.L. Fallick, A.E. Nedwell, D.B. |
author_facet |
Purdy, K.J. Hawes, I. Bryant, C.L. Fallick, A.E. Nedwell, D.B. |
author_sort |
Purdy, K.J. |
title |
Estimates of sulphate reduction rates in Lake Vanda, Antarctica support the proposed recent history of the lake |
title_short |
Estimates of sulphate reduction rates in Lake Vanda, Antarctica support the proposed recent history of the lake |
title_full |
Estimates of sulphate reduction rates in Lake Vanda, Antarctica support the proposed recent history of the lake |
title_fullStr |
Estimates of sulphate reduction rates in Lake Vanda, Antarctica support the proposed recent history of the lake |
title_full_unstemmed |
Estimates of sulphate reduction rates in Lake Vanda, Antarctica support the proposed recent history of the lake |
title_sort |
estimates of sulphate reduction rates in lake vanda, antarctica support the proposed recent history of the lake |
publisher |
Cambridge University Press (CUP) |
publishDate |
2001 |
url |
http://dx.doi.org/10.1017/s0954102001000554 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102001000554 |
genre |
Antarc* Antarctic Antarctic Science Antarctica |
genre_facet |
Antarc* Antarctic Antarctic Science Antarctica |
op_source |
Antarctic Science volume 13, issue 4, page 393-399 ISSN 0954-1020 1365-2079 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0954102001000554 |
container_title |
Antarctic Science |
container_volume |
13 |
container_issue |
4 |
container_start_page |
393 |
op_container_end_page |
399 |
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1797572183758733312 |