Supersaturated N2O in a perennially ice‐covered Antarctic lake: Molecular and stable isotopic evidence for a biogeochemical relict
The east lobe of Lake Bonney, a permanently ice‐covered lake in the McMurdo Dry Valleys, Antarctica, has a mid‐depth maximum N 2 O concentration of 43.3 [mol N L ‐1 (>700,000% saturation with respect to air), representing one of the highest concentrations reported for a natural aquatic system. δ...
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crwiley:10.4319/lo.2008.53.6.2439 2024-09-15T17:44:02+00:00 Supersaturated N2O in a perennially ice‐covered Antarctic lake: Molecular and stable isotopic evidence for a biogeochemical relict Priscu, John C. Christner, Brent C. Dore, John E. Popp, Brian N. Casciotti, Karen L. Lyons, W. Berry 2008 http://dx.doi.org/10.4319/lo.2008.53.6.2439 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2008.53.6.2439 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2008.53.6.2439 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 53, issue 6, page 2439-2450 ISSN 0024-3590 1939-5590 journal-article 2008 crwiley https://doi.org/10.4319/lo.2008.53.6.2439 2024-08-22T04:18:06Z The east lobe of Lake Bonney, a permanently ice‐covered lake in the McMurdo Dry Valleys, Antarctica, has a mid‐depth maximum N 2 O concentration of 43.3 [mol N L ‐1 (>700,000% saturation with respect to air), representing one of the highest concentrations reported for a natural aquatic system. δ 15 N and δ 18 O measurements indicate that this is the most isotopically depleted N 2 O yet observed in a natural environment (minimum δ 15 N‐N 2 O of ‐79.6‰ vs. air‐N 2 minimum δ 18 O‐N 2 O of ‐4.7‰ vs. Vienna standard mean ocean water), providing new end points for these parameters in natural systems. The extremely depleted nitrogen and oxygen isotopes, together with nitrogen isotopic isomer data for N 2 O, imply that most of the N 2 O was produced via incomplete nitrification and has undergone virtually no subsequent consumption. However, molecular evidence provides little support for metabolically active nitrifying populations at depths where the maximal N 2 O concentrations occur and contemporary biogeochemical reactions cannot explain the extreme excesses of N 2 O in Lake Bonney. The gas appears to be a legacy of past biogeochemical conditions within the lake, and in the absence of a significant sink and the presence of a highly stable water column, gradients in N 2 O produced by past microbial activity could persist in the cold saline waters of Lake Bonney for >10 4 years. Article in Journal/Newspaper Antarc* Antarctic Antarctica McMurdo Dry Valleys Wiley Online Library Limnology and Oceanography 53 6 2439 2450 |
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English |
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The east lobe of Lake Bonney, a permanently ice‐covered lake in the McMurdo Dry Valleys, Antarctica, has a mid‐depth maximum N 2 O concentration of 43.3 [mol N L ‐1 (>700,000% saturation with respect to air), representing one of the highest concentrations reported for a natural aquatic system. δ 15 N and δ 18 O measurements indicate that this is the most isotopically depleted N 2 O yet observed in a natural environment (minimum δ 15 N‐N 2 O of ‐79.6‰ vs. air‐N 2 minimum δ 18 O‐N 2 O of ‐4.7‰ vs. Vienna standard mean ocean water), providing new end points for these parameters in natural systems. The extremely depleted nitrogen and oxygen isotopes, together with nitrogen isotopic isomer data for N 2 O, imply that most of the N 2 O was produced via incomplete nitrification and has undergone virtually no subsequent consumption. However, molecular evidence provides little support for metabolically active nitrifying populations at depths where the maximal N 2 O concentrations occur and contemporary biogeochemical reactions cannot explain the extreme excesses of N 2 O in Lake Bonney. The gas appears to be a legacy of past biogeochemical conditions within the lake, and in the absence of a significant sink and the presence of a highly stable water column, gradients in N 2 O produced by past microbial activity could persist in the cold saline waters of Lake Bonney for >10 4 years. |
format |
Article in Journal/Newspaper |
author |
Priscu, John C. Christner, Brent C. Dore, John E. Popp, Brian N. Casciotti, Karen L. Lyons, W. Berry |
spellingShingle |
Priscu, John C. Christner, Brent C. Dore, John E. Popp, Brian N. Casciotti, Karen L. Lyons, W. Berry Supersaturated N2O in a perennially ice‐covered Antarctic lake: Molecular and stable isotopic evidence for a biogeochemical relict |
author_facet |
Priscu, John C. Christner, Brent C. Dore, John E. Popp, Brian N. Casciotti, Karen L. Lyons, W. Berry |
author_sort |
Priscu, John C. |
title |
Supersaturated N2O in a perennially ice‐covered Antarctic lake: Molecular and stable isotopic evidence for a biogeochemical relict |
title_short |
Supersaturated N2O in a perennially ice‐covered Antarctic lake: Molecular and stable isotopic evidence for a biogeochemical relict |
title_full |
Supersaturated N2O in a perennially ice‐covered Antarctic lake: Molecular and stable isotopic evidence for a biogeochemical relict |
title_fullStr |
Supersaturated N2O in a perennially ice‐covered Antarctic lake: Molecular and stable isotopic evidence for a biogeochemical relict |
title_full_unstemmed |
Supersaturated N2O in a perennially ice‐covered Antarctic lake: Molecular and stable isotopic evidence for a biogeochemical relict |
title_sort |
supersaturated n2o in a perennially ice‐covered antarctic lake: molecular and stable isotopic evidence for a biogeochemical relict |
publisher |
Wiley |
publishDate |
2008 |
url |
http://dx.doi.org/10.4319/lo.2008.53.6.2439 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2008.53.6.2439 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2008.53.6.2439 |
genre |
Antarc* Antarctic Antarctica McMurdo Dry Valleys |
genre_facet |
Antarc* Antarctic Antarctica McMurdo Dry Valleys |
op_source |
Limnology and Oceanography volume 53, issue 6, page 2439-2450 ISSN 0024-3590 1939-5590 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.4319/lo.2008.53.6.2439 |
container_title |
Limnology and Oceanography |
container_volume |
53 |
container_issue |
6 |
container_start_page |
2439 |
op_container_end_page |
2450 |
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1810491317205073920 |