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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Published in:Limnology and Oceanography
Main Authors: Priscu, John C., Christner, Brent C., Dore, John E., Popp, Brian N., Casciotti, Karen L., Lyons, W. Berry
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2008
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Online Access:http://dx.doi.org/10.4319/lo.2008.53.6.2439
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spelling 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
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description 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
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