Nitrate and ammonium uptake in Antarctic waters1

Nitrate and ammonium uptake rates were measured by the 15 N tracer technique in Antarctic waters. The ratio urn:x-wiley:00243590:media:lno19802561064:lno19802561064-math-0001 averaged 0.54 in the Scotia Sea in early spring and 0.40 in the Ross Sea in summer, indicating that NO 3 − and NH 4 + contrib...

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Published in:Limnology and Oceanography
Main Author: Olson, Robert J.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1980
Subjects:
Online Access:http://dx.doi.org/10.4319/lo.1980.25.6.1064
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spelling crwiley:10.4319/lo.1980.25.6.1064 2024-09-15T17:48:01+00:00 Nitrate and ammonium uptake in Antarctic waters1 Olson, Robert J. 1980 http://dx.doi.org/10.4319/lo.1980.25.6.1064 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1980.25.6.1064 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1980.25.6.1064 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 25, issue 6, page 1064-1074 ISSN 0024-3590 1939-5590 journal-article 1980 crwiley https://doi.org/10.4319/lo.1980.25.6.1064 2024-08-30T04:08:45Z Nitrate and ammonium uptake rates were measured by the 15 N tracer technique in Antarctic waters. The ratio urn:x-wiley:00243590:media:lno19802561064:lno19802561064-math-0001 averaged 0.54 in the Scotia Sea in early spring and 0.40 in the Ross Sea in summer, indicating that NO 3 − and NH 4 + contribute about equally to primary production in these regions and that a large proportion of the primary production is exported from the surface layers. Uptake rates in laboratory experiments increased with increasing temperature and the relative uptake of NH 4 + was positively correlated with increasing mean ambient NH 4 + concentration and depth in the water column. Article in Journal/Newspaper Antarc* Antarctic Ross Sea Scotia Sea Wiley Online Library Limnology and Oceanography 25 6 1064 1074
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Nitrate and ammonium uptake rates were measured by the 15 N tracer technique in Antarctic waters. The ratio urn:x-wiley:00243590:media:lno19802561064:lno19802561064-math-0001 averaged 0.54 in the Scotia Sea in early spring and 0.40 in the Ross Sea in summer, indicating that NO 3 − and NH 4 + contribute about equally to primary production in these regions and that a large proportion of the primary production is exported from the surface layers. Uptake rates in laboratory experiments increased with increasing temperature and the relative uptake of NH 4 + was positively correlated with increasing mean ambient NH 4 + concentration and depth in the water column.
format Article in Journal/Newspaper
author Olson, Robert J.
spellingShingle Olson, Robert J.
Nitrate and ammonium uptake in Antarctic waters1
author_facet Olson, Robert J.
author_sort Olson, Robert J.
title Nitrate and ammonium uptake in Antarctic waters1
title_short Nitrate and ammonium uptake in Antarctic waters1
title_full Nitrate and ammonium uptake in Antarctic waters1
title_fullStr Nitrate and ammonium uptake in Antarctic waters1
title_full_unstemmed Nitrate and ammonium uptake in Antarctic waters1
title_sort nitrate and ammonium uptake in antarctic waters1
publisher Wiley
publishDate 1980
url http://dx.doi.org/10.4319/lo.1980.25.6.1064
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1980.25.6.1064
https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1980.25.6.1064
genre Antarc*
Antarctic
Ross Sea
Scotia Sea
genre_facet Antarc*
Antarctic
Ross Sea
Scotia Sea
op_source Limnology and Oceanography
volume 25, issue 6, page 1064-1074
ISSN 0024-3590 1939-5590
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.4319/lo.1980.25.6.1064
container_title Limnology and Oceanography
container_volume 25
container_issue 6
container_start_page 1064
op_container_end_page 1074
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