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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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 |
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Open Polar |
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Wiley Online Library |
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crwiley |
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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 |
_version_ |
1810288666772242432 |