Inorganic carbon uptake by Southern Ocean phytoplankton
We report the results of laboratory and field studies examining inorganic carbon (C i ) utilization by Southern Ocean phytoplankton. Both in monospecific laboratory cultures of diatoms and Phaeocystis antarctica and in natural assemblages in the Ross Sea, C i uptake by phytoplankton was dominated by...
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crwiley:10.4319/lo.2008.53.4.1266 2024-09-15T17:48:06+00:00 Inorganic carbon uptake by Southern Ocean phytoplankton Tortell, Philippe D. Payne, Chris Gueguen, Celine Strzepek, Robert F. Boyd, Philip W. Rost, Björn 2008 http://dx.doi.org/10.4319/lo.2008.53.4.1266 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2008.53.4.1266 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2008.53.4.1266 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 53, issue 4, page 1266-1278 ISSN 0024-3590 1939-5590 journal-article 2008 crwiley https://doi.org/10.4319/lo.2008.53.4.1266 2024-07-30T04:17:26Z We report the results of laboratory and field studies examining inorganic carbon (C i ) utilization by Southern Ocean phytoplankton. Both in monospecific laboratory cultures of diatoms and Phaeocystis antarctica and in natural assemblages in the Ross Sea, C i uptake by phytoplankton was dominated by direct HCO 3 1 transport. The contribution of HCO 3 1 transport to total C i uptake ranged from 65% to 95%, with an overall average of ∼80%. There was no significant difference among diatoms and Phaeocystis in the extent of HCO 3 1 transport. Extracellular carbonic anhydrase activity (eCA) was detected in eight of nine laboratory phytoplankton cultures and in all natural assemblages in the Ross Sea. The effective catalytic enhancement of HCO 3 1 : CO 2 interconversion ranged from 1.5‐ to 13‐fold (overall mean ∼4‐fold). Diatom‐dominated Ross Sea assemblages had significantly greater eCA levels than did Phaeocystis‐dominated assemblages. We found no strong correlations between C i uptake parameters and in situ CO 2 concentrations or chlorophyll a levels in the Ross Sea assemblages. Incubation experiments with natural assemblages showed that HCO 3 1 uptake and eCA expression did not change significantly over an 8‐fold range in pCO 2 (10.1‐81.1 Pa), although total short‐term C fixation rates increased under low CO 2 conditions. Carbon‐concentrating mechanisms are widespread among Southern Ocean phytoplankton and constitutively expressed by natural assemblages in the Ross Sea. Article in Journal/Newspaper Antarc* Antarctica Ross Sea Southern Ocean Wiley Online Library Limnology and Oceanography 53 4 1266 1278 |
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Wiley Online Library |
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crwiley |
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English |
description |
We report the results of laboratory and field studies examining inorganic carbon (C i ) utilization by Southern Ocean phytoplankton. Both in monospecific laboratory cultures of diatoms and Phaeocystis antarctica and in natural assemblages in the Ross Sea, C i uptake by phytoplankton was dominated by direct HCO 3 1 transport. The contribution of HCO 3 1 transport to total C i uptake ranged from 65% to 95%, with an overall average of ∼80%. There was no significant difference among diatoms and Phaeocystis in the extent of HCO 3 1 transport. Extracellular carbonic anhydrase activity (eCA) was detected in eight of nine laboratory phytoplankton cultures and in all natural assemblages in the Ross Sea. The effective catalytic enhancement of HCO 3 1 : CO 2 interconversion ranged from 1.5‐ to 13‐fold (overall mean ∼4‐fold). Diatom‐dominated Ross Sea assemblages had significantly greater eCA levels than did Phaeocystis‐dominated assemblages. We found no strong correlations between C i uptake parameters and in situ CO 2 concentrations or chlorophyll a levels in the Ross Sea assemblages. Incubation experiments with natural assemblages showed that HCO 3 1 uptake and eCA expression did not change significantly over an 8‐fold range in pCO 2 (10.1‐81.1 Pa), although total short‐term C fixation rates increased under low CO 2 conditions. Carbon‐concentrating mechanisms are widespread among Southern Ocean phytoplankton and constitutively expressed by natural assemblages in the Ross Sea. |
format |
Article in Journal/Newspaper |
author |
Tortell, Philippe D. Payne, Chris Gueguen, Celine Strzepek, Robert F. Boyd, Philip W. Rost, Björn |
spellingShingle |
Tortell, Philippe D. Payne, Chris Gueguen, Celine Strzepek, Robert F. Boyd, Philip W. Rost, Björn Inorganic carbon uptake by Southern Ocean phytoplankton |
author_facet |
Tortell, Philippe D. Payne, Chris Gueguen, Celine Strzepek, Robert F. Boyd, Philip W. Rost, Björn |
author_sort |
Tortell, Philippe D. |
title |
Inorganic carbon uptake by Southern Ocean phytoplankton |
title_short |
Inorganic carbon uptake by Southern Ocean phytoplankton |
title_full |
Inorganic carbon uptake by Southern Ocean phytoplankton |
title_fullStr |
Inorganic carbon uptake by Southern Ocean phytoplankton |
title_full_unstemmed |
Inorganic carbon uptake by Southern Ocean phytoplankton |
title_sort |
inorganic carbon uptake by southern ocean phytoplankton |
publisher |
Wiley |
publishDate |
2008 |
url |
http://dx.doi.org/10.4319/lo.2008.53.4.1266 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2008.53.4.1266 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2008.53.4.1266 |
genre |
Antarc* Antarctica Ross Sea Southern Ocean |
genre_facet |
Antarc* Antarctica Ross Sea Southern Ocean |
op_source |
Limnology and Oceanography volume 53, issue 4, page 1266-1278 ISSN 0024-3590 1939-5590 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.4319/lo.2008.53.4.1266 |
container_title |
Limnology and Oceanography |
container_volume |
53 |
container_issue |
4 |
container_start_page |
1266 |
op_container_end_page |
1278 |
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1810289138481496064 |