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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Published in:Limnology and Oceanography
Main Authors: Tortell, Philippe D., Payne, Chris, Gueguen, Celine, Strzepek, Robert F., Boyd, Philip W., Rost, Björn
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2008
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Online Access:http://dx.doi.org/10.4319/lo.2008.53.4.1266
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spelling 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
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language 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
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