Iron‐light interactions differ in Southern Ocean phytoplankton

In laboratory experiments we examined the interplay of light and iron availability on the intracellular iron concentrations, specific growth rates, and photosynthetic physiology of Southern (S.) Ocean diatoms ( Eucampia antarctica and Proboscia inermis ) and the haptophyte Phaeocystis antarctica . I...

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Published in:Limnology and Oceanography
Main Authors: Strzepek, Robert F., Hunter, Keith A., Frew, Russell D., Harrison, Paul J., Boyd, Philip W.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2012
Subjects:
Online Access:http://dx.doi.org/10.4319/lo.2012.57.4.1182
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spelling crwiley:10.4319/lo.2012.57.4.1182 2024-09-15T17:48:49+00:00 Iron‐light interactions differ in Southern Ocean phytoplankton Strzepek, Robert F. Hunter, Keith A. Frew, Russell D. Harrison, Paul J. Boyd, Philip W. 2012 http://dx.doi.org/10.4319/lo.2012.57.4.1182 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2012.57.4.1182 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2012.57.4.1182 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 57, issue 4, page 1182-1200 ISSN 0024-3590 1939-5590 journal-article 2012 crwiley https://doi.org/10.4319/lo.2012.57.4.1182 2024-09-05T05:08:18Z In laboratory experiments we examined the interplay of light and iron availability on the intracellular iron concentrations, specific growth rates, and photosynthetic physiology of Southern (S.) Ocean diatoms ( Eucampia antarctica and Proboscia inermis ) and the haptophyte Phaeocystis antarctica . Intracellular iron concentrations and iron : carbon (Fe : C) molar ratios increased with decreasing irradiance in temperate coastal ( Thalassiosira weissflogii ) and oceanic ( Thalassiosira oceanica ) diatoms, in support of the well‐established antagonistic iron‐light relationship. In contrast, S. Ocean species required lower cellular iron concentrations and Fe : C ratios than temperate diatoms to grow at comparable rates, and their iron requirements decreased or remained relatively constant with decreasing light. These results suggest that the current paradigm that low light increases algal cellular iron requirements (supplied through “biodilution”) is not applicable to S. Ocean phytoplankton. Although iron use efficiencies decreased at sub‐saturating light in all species, these reductions were due primarily to lower growth rates, but not higher intracellular Fe : C ratios, in S. Ocean species. We propose that S. Ocean species have overcome the antagonistic iron‐light relationship by increasing the size, rather than the number, of photosynthetic units under low irradiances, resulting in an acclimation strategy that does not increase their cellular iron requirements. Article in Journal/Newspaper Antarc* Antarctica Southern Ocean Wiley Online Library Limnology and Oceanography 57 4 1182 1200
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description In laboratory experiments we examined the interplay of light and iron availability on the intracellular iron concentrations, specific growth rates, and photosynthetic physiology of Southern (S.) Ocean diatoms ( Eucampia antarctica and Proboscia inermis ) and the haptophyte Phaeocystis antarctica . Intracellular iron concentrations and iron : carbon (Fe : C) molar ratios increased with decreasing irradiance in temperate coastal ( Thalassiosira weissflogii ) and oceanic ( Thalassiosira oceanica ) diatoms, in support of the well‐established antagonistic iron‐light relationship. In contrast, S. Ocean species required lower cellular iron concentrations and Fe : C ratios than temperate diatoms to grow at comparable rates, and their iron requirements decreased or remained relatively constant with decreasing light. These results suggest that the current paradigm that low light increases algal cellular iron requirements (supplied through “biodilution”) is not applicable to S. Ocean phytoplankton. Although iron use efficiencies decreased at sub‐saturating light in all species, these reductions were due primarily to lower growth rates, but not higher intracellular Fe : C ratios, in S. Ocean species. We propose that S. Ocean species have overcome the antagonistic iron‐light relationship by increasing the size, rather than the number, of photosynthetic units under low irradiances, resulting in an acclimation strategy that does not increase their cellular iron requirements.
format Article in Journal/Newspaper
author Strzepek, Robert F.
Hunter, Keith A.
Frew, Russell D.
Harrison, Paul J.
Boyd, Philip W.
spellingShingle Strzepek, Robert F.
Hunter, Keith A.
Frew, Russell D.
Harrison, Paul J.
Boyd, Philip W.
Iron‐light interactions differ in Southern Ocean phytoplankton
author_facet Strzepek, Robert F.
Hunter, Keith A.
Frew, Russell D.
Harrison, Paul J.
Boyd, Philip W.
author_sort Strzepek, Robert F.
title Iron‐light interactions differ in Southern Ocean phytoplankton
title_short Iron‐light interactions differ in Southern Ocean phytoplankton
title_full Iron‐light interactions differ in Southern Ocean phytoplankton
title_fullStr Iron‐light interactions differ in Southern Ocean phytoplankton
title_full_unstemmed Iron‐light interactions differ in Southern Ocean phytoplankton
title_sort iron‐light interactions differ in southern ocean phytoplankton
publisher Wiley
publishDate 2012
url http://dx.doi.org/10.4319/lo.2012.57.4.1182
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2012.57.4.1182
https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2012.57.4.1182
genre Antarc*
Antarctica
Southern Ocean
genre_facet Antarc*
Antarctica
Southern Ocean
op_source Limnology and Oceanography
volume 57, issue 4, page 1182-1200
ISSN 0024-3590 1939-5590
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.4319/lo.2012.57.4.1182
container_title Limnology and Oceanography
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container_start_page 1182
op_container_end_page 1200
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