Predominance of heavily calcified coccolithophores at low CaCO3 saturation during winter in the Bay of Biscay

Coccolithophores are an important component of the Earth system, and, as calcifiers, their possible susceptibility to ocean acidification is of major concern. Laboratory studies at enhanced pCO2 levels have produced divergent results without overall consensus. However, it has been predicted from the...

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Published in:Proceedings of the National Academy of Sciences
Main Authors: Smith, H. E. K., Tyrrell, T., Charalampopoulou, A., Dumousseaud, C., Legge, O. J., Birchenough, S., Pettit, L. R., Garley, R., Hartman, S. E., Hartman, M. C., Sagoo, N., Daniels, C. J., Achterberg, Eric P., Hydes, D. J.
Format: Article in Journal/Newspaper
Language:English
Published: National Academy of Sciences 2012
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/21745/
https://oceanrep.geomar.de/id/eprint/21745/1/PNAS-2012-Smith-8845-9.pdf
https://doi.org/10.1073/pnas.1117508109
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spelling ftoceanrep:oai:oceanrep.geomar.de:21745 2023-05-15T17:51:28+02:00 Predominance of heavily calcified coccolithophores at low CaCO3 saturation during winter in the Bay of Biscay Smith, H. E. K. Tyrrell, T. Charalampopoulou, A. Dumousseaud, C. Legge, O. J. Birchenough, S. Pettit, L. R. Garley, R. Hartman, S. E. Hartman, M. C. Sagoo, N. Daniels, C. J. Achterberg, Eric P. Hydes, D. J. 2012 text https://oceanrep.geomar.de/id/eprint/21745/ https://oceanrep.geomar.de/id/eprint/21745/1/PNAS-2012-Smith-8845-9.pdf https://doi.org/10.1073/pnas.1117508109 en eng National Academy of Sciences https://oceanrep.geomar.de/id/eprint/21745/1/PNAS-2012-Smith-8845-9.pdf Smith, H. E. K., Tyrrell, T., Charalampopoulou, A., Dumousseaud, C., Legge, O. J., Birchenough, S., Pettit, L. R., Garley, R., Hartman, S. E., Hartman, M. C., Sagoo, N., Daniels, C. J., Achterberg, E. P. and Hydes, D. J. (2012) Predominance of heavily calcified coccolithophores at low CaCO3 saturation during winter in the Bay of Biscay. PNAS Proceedings of the National Academy of Sciences of the United States of America, 109 (23). pp. 8845-8849. DOI 10.1073/pnas.1117508109 <https://doi.org/10.1073/pnas.1117508109>. doi:10.1073/pnas.1117508109 Article PeerReviewed 2012 ftoceanrep https://doi.org/10.1073/pnas.1117508109 2023-04-07T15:09:49Z Coccolithophores are an important component of the Earth system, and, as calcifiers, their possible susceptibility to ocean acidification is of major concern. Laboratory studies at enhanced pCO2 levels have produced divergent results without overall consensus. However, it has been predicted from these studies that, although calcification may not be depressed in all species, acidification will produce "a transition in dominance from more to less heavily calcified coccolithophores"Ridgwell A, et al., (2009) Biogeosciences 6:2611-2623. A recent observational study Beaufort L, et al., (2011) Nature 476:80-83 also suggested that coccolithophores are less calcified in more acidic conditions.We present the results of a large observational study of coccolithophore morphology in the Bay of Biscay. Samples were collected once a month for over a year, along a 1,000-km-long transect. Our data clearly show that there is a pronounced seasonality in the morphotypes of Emiliania huxleyi, the most abundant coccolithophore species. Whereas pH and CaCO 3saturation are lowest in winter, the E. huxleyi population shifts from <10% (summer) to >90% (winter) of the heavily calcified form. However, it is unlikely that the shifts in carbonate chemistry alone caused the morphotype shift. Our finding that the most heavily calcified morphotype dominates when conditions are most acidic is contrary to the earlier predictions and raises further questions about the fate of coccolithophores in a high-CO2 world. Article in Journal/Newspaper Ocean acidification OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Proceedings of the National Academy of Sciences 109 23 8845 8849
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
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language English
description Coccolithophores are an important component of the Earth system, and, as calcifiers, their possible susceptibility to ocean acidification is of major concern. Laboratory studies at enhanced pCO2 levels have produced divergent results without overall consensus. However, it has been predicted from these studies that, although calcification may not be depressed in all species, acidification will produce "a transition in dominance from more to less heavily calcified coccolithophores"Ridgwell A, et al., (2009) Biogeosciences 6:2611-2623. A recent observational study Beaufort L, et al., (2011) Nature 476:80-83 also suggested that coccolithophores are less calcified in more acidic conditions.We present the results of a large observational study of coccolithophore morphology in the Bay of Biscay. Samples were collected once a month for over a year, along a 1,000-km-long transect. Our data clearly show that there is a pronounced seasonality in the morphotypes of Emiliania huxleyi, the most abundant coccolithophore species. Whereas pH and CaCO 3saturation are lowest in winter, the E. huxleyi population shifts from <10% (summer) to >90% (winter) of the heavily calcified form. However, it is unlikely that the shifts in carbonate chemistry alone caused the morphotype shift. Our finding that the most heavily calcified morphotype dominates when conditions are most acidic is contrary to the earlier predictions and raises further questions about the fate of coccolithophores in a high-CO2 world.
format Article in Journal/Newspaper
author Smith, H. E. K.
Tyrrell, T.
Charalampopoulou, A.
Dumousseaud, C.
Legge, O. J.
Birchenough, S.
Pettit, L. R.
Garley, R.
Hartman, S. E.
Hartman, M. C.
Sagoo, N.
Daniels, C. J.
Achterberg, Eric P.
Hydes, D. J.
spellingShingle Smith, H. E. K.
Tyrrell, T.
Charalampopoulou, A.
Dumousseaud, C.
Legge, O. J.
Birchenough, S.
Pettit, L. R.
Garley, R.
Hartman, S. E.
Hartman, M. C.
Sagoo, N.
Daniels, C. J.
Achterberg, Eric P.
Hydes, D. J.
Predominance of heavily calcified coccolithophores at low CaCO3 saturation during winter in the Bay of Biscay
author_facet Smith, H. E. K.
Tyrrell, T.
Charalampopoulou, A.
Dumousseaud, C.
Legge, O. J.
Birchenough, S.
Pettit, L. R.
Garley, R.
Hartman, S. E.
Hartman, M. C.
Sagoo, N.
Daniels, C. J.
Achterberg, Eric P.
Hydes, D. J.
author_sort Smith, H. E. K.
title Predominance of heavily calcified coccolithophores at low CaCO3 saturation during winter in the Bay of Biscay
title_short Predominance of heavily calcified coccolithophores at low CaCO3 saturation during winter in the Bay of Biscay
title_full Predominance of heavily calcified coccolithophores at low CaCO3 saturation during winter in the Bay of Biscay
title_fullStr Predominance of heavily calcified coccolithophores at low CaCO3 saturation during winter in the Bay of Biscay
title_full_unstemmed Predominance of heavily calcified coccolithophores at low CaCO3 saturation during winter in the Bay of Biscay
title_sort predominance of heavily calcified coccolithophores at low caco3 saturation during winter in the bay of biscay
publisher National Academy of Sciences
publishDate 2012
url https://oceanrep.geomar.de/id/eprint/21745/
https://oceanrep.geomar.de/id/eprint/21745/1/PNAS-2012-Smith-8845-9.pdf
https://doi.org/10.1073/pnas.1117508109
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://oceanrep.geomar.de/id/eprint/21745/1/PNAS-2012-Smith-8845-9.pdf
Smith, H. E. K., Tyrrell, T., Charalampopoulou, A., Dumousseaud, C., Legge, O. J., Birchenough, S., Pettit, L. R., Garley, R., Hartman, S. E., Hartman, M. C., Sagoo, N., Daniels, C. J., Achterberg, E. P. and Hydes, D. J. (2012) Predominance of heavily calcified coccolithophores at low CaCO3 saturation during winter in the Bay of Biscay. PNAS Proceedings of the National Academy of Sciences of the United States of America, 109 (23). pp. 8845-8849. DOI 10.1073/pnas.1117508109 <https://doi.org/10.1073/pnas.1117508109>.
doi:10.1073/pnas.1117508109
op_doi https://doi.org/10.1073/pnas.1117508109
container_title Proceedings of the National Academy of Sciences
container_volume 109
container_issue 23
container_start_page 8845
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