www.biogeosciences.net/7/289/2010/ © Author(s) 2010. This work is distributed under the Creative Commons Attribution 3.0 License.
Abstract. Atmospheric CO2 partial pressure (pCO2) is ex-pected to increase to 700 µatm or more by the end of the present century. Anthropogenic CO2 is absorbed by the oceans, leading to decreases in pH and the CaCO3 saturation state () of the seawater. Elevated pCO2 was shown to dras-tically decreas...
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.461.2672 http://www.biogeosciences.net/7/289/2010/bg-7-289-2010.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.461.2672 2023-05-15T17:51:19+02:00 www.biogeosciences.net/7/289/2010/ © Author(s) 2010. This work is distributed under the Creative Commons Attribution 3.0 License. R. Rodolfo-metalpa S. Martin J. -p. Gattuso The Pennsylvania State University CiteSeerX Archives 2009 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.461.2672 http://www.biogeosciences.net/7/289/2010/bg-7-289-2010.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.461.2672 http://www.biogeosciences.net/7/289/2010/bg-7-289-2010.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.biogeosciences.net/7/289/2010/bg-7-289-2010.pdf text 2009 ftciteseerx 2016-01-08T06:36:19Z Abstract. Atmospheric CO2 partial pressure (pCO2) is ex-pected to increase to 700 µatm or more by the end of the present century. Anthropogenic CO2 is absorbed by the oceans, leading to decreases in pH and the CaCO3 saturation state () of the seawater. Elevated pCO2 was shown to dras-tically decrease calcification rates in tropical zooxanthellate corals. Here we show, using the Mediterranean zooxanthel-late coral Cladocora caespitosa, that an increase in pCO2, in the range predicted for 2100, does not reduce its calcifi-cation rate. Therefore, the conventional belief that calcifica-tion rates will be affected by ocean acidification may not be widespread in temperate corals. Seasonal change in temper-ature is the predominant factor controlling photosynthesis, respiration, calcification and symbiont density. An increase in pCO2, alone or in combination with elevated temperature, had no significant effect on photosynthesis, photosynthetic efficiency and calcification. The lack of sensitivity C. cae-spitosa to elevated pCO2 might be due to its slow growth rates, which seem to be more dependent on temperature than on the saturation state of calcium carbonate in the range pro-jected for the end of the century. Text Ocean acidification Unknown |
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ftciteseerx |
language |
English |
description |
Abstract. Atmospheric CO2 partial pressure (pCO2) is ex-pected to increase to 700 µatm or more by the end of the present century. Anthropogenic CO2 is absorbed by the oceans, leading to decreases in pH and the CaCO3 saturation state () of the seawater. Elevated pCO2 was shown to dras-tically decrease calcification rates in tropical zooxanthellate corals. Here we show, using the Mediterranean zooxanthel-late coral Cladocora caespitosa, that an increase in pCO2, in the range predicted for 2100, does not reduce its calcifi-cation rate. Therefore, the conventional belief that calcifica-tion rates will be affected by ocean acidification may not be widespread in temperate corals. Seasonal change in temper-ature is the predominant factor controlling photosynthesis, respiration, calcification and symbiont density. An increase in pCO2, alone or in combination with elevated temperature, had no significant effect on photosynthesis, photosynthetic efficiency and calcification. The lack of sensitivity C. cae-spitosa to elevated pCO2 might be due to its slow growth rates, which seem to be more dependent on temperature than on the saturation state of calcium carbonate in the range pro-jected for the end of the century. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
R. Rodolfo-metalpa S. Martin J. -p. Gattuso |
spellingShingle |
R. Rodolfo-metalpa S. Martin J. -p. Gattuso www.biogeosciences.net/7/289/2010/ © Author(s) 2010. This work is distributed under the Creative Commons Attribution 3.0 License. |
author_facet |
R. Rodolfo-metalpa S. Martin J. -p. Gattuso |
author_sort |
R. Rodolfo-metalpa |
title |
www.biogeosciences.net/7/289/2010/ © Author(s) 2010. This work is distributed under the Creative Commons Attribution 3.0 License. |
title_short |
www.biogeosciences.net/7/289/2010/ © Author(s) 2010. This work is distributed under the Creative Commons Attribution 3.0 License. |
title_full |
www.biogeosciences.net/7/289/2010/ © Author(s) 2010. This work is distributed under the Creative Commons Attribution 3.0 License. |
title_fullStr |
www.biogeosciences.net/7/289/2010/ © Author(s) 2010. This work is distributed under the Creative Commons Attribution 3.0 License. |
title_full_unstemmed |
www.biogeosciences.net/7/289/2010/ © Author(s) 2010. This work is distributed under the Creative Commons Attribution 3.0 License. |
title_sort |
www.biogeosciences.net/7/289/2010/ © author(s) 2010. this work is distributed under the creative commons attribution 3.0 license. |
publishDate |
2009 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.461.2672 http://www.biogeosciences.net/7/289/2010/bg-7-289-2010.pdf |
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Ocean acidification |
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Ocean acidification |
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http://www.biogeosciences.net/7/289/2010/bg-7-289-2010.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.461.2672 http://www.biogeosciences.net/7/289/2010/bg-7-289-2010.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766158422424682496 |