Coral reefs modify their seawater carbon chemistry - Implications for impacts of ocean acidification
Reviews suggest that that the biogeochemical threshold for sustained coral reef growth will be reached during this century due to ocean acidification caused by increased uptake of atmospheric CO₂. Projections of ocean acidification, however, are based on air-sea fluxes in the open ocean, and not for...
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2011
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ftncar:oai:drupal-site.org:articles_11633 2023-09-05T13:22:05+02:00 Coral reefs modify their seawater carbon chemistry - Implications for impacts of ocean acidification Anthony, Kenneth (author) Kleypas, Joanie (author) Gattuso, Jean-Pierre (author) 2011-12 http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-861 https://doi.org/10.1111/j.1365-2486.2011.02510.x en eng John Wiley & Sons Global Change Biology http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-861 doi:10.1111/j.1365-2486.2011.02510.x ark:/85065/d7sb46b6 Copyright 2011 John Wiley & Sons. Text article 2011 ftncar https://doi.org/10.1111/j.1365-2486.2011.02510.x 2023-08-14T18:39:47Z Reviews suggest that that the biogeochemical threshold for sustained coral reef growth will be reached during this century due to ocean acidification caused by increased uptake of atmospheric CO₂. Projections of ocean acidification, however, are based on air-sea fluxes in the open ocean, and not for shallow-water systems such as coral reefs. Like the open ocean, reef waters are subject to the chemical forcing of increasing atmospheric pCO₂. However, for reefs with long water residence times, we illustrate that benthic carbon fluxes can drive spatial variation in pH, pCO₂ and aragonite saturation state (Ωa) that can mask the effects of ocean acidification in some downstream habitats. We use a carbon flux model for photosynthesis, respiration, calcification and dissolution coupled with Lagrangian transport to examine how key groups of calcifiers (zooxanthellate corals) and primary producers (macroalgae) on coral reefs contribute to changes in the seawater carbonate system as a function of water residence time. Analyses based on flume data showed that the carbon fluxes of corals and macroalgae drive Ωain opposing directions. Areas dominated by corals elevate pCO₂ and reduce Ωa, thereby compounding ocean acidification effects in downstream habitats, whereas algal beds draw CO₂ down and elevate Ωa, potentially offsetting ocean acidification impacts at the local scale. Simulations for two CO₂ scenarios (600 and 900 ppm CO₂) suggested that a potential shift from coral to algal abundance under ocean acidification can lead to improved conditions for calcification in downstream habitats, depending on reef size, water residence time and circulation patterns. Although the carbon fluxes of benthic reef communities cannot significantly counter changes in carbon chemistry at the scale of oceans, they provide a significant mechanism of buffering ocean acidification impacts at the scale of habitat to reef. Article in Journal/Newspaper Ocean acidification OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Global Change Biology 17 12 3655 3666 |
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Open Polar |
collection |
OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) |
op_collection_id |
ftncar |
language |
English |
description |
Reviews suggest that that the biogeochemical threshold for sustained coral reef growth will be reached during this century due to ocean acidification caused by increased uptake of atmospheric CO₂. Projections of ocean acidification, however, are based on air-sea fluxes in the open ocean, and not for shallow-water systems such as coral reefs. Like the open ocean, reef waters are subject to the chemical forcing of increasing atmospheric pCO₂. However, for reefs with long water residence times, we illustrate that benthic carbon fluxes can drive spatial variation in pH, pCO₂ and aragonite saturation state (Ωa) that can mask the effects of ocean acidification in some downstream habitats. We use a carbon flux model for photosynthesis, respiration, calcification and dissolution coupled with Lagrangian transport to examine how key groups of calcifiers (zooxanthellate corals) and primary producers (macroalgae) on coral reefs contribute to changes in the seawater carbonate system as a function of water residence time. Analyses based on flume data showed that the carbon fluxes of corals and macroalgae drive Ωain opposing directions. Areas dominated by corals elevate pCO₂ and reduce Ωa, thereby compounding ocean acidification effects in downstream habitats, whereas algal beds draw CO₂ down and elevate Ωa, potentially offsetting ocean acidification impacts at the local scale. Simulations for two CO₂ scenarios (600 and 900 ppm CO₂) suggested that a potential shift from coral to algal abundance under ocean acidification can lead to improved conditions for calcification in downstream habitats, depending on reef size, water residence time and circulation patterns. Although the carbon fluxes of benthic reef communities cannot significantly counter changes in carbon chemistry at the scale of oceans, they provide a significant mechanism of buffering ocean acidification impacts at the scale of habitat to reef. |
author2 |
Anthony, Kenneth (author) Kleypas, Joanie (author) Gattuso, Jean-Pierre (author) |
format |
Article in Journal/Newspaper |
title |
Coral reefs modify their seawater carbon chemistry - Implications for impacts of ocean acidification |
spellingShingle |
Coral reefs modify their seawater carbon chemistry - Implications for impacts of ocean acidification |
title_short |
Coral reefs modify their seawater carbon chemistry - Implications for impacts of ocean acidification |
title_full |
Coral reefs modify their seawater carbon chemistry - Implications for impacts of ocean acidification |
title_fullStr |
Coral reefs modify their seawater carbon chemistry - Implications for impacts of ocean acidification |
title_full_unstemmed |
Coral reefs modify their seawater carbon chemistry - Implications for impacts of ocean acidification |
title_sort |
coral reefs modify their seawater carbon chemistry - implications for impacts of ocean acidification |
publisher |
John Wiley & Sons |
publishDate |
2011 |
url |
http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-861 https://doi.org/10.1111/j.1365-2486.2011.02510.x |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
Global Change Biology http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-861 doi:10.1111/j.1365-2486.2011.02510.x ark:/85065/d7sb46b6 |
op_rights |
Copyright 2011 John Wiley & Sons. |
op_doi |
https://doi.org/10.1111/j.1365-2486.2011.02510.x |
container_title |
Global Change Biology |
container_volume |
17 |
container_issue |
12 |
container_start_page |
3655 |
op_container_end_page |
3666 |
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1776202614271115264 |