Seawater carbonate chemistry and biological processes of Porites panamensis during experiments, 2011
Survival of coral planulae, and the successful settlement and healthy growth of primary polyps are critical for the dispersal of scleractinian corals and hence the recovery of degraded coral reefs. It is therefore important to explore how the warmer and more acidic oceanic conditions predicted for t...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.761769 2024-09-15T18:28:06+00:00 Seawater carbonate chemistry and biological processes of Porites panamensis during experiments, 2011 Anlauf, Holger D'Croz, Luis O'Dea, Aaron 2011 text/tab-separated-values, 1881 data points https://doi.pangaea.de/10.1594/PANGAEA.761769 https://doi.org/10.1594/PANGAEA.761769 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.761769 https://doi.org/10.1594/PANGAEA.761769 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Anlauf, Holger; D'Croz, Luis; O'Dea, Aaron (2011): A corrosive concoction: The combined effects of ocean warming and acidification on the early growth of a stony coral are multiplicative. Journal of Experimental Marine Biology and Ecology, 397(1), 13-20, https://doi.org/10.1016/j.jembe.2010.11.009 Alkalinity total Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cnidaria Coast and continental shelf Containers and aquaria (20-1000 L or < 1 m**2) EPOCA EUR-OCEANS European network of excellence for Ocean Ecosystems Analysis European Project on Ocean Acidification Experimental treatment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Identification Laboratory experiment Mortality/Survival North Pacific OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Porites panamensis dead mortality post settlement motile settled Reproduction Salinity Single species Temperature water Titration dataset 2011 ftpangaea https://doi.org/10.1594/PANGAEA.76176910.1016/j.jembe.2010.11.009 2024-07-24T02:31:31Z Survival of coral planulae, and the successful settlement and healthy growth of primary polyps are critical for the dispersal of scleractinian corals and hence the recovery of degraded coral reefs. It is therefore important to explore how the warmer and more acidic oceanic conditions predicted for the future could affect these processes. This study used controlled culture to investigate the effects of a 1 °C increase in temperature and a 0.2-0.25 unit decrease in pH on the settlement and survival of planulae and the growth of primary polyps in the Tropical Eastern Pacific coral Porites panamensis. We found that primary polyp growth was reduced only marginally by more acidic seawater but the combined effect of high temperature and lowered pH caused a significant reduction in growth of primary polyps by almost a third. Elevated temperature was found to significantly reduce the amount of zooxanthellae in primary polyps, and when combined with lowered pH resulted in a significant reduction in biomass of primary polyps. However, survival and settlement of planula larvae were unaffected by increased temperature, lowered acidity or the combination of both. These results indicate that in future scenarios of increased temperature and oceanic acidity coral planulae will be able to disperse and settle successfully but primary polyp growth may be hampered. The recovery of reefs may therefore be impeded by global change even if local stressors are curbed and sufficient sources of planulae are available. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Alkalinity total Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cnidaria Coast and continental shelf Containers and aquaria (20-1000 L or < 1 m**2) EPOCA EUR-OCEANS European network of excellence for Ocean Ecosystems Analysis European Project on Ocean Acidification Experimental treatment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Identification Laboratory experiment Mortality/Survival North Pacific OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Porites panamensis dead mortality post settlement motile settled Reproduction Salinity Single species Temperature water Titration |
spellingShingle |
Alkalinity total Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cnidaria Coast and continental shelf Containers and aquaria (20-1000 L or < 1 m**2) EPOCA EUR-OCEANS European network of excellence for Ocean Ecosystems Analysis European Project on Ocean Acidification Experimental treatment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Identification Laboratory experiment Mortality/Survival North Pacific OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Porites panamensis dead mortality post settlement motile settled Reproduction Salinity Single species Temperature water Titration Anlauf, Holger D'Croz, Luis O'Dea, Aaron Seawater carbonate chemistry and biological processes of Porites panamensis during experiments, 2011 |
topic_facet |
Alkalinity total Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cnidaria Coast and continental shelf Containers and aquaria (20-1000 L or < 1 m**2) EPOCA EUR-OCEANS European network of excellence for Ocean Ecosystems Analysis European Project on Ocean Acidification Experimental treatment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Identification Laboratory experiment Mortality/Survival North Pacific OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Porites panamensis dead mortality post settlement motile settled Reproduction Salinity Single species Temperature water Titration |
description |
Survival of coral planulae, and the successful settlement and healthy growth of primary polyps are critical for the dispersal of scleractinian corals and hence the recovery of degraded coral reefs. It is therefore important to explore how the warmer and more acidic oceanic conditions predicted for the future could affect these processes. This study used controlled culture to investigate the effects of a 1 °C increase in temperature and a 0.2-0.25 unit decrease in pH on the settlement and survival of planulae and the growth of primary polyps in the Tropical Eastern Pacific coral Porites panamensis. We found that primary polyp growth was reduced only marginally by more acidic seawater but the combined effect of high temperature and lowered pH caused a significant reduction in growth of primary polyps by almost a third. Elevated temperature was found to significantly reduce the amount of zooxanthellae in primary polyps, and when combined with lowered pH resulted in a significant reduction in biomass of primary polyps. However, survival and settlement of planula larvae were unaffected by increased temperature, lowered acidity or the combination of both. These results indicate that in future scenarios of increased temperature and oceanic acidity coral planulae will be able to disperse and settle successfully but primary polyp growth may be hampered. The recovery of reefs may therefore be impeded by global change even if local stressors are curbed and sufficient sources of planulae are available. |
format |
Dataset |
author |
Anlauf, Holger D'Croz, Luis O'Dea, Aaron |
author_facet |
Anlauf, Holger D'Croz, Luis O'Dea, Aaron |
author_sort |
Anlauf, Holger |
title |
Seawater carbonate chemistry and biological processes of Porites panamensis during experiments, 2011 |
title_short |
Seawater carbonate chemistry and biological processes of Porites panamensis during experiments, 2011 |
title_full |
Seawater carbonate chemistry and biological processes of Porites panamensis during experiments, 2011 |
title_fullStr |
Seawater carbonate chemistry and biological processes of Porites panamensis during experiments, 2011 |
title_full_unstemmed |
Seawater carbonate chemistry and biological processes of Porites panamensis during experiments, 2011 |
title_sort |
seawater carbonate chemistry and biological processes of porites panamensis during experiments, 2011 |
publisher |
PANGAEA |
publishDate |
2011 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.761769 https://doi.org/10.1594/PANGAEA.761769 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Supplement to: Anlauf, Holger; D'Croz, Luis; O'Dea, Aaron (2011): A corrosive concoction: The combined effects of ocean warming and acidification on the early growth of a stony coral are multiplicative. Journal of Experimental Marine Biology and Ecology, 397(1), 13-20, https://doi.org/10.1016/j.jembe.2010.11.009 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.761769 https://doi.org/10.1594/PANGAEA.761769 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.76176910.1016/j.jembe.2010.11.009 |
_version_ |
1810469420757155840 |