Seawater carbonate chemistry and live coral performance vs. framework dissolution and bioerosion ...
Physiological sensitivity of cold-water corals to ocean change is far less understood than of tropical corals and very little is known about the impacts of ocean acidification and warming on degradative processes of dead coral framework. In a 13-month laboratory experiment, we examined the interacti...
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Online Access: | https://dx.doi.org/10.1594/pangaea.952909 https://doi.pangaea.de/10.1594/PANGAEA.952909 |
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ftdatacite:10.1594/pangaea.952909 2024-04-28T08:27:58+00:00 Seawater carbonate chemistry and live coral performance vs. framework dissolution and bioerosion ... Büscher, Janina Form, Armin Wisshak, Max Kiko, Rainer Riebesell, Ulf 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.952909 https://doi.pangaea.de/10.1594/PANGAEA.952909 en eng PANGAEA https://cran.r-project.org/web/packages/seacarb/index.html https://dx.doi.org/10.1002/lno.12217 https://dx.doi.org/10.1594/pangaea.947285 https://cran.r-project.org/web/packages/seacarb/index.html Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Animalia Benthic animals Benthos Calcification/Dissolution Cnidaria Coast and continental shelf Containers and aquaria 20-1000 L or < 1 m**2 Growth/Morphology Laboratory experiment Lophelia pertusa Mortality/Survival North Atlantic Respiration Single species Temperate Temperature Type Species, unique identification Species, unique identification URI Species, unique identification Semantic URI Morphotype Interval Treatment Group Replicate Experimental treatment Temperature, water Salinity Alkalinity, total Carbon, inorganic, dissolved Partial pressure of carbon dioxide water at sea surface temperature wet air Dissolution rate Respiration rate, oxygen Mortality Dry mass Ash free dry mass Coral polyp Carbonate system computation flag pH Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Aragonite saturation state Calcite saturation state Submersible JAGO Calculated using seacarb after Nisumaa et al. 2010 POS455 Poseidon dataset Dataset 2022 ftdatacite https://doi.org/10.1594/pangaea.95290910.1002/lno.1221710.1594/pangaea.947285 2024-04-02T11:36:31Z Physiological sensitivity of cold-water corals to ocean change is far less understood than of tropical corals and very little is known about the impacts of ocean acidification and warming on degradative processes of dead coral framework. In a 13-month laboratory experiment, we examined the interactive effects of gradually increasing temperature and pCO2 levels on survival, growth, and respiration of two prominent color morphotypes (colormorphs) of the framework-forming cold-water coral Lophelia pertusa, as well as bioerosion and dissolution of dead framework. Calcification rates tended to increase with warming, showing temperature optima at ~ 14°C (white colormorph) and 10–12°C (orange colormorph) and decreased with increasing pCO2. Net dissolution occurred at aragonite undersaturation (ΩAr < 1) at ~ 1000 μatm pCO2. Under combined warming and acidification, the negative effects of acidification on growth were initially mitigated, but at ~ 1600 μatm dissolution prevailed. Respiration rates increased with ... : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2021) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2022-12-21. ... Dataset Lophelia pertusa North Atlantic Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Animalia Benthic animals Benthos Calcification/Dissolution Cnidaria Coast and continental shelf Containers and aquaria 20-1000 L or < 1 m**2 Growth/Morphology Laboratory experiment Lophelia pertusa Mortality/Survival North Atlantic Respiration Single species Temperate Temperature Type Species, unique identification Species, unique identification URI Species, unique identification Semantic URI Morphotype Interval Treatment Group Replicate Experimental treatment Temperature, water Salinity Alkalinity, total Carbon, inorganic, dissolved Partial pressure of carbon dioxide water at sea surface temperature wet air Dissolution rate Respiration rate, oxygen Mortality Dry mass Ash free dry mass Coral polyp Carbonate system computation flag pH Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Aragonite saturation state Calcite saturation state Submersible JAGO Calculated using seacarb after Nisumaa et al. 2010 POS455 Poseidon |
spellingShingle |
Animalia Benthic animals Benthos Calcification/Dissolution Cnidaria Coast and continental shelf Containers and aquaria 20-1000 L or < 1 m**2 Growth/Morphology Laboratory experiment Lophelia pertusa Mortality/Survival North Atlantic Respiration Single species Temperate Temperature Type Species, unique identification Species, unique identification URI Species, unique identification Semantic URI Morphotype Interval Treatment Group Replicate Experimental treatment Temperature, water Salinity Alkalinity, total Carbon, inorganic, dissolved Partial pressure of carbon dioxide water at sea surface temperature wet air Dissolution rate Respiration rate, oxygen Mortality Dry mass Ash free dry mass Coral polyp Carbonate system computation flag pH Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Aragonite saturation state Calcite saturation state Submersible JAGO Calculated using seacarb after Nisumaa et al. 2010 POS455 Poseidon Büscher, Janina Form, Armin Wisshak, Max Kiko, Rainer Riebesell, Ulf Seawater carbonate chemistry and live coral performance vs. framework dissolution and bioerosion ... |
topic_facet |
Animalia Benthic animals Benthos Calcification/Dissolution Cnidaria Coast and continental shelf Containers and aquaria 20-1000 L or < 1 m**2 Growth/Morphology Laboratory experiment Lophelia pertusa Mortality/Survival North Atlantic Respiration Single species Temperate Temperature Type Species, unique identification Species, unique identification URI Species, unique identification Semantic URI Morphotype Interval Treatment Group Replicate Experimental treatment Temperature, water Salinity Alkalinity, total Carbon, inorganic, dissolved Partial pressure of carbon dioxide water at sea surface temperature wet air Dissolution rate Respiration rate, oxygen Mortality Dry mass Ash free dry mass Coral polyp Carbonate system computation flag pH Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Aragonite saturation state Calcite saturation state Submersible JAGO Calculated using seacarb after Nisumaa et al. 2010 POS455 Poseidon |
description |
Physiological sensitivity of cold-water corals to ocean change is far less understood than of tropical corals and very little is known about the impacts of ocean acidification and warming on degradative processes of dead coral framework. In a 13-month laboratory experiment, we examined the interactive effects of gradually increasing temperature and pCO2 levels on survival, growth, and respiration of two prominent color morphotypes (colormorphs) of the framework-forming cold-water coral Lophelia pertusa, as well as bioerosion and dissolution of dead framework. Calcification rates tended to increase with warming, showing temperature optima at ~ 14°C (white colormorph) and 10–12°C (orange colormorph) and decreased with increasing pCO2. Net dissolution occurred at aragonite undersaturation (ΩAr < 1) at ~ 1000 μatm pCO2. Under combined warming and acidification, the negative effects of acidification on growth were initially mitigated, but at ~ 1600 μatm dissolution prevailed. Respiration rates increased with ... : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2021) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2022-12-21. ... |
format |
Dataset |
author |
Büscher, Janina Form, Armin Wisshak, Max Kiko, Rainer Riebesell, Ulf |
author_facet |
Büscher, Janina Form, Armin Wisshak, Max Kiko, Rainer Riebesell, Ulf |
author_sort |
Büscher, Janina |
title |
Seawater carbonate chemistry and live coral performance vs. framework dissolution and bioerosion ... |
title_short |
Seawater carbonate chemistry and live coral performance vs. framework dissolution and bioerosion ... |
title_full |
Seawater carbonate chemistry and live coral performance vs. framework dissolution and bioerosion ... |
title_fullStr |
Seawater carbonate chemistry and live coral performance vs. framework dissolution and bioerosion ... |
title_full_unstemmed |
Seawater carbonate chemistry and live coral performance vs. framework dissolution and bioerosion ... |
title_sort |
seawater carbonate chemistry and live coral performance vs. framework dissolution and bioerosion ... |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://dx.doi.org/10.1594/pangaea.952909 https://doi.pangaea.de/10.1594/PANGAEA.952909 |
genre |
Lophelia pertusa North Atlantic Ocean acidification |
genre_facet |
Lophelia pertusa North Atlantic Ocean acidification |
op_relation |
https://cran.r-project.org/web/packages/seacarb/index.html https://dx.doi.org/10.1002/lno.12217 https://dx.doi.org/10.1594/pangaea.947285 https://cran.r-project.org/web/packages/seacarb/index.html |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.95290910.1002/lno.1221710.1594/pangaea.947285 |
_version_ |
1797586676056326144 |