Galápagos coral reef persistence after ENSO warming across an acidification gradient, supplement to: Manzello, Derek P; Enochs, I C; Bruckner, Andrew; Renaud, Philip G; Kolodziej, Graham; Budd, David A; Carlton, R; Glynn, Peter W (2014): Galápagos coral reef persistence after ENSO warming across an acidification gradient. Geophysical Research Letters, 41(24), 9001-9008
Anthropogenic CO2 is causing warming and ocean acidification. Coral reefs are being severely impacted, yet confusion lingers regarding how reefs will respond to these stressors over this century. Since the 1982-1983 El Niño-Southern Oscillation warming event, the persistence of reefs around the Galá...
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PANGAEA - Data Publisher for Earth & Environmental Science
2014
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Online Access: | https://dx.doi.org/10.1594/pangaea.847762 https://doi.pangaea.de/10.1594/PANGAEA.847762 |
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ftdatacite:10.1594/pangaea.847762 2023-05-15T17:50:36+02:00 Galápagos coral reef persistence after ENSO warming across an acidification gradient, supplement to: Manzello, Derek P; Enochs, I C; Bruckner, Andrew; Renaud, Philip G; Kolodziej, Graham; Budd, David A; Carlton, R; Glynn, Peter W (2014): Galápagos coral reef persistence after ENSO warming across an acidification gradient. Geophysical Research Letters, 41(24), 9001-9008 Manzello, Derek P Enochs, I C Bruckner, Andrew Renaud, Philip G Kolodziej, Graham Budd, David A Carlton, R Glynn, Peter W 2014 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.847762 https://doi.pangaea.de/10.1594/PANGAEA.847762 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://cran.r-project.org/package=seacarb https://dx.doi.org/10.1002/2014gl062501 https://cran.r-project.org/package=seacarb Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Benthos Biomass/Abundance/Elemental composition Calcification/Dissolution Coast and continental shelf Entire community Field observation Growth/Morphology Rocky-shore community South Pacific Temperature Tropical Table Site Replicates Date/time start Date/time end DEPTH, water Depth, water, standard error Extension rate Extension rate, standard error Density Density, standard error Calcification rate Calcification rate, standard error Phosphorus/Calcium ratio Phosphorus/Calcium ratio, standard error Temperature, water Salinity Alkalinity, total Carbon, inorganic, dissolved Partial pressure of carbon dioxide water at sea surface temperature wet air pH Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Aragonite saturation state Calcite saturation state Potentiometric titration Coulometric titration Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC Supplementary Dataset dataset Dataset 2014 ftdatacite https://doi.org/10.1594/pangaea.847762 https://doi.org/10.1002/2014gl062501 2021-11-05T12:55:41Z Anthropogenic CO2 is causing warming and ocean acidification. Coral reefs are being severely impacted, yet confusion lingers regarding how reefs will respond to these stressors over this century. Since the 1982-1983 El Niño-Southern Oscillation warming event, the persistence of reefs around the Galápagos Islands has differed across an acidification gradient. Reefs disappeared where pH<8.0 and aragonite saturation state (Omega arag)<=3 and have not recovered, whereas one reef has persisted where pH>8.0 and Omega arag>3. Where upwelling is greatest, calcification by massive Porites is higher than predicted by a published relationship with temperature despite high CO2, possibly due to elevated nutrients. However, skeletal P/Ca, a proxy for phosphate exposure, negatively correlates with density (R=-0.822, p<0.0001). We propose that elevated nutrients have the potential to exacerbate acidification by depressing coral skeletal densities and further increasing bioerosion already accelerated by low pH. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2015) 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 is 2015-07-03. Dataset Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) Pacific Renaud ENVELOPE(-67.950,-67.950,-65.700,-65.700) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Benthos Biomass/Abundance/Elemental composition Calcification/Dissolution Coast and continental shelf Entire community Field observation Growth/Morphology Rocky-shore community South Pacific Temperature Tropical Table Site Replicates Date/time start Date/time end DEPTH, water Depth, water, standard error Extension rate Extension rate, standard error Density Density, standard error Calcification rate Calcification rate, standard error Phosphorus/Calcium ratio Phosphorus/Calcium ratio, standard error Temperature, water Salinity Alkalinity, total Carbon, inorganic, dissolved Partial pressure of carbon dioxide water at sea surface temperature wet air pH Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Aragonite saturation state Calcite saturation state Potentiometric titration Coulometric titration Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC |
spellingShingle |
Benthos Biomass/Abundance/Elemental composition Calcification/Dissolution Coast and continental shelf Entire community Field observation Growth/Morphology Rocky-shore community South Pacific Temperature Tropical Table Site Replicates Date/time start Date/time end DEPTH, water Depth, water, standard error Extension rate Extension rate, standard error Density Density, standard error Calcification rate Calcification rate, standard error Phosphorus/Calcium ratio Phosphorus/Calcium ratio, standard error Temperature, water Salinity Alkalinity, total Carbon, inorganic, dissolved Partial pressure of carbon dioxide water at sea surface temperature wet air pH Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Aragonite saturation state Calcite saturation state Potentiometric titration Coulometric titration Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC Manzello, Derek P Enochs, I C Bruckner, Andrew Renaud, Philip G Kolodziej, Graham Budd, David A Carlton, R Glynn, Peter W Galápagos coral reef persistence after ENSO warming across an acidification gradient, supplement to: Manzello, Derek P; Enochs, I C; Bruckner, Andrew; Renaud, Philip G; Kolodziej, Graham; Budd, David A; Carlton, R; Glynn, Peter W (2014): Galápagos coral reef persistence after ENSO warming across an acidification gradient. Geophysical Research Letters, 41(24), 9001-9008 |
topic_facet |
Benthos Biomass/Abundance/Elemental composition Calcification/Dissolution Coast and continental shelf Entire community Field observation Growth/Morphology Rocky-shore community South Pacific Temperature Tropical Table Site Replicates Date/time start Date/time end DEPTH, water Depth, water, standard error Extension rate Extension rate, standard error Density Density, standard error Calcification rate Calcification rate, standard error Phosphorus/Calcium ratio Phosphorus/Calcium ratio, standard error Temperature, water Salinity Alkalinity, total Carbon, inorganic, dissolved Partial pressure of carbon dioxide water at sea surface temperature wet air pH Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Aragonite saturation state Calcite saturation state Potentiometric titration Coulometric titration Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC |
description |
Anthropogenic CO2 is causing warming and ocean acidification. Coral reefs are being severely impacted, yet confusion lingers regarding how reefs will respond to these stressors over this century. Since the 1982-1983 El Niño-Southern Oscillation warming event, the persistence of reefs around the Galápagos Islands has differed across an acidification gradient. Reefs disappeared where pH<8.0 and aragonite saturation state (Omega arag)<=3 and have not recovered, whereas one reef has persisted where pH>8.0 and Omega arag>3. Where upwelling is greatest, calcification by massive Porites is higher than predicted by a published relationship with temperature despite high CO2, possibly due to elevated nutrients. However, skeletal P/Ca, a proxy for phosphate exposure, negatively correlates with density (R=-0.822, p<0.0001). We propose that elevated nutrients have the potential to exacerbate acidification by depressing coral skeletal densities and further increasing bioerosion already accelerated by low pH. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2015) 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 is 2015-07-03. |
format |
Dataset |
author |
Manzello, Derek P Enochs, I C Bruckner, Andrew Renaud, Philip G Kolodziej, Graham Budd, David A Carlton, R Glynn, Peter W |
author_facet |
Manzello, Derek P Enochs, I C Bruckner, Andrew Renaud, Philip G Kolodziej, Graham Budd, David A Carlton, R Glynn, Peter W |
author_sort |
Manzello, Derek P |
title |
Galápagos coral reef persistence after ENSO warming across an acidification gradient, supplement to: Manzello, Derek P; Enochs, I C; Bruckner, Andrew; Renaud, Philip G; Kolodziej, Graham; Budd, David A; Carlton, R; Glynn, Peter W (2014): Galápagos coral reef persistence after ENSO warming across an acidification gradient. Geophysical Research Letters, 41(24), 9001-9008 |
title_short |
Galápagos coral reef persistence after ENSO warming across an acidification gradient, supplement to: Manzello, Derek P; Enochs, I C; Bruckner, Andrew; Renaud, Philip G; Kolodziej, Graham; Budd, David A; Carlton, R; Glynn, Peter W (2014): Galápagos coral reef persistence after ENSO warming across an acidification gradient. Geophysical Research Letters, 41(24), 9001-9008 |
title_full |
Galápagos coral reef persistence after ENSO warming across an acidification gradient, supplement to: Manzello, Derek P; Enochs, I C; Bruckner, Andrew; Renaud, Philip G; Kolodziej, Graham; Budd, David A; Carlton, R; Glynn, Peter W (2014): Galápagos coral reef persistence after ENSO warming across an acidification gradient. Geophysical Research Letters, 41(24), 9001-9008 |
title_fullStr |
Galápagos coral reef persistence after ENSO warming across an acidification gradient, supplement to: Manzello, Derek P; Enochs, I C; Bruckner, Andrew; Renaud, Philip G; Kolodziej, Graham; Budd, David A; Carlton, R; Glynn, Peter W (2014): Galápagos coral reef persistence after ENSO warming across an acidification gradient. Geophysical Research Letters, 41(24), 9001-9008 |
title_full_unstemmed |
Galápagos coral reef persistence after ENSO warming across an acidification gradient, supplement to: Manzello, Derek P; Enochs, I C; Bruckner, Andrew; Renaud, Philip G; Kolodziej, Graham; Budd, David A; Carlton, R; Glynn, Peter W (2014): Galápagos coral reef persistence after ENSO warming across an acidification gradient. Geophysical Research Letters, 41(24), 9001-9008 |
title_sort |
galápagos coral reef persistence after enso warming across an acidification gradient, supplement to: manzello, derek p; enochs, i c; bruckner, andrew; renaud, philip g; kolodziej, graham; budd, david a; carlton, r; glynn, peter w (2014): galápagos coral reef persistence after enso warming across an acidification gradient. geophysical research letters, 41(24), 9001-9008 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2014 |
url |
https://dx.doi.org/10.1594/pangaea.847762 https://doi.pangaea.de/10.1594/PANGAEA.847762 |
long_lat |
ENVELOPE(-67.950,-67.950,-65.700,-65.700) |
geographic |
Pacific Renaud |
geographic_facet |
Pacific Renaud |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
https://cran.r-project.org/package=seacarb https://dx.doi.org/10.1002/2014gl062501 https://cran.r-project.org/package=seacarb |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.847762 https://doi.org/10.1002/2014gl062501 |
_version_ |
1766157441924333568 |