Seawater carbonate chemistry and processes during experiments with a coral community, 2008, supplement to: Anthony, Kenneth R N; Kline, David I; Diaz-Pulido, Guillermo; Dove, Sophie; Hoegh-Guldberg, Ove (2008): Ocean acidification causes bleaching and productivity loss in coral reef builders. Proceedings of the National Academy of Sciences of the United States of America, 105(45), 7442-7446

Ocean acidification represents a key threat to coral reefs by reducing the calcification rate of framework builders. In addition, acidification is likely to affect the relationship between corals and their symbiotic dinoflagellates and the productivity of this association. However, little is known a...

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Main Authors: Anthony, Kenneth R N, Kline, David I, Diaz-Pulido, Guillermo, Dove, Sophie, Hoegh-Guldberg, Ove
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2008
Subjects:
pH
Online Access:https://dx.doi.org/10.1594/pangaea.727744
https://doi.pangaea.de/10.1594/PANGAEA.727744
id ftdatacite:10.1594/pangaea.727744
record_format openpolar
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Acropora intermedia
Animalia
Benthic animals
Benthos
Calcification/Dissolution
Cnidaria
Coast and continental shelf
Containers and aquaria 20-1000 L or < 1 m**2
Laboratory experiment
Macroalgae
Other studied parameter or process
Plantae
Porites lobata
Porolithon onkodes
Primary production/Photosynthesis
Rhodophyta
Single species
South Pacific
Temperate
Temperature
Salinity
Temperature, water
Carbonate system computation flag
pH
Alkalinity, total
Carbon, inorganic, dissolved
Partial pressure of carbon dioxide water at sea surface temperature wet air
Bicarbonate ion
Carbonate ion
Aragonite saturation state
Carbon dioxide
Fugacity of carbon dioxide water at sea surface temperature wet air
Calcite saturation state
Bleaching
Net productivity of oxygen
Calcification rate
Experiment
Refractometer, Bellingham Stanley
Calculated using seacarb after Nisumaa et al. 2010
pH logger, MicroChem interface TPS Australia
Alkalinity, Gran titration Gran, 1950
Calculated using CO2SYS
Calculated, see references
Buoyant weighing technique Davies, 1989
European network of excellence for Ocean Ecosystems Analysis EUR-OCEANS
European Project on Ocean Acidification EPOCA
Ocean Acidification International Coordination Centre OA-ICC
spellingShingle Acropora intermedia
Animalia
Benthic animals
Benthos
Calcification/Dissolution
Cnidaria
Coast and continental shelf
Containers and aquaria 20-1000 L or < 1 m**2
Laboratory experiment
Macroalgae
Other studied parameter or process
Plantae
Porites lobata
Porolithon onkodes
Primary production/Photosynthesis
Rhodophyta
Single species
South Pacific
Temperate
Temperature
Salinity
Temperature, water
Carbonate system computation flag
pH
Alkalinity, total
Carbon, inorganic, dissolved
Partial pressure of carbon dioxide water at sea surface temperature wet air
Bicarbonate ion
Carbonate ion
Aragonite saturation state
Carbon dioxide
Fugacity of carbon dioxide water at sea surface temperature wet air
Calcite saturation state
Bleaching
Net productivity of oxygen
Calcification rate
Experiment
Refractometer, Bellingham Stanley
Calculated using seacarb after Nisumaa et al. 2010
pH logger, MicroChem interface TPS Australia
Alkalinity, Gran titration Gran, 1950
Calculated using CO2SYS
Calculated, see references
Buoyant weighing technique Davies, 1989
European network of excellence for Ocean Ecosystems Analysis EUR-OCEANS
European Project on Ocean Acidification EPOCA
Ocean Acidification International Coordination Centre OA-ICC
Anthony, Kenneth R N
Kline, David I
Diaz-Pulido, Guillermo
Dove, Sophie
Hoegh-Guldberg, Ove
Seawater carbonate chemistry and processes during experiments with a coral community, 2008, supplement to: Anthony, Kenneth R N; Kline, David I; Diaz-Pulido, Guillermo; Dove, Sophie; Hoegh-Guldberg, Ove (2008): Ocean acidification causes bleaching and productivity loss in coral reef builders. Proceedings of the National Academy of Sciences of the United States of America, 105(45), 7442-7446
topic_facet Acropora intermedia
Animalia
Benthic animals
Benthos
Calcification/Dissolution
Cnidaria
Coast and continental shelf
Containers and aquaria 20-1000 L or < 1 m**2
Laboratory experiment
Macroalgae
Other studied parameter or process
Plantae
Porites lobata
Porolithon onkodes
Primary production/Photosynthesis
Rhodophyta
Single species
South Pacific
Temperate
Temperature
Salinity
Temperature, water
Carbonate system computation flag
pH
Alkalinity, total
Carbon, inorganic, dissolved
Partial pressure of carbon dioxide water at sea surface temperature wet air
Bicarbonate ion
Carbonate ion
Aragonite saturation state
Carbon dioxide
Fugacity of carbon dioxide water at sea surface temperature wet air
Calcite saturation state
Bleaching
Net productivity of oxygen
Calcification rate
Experiment
Refractometer, Bellingham Stanley
Calculated using seacarb after Nisumaa et al. 2010
pH logger, MicroChem interface TPS Australia
Alkalinity, Gran titration Gran, 1950
Calculated using CO2SYS
Calculated, see references
Buoyant weighing technique Davies, 1989
European network of excellence for Ocean Ecosystems Analysis EUR-OCEANS
European Project on Ocean Acidification EPOCA
Ocean Acidification International Coordination Centre OA-ICC
description Ocean acidification represents a key threat to coral reefs by reducing the calcification rate of framework builders. In addition, acidification is likely to affect the relationship between corals and their symbiotic dinoflagellates and the productivity of this association. However, little is known about how acidification impacts on the physiology of reef builders and how acidification interacts with warming. Here, we report on an 8-week study that compared bleaching, productivity, and calcification responses of crustose coralline algae (CCA) and branching (Acropora) and massive (Porites) coral species in response to acidification and warming. Using a 30-tank experimental system, we manipulated CO2 levels to simulate doubling and three- to fourfold increases [Intergovernmental Panel on Climate Change (IPCC) projection categories IV and VI] relative to present-day levels under cool and warm scenarios. Results indicated that high CO2 is a bleaching agent for corals and CCA under high irradiance, acting synergistically with warming to lower thermal bleaching thresholds. We propose that CO2 induces bleaching via its impact on photoprotective mechanisms of the photosystems. Overall, acidification impacted more strongly on bleaching and productivity than on calcification. Interestingly, the intermediate, warm CO2 scenario led to a 30% increase in productivity in Acropora, whereas high CO2 lead to zero productivity in both corals. CCA were most sensitive to acidification, with high CO2 leading to negative productivity and high rates of net dissolution. Our findings suggest that sensitive reef-building species such as CCA may be pushed beyond their thresholds for growth and survival within the next few decades whereas corals will show delayed and mixed responses. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) 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).
format Dataset
author Anthony, Kenneth R N
Kline, David I
Diaz-Pulido, Guillermo
Dove, Sophie
Hoegh-Guldberg, Ove
author_facet Anthony, Kenneth R N
Kline, David I
Diaz-Pulido, Guillermo
Dove, Sophie
Hoegh-Guldberg, Ove
author_sort Anthony, Kenneth R N
title Seawater carbonate chemistry and processes during experiments with a coral community, 2008, supplement to: Anthony, Kenneth R N; Kline, David I; Diaz-Pulido, Guillermo; Dove, Sophie; Hoegh-Guldberg, Ove (2008): Ocean acidification causes bleaching and productivity loss in coral reef builders. Proceedings of the National Academy of Sciences of the United States of America, 105(45), 7442-7446
title_short Seawater carbonate chemistry and processes during experiments with a coral community, 2008, supplement to: Anthony, Kenneth R N; Kline, David I; Diaz-Pulido, Guillermo; Dove, Sophie; Hoegh-Guldberg, Ove (2008): Ocean acidification causes bleaching and productivity loss in coral reef builders. Proceedings of the National Academy of Sciences of the United States of America, 105(45), 7442-7446
title_full Seawater carbonate chemistry and processes during experiments with a coral community, 2008, supplement to: Anthony, Kenneth R N; Kline, David I; Diaz-Pulido, Guillermo; Dove, Sophie; Hoegh-Guldberg, Ove (2008): Ocean acidification causes bleaching and productivity loss in coral reef builders. Proceedings of the National Academy of Sciences of the United States of America, 105(45), 7442-7446
title_fullStr Seawater carbonate chemistry and processes during experiments with a coral community, 2008, supplement to: Anthony, Kenneth R N; Kline, David I; Diaz-Pulido, Guillermo; Dove, Sophie; Hoegh-Guldberg, Ove (2008): Ocean acidification causes bleaching and productivity loss in coral reef builders. Proceedings of the National Academy of Sciences of the United States of America, 105(45), 7442-7446
title_full_unstemmed Seawater carbonate chemistry and processes during experiments with a coral community, 2008, supplement to: Anthony, Kenneth R N; Kline, David I; Diaz-Pulido, Guillermo; Dove, Sophie; Hoegh-Guldberg, Ove (2008): Ocean acidification causes bleaching and productivity loss in coral reef builders. Proceedings of the National Academy of Sciences of the United States of America, 105(45), 7442-7446
title_sort seawater carbonate chemistry and processes during experiments with a coral community, 2008, supplement to: anthony, kenneth r n; kline, david i; diaz-pulido, guillermo; dove, sophie; hoegh-guldberg, ove (2008): ocean acidification causes bleaching and productivity loss in coral reef builders. proceedings of the national academy of sciences of the united states of america, 105(45), 7442-7446
publisher PANGAEA - Data Publisher for Earth & Environmental Science
publishDate 2008
url https://dx.doi.org/10.1594/pangaea.727744
https://doi.pangaea.de/10.1594/PANGAEA.727744
long_lat ENVELOPE(-60.667,-60.667,-63.783,-63.783)
ENVELOPE(-62.777,-62.777,-64.830,-64.830)
geographic Diaz
Hoegh
Pacific
geographic_facet Diaz
Hoegh
Pacific
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://dx.doi.org/10.1073/pnas.0804478105
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.727744
https://doi.org/10.1073/pnas.0804478105
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spelling ftdatacite:10.1594/pangaea.727744 2023-05-15T17:50:15+02:00 Seawater carbonate chemistry and processes during experiments with a coral community, 2008, supplement to: Anthony, Kenneth R N; Kline, David I; Diaz-Pulido, Guillermo; Dove, Sophie; Hoegh-Guldberg, Ove (2008): Ocean acidification causes bleaching and productivity loss in coral reef builders. Proceedings of the National Academy of Sciences of the United States of America, 105(45), 7442-7446 Anthony, Kenneth R N Kline, David I Diaz-Pulido, Guillermo Dove, Sophie Hoegh-Guldberg, Ove 2008 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.727744 https://doi.pangaea.de/10.1594/PANGAEA.727744 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://dx.doi.org/10.1073/pnas.0804478105 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Acropora intermedia Animalia Benthic animals Benthos Calcification/Dissolution Cnidaria Coast and continental shelf Containers and aquaria 20-1000 L or < 1 m**2 Laboratory experiment Macroalgae Other studied parameter or process Plantae Porites lobata Porolithon onkodes Primary production/Photosynthesis Rhodophyta Single species South Pacific Temperate Temperature Salinity Temperature, water Carbonate system computation flag pH Alkalinity, total Carbon, inorganic, dissolved Partial pressure of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Aragonite saturation state Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Calcite saturation state Bleaching Net productivity of oxygen Calcification rate Experiment Refractometer, Bellingham Stanley Calculated using seacarb after Nisumaa et al. 2010 pH logger, MicroChem interface TPS Australia Alkalinity, Gran titration Gran, 1950 Calculated using CO2SYS Calculated, see references Buoyant weighing technique Davies, 1989 European network of excellence for Ocean Ecosystems Analysis EUR-OCEANS European Project on Ocean Acidification EPOCA Ocean Acidification International Coordination Centre OA-ICC Dataset dataset Supplementary Dataset 2008 ftdatacite https://doi.org/10.1594/pangaea.727744 https://doi.org/10.1073/pnas.0804478105 2022-02-09T12:06:21Z Ocean acidification represents a key threat to coral reefs by reducing the calcification rate of framework builders. In addition, acidification is likely to affect the relationship between corals and their symbiotic dinoflagellates and the productivity of this association. However, little is known about how acidification impacts on the physiology of reef builders and how acidification interacts with warming. Here, we report on an 8-week study that compared bleaching, productivity, and calcification responses of crustose coralline algae (CCA) and branching (Acropora) and massive (Porites) coral species in response to acidification and warming. Using a 30-tank experimental system, we manipulated CO2 levels to simulate doubling and three- to fourfold increases [Intergovernmental Panel on Climate Change (IPCC) projection categories IV and VI] relative to present-day levels under cool and warm scenarios. Results indicated that high CO2 is a bleaching agent for corals and CCA under high irradiance, acting synergistically with warming to lower thermal bleaching thresholds. We propose that CO2 induces bleaching via its impact on photoprotective mechanisms of the photosystems. Overall, acidification impacted more strongly on bleaching and productivity than on calcification. Interestingly, the intermediate, warm CO2 scenario led to a 30% increase in productivity in Acropora, whereas high CO2 lead to zero productivity in both corals. CCA were most sensitive to acidification, with high CO2 leading to negative productivity and high rates of net dissolution. Our findings suggest that sensitive reef-building species such as CCA may be pushed beyond their thresholds for growth and survival within the next few decades whereas corals will show delayed and mixed responses. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) 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). Dataset Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) Diaz ENVELOPE(-60.667,-60.667,-63.783,-63.783) Hoegh ENVELOPE(-62.777,-62.777,-64.830,-64.830) Pacific