Annual response of two Mediterranean azooxanthellate temperate corals to low-pH and high-temperature conditions

Ocean acidification (OA) and warming related to the anthropogenic increase in atmospheric CO2 have been shown to have detrimental effects on several marine organisms, especially those with calcium carbonate structures such as corals. In this study, we evaluate the response of two Mediterranean shall...

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Bibliographic Details
Main Authors: Movilla, Juancho, Calvo, Eva, Coma, Rafel, Serrano, Eduard, Lopez-Sanz, Angel, Pelejero, Carles
Format: Dataset
Language:English
Published: PANGAEA 2016
Subjects:
EXP
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.861963
https://doi.org/10.1594/PANGAEA.861963
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.861963
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Alkalinity
total
standard error
Animalia
Aragonite saturation state
Astroides calycularis
Benthic animals
Benthos
Bicarbonate ion
Biomass/Abundance/Elemental composition
Bottles or small containers/Aquaria (<20 L)
Calcification/Dissolution
Calcification rate of calcium carbonate
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Cartagena_OA
Cnidaria
Coast and continental shelf
Density
Event label
EXP
Experiment
Figure
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Identification
L_Estartit
Laboratory experiment
Leptopsammia pruvoti
Lipids
Mediterranean Sea
OA-ICC
Ocean Acidification International Coordination Centre
Organic matter
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
pH
Porosity
Potentiometric
Potentiometric titration
Proteins
spellingShingle Alkalinity
total
standard error
Animalia
Aragonite saturation state
Astroides calycularis
Benthic animals
Benthos
Bicarbonate ion
Biomass/Abundance/Elemental composition
Bottles or small containers/Aquaria (<20 L)
Calcification/Dissolution
Calcification rate of calcium carbonate
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Cartagena_OA
Cnidaria
Coast and continental shelf
Density
Event label
EXP
Experiment
Figure
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Identification
L_Estartit
Laboratory experiment
Leptopsammia pruvoti
Lipids
Mediterranean Sea
OA-ICC
Ocean Acidification International Coordination Centre
Organic matter
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
pH
Porosity
Potentiometric
Potentiometric titration
Proteins
Movilla, Juancho
Calvo, Eva
Coma, Rafel
Serrano, Eduard
Lopez-Sanz, Angel
Pelejero, Carles
Annual response of two Mediterranean azooxanthellate temperate corals to low-pH and high-temperature conditions
topic_facet Alkalinity
total
standard error
Animalia
Aragonite saturation state
Astroides calycularis
Benthic animals
Benthos
Bicarbonate ion
Biomass/Abundance/Elemental composition
Bottles or small containers/Aquaria (<20 L)
Calcification/Dissolution
Calcification rate of calcium carbonate
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Cartagena_OA
Cnidaria
Coast and continental shelf
Density
Event label
EXP
Experiment
Figure
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Identification
L_Estartit
Laboratory experiment
Leptopsammia pruvoti
Lipids
Mediterranean Sea
OA-ICC
Ocean Acidification International Coordination Centre
Organic matter
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
pH
Porosity
Potentiometric
Potentiometric titration
Proteins
description Ocean acidification (OA) and warming related to the anthropogenic increase in atmospheric CO2 have been shown to have detrimental effects on several marine organisms, especially those with calcium carbonate structures such as corals. In this study, we evaluate the response of two Mediterranean shallow-water azooxanthellate corals to the projected pH and seawater temperature (ST) scenarios for the end of this century. The colonial coral Astroides calycularis and the solitary Leptopsammia pruvoti were grown in aquaria over a year under two fixed pH conditions, control (8.05 pHT units) and low (7.72 pHT units), and simulating two annual ST cycles, natural and high (+3 °C). The organic matter (OM), lipid and protein content of the tissue and the skeletal microdensity of A. calycularis were not affected by the stress conditions (low pH, high ST), but the species exhibited a mean 25 % decrease in calcification rate at high-ST conditions at the end of the warm period and a mean 10 % increase in skeletal porosity under the acidified treatment after a full year cycle. Conversely, an absence of effects on calcification and skeletal microdensity of L. pruvoti exposed to low-pH and high-ST treatments contrasted with a significant decrease in the OM, lipid and protein content of the tissue at high-ST conditions and a 13 % mean increase in the skeletal porosity under low-pH conditions following a full year of exposure. This species-specific response suggests that different internal self-regulation strategies for energy reallocation may allow certain shallow-water azooxanthellate corals to cope more successfully than others with global environmental changes.
format Dataset
author Movilla, Juancho
Calvo, Eva
Coma, Rafel
Serrano, Eduard
Lopez-Sanz, Angel
Pelejero, Carles
author_facet Movilla, Juancho
Calvo, Eva
Coma, Rafel
Serrano, Eduard
Lopez-Sanz, Angel
Pelejero, Carles
author_sort Movilla, Juancho
title Annual response of two Mediterranean azooxanthellate temperate corals to low-pH and high-temperature conditions
title_short Annual response of two Mediterranean azooxanthellate temperate corals to low-pH and high-temperature conditions
title_full Annual response of two Mediterranean azooxanthellate temperate corals to low-pH and high-temperature conditions
title_fullStr Annual response of two Mediterranean azooxanthellate temperate corals to low-pH and high-temperature conditions
title_full_unstemmed Annual response of two Mediterranean azooxanthellate temperate corals to low-pH and high-temperature conditions
title_sort annual response of two mediterranean azooxanthellate temperate corals to low-ph and high-temperature conditions
publisher PANGAEA
publishDate 2016
url https://doi.pangaea.de/10.1594/PANGAEA.861963
https://doi.org/10.1594/PANGAEA.861963
op_coverage MEDIAN LATITUDE: 39.800000 * MEDIAN LONGITUDE: 1.125000 * SOUTH-BOUND LATITUDE: 37.550000 * WEST-BOUND LONGITUDE: -0.966670 * NORTH-BOUND LATITUDE: 42.050000 * EAST-BOUND LONGITUDE: 3.216670 * DATE/TIME START: 2011-01-01T00:00:00 * DATE/TIME END: 2011-01-31T00:00:00
long_lat ENVELOPE(-0.966670,3.216670,42.050000,37.550000)
genre Ocean acidification
genre_facet Ocean acidification
op_source Supplement to: Movilla, Juancho; Calvo, Eva; Coma, Rafel; Serrano, Eduard; Lopez-Sanz, Angel; Pelejero, Carles (2016): Annual response of two Mediterranean azooxanthellate temperate corals to low-pH and high-temperature conditions. Marine Biology, 163(6), https://doi.org/10.1007/s00227-016-2908-9
op_relation Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse (2015): seacarb: seawater carbonate chemistry with R. R package version 3.0.8. https://cran.r-project.org/package=seacarb
https://doi.pangaea.de/10.1594/PANGAEA.861963
https://doi.org/10.1594/PANGAEA.861963
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.861963
https://doi.org/10.1007/s00227-016-2908-9
_version_ 1766158376017854464
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.861963 2023-05-15T17:51:16+02:00 Annual response of two Mediterranean azooxanthellate temperate corals to low-pH and high-temperature conditions Movilla, Juancho Calvo, Eva Coma, Rafel Serrano, Eduard Lopez-Sanz, Angel Pelejero, Carles MEDIAN LATITUDE: 39.800000 * MEDIAN LONGITUDE: 1.125000 * SOUTH-BOUND LATITUDE: 37.550000 * WEST-BOUND LONGITUDE: -0.966670 * NORTH-BOUND LATITUDE: 42.050000 * EAST-BOUND LONGITUDE: 3.216670 * DATE/TIME START: 2011-01-01T00:00:00 * DATE/TIME END: 2011-01-31T00:00:00 2016-06-24 text/tab-separated-values, 12233 data points https://doi.pangaea.de/10.1594/PANGAEA.861963 https://doi.org/10.1594/PANGAEA.861963 en eng PANGAEA Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse (2015): seacarb: seawater carbonate chemistry with R. R package version 3.0.8. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.861963 https://doi.org/10.1594/PANGAEA.861963 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Movilla, Juancho; Calvo, Eva; Coma, Rafel; Serrano, Eduard; Lopez-Sanz, Angel; Pelejero, Carles (2016): Annual response of two Mediterranean azooxanthellate temperate corals to low-pH and high-temperature conditions. Marine Biology, 163(6), https://doi.org/10.1007/s00227-016-2908-9 Alkalinity total standard error Animalia Aragonite saturation state Astroides calycularis Benthic animals Benthos Bicarbonate ion Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcification/Dissolution Calcification rate of calcium carbonate Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cartagena_OA Cnidaria Coast and continental shelf Density Event label EXP Experiment Figure Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Identification L_Estartit Laboratory experiment Leptopsammia pruvoti Lipids Mediterranean Sea OA-ICC Ocean Acidification International Coordination Centre Organic matter Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Porosity Potentiometric Potentiometric titration Proteins Dataset 2016 ftpangaea https://doi.org/10.1594/PANGAEA.861963 https://doi.org/10.1007/s00227-016-2908-9 2023-01-20T09:07:25Z Ocean acidification (OA) and warming related to the anthropogenic increase in atmospheric CO2 have been shown to have detrimental effects on several marine organisms, especially those with calcium carbonate structures such as corals. In this study, we evaluate the response of two Mediterranean shallow-water azooxanthellate corals to the projected pH and seawater temperature (ST) scenarios for the end of this century. The colonial coral Astroides calycularis and the solitary Leptopsammia pruvoti were grown in aquaria over a year under two fixed pH conditions, control (8.05 pHT units) and low (7.72 pHT units), and simulating two annual ST cycles, natural and high (+3 °C). The organic matter (OM), lipid and protein content of the tissue and the skeletal microdensity of A. calycularis were not affected by the stress conditions (low pH, high ST), but the species exhibited a mean 25 % decrease in calcification rate at high-ST conditions at the end of the warm period and a mean 10 % increase in skeletal porosity under the acidified treatment after a full year cycle. Conversely, an absence of effects on calcification and skeletal microdensity of L. pruvoti exposed to low-pH and high-ST treatments contrasted with a significant decrease in the OM, lipid and protein content of the tissue at high-ST conditions and a 13 % mean increase in the skeletal porosity under low-pH conditions following a full year of exposure. This species-specific response suggests that different internal self-regulation strategies for energy reallocation may allow certain shallow-water azooxanthellate corals to cope more successfully than others with global environmental changes. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-0.966670,3.216670,42.050000,37.550000)