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spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.831099 2024-09-15T18:28:06+00:00 Seawater carbonate chemistry and larval growth response of the Portuguese oyster (Crassostrea angulata) in a laboratory experiment Thiyagarajan, Vengatesen Ko, W K Ginger LATITUDE: 26.098160 * LONGITUDE: 119.796060 * DATE/TIME START: 2011-09-01T00:00:00 * DATE/TIME END: 2011-11-30T00:00:00 2012 text/tab-separated-values, 405 data points https://doi.pangaea.de/10.1594/PANGAEA.831099 https://doi.org/10.1594/PANGAEA.831099 en eng PANGAEA Lavigne, Héloïse; Gattuso, Jean-Pierre (2011): seacarb: seawater carbonate chemistry with R. R package version 2.4 [webpage]. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.831099 https://doi.org/10.1594/PANGAEA.831099 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Thiyagarajan, Vengatesen; Ko, W K Ginger (2012): Larval growth response of the Portuguese oyster (Crassostrea angulata) to multiple climate change stressors. Aquaculture, 370-371, 90-95, https://doi.org/10.1016/j.aquaculture.2012.09.025 Alkalinity total standard deviation Animalia Aragonite saturation state Area 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 Coast and continental shelf Containers and aquaria (20-1000 L or < 1 m**2) Crassostrea angulata EXP Experiment Figure Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Fujian Growth/Morphology Laboratory experiment Mollusca North Pacific OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Potentiometric titration Salinity Single species Species Temperate Temperature water dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.83109910.1016/j.aquaculture.2012.09.025 2024-07-24T02:31:32Z Rising anthropogenic carbon dioxide (CO2) dissolving into coastal waters is decreasing the pH and carbonate ion concentration, thereby lowering the saturation state of calcium carbonate (CaCO3) minerals through a process named ocean acidification (OA). The unprecedented threats posed by such low pH on calcifying larvae of several edible oyster species have not yet been fully explored. Effects of low pH (7.9, 7.6, 7.4) on the early growth phase of Portuguese oyster (Crassostrea angulata) veliger larvae was examined at ambient salinity (34 ppt) and the low-salinity (27 ppt) treatment. Additionally, the combined effect of pH (8.1, 7.6), salinity (24 and 34 ppt) and temperature (24 °C and 30 °C) was examined using factorial experimental design. Surprisingly, the early growth phase from hatching to 5-day-old veliger stage showed high tolerance to pH 7.9 and pH 7.6 at both 34 ppt and 27 ppt. Larval shell area was significantly smaller at pH 7.4 only in low-salinity. In the 3-factor experiment, shell area was affected by salinity and the interaction between salinity and temperature but not by other combinations. Larvae produced the largest shell at the elevated temperature in low-salinity, regardless of pH. Thus the growth of the Portuguese oyster larvae appears to be robust to near-future pH level (> 7.6) when combined with projected elevated temperature and low-salinity in the coastal aquaculture zones of South China Sea. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(119.796060,119.796060,26.098160,26.098160)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Alkalinity
total
standard deviation
Animalia
Aragonite saturation state
Area
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
Coast and continental shelf
Containers and aquaria (20-1000 L or < 1 m**2)
Crassostrea angulata
EXP
Experiment
Figure
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Fujian
Growth/Morphology
Laboratory experiment
Mollusca
North Pacific
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
pH
Potentiometric titration
Salinity
Single species
Species
Temperate
Temperature
water
spellingShingle Alkalinity
total
standard deviation
Animalia
Aragonite saturation state
Area
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
Coast and continental shelf
Containers and aquaria (20-1000 L or < 1 m**2)
Crassostrea angulata
EXP
Experiment
Figure
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Fujian
Growth/Morphology
Laboratory experiment
Mollusca
North Pacific
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
pH
Potentiometric titration
Salinity
Single species
Species
Temperate
Temperature
water
Thiyagarajan, Vengatesen
Ko, W K Ginger
Seawater carbonate chemistry and larval growth response of the Portuguese oyster (Crassostrea angulata) in a laboratory experiment
topic_facet Alkalinity
total
standard deviation
Animalia
Aragonite saturation state
Area
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
Coast and continental shelf
Containers and aquaria (20-1000 L or < 1 m**2)
Crassostrea angulata
EXP
Experiment
Figure
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Fujian
Growth/Morphology
Laboratory experiment
Mollusca
North Pacific
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
pH
Potentiometric titration
Salinity
Single species
Species
Temperate
Temperature
water
description Rising anthropogenic carbon dioxide (CO2) dissolving into coastal waters is decreasing the pH and carbonate ion concentration, thereby lowering the saturation state of calcium carbonate (CaCO3) minerals through a process named ocean acidification (OA). The unprecedented threats posed by such low pH on calcifying larvae of several edible oyster species have not yet been fully explored. Effects of low pH (7.9, 7.6, 7.4) on the early growth phase of Portuguese oyster (Crassostrea angulata) veliger larvae was examined at ambient salinity (34 ppt) and the low-salinity (27 ppt) treatment. Additionally, the combined effect of pH (8.1, 7.6), salinity (24 and 34 ppt) and temperature (24 °C and 30 °C) was examined using factorial experimental design. Surprisingly, the early growth phase from hatching to 5-day-old veliger stage showed high tolerance to pH 7.9 and pH 7.6 at both 34 ppt and 27 ppt. Larval shell area was significantly smaller at pH 7.4 only in low-salinity. In the 3-factor experiment, shell area was affected by salinity and the interaction between salinity and temperature but not by other combinations. Larvae produced the largest shell at the elevated temperature in low-salinity, regardless of pH. Thus the growth of the Portuguese oyster larvae appears to be robust to near-future pH level (> 7.6) when combined with projected elevated temperature and low-salinity in the coastal aquaculture zones of South China Sea.
format Dataset
author Thiyagarajan, Vengatesen
Ko, W K Ginger
author_facet Thiyagarajan, Vengatesen
Ko, W K Ginger
author_sort Thiyagarajan, Vengatesen
title Seawater carbonate chemistry and larval growth response of the Portuguese oyster (Crassostrea angulata) in a laboratory experiment
title_short Seawater carbonate chemistry and larval growth response of the Portuguese oyster (Crassostrea angulata) in a laboratory experiment
title_full Seawater carbonate chemistry and larval growth response of the Portuguese oyster (Crassostrea angulata) in a laboratory experiment
title_fullStr Seawater carbonate chemistry and larval growth response of the Portuguese oyster (Crassostrea angulata) in a laboratory experiment
title_full_unstemmed Seawater carbonate chemistry and larval growth response of the Portuguese oyster (Crassostrea angulata) in a laboratory experiment
title_sort seawater carbonate chemistry and larval growth response of the portuguese oyster (crassostrea angulata) in a laboratory experiment
publisher PANGAEA
publishDate 2012
url https://doi.pangaea.de/10.1594/PANGAEA.831099
https://doi.org/10.1594/PANGAEA.831099
op_coverage LATITUDE: 26.098160 * LONGITUDE: 119.796060 * DATE/TIME START: 2011-09-01T00:00:00 * DATE/TIME END: 2011-11-30T00:00:00
long_lat ENVELOPE(119.796060,119.796060,26.098160,26.098160)
genre Ocean acidification
genre_facet Ocean acidification
op_source Supplement to: Thiyagarajan, Vengatesen; Ko, W K Ginger (2012): Larval growth response of the Portuguese oyster (Crassostrea angulata) to multiple climate change stressors. Aquaculture, 370-371, 90-95, https://doi.org/10.1016/j.aquaculture.2012.09.025
op_relation Lavigne, Héloïse; Gattuso, Jean-Pierre (2011): seacarb: seawater carbonate chemistry with R. R package version 2.4 [webpage]. https://cran.r-project.org/package=seacarb
https://doi.pangaea.de/10.1594/PANGAEA.831099
https://doi.org/10.1594/PANGAEA.831099
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.83109910.1016/j.aquaculture.2012.09.025
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