Seawater carbonate chemistry and survival, larval development, shell growth and normal shell development of great scallop (Pecten maximus Lamarck)

The increasing amount of dissolved anthropogenic CO2 has caused a drop in pH values in the open ocean known as ocean acidification. This change in seawater carbonate chemistry has been shown to have a negative effect on a number of marine organisms. Early life stages are the most vulnerable, and esp...

Full description

Bibliographic Details
Main Authors: Andersen, Sissel, Grefsrud, E S, Harboe, T
Format: Dataset
Language:English
Published: PANGAEA 2017
Subjects:
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.880379
https://doi.org/10.1594/PANGAEA.880379
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.880379
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.880379 2024-09-15T18:24:30+00:00 Seawater carbonate chemistry and survival, larval development, shell growth and normal shell development of great scallop (Pecten maximus Lamarck) Andersen, Sissel Grefsrud, E S Harboe, T 2017 text/tab-separated-values, 4392 data points https://doi.pangaea.de/10.1594/PANGAEA.880379 https://doi.org/10.1594/PANGAEA.880379 en eng PANGAEA Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James C; Gentili, Bernard; Proye, Aurélien; Soetaert, Karline; Rae, James (2016): seacarb: seawater carbonate chemistry with R. R package version 3.1. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.880379 https://doi.org/10.1594/PANGAEA.880379 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Andersen, Sissel; Grefsrud, E S; Harboe, T (2017): Sensitivity towards elevated pCO2 in great scallop (Pecten maximus Lamarck) embryos and fed larvae. Biogeosciences, 14(3), 529-539, https://doi.org/10.5194/bg-14-529-2017 Alkalinity total Animalia Aragonite saturation state Benthic animals Benthos 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) Development Experiment duration Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Identification Laboratory experiment Larvae Mollusca Mortality/Survival North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pecten maximus pH Potentiometric Potentiometric titration Registration number of species Replicates Salinity Shell length standard deviation Single species Species Survival Temperate Temperature water Time in days Type Uniform resource locator/link to reference dataset 2017 ftpangaea https://doi.org/10.1594/PANGAEA.88037910.5194/bg-14-529-2017 2024-07-24T02:31:33Z The increasing amount of dissolved anthropogenic CO2 has caused a drop in pH values in the open ocean known as ocean acidification. This change in seawater carbonate chemistry has been shown to have a negative effect on a number of marine organisms. Early life stages are the most vulnerable, and especially the organisms that produce calcified structures in the phylum Mollusca. Few studies have looked at effects on scallops, and this is the first study presented including fed larvae of the great scallop (Pecten maximus) followed until day 14 post-fertilization. Fertilized eggs from unexposed parents were exposed to three levels of pCO2 using four replicate units: 465 (ambient), 768 and 1294 µatm, corresponding to pHNIST of 7.94, 7.75 (-0.19 units) and 7.54 (-0.40 units), respectively. All of the observed parameters were negatively affected by elevated pCO2: survival, larval development, shell growth and normal shell development. The latter was observed to be affected only 2 days after fertilization. Negative effects on the fed larvae at day 7 were similar to what was shown earlier for unfed P. maximus larvae. Growth rate in the group at 768?µatm seemed to decline after day 7, indicating that the ability to overcome the environmental change at moderately elevated pCO2 was lost over time. The present study shows that food availability does not decrease the sensitivity to elevated pCO2 in P. maximus larvae. Unless genetic adaptation and acclimatization counteract the negative effects of long term elevated pCO2, recruitment in populations of P. maximus will most likely be negatively affected by the projected drop of 0.06-0.32 units in pH within year 2100. Dataset North Atlantic Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Alkalinity
total
Animalia
Aragonite saturation state
Benthic animals
Benthos
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)
Development
Experiment duration
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Growth/Morphology
Identification
Laboratory experiment
Larvae
Mollusca
Mortality/Survival
North Atlantic
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pecten maximus
pH
Potentiometric
Potentiometric titration
Registration number of species
Replicates
Salinity
Shell length
standard deviation
Single species
Species
Survival
Temperate
Temperature
water
Time in days
Type
Uniform resource locator/link to reference
spellingShingle Alkalinity
total
Animalia
Aragonite saturation state
Benthic animals
Benthos
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)
Development
Experiment duration
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Growth/Morphology
Identification
Laboratory experiment
Larvae
Mollusca
Mortality/Survival
North Atlantic
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pecten maximus
pH
Potentiometric
Potentiometric titration
Registration number of species
Replicates
Salinity
Shell length
standard deviation
Single species
Species
Survival
Temperate
Temperature
water
Time in days
Type
Uniform resource locator/link to reference
Andersen, Sissel
Grefsrud, E S
Harboe, T
Seawater carbonate chemistry and survival, larval development, shell growth and normal shell development of great scallop (Pecten maximus Lamarck)
topic_facet Alkalinity
total
Animalia
Aragonite saturation state
Benthic animals
Benthos
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)
Development
Experiment duration
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Growth/Morphology
Identification
Laboratory experiment
Larvae
Mollusca
Mortality/Survival
North Atlantic
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pecten maximus
pH
Potentiometric
Potentiometric titration
Registration number of species
Replicates
Salinity
Shell length
standard deviation
Single species
Species
Survival
Temperate
Temperature
water
Time in days
Type
Uniform resource locator/link to reference
description The increasing amount of dissolved anthropogenic CO2 has caused a drop in pH values in the open ocean known as ocean acidification. This change in seawater carbonate chemistry has been shown to have a negative effect on a number of marine organisms. Early life stages are the most vulnerable, and especially the organisms that produce calcified structures in the phylum Mollusca. Few studies have looked at effects on scallops, and this is the first study presented including fed larvae of the great scallop (Pecten maximus) followed until day 14 post-fertilization. Fertilized eggs from unexposed parents were exposed to three levels of pCO2 using four replicate units: 465 (ambient), 768 and 1294 µatm, corresponding to pHNIST of 7.94, 7.75 (-0.19 units) and 7.54 (-0.40 units), respectively. All of the observed parameters were negatively affected by elevated pCO2: survival, larval development, shell growth and normal shell development. The latter was observed to be affected only 2 days after fertilization. Negative effects on the fed larvae at day 7 were similar to what was shown earlier for unfed P. maximus larvae. Growth rate in the group at 768?µatm seemed to decline after day 7, indicating that the ability to overcome the environmental change at moderately elevated pCO2 was lost over time. The present study shows that food availability does not decrease the sensitivity to elevated pCO2 in P. maximus larvae. Unless genetic adaptation and acclimatization counteract the negative effects of long term elevated pCO2, recruitment in populations of P. maximus will most likely be negatively affected by the projected drop of 0.06-0.32 units in pH within year 2100.
format Dataset
author Andersen, Sissel
Grefsrud, E S
Harboe, T
author_facet Andersen, Sissel
Grefsrud, E S
Harboe, T
author_sort Andersen, Sissel
title Seawater carbonate chemistry and survival, larval development, shell growth and normal shell development of great scallop (Pecten maximus Lamarck)
title_short Seawater carbonate chemistry and survival, larval development, shell growth and normal shell development of great scallop (Pecten maximus Lamarck)
title_full Seawater carbonate chemistry and survival, larval development, shell growth and normal shell development of great scallop (Pecten maximus Lamarck)
title_fullStr Seawater carbonate chemistry and survival, larval development, shell growth and normal shell development of great scallop (Pecten maximus Lamarck)
title_full_unstemmed Seawater carbonate chemistry and survival, larval development, shell growth and normal shell development of great scallop (Pecten maximus Lamarck)
title_sort seawater carbonate chemistry and survival, larval development, shell growth and normal shell development of great scallop (pecten maximus lamarck)
publisher PANGAEA
publishDate 2017
url https://doi.pangaea.de/10.1594/PANGAEA.880379
https://doi.org/10.1594/PANGAEA.880379
genre North Atlantic
Ocean acidification
genre_facet North Atlantic
Ocean acidification
op_source Supplement to: Andersen, Sissel; Grefsrud, E S; Harboe, T (2017): Sensitivity towards elevated pCO2 in great scallop (Pecten maximus Lamarck) embryos and fed larvae. Biogeosciences, 14(3), 529-539, https://doi.org/10.5194/bg-14-529-2017
op_relation Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James C; Gentili, Bernard; Proye, Aurélien; Soetaert, Karline; Rae, James (2016): seacarb: seawater carbonate chemistry with R. R package version 3.1. https://cran.r-project.org/package=seacarb
https://doi.pangaea.de/10.1594/PANGAEA.880379
https://doi.org/10.1594/PANGAEA.880379
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.88037910.5194/bg-14-529-2017
_version_ 1810464870218334208