Impact of seawater carbonate chemistry on the calcification of marine bivalves
Bivalve calcification, particularly of the early larval stages, is highly sensitive to the change in ocean carbonate chemistry resulting from atmospheric CO2 uptake. Earlier studies suggested that declining seawater [CO32−] and thereby lowered carbonate saturation affect shell production. However, d...
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PANGAEA
2015
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.862531 https://doi.org/10.1594/PANGAEA.862531 |
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openpolar |
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Open Polar |
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PANGAEA - Data Publisher for Earth & Environmental Science |
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ftpangaea |
language |
English |
topic |
Alkalinity total standard deviation Animalia Aragonite saturation state Baltic Sea Benthic animals Benthos Bicarbonate ion Bottles or small containers/Aquaria (<20 L) 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 Experiment Figure Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Laboratory experiment Life stage Mass Mollusca Mytilus edulis OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos Percentage |
spellingShingle |
Alkalinity total standard deviation Animalia Aragonite saturation state Baltic Sea Benthic animals Benthos Bicarbonate ion Bottles or small containers/Aquaria (<20 L) 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 Experiment Figure Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Laboratory experiment Life stage Mass Mollusca Mytilus edulis OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos Percentage Thomsen, Jörn Haynert, Kristin Wegner, K Mathias Melzner, Frank Impact of seawater carbonate chemistry on the calcification of marine bivalves |
topic_facet |
Alkalinity total standard deviation Animalia Aragonite saturation state Baltic Sea Benthic animals Benthos Bicarbonate ion Bottles or small containers/Aquaria (<20 L) 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 Experiment Figure Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Laboratory experiment Life stage Mass Mollusca Mytilus edulis OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos Percentage |
description |
Bivalve calcification, particularly of the early larval stages, is highly sensitive to the change in ocean carbonate chemistry resulting from atmospheric CO2 uptake. Earlier studies suggested that declining seawater [CO32−] and thereby lowered carbonate saturation affect shell production. However, disturbances of physiological processes such as acid-base regulation by adverse seawater pCO2 and pH can affect calcification in a secondary fashion. In order to determine the exact carbonate system component by which growth and calcification are affected it is necessary to utilize more complex carbonate chemistry manipulations. As single factors, pCO2 had no effects and [HCO3-] and pH had only limited effects on shell growth, while lowered [CO32−] strongly impacted calcification. Dissolved inorganic carbon (CT) limiting conditions led to strong reductions in calcification, despite high [CO32−], indicating that [HCO3-] rather than [CO32−] is the inorganic carbon source utilized for calcification by mytilid mussels. However, as the ratio [HCO3-] / [H+] is linearly correlated with [CO32−] it is not possible to differentiate between these under natural seawater conditions. An equivalent of about 80 μmol kg−1 [CO32−] is required to saturate inorganic carbon supply for calcification in bivalves. Below this threshold biomineralization rates rapidly decline. A comparison of literature data available for larvae and juvenile mussels and oysters originating from habitats differing substantially with respect to prevailing carbonate chemistry conditions revealed similar response curves. This suggests that the mechanisms which determine sensitivity of calcification in this group are highly conserved. The higher sensitivity of larval calcification seems to primarily result from the much higher relative calcification rates in early life stages. In order to reveal and understand the mechanisms that limit or facilitate adaptation to future ocean acidification, it is necessary to better understand the physiological processes and their ... |
format |
Dataset |
author |
Thomsen, Jörn Haynert, Kristin Wegner, K Mathias Melzner, Frank |
author_facet |
Thomsen, Jörn Haynert, Kristin Wegner, K Mathias Melzner, Frank |
author_sort |
Thomsen, Jörn |
title |
Impact of seawater carbonate chemistry on the calcification of marine bivalves |
title_short |
Impact of seawater carbonate chemistry on the calcification of marine bivalves |
title_full |
Impact of seawater carbonate chemistry on the calcification of marine bivalves |
title_fullStr |
Impact of seawater carbonate chemistry on the calcification of marine bivalves |
title_full_unstemmed |
Impact of seawater carbonate chemistry on the calcification of marine bivalves |
title_sort |
impact of seawater carbonate chemistry on the calcification of marine bivalves |
publisher |
PANGAEA |
publishDate |
2015 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.862531 https://doi.org/10.1594/PANGAEA.862531 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Supplement to: Thomsen, Jörn; Haynert, Kristin; Wegner, K Mathias; Melzner, Frank (2015): Impact of seawater carbonate chemistry on the calcification of marine bivalves. Biogeosciences, 12(14), 4209-4220, https://doi.org/10.5194/bg-12-4209-2015 |
op_relation |
Thomsen, Jörn; Haynert, Kristin; Wegner, K Mathias; Melzner, Frank (2016): Calcification repsonse of m,arione bivalves to changed carbonate chemistry [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.856883 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.862531 https://doi.org/10.1594/PANGAEA.862531 |
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.86253110.5194/bg-12-4209-201510.1594/PANGAEA.856883 |
_version_ |
1810469468152791040 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.862531 2024-09-15T18:28:09+00:00 Impact of seawater carbonate chemistry on the calcification of marine bivalves Thomsen, Jörn Haynert, Kristin Wegner, K Mathias Melzner, Frank 2015 text/tab-separated-values, 1491 data points https://doi.pangaea.de/10.1594/PANGAEA.862531 https://doi.org/10.1594/PANGAEA.862531 en eng PANGAEA Thomsen, Jörn; Haynert, Kristin; Wegner, K Mathias; Melzner, Frank (2016): Calcification repsonse of m,arione bivalves to changed carbonate chemistry [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.856883 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.862531 https://doi.org/10.1594/PANGAEA.862531 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Thomsen, Jörn; Haynert, Kristin; Wegner, K Mathias; Melzner, Frank (2015): Impact of seawater carbonate chemistry on the calcification of marine bivalves. Biogeosciences, 12(14), 4209-4220, https://doi.org/10.5194/bg-12-4209-2015 Alkalinity total standard deviation Animalia Aragonite saturation state Baltic Sea Benthic animals Benthos Bicarbonate ion Bottles or small containers/Aquaria (<20 L) 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 Experiment Figure Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Laboratory experiment Life stage Mass Mollusca Mytilus edulis OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos Percentage dataset 2015 ftpangaea https://doi.org/10.1594/PANGAEA.86253110.5194/bg-12-4209-201510.1594/PANGAEA.856883 2024-07-24T02:31:33Z Bivalve calcification, particularly of the early larval stages, is highly sensitive to the change in ocean carbonate chemistry resulting from atmospheric CO2 uptake. Earlier studies suggested that declining seawater [CO32−] and thereby lowered carbonate saturation affect shell production. However, disturbances of physiological processes such as acid-base regulation by adverse seawater pCO2 and pH can affect calcification in a secondary fashion. In order to determine the exact carbonate system component by which growth and calcification are affected it is necessary to utilize more complex carbonate chemistry manipulations. As single factors, pCO2 had no effects and [HCO3-] and pH had only limited effects on shell growth, while lowered [CO32−] strongly impacted calcification. Dissolved inorganic carbon (CT) limiting conditions led to strong reductions in calcification, despite high [CO32−], indicating that [HCO3-] rather than [CO32−] is the inorganic carbon source utilized for calcification by mytilid mussels. However, as the ratio [HCO3-] / [H+] is linearly correlated with [CO32−] it is not possible to differentiate between these under natural seawater conditions. An equivalent of about 80 μmol kg−1 [CO32−] is required to saturate inorganic carbon supply for calcification in bivalves. Below this threshold biomineralization rates rapidly decline. A comparison of literature data available for larvae and juvenile mussels and oysters originating from habitats differing substantially with respect to prevailing carbonate chemistry conditions revealed similar response curves. This suggests that the mechanisms which determine sensitivity of calcification in this group are highly conserved. The higher sensitivity of larval calcification seems to primarily result from the much higher relative calcification rates in early life stages. In order to reveal and understand the mechanisms that limit or facilitate adaptation to future ocean acidification, it is necessary to better understand the physiological processes and their ... Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science |