Seawater carbonate chemistry, survival rate, shell size, calcification rate of the planktonic foraminifer Neogloboquadrina pachyderma (sinistral) in a laboratory experiment

The present study investigated the effects of ocean acidification and temperature increase on Neogloboquadrina pachyderma (sinistral), the dominant planktonic foraminifer in the Arctic Ocean. Due to the naturally low concentration of [CO3] 2- in the Arctic, this foraminifer could be particularly sen...

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Main Authors: Manno, Clara, Morata, Nathalie, Bellerby, Richard G J
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.830908
https://doi.org/10.1594/PANGAEA.830908
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.830908
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.830908 2024-09-15T17:54:14+00:00 Seawater carbonate chemistry, survival rate, shell size, calcification rate of the planktonic foraminifer Neogloboquadrina pachyderma (sinistral) in a laboratory experiment Manno, Clara Morata, Nathalie Bellerby, Richard G J 2012 text/tab-separated-values, 7932 data points https://doi.pangaea.de/10.1594/PANGAEA.830908 https://doi.org/10.1594/PANGAEA.830908 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.830908 https://doi.org/10.1594/PANGAEA.830908 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Manno, Clara; Morata, Nathalie; Bellerby, Richard G J (2012): Effect of ocean acidification and temperature increase on the planktonic foraminifer Neogloboquadrina pachyderma (sinistral). Polar Biology, 35(9), 1311-1319, https://doi.org/10.1007/s00300-012-1174-7 Alkalinity total Aragonite saturation state Arctic Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcification/Dissolution Calcification rate 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 Chromista Coulometric titration Diameter Foraminifera Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Heterotrophic prokaryotes Laboratory experiment Mortality/Survival Neogloboquadrina pachyderma OA-ICC Ocean Acidification International Coordination Centre Open ocean Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Polar Potentiometric titration Replicate Salinity Sample code/label Single species Species Stage Survival Temperature water Treatment dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.83090810.1007/s00300-012-1174-7 2024-07-24T02:31:32Z The present study investigated the effects of ocean acidification and temperature increase on Neogloboquadrina pachyderma (sinistral), the dominant planktonic foraminifer in the Arctic Ocean. Due to the naturally low concentration of [CO3] 2- in the Arctic, this foraminifer could be particularly sensitive to the forecast changes in seawater carbonate chemistry. To assess potential responses to ocean acidification and climate change, perturbation experiments were performed on juvenile and adult specimens by manipulating seawater to mimic the present-day carbon dioxide level and a future ocean acidification scenario (end of the century) under controlled (in situ) and elevated temperatures (1 and 4 °C, respectively). Foraminifera mortality was unaffected under all the different experiment treatments. Under low pH, N. pachyderma (s) shell net calcification rates decreased. This decrease was higher (30 %) in the juvenile specimens than decrease observed in the adults (21 %) ones. However, decrease in net calcification was moderated when both, pH decreased and temperature increased simultaneously. When only temperature increased, a net calcification rate for both life stages was not affected. These results show that forecast changes in seawater chemistry would impact calcite production in N. pachyderma (s), possibly leading to a reduction of calcite flux contribution and consequently a decrease in biologic pump efficiency. Dataset Arctic Ocean Climate change Foraminifera* Neogloboquadrina pachyderma Ocean acidification Polar Biology 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
Aragonite saturation state
Arctic
Bicarbonate ion
Bottles or small containers/Aquaria (<20 L)
Calcification/Dissolution
Calcification rate
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
Chromista
Coulometric titration
Diameter
Foraminifera
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Growth/Morphology
Heterotrophic prokaryotes
Laboratory experiment
Mortality/Survival
Neogloboquadrina pachyderma
OA-ICC
Ocean Acidification International Coordination Centre
Open ocean
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
pH
Polar
Potentiometric titration
Replicate
Salinity
Sample code/label
Single species
Species
Stage
Survival
Temperature
water
Treatment
spellingShingle Alkalinity
total
Aragonite saturation state
Arctic
Bicarbonate ion
Bottles or small containers/Aquaria (<20 L)
Calcification/Dissolution
Calcification rate
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
Chromista
Coulometric titration
Diameter
Foraminifera
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Growth/Morphology
Heterotrophic prokaryotes
Laboratory experiment
Mortality/Survival
Neogloboquadrina pachyderma
OA-ICC
Ocean Acidification International Coordination Centre
Open ocean
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
pH
Polar
Potentiometric titration
Replicate
Salinity
Sample code/label
Single species
Species
Stage
Survival
Temperature
water
Treatment
Manno, Clara
Morata, Nathalie
Bellerby, Richard G J
Seawater carbonate chemistry, survival rate, shell size, calcification rate of the planktonic foraminifer Neogloboquadrina pachyderma (sinistral) in a laboratory experiment
topic_facet Alkalinity
total
Aragonite saturation state
Arctic
Bicarbonate ion
Bottles or small containers/Aquaria (<20 L)
Calcification/Dissolution
Calcification rate
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
Chromista
Coulometric titration
Diameter
Foraminifera
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Growth/Morphology
Heterotrophic prokaryotes
Laboratory experiment
Mortality/Survival
Neogloboquadrina pachyderma
OA-ICC
Ocean Acidification International Coordination Centre
Open ocean
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
pH
Polar
Potentiometric titration
Replicate
Salinity
Sample code/label
Single species
Species
Stage
Survival
Temperature
water
Treatment
description The present study investigated the effects of ocean acidification and temperature increase on Neogloboquadrina pachyderma (sinistral), the dominant planktonic foraminifer in the Arctic Ocean. Due to the naturally low concentration of [CO3] 2- in the Arctic, this foraminifer could be particularly sensitive to the forecast changes in seawater carbonate chemistry. To assess potential responses to ocean acidification and climate change, perturbation experiments were performed on juvenile and adult specimens by manipulating seawater to mimic the present-day carbon dioxide level and a future ocean acidification scenario (end of the century) under controlled (in situ) and elevated temperatures (1 and 4 °C, respectively). Foraminifera mortality was unaffected under all the different experiment treatments. Under low pH, N. pachyderma (s) shell net calcification rates decreased. This decrease was higher (30 %) in the juvenile specimens than decrease observed in the adults (21 %) ones. However, decrease in net calcification was moderated when both, pH decreased and temperature increased simultaneously. When only temperature increased, a net calcification rate for both life stages was not affected. These results show that forecast changes in seawater chemistry would impact calcite production in N. pachyderma (s), possibly leading to a reduction of calcite flux contribution and consequently a decrease in biologic pump efficiency.
format Dataset
author Manno, Clara
Morata, Nathalie
Bellerby, Richard G J
author_facet Manno, Clara
Morata, Nathalie
Bellerby, Richard G J
author_sort Manno, Clara
title Seawater carbonate chemistry, survival rate, shell size, calcification rate of the planktonic foraminifer Neogloboquadrina pachyderma (sinistral) in a laboratory experiment
title_short Seawater carbonate chemistry, survival rate, shell size, calcification rate of the planktonic foraminifer Neogloboquadrina pachyderma (sinistral) in a laboratory experiment
title_full Seawater carbonate chemistry, survival rate, shell size, calcification rate of the planktonic foraminifer Neogloboquadrina pachyderma (sinistral) in a laboratory experiment
title_fullStr Seawater carbonate chemistry, survival rate, shell size, calcification rate of the planktonic foraminifer Neogloboquadrina pachyderma (sinistral) in a laboratory experiment
title_full_unstemmed Seawater carbonate chemistry, survival rate, shell size, calcification rate of the planktonic foraminifer Neogloboquadrina pachyderma (sinistral) in a laboratory experiment
title_sort seawater carbonate chemistry, survival rate, shell size, calcification rate of the planktonic foraminifer neogloboquadrina pachyderma (sinistral) in a laboratory experiment
publisher PANGAEA
publishDate 2012
url https://doi.pangaea.de/10.1594/PANGAEA.830908
https://doi.org/10.1594/PANGAEA.830908
genre Arctic Ocean
Climate change
Foraminifera*
Neogloboquadrina pachyderma
Ocean acidification
Polar Biology
genre_facet Arctic Ocean
Climate change
Foraminifera*
Neogloboquadrina pachyderma
Ocean acidification
Polar Biology
op_source Supplement to: Manno, Clara; Morata, Nathalie; Bellerby, Richard G J (2012): Effect of ocean acidification and temperature increase on the planktonic foraminifer Neogloboquadrina pachyderma (sinistral). Polar Biology, 35(9), 1311-1319, https://doi.org/10.1007/s00300-012-1174-7
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.830908
https://doi.org/10.1594/PANGAEA.830908
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.83090810.1007/s00300-012-1174-7
_version_ 1810430479602548736