Effect of ocean acidification and pH fluctuations on the growth and development of coralline algal recruits, and an associated benthic algal assemblage

Coralline algae are susceptible to the changes in the seawater carbonate system associated with ocean acidification (OA). However, the coastal environments in which corallines grow are subject to large daily pH fluctuations which may affect their responses to OA. Here, we followed the growth and dev...

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Bibliographic Details
Main Authors: Roleda, Michael Y, Cornwall, Christopher Edward, Feng, Yuanyuan, McGraw, Christina M, Smith, Abigail M, Hurd, Catriona L
Format: Dataset
Language:English
Published: PANGAEA 2015
Subjects:
EXP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.859434
https://doi.org/10.1594/PANGAEA.859434
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.859434
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
Aragonite saturation state
Area
Arthrocardia corymbosa
Benthos
Bicarbonate ion
Biogenic silica per chlorophyll a
Biomass/Abundance/Elemental composition
Bottles or small containers/Aquaria (<20 L)
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Chlorophyll a/particulate organic carbon ratio
Coast and continental shelf
Date
EXP
Experiment
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Growth/Morphology
Growth rate
Karitane
Laboratory experiment
Macroalgae
Magnesium carbonate
magnesite
Number
OA-ICC
Ocean Acidification International Coordination Centre
spellingShingle Alkalinity
total
standard error
Aragonite saturation state
Area
Arthrocardia corymbosa
Benthos
Bicarbonate ion
Biogenic silica per chlorophyll a
Biomass/Abundance/Elemental composition
Bottles or small containers/Aquaria (<20 L)
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Chlorophyll a/particulate organic carbon ratio
Coast and continental shelf
Date
EXP
Experiment
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Growth/Morphology
Growth rate
Karitane
Laboratory experiment
Macroalgae
Magnesium carbonate
magnesite
Number
OA-ICC
Ocean Acidification International Coordination Centre
Roleda, Michael Y
Cornwall, Christopher Edward
Feng, Yuanyuan
McGraw, Christina M
Smith, Abigail M
Hurd, Catriona L
Effect of ocean acidification and pH fluctuations on the growth and development of coralline algal recruits, and an associated benthic algal assemblage
topic_facet Alkalinity
total
standard error
Aragonite saturation state
Area
Arthrocardia corymbosa
Benthos
Bicarbonate ion
Biogenic silica per chlorophyll a
Biomass/Abundance/Elemental composition
Bottles or small containers/Aquaria (<20 L)
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Chlorophyll a/particulate organic carbon ratio
Coast and continental shelf
Date
EXP
Experiment
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Growth/Morphology
Growth rate
Karitane
Laboratory experiment
Macroalgae
Magnesium carbonate
magnesite
Number
OA-ICC
Ocean Acidification International Coordination Centre
description Coralline algae are susceptible to the changes in the seawater carbonate system associated with ocean acidification (OA). However, the coastal environments in which corallines grow are subject to large daily pH fluctuations which may affect their responses to OA. Here, we followed the growth and development of the juvenile coralline alga Arthrocardia corymbosa, which had recruited into experimental conditions during a prior experiment, using a novel OA laboratory culture system to simulate the pH fluctuations observed within a kelp forest. Microscopic life history stages are considered more susceptible to environmental stress than adult stages; we compared the responses of newly recruited A. corymbosa to static and fluctuating seawater pH with those of their field-collected parents. Recruits were cultivated for 16 weeks under static pH 8.05 and 7.65, representing ambient and 4*preindustrial pCO2 concentrations, respectively, and two fluctuating pH treatments of daily (daytime pH = 8.45, night-time pH = 7.65) and daily (daytime pH = 8.05, night-time pH = 7.25). Positive growth rates of new recruits were recorded in all treatments, and were highest under static pH 8.05 and lowest under fluctuating pH 7.65. This pattern was similar to the adults' response, except that adults had zero growth under fluctuating pH 7.65. The % dry weight of MgCO3 in calcite of the juveniles was reduced from 10% at pH 8.05 to 8% at pH 7.65, but there was no effect of pH fluctuation. A wide range of fleshy macroalgae and at least 6 species of benthic diatoms recruited across all experimental treatments, from cryptic spores associated with the adult A. corymbosa. There was no effect of experimental treatment on the growth of the benthic diatoms. On the community level, pH-sensitive species may survive lower pH in the presence of diatoms and fleshy macroalgae, whose high metabolic activity may raise the pH of the local microhabitat.
format Dataset
author Roleda, Michael Y
Cornwall, Christopher Edward
Feng, Yuanyuan
McGraw, Christina M
Smith, Abigail M
Hurd, Catriona L
author_facet Roleda, Michael Y
Cornwall, Christopher Edward
Feng, Yuanyuan
McGraw, Christina M
Smith, Abigail M
Hurd, Catriona L
author_sort Roleda, Michael Y
title Effect of ocean acidification and pH fluctuations on the growth and development of coralline algal recruits, and an associated benthic algal assemblage
title_short Effect of ocean acidification and pH fluctuations on the growth and development of coralline algal recruits, and an associated benthic algal assemblage
title_full Effect of ocean acidification and pH fluctuations on the growth and development of coralline algal recruits, and an associated benthic algal assemblage
title_fullStr Effect of ocean acidification and pH fluctuations on the growth and development of coralline algal recruits, and an associated benthic algal assemblage
title_full_unstemmed Effect of ocean acidification and pH fluctuations on the growth and development of coralline algal recruits, and an associated benthic algal assemblage
title_sort effect of ocean acidification and ph fluctuations on the growth and development of coralline algal recruits, and an associated benthic algal assemblage
publisher PANGAEA
publishDate 2015
url https://doi.pangaea.de/10.1594/PANGAEA.859434
https://doi.org/10.1594/PANGAEA.859434
op_coverage LATITUDE: -45.638890 * LONGITUDE: 170.670830 * DATE/TIME START: 2011-03-13T00:00:00 * DATE/TIME END: 2011-04-30T00:00:00
long_lat ENVELOPE(170.670830,170.670830,-45.638890,-45.638890)
genre Ocean acidification
genre_facet Ocean acidification
op_source Supplement to: Roleda, Michael Y; Cornwall, Christopher Edward; Feng, Yuanyuan; McGraw, Christina M; Smith, Abigail M; Hurd, Catriona L (2015): Effect of ocean acidification and pH fluctuations on the growth and development of coralline algal recruits, and an associated benthic algal assemblage. PLoS ONE, 10(10), e0140394, https://doi.org/10.1371/journal.pone.0140394
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.859434
https://doi.org/10.1594/PANGAEA.859434
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.85943410.1371/journal.pone.0140394
_version_ 1810469337815842816
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.859434 2024-09-15T18:28:02+00:00 Effect of ocean acidification and pH fluctuations on the growth and development of coralline algal recruits, and an associated benthic algal assemblage Roleda, Michael Y Cornwall, Christopher Edward Feng, Yuanyuan McGraw, Christina M Smith, Abigail M Hurd, Catriona L LATITUDE: -45.638890 * LONGITUDE: 170.670830 * DATE/TIME START: 2011-03-13T00:00:00 * DATE/TIME END: 2011-04-30T00:00:00 2015 text/tab-separated-values, 1488 data points https://doi.pangaea.de/10.1594/PANGAEA.859434 https://doi.org/10.1594/PANGAEA.859434 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.859434 https://doi.org/10.1594/PANGAEA.859434 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Roleda, Michael Y; Cornwall, Christopher Edward; Feng, Yuanyuan; McGraw, Christina M; Smith, Abigail M; Hurd, Catriona L (2015): Effect of ocean acidification and pH fluctuations on the growth and development of coralline algal recruits, and an associated benthic algal assemblage. PLoS ONE, 10(10), e0140394, https://doi.org/10.1371/journal.pone.0140394 Alkalinity total standard error Aragonite saturation state Area Arthrocardia corymbosa Benthos Bicarbonate ion Biogenic silica per chlorophyll a Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chlorophyll a/particulate organic carbon ratio Coast and continental shelf Date EXP Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate Karitane Laboratory experiment Macroalgae Magnesium carbonate magnesite Number OA-ICC Ocean Acidification International Coordination Centre dataset 2015 ftpangaea https://doi.org/10.1594/PANGAEA.85943410.1371/journal.pone.0140394 2024-07-24T02:31:33Z Coralline algae are susceptible to the changes in the seawater carbonate system associated with ocean acidification (OA). However, the coastal environments in which corallines grow are subject to large daily pH fluctuations which may affect their responses to OA. Here, we followed the growth and development of the juvenile coralline alga Arthrocardia corymbosa, which had recruited into experimental conditions during a prior experiment, using a novel OA laboratory culture system to simulate the pH fluctuations observed within a kelp forest. Microscopic life history stages are considered more susceptible to environmental stress than adult stages; we compared the responses of newly recruited A. corymbosa to static and fluctuating seawater pH with those of their field-collected parents. Recruits were cultivated for 16 weeks under static pH 8.05 and 7.65, representing ambient and 4*preindustrial pCO2 concentrations, respectively, and two fluctuating pH treatments of daily (daytime pH = 8.45, night-time pH = 7.65) and daily (daytime pH = 8.05, night-time pH = 7.25). Positive growth rates of new recruits were recorded in all treatments, and were highest under static pH 8.05 and lowest under fluctuating pH 7.65. This pattern was similar to the adults' response, except that adults had zero growth under fluctuating pH 7.65. The % dry weight of MgCO3 in calcite of the juveniles was reduced from 10% at pH 8.05 to 8% at pH 7.65, but there was no effect of pH fluctuation. A wide range of fleshy macroalgae and at least 6 species of benthic diatoms recruited across all experimental treatments, from cryptic spores associated with the adult A. corymbosa. There was no effect of experimental treatment on the growth of the benthic diatoms. On the community level, pH-sensitive species may survive lower pH in the presence of diatoms and fleshy macroalgae, whose high metabolic activity may raise the pH of the local microhabitat. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(170.670830,170.670830,-45.638890,-45.638890)