Seawater carbonate chemistry and adhesion and shell formation of the Barnacle Amphibalanus amphitrite

Barnacles are dominant members of marine intertidal communities. Their success depends on firm attachment provided by their proteinaceous adhesive and protection imparted by their calcified shell plates. Little is known about how variations in the environment affect adhesion and shell formation proc...

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Main Authors: Nardone, Jessica A, Patel, Shrey, Siegel, Kyle R, Tedesco, Dana, McNicholl, Conall G, O'Malley, Jessica, Herrick, Jack, Metzler, Rebecca A, Orihuela, Beatriz, Rittschof, Daniel, Dickinson, Gary H
Format: Dataset
Language:English
Published: PANGAEA 2018
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.922978
https://doi.org/10.1594/PANGAEA.922978
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.922978
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Adhesive strength
standard error
Alkalinity
total
standard deviation
Amphibalanus amphitrite
Animalia
Aragonite saturation state
Area
Arthropoda
Atomic disorder
Benthic animals
Benthos
Bicarbonate ion
Biomass/Abundance/Elemental composition
Bottles or small containers/Aquaria (<20 L)
Calcite crystal area
Calcite saturation state
Calcium
Calculated using CO2calc
Calculated using seacarb after Nisumaa et al. (2010)
Calculated using seacarb after Orr et al. (2018)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
spellingShingle Adhesive strength
standard error
Alkalinity
total
standard deviation
Amphibalanus amphitrite
Animalia
Aragonite saturation state
Area
Arthropoda
Atomic disorder
Benthic animals
Benthos
Bicarbonate ion
Biomass/Abundance/Elemental composition
Bottles or small containers/Aquaria (<20 L)
Calcite crystal area
Calcite saturation state
Calcium
Calculated using CO2calc
Calculated using seacarb after Nisumaa et al. (2010)
Calculated using seacarb after Orr et al. (2018)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Nardone, Jessica A
Patel, Shrey
Siegel, Kyle R
Tedesco, Dana
McNicholl, Conall G
O'Malley, Jessica
Herrick, Jack
Metzler, Rebecca A
Orihuela, Beatriz
Rittschof, Daniel
Dickinson, Gary H
Seawater carbonate chemistry and adhesion and shell formation of the Barnacle Amphibalanus amphitrite
topic_facet Adhesive strength
standard error
Alkalinity
total
standard deviation
Amphibalanus amphitrite
Animalia
Aragonite saturation state
Area
Arthropoda
Atomic disorder
Benthic animals
Benthos
Bicarbonate ion
Biomass/Abundance/Elemental composition
Bottles or small containers/Aquaria (<20 L)
Calcite crystal area
Calcite saturation state
Calcium
Calculated using CO2calc
Calculated using seacarb after Nisumaa et al. (2010)
Calculated using seacarb after Orr et al. (2018)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
description Barnacles are dominant members of marine intertidal communities. Their success depends on firm attachment provided by their proteinaceous adhesive and protection imparted by their calcified shell plates. Little is known about how variations in the environment affect adhesion and shell formation processes in barnacles. Increased levels of atmospheric CO2 have led to a reduction in the pH of ocean waters (i.e., ocean acidification), a trend that is expected to continue into the future. Here, we assessed if a reduction in seawater pH, at levels predicted within the next 200 years, would alter physiology, adhesion, and shell formation in the cosmopolitan barnacle Amphibalanus (=Balanus) amphitrite. Juvenile barnacles, settled on silicone substrates, were exposed to one of three static levels of pHT, 8.01, 7.78, or 7.50, for 13 weeks. We found that barnacles were robust to reduced pH, with no effect of pH on physiological metrics (mortality, tissue mass, and presence of eggs). Likewise, adhesive properties (adhesion strength and adhesive plaque gross morphology) were not affected by reduced pH. Shell formation, however, was affected by seawater pH. Shell mass and base plate area were higher in barnacles exposed to reduced pH; barnacles grown at pHT 8.01 exhibited approximately 30% lower shell mass and 20% smaller base plate area as compared to those at pHT 7.50 or 7.78. Enhanced growth at reduced pH appears to be driven by the increased size of the calcite crystals that comprise the shell. Despite enhanced growth, mechanical properties of the base plate (but not the parietal plates) were compromised at the lowest pH level. Barnacle base plates at pHT 7.50 broke more easily and crack propagation, measured through microhardness testing, was significantly affected by seawater pH. Other shell metrics (plate thickness, relative crystallinity, and atomic disorder) were not affected by seawater pH. Hence, a reduction in pH resulted in larger barnacles but with base plates that would crack more readily. It is yet to be ...
format Dataset
author Nardone, Jessica A
Patel, Shrey
Siegel, Kyle R
Tedesco, Dana
McNicholl, Conall G
O'Malley, Jessica
Herrick, Jack
Metzler, Rebecca A
Orihuela, Beatriz
Rittschof, Daniel
Dickinson, Gary H
author_facet Nardone, Jessica A
Patel, Shrey
Siegel, Kyle R
Tedesco, Dana
McNicholl, Conall G
O'Malley, Jessica
Herrick, Jack
Metzler, Rebecca A
Orihuela, Beatriz
Rittschof, Daniel
Dickinson, Gary H
author_sort Nardone, Jessica A
title Seawater carbonate chemistry and adhesion and shell formation of the Barnacle Amphibalanus amphitrite
title_short Seawater carbonate chemistry and adhesion and shell formation of the Barnacle Amphibalanus amphitrite
title_full Seawater carbonate chemistry and adhesion and shell formation of the Barnacle Amphibalanus amphitrite
title_fullStr Seawater carbonate chemistry and adhesion and shell formation of the Barnacle Amphibalanus amphitrite
title_full_unstemmed Seawater carbonate chemistry and adhesion and shell formation of the Barnacle Amphibalanus amphitrite
title_sort seawater carbonate chemistry and adhesion and shell formation of the barnacle amphibalanus amphitrite
publisher PANGAEA
publishDate 2018
url https://doi.pangaea.de/10.1594/PANGAEA.922978
https://doi.org/10.1594/PANGAEA.922978
genre Ocean acidification
genre_facet Ocean acidification
op_relation Nardone, Jessica A; Patel, Shrey; Siegel, Kyle R; Tedesco, Dana; McNicholl, Conall G; O'Malley, Jessica; Herrick, Jack; Metzler, Rebecca A; Orihuela, Beatriz; Rittschof, Daniel; Dickinson, Gary H (2018): Assessing the Impacts of Ocean Acidification on Adhesion and Shell Formation in the Barnacle Amphibalanus amphitrite. Frontiers in Marine Science, 5, https://doi.org/10.3389/fmars.2018.00369
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James C; Gentili, Bernard; Hagens, Mathilde; Hofmann, Andreas; Mueller, Jens-Daniel; Proye, Aurélien; Rae, James; Soetaert, Karline (2019): seacarb: seawater carbonate chemistry with R. R package version 3.2.12. https://CRAN.R-project.org/package=seacarb
https://doi.pangaea.de/10.1594/PANGAEA.922978
https://doi.org/10.1594/PANGAEA.922978
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.92297810.3389/fmars.2018.00369
_version_ 1810469845892857856
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.922978 2024-09-15T18:28:28+00:00 Seawater carbonate chemistry and adhesion and shell formation of the Barnacle Amphibalanus amphitrite Nardone, Jessica A Patel, Shrey Siegel, Kyle R Tedesco, Dana McNicholl, Conall G O'Malley, Jessica Herrick, Jack Metzler, Rebecca A Orihuela, Beatriz Rittschof, Daniel Dickinson, Gary H 2018 text/tab-separated-values, 294 data points https://doi.pangaea.de/10.1594/PANGAEA.922978 https://doi.org/10.1594/PANGAEA.922978 en eng PANGAEA Nardone, Jessica A; Patel, Shrey; Siegel, Kyle R; Tedesco, Dana; McNicholl, Conall G; O'Malley, Jessica; Herrick, Jack; Metzler, Rebecca A; Orihuela, Beatriz; Rittschof, Daniel; Dickinson, Gary H (2018): Assessing the Impacts of Ocean Acidification on Adhesion and Shell Formation in the Barnacle Amphibalanus amphitrite. Frontiers in Marine Science, 5, https://doi.org/10.3389/fmars.2018.00369 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James C; Gentili, Bernard; Hagens, Mathilde; Hofmann, Andreas; Mueller, Jens-Daniel; Proye, Aurélien; Rae, James; Soetaert, Karline (2019): seacarb: seawater carbonate chemistry with R. R package version 3.2.12. https://CRAN.R-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.922978 https://doi.org/10.1594/PANGAEA.922978 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Adhesive strength standard error Alkalinity total standard deviation Amphibalanus amphitrite Animalia Aragonite saturation state Area Arthropoda Atomic disorder Benthic animals Benthos Bicarbonate ion Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite crystal area Calcite saturation state Calcium Calculated using CO2calc Calculated using seacarb after Nisumaa et al. (2010) Calculated using seacarb after Orr et al. (2018) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag dataset 2018 ftpangaea https://doi.org/10.1594/PANGAEA.92297810.3389/fmars.2018.00369 2024-07-24T02:31:34Z Barnacles are dominant members of marine intertidal communities. Their success depends on firm attachment provided by their proteinaceous adhesive and protection imparted by their calcified shell plates. Little is known about how variations in the environment affect adhesion and shell formation processes in barnacles. Increased levels of atmospheric CO2 have led to a reduction in the pH of ocean waters (i.e., ocean acidification), a trend that is expected to continue into the future. Here, we assessed if a reduction in seawater pH, at levels predicted within the next 200 years, would alter physiology, adhesion, and shell formation in the cosmopolitan barnacle Amphibalanus (=Balanus) amphitrite. Juvenile barnacles, settled on silicone substrates, were exposed to one of three static levels of pHT, 8.01, 7.78, or 7.50, for 13 weeks. We found that barnacles were robust to reduced pH, with no effect of pH on physiological metrics (mortality, tissue mass, and presence of eggs). Likewise, adhesive properties (adhesion strength and adhesive plaque gross morphology) were not affected by reduced pH. Shell formation, however, was affected by seawater pH. Shell mass and base plate area were higher in barnacles exposed to reduced pH; barnacles grown at pHT 8.01 exhibited approximately 30% lower shell mass and 20% smaller base plate area as compared to those at pHT 7.50 or 7.78. Enhanced growth at reduced pH appears to be driven by the increased size of the calcite crystals that comprise the shell. Despite enhanced growth, mechanical properties of the base plate (but not the parietal plates) were compromised at the lowest pH level. Barnacle base plates at pHT 7.50 broke more easily and crack propagation, measured through microhardness testing, was significantly affected by seawater pH. Other shell metrics (plate thickness, relative crystallinity, and atomic disorder) were not affected by seawater pH. Hence, a reduction in pH resulted in larger barnacles but with base plates that would crack more readily. It is yet to be ... Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science