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Main Authors: Saley, Alisha M, Ninokawa, Aaron, Doan, Abigail, Gaylord, B
Format: Dataset Open Access
Language:en
Published: PANGAEA 2025
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Online Access:https://doi.org/10.1594/PANGAEA.984409
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author Saley, Alisha M
Ninokawa, Aaron
Doan, Abigail
Gaylord, B
author_facet Saley, Alisha M
Ninokawa, Aaron
Doan, Abigail
Gaylord, B
collection Datos científicos de ciencias marinas y ambientales
contents We tested this hypothesis in adult California mussels, Mytilus californianus. We quantified shell dissolution rates as a function of periostracum cover across three levels of reduced pH (7.7, 7.5, and 7.4 on the total scale). Since periostracum can also be eroded over time, we additionally conducted a first-pass examination of whether differing surface textures induced by abrasional processes might influence dissolution rates. We contextualized this set of experiments with measurements of mussel periostracum cover in multiple intertidal habitats. This dataset is included in the OA-ICC data compilation maintained in the framework of the IAEA Ocean Acidification International Coordination Centre (see https://oa-icc.ipsl.fr). Original data were downloaded from Biological and Chemical Oceanography Data Management Office (see Source) by the OA-ICC data curator. In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2024) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2025-08-19.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_984409
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle Seawater carbonate chemistry and influence of periostracum cover, pH and simulated abrasion of periostracum on external shell dissolution at Marshall Gulch Beach, CA
Saley, Alisha M
Ninokawa, Aaron
Doan, Abigail
Gaylord, B
Alkalinity, total; Animalia; Aragonite saturation state; Area; Benthic animals; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Change in alkalinity, total; Coast and continental shelf; Coverage; Date/time end, experiment; Date/time start, experiment; Dissolution rate; Dissolution rate, normalized to individual shell area; Duration; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Incubation duration; Laboratory experiment; Length; Marshall_Gulch; Method comment; Mollusca; Mytilus californianus; North Pacific; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH, total scale; Salinity; Single species; Species, unique identification; Species, unique identification (Semantic URI); Species, unique identification (URI); Spectrophotometric; Temperate; Temperature, water; Treatment; Type of study; Width
We tested this hypothesis in adult California mussels, Mytilus californianus. We quantified shell dissolution rates as a function of periostracum cover across three levels of reduced pH (7.7, 7.5, and 7.4 on the total scale). Since periostracum can also be eroded over time, we additionally conducted a first-pass examination of whether differing surface textures induced by abrasional processes might influence dissolution rates. We contextualized this set of experiments with measurements of mussel periostracum cover in multiple intertidal habitats. This dataset is included in the OA-ICC data compilation maintained in the framework of the IAEA Ocean Acidification International Coordination Centre (see https://oa-icc.ipsl.fr). Original data were downloaded from Biological and Chemical Oceanography Data Management Office (see Source) by the OA-ICC data curator. In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2024) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2025-08-19.
title Seawater carbonate chemistry and influence of periostracum cover, pH and simulated abrasion of periostracum on external shell dissolution at Marshall Gulch Beach, CA
topic Alkalinity, total; Animalia; Aragonite saturation state; Area; Benthic animals; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Change in alkalinity, total; Coast and continental shelf; Coverage; Date/time end, experiment; Date/time start, experiment; Dissolution rate; Dissolution rate, normalized to individual shell area; Duration; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Incubation duration; Laboratory experiment; Length; Marshall_Gulch; Method comment; Mollusca; Mytilus californianus; North Pacific; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH, total scale; Salinity; Single species; Species, unique identification; Species, unique identification (Semantic URI); Species, unique identification (URI); Spectrophotometric; Temperate; Temperature, water; Treatment; Type of study; Width
url https://doi.org/10.1594/PANGAEA.984409