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Ocean Acidification Has Multiple Modes of Action on Bivalve Larvae

Ocean acidification (OA) is altering the chemistry of the world’s oceans at rates unparalleled in the past roughly 1 million years. Understanding the impacts of this rapid change in baseline carbonate chemistry on marine organisms needs a precise, mechanistic understanding of physiological responses...

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Autores principales: Waldbusser, George G., Hales, Burke, Langdon, Chris J., Haley, Brian A., Schrader, Paul, Brunner, Elizabeth L., Gray, Matthew W., Miller, Cale A., Gimenez, Iria, Hutchinson, Greg
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2015
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4465621/
https://www.ncbi.nlm.nih.gov/pubmed/26061095
http://dx.doi.org/10.1371/journal.pone.0128376
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author Waldbusser, George G.
Hales, Burke
Langdon, Chris J.
Haley, Brian A.
Schrader, Paul
Brunner, Elizabeth L.
Gray, Matthew W.
Miller, Cale A.
Gimenez, Iria
Hutchinson, Greg
author_facet Waldbusser, George G.
Hales, Burke
Langdon, Chris J.
Haley, Brian A.
Schrader, Paul
Brunner, Elizabeth L.
Gray, Matthew W.
Miller, Cale A.
Gimenez, Iria
Hutchinson, Greg
author_sort Waldbusser, George G.
collection PubMed
description Ocean acidification (OA) is altering the chemistry of the world’s oceans at rates unparalleled in the past roughly 1 million years. Understanding the impacts of this rapid change in baseline carbonate chemistry on marine organisms needs a precise, mechanistic understanding of physiological responses to carbonate chemistry. Recent experimental work has shown shell development and growth in some bivalve larvae, have direct sensitivities to calcium carbonate saturation state that is not modulated through organismal acid-base chemistry. To understand different modes of action of OA on bivalve larvae, we experimentally tested how pH, P(CO2), and saturation state independently affect shell growth and development, respiration rate, and initiation of feeding in Mytilus californianus embryos and larvae. We found, as documented in other bivalve larvae, that shell development and growth were affected by aragonite saturation state, and not by pH or P(CO2). Respiration rate was elevated under very low pH (~7.4) with no change between pH of ~ 8.3 to ~7.8. Initiation of feeding appeared to be most sensitive to P(CO2), and possibly minor response to pH under elevated P(CO2). Although different components of physiology responded to different carbonate system variables, the inability to normally develop a shell due to lower saturation state precludes pH or P(CO2) effects later in the life history. However, saturation state effects during early shell development will carry-over to later stages, where pH or P(CO2) effects can compound OA effects on bivalve larvae. Our findings suggest OA may be a multi-stressor unto itself. Shell development and growth of the native mussel, M. californianus, was indistinguishable from the Mediterranean mussel, Mytilus galloprovincialis, collected from the southern U.S. Pacific coast, an area not subjected to seasonal upwelling. The concordance in responses suggests a fundamental OA bottleneck during development of the first shell material affected only by saturation state.
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spelling pubmed-44656212015-06-25 Ocean Acidification Has Multiple Modes of Action on Bivalve Larvae Waldbusser, George G. Hales, Burke Langdon, Chris J. Haley, Brian A. Schrader, Paul Brunner, Elizabeth L. Gray, Matthew W. Miller, Cale A. Gimenez, Iria Hutchinson, Greg PLoS One Research Article Ocean acidification (OA) is altering the chemistry of the world’s oceans at rates unparalleled in the past roughly 1 million years. Understanding the impacts of this rapid change in baseline carbonate chemistry on marine organisms needs a precise, mechanistic understanding of physiological responses to carbonate chemistry. Recent experimental work has shown shell development and growth in some bivalve larvae, have direct sensitivities to calcium carbonate saturation state that is not modulated through organismal acid-base chemistry. To understand different modes of action of OA on bivalve larvae, we experimentally tested how pH, P(CO2), and saturation state independently affect shell growth and development, respiration rate, and initiation of feeding in Mytilus californianus embryos and larvae. We found, as documented in other bivalve larvae, that shell development and growth were affected by aragonite saturation state, and not by pH or P(CO2). Respiration rate was elevated under very low pH (~7.4) with no change between pH of ~ 8.3 to ~7.8. Initiation of feeding appeared to be most sensitive to P(CO2), and possibly minor response to pH under elevated P(CO2). Although different components of physiology responded to different carbonate system variables, the inability to normally develop a shell due to lower saturation state precludes pH or P(CO2) effects later in the life history. However, saturation state effects during early shell development will carry-over to later stages, where pH or P(CO2) effects can compound OA effects on bivalve larvae. Our findings suggest OA may be a multi-stressor unto itself. Shell development and growth of the native mussel, M. californianus, was indistinguishable from the Mediterranean mussel, Mytilus galloprovincialis, collected from the southern U.S. Pacific coast, an area not subjected to seasonal upwelling. The concordance in responses suggests a fundamental OA bottleneck during development of the first shell material affected only by saturation state. Public Library of Science 2015-06-10 /pmc/articles/PMC4465621/ /pubmed/26061095 http://dx.doi.org/10.1371/journal.pone.0128376 Text en © 2015 Waldbusser et al http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are properly credited.
spellingShingle Research Article
Waldbusser, George G.
Hales, Burke
Langdon, Chris J.
Haley, Brian A.
Schrader, Paul
Brunner, Elizabeth L.
Gray, Matthew W.
Miller, Cale A.
Gimenez, Iria
Hutchinson, Greg
Ocean Acidification Has Multiple Modes of Action on Bivalve Larvae
title Ocean Acidification Has Multiple Modes of Action on Bivalve Larvae
title_full Ocean Acidification Has Multiple Modes of Action on Bivalve Larvae
title_fullStr Ocean Acidification Has Multiple Modes of Action on Bivalve Larvae
title_full_unstemmed Ocean Acidification Has Multiple Modes of Action on Bivalve Larvae
title_short Ocean Acidification Has Multiple Modes of Action on Bivalve Larvae
title_sort ocean acidification has multiple modes of action on bivalve larvae
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4465621/
https://www.ncbi.nlm.nih.gov/pubmed/26061095
http://dx.doi.org/10.1371/journal.pone.0128376
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