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Published byAshlie Rodgers Modified over 6 years ago
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Impact of ocean acidification on calcification rate, shell properties, pallial fluid pH, and epigenetics of commercially important mollusks across critical life stages Justin B. Ries Carolina Bastidas (co-PI) Katie Lotterhos (collaborator) Louise Cameron (graduate student) Northeastern University
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OBJECTIVE: To investigate the vulnerability of commercially important calcifying marine mollusks to ocean acidification at various stages of their life history. PROJECTS: Impact of OA and warming on calcification rate and shell properties of larval-stage limpets (Crepidula fornicata); Impact of OA and warming on calcification rate, shell properties, pallial fluid pH, and proteomics of adult sea scallops (Placopecten magellanicus); and Impact of OA on calcification rate, shell properties, and epigenetics of juvenile- and larval-stage eastern oysters (Crassostrea virginica).
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Project 1: Impact of OA and warming on limpet calcification
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Project 1: Impact of OA and warming on limpet calcification
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Project 1: Impact of OA and warming on limpet calcification
aragonite Calcification rate (wt-% per day) 2850 ppm 900 ppm 600 ppm 400 ppm pCO2 = 2850 ppm pCO2 = 400 ppm 1 mm 1 mm
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in calcification response to OA?
Role of dissolution in calcification response to OA? Gross Calcification (beneath tissue) – Gross Dissolution (of exposed skeleton) Net Calcification
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Ries, 2016, GCA
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Project 2: Impact of OA on scallop pallial fluid pH and calcification
ΩAragonite
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Project 2: Impact of OA on scallop pallial fluid pH and calcification
Photo credit: Louise Cameron (graduate student)
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Project 2: Impact of OA on scallop pallial fluid pH and calcification
Photo credit: Louise Cameron (graduate student)
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Ωaragonite Ωaragonite Ωaragonite Positive Calcification rate Parabolic
high CO2 ambient CO2 Calcification rate Ωaragonite Parabolic high CO2 ambient CO2 Calcification rate Ωaragonite Calcification rate Negative high CO2 ambient CO2 Ries, 2011, GCA
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Project 3: Impact of OA on calcification and epigenetics of oysters
(1) Does OA induce adaptive modifications to gene activity without alterating the underlying DNA sequence (e.g., via DNA methylation)? (2) Are these modifications heritable and, thus, a mechanism for rapidly evolving in response to OA? Collaboration with Katie Lotterhos
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Whole shell Internal view
Low pCO2 Moderate pCO2 High pCO2 A 2 mm 5 mm 500 µm 20 µm 5 µm B C Whole shell Internal view D E F Whole shell External view G H I Shell edge External view J K L Crystal structure Prismatic layer M N O Crystal structure Foliated layer
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Biomechanical Analyses
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Summary: Initial results suggest that early-life-stage mollusks exhibit variable degrees of resilience to moderate levels of CO2-induced ocean acidification (700 – 1000 ppm), but converge on a nonlinear (exponential) increase in vulnerability to more extreme acidification (2000 – 3000 ppm) Ongoing microelectrode studies of pallial fluid pH, coupled with targeted epigenetic and proteomic studies, aim to identify the mechanism(s) behind this non-linearity in mollusks’ response to ocean acidification at various stages of development.
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