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dc.contributor.authorNardone, Jessica
dc.contributor.authorPatel, Shrey
dc.contributor.authorSiegel, Kyle
dc.contributor.authorTedesco, Dana
dc.contributor.authorMcNicholl, Conall G.
dc.contributor.authorO'Malley, Jessica
dc.contributor.authorHerrick, Jack
dc.contributor.authorMetzler, Rebecca A.
dc.contributor.authorOrihuela, Beatriz
dc.contributor.authorRittschof, Daniel
dc.contributor.authorDickinson, Gary H.
dc.date.accessioned2022-08-16T15:15:13Z
dc.date.available2022-08-16T15:15:13Z
dc.date.issued2018-10-22
dc.identifier.citationNardone, J. A., Patel, S., Siegel, K. R., Tedesco, D., McNicholl, C. G., O'Malley, J., Herrick, J., Metzler, R. A., Orihuela, B., Rittschof, D. & Dickinson, G. H. (2018). Assessing the impacts of ocean acidification on adhesion and shell formation in the barnacle Amphibalanus amphitrite. Frontiers in Marine Science, 5, 369.en_US
dc.identifier.urihttps://doi.org/10.3389/fmars.2018.00369
dc.identifier.urihttp://dr.tcnj.edu/handle/2900/4034
dc.descriptionDepartment of Biologyen_US
dc.description.abstractBarnacles 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 determined if such changes would alter the survival of A. amphitrite in the field, but changes in the abundance of this ecologically dominant species would undoubtedly affect the composition of biofouling communities.en_US
dc.language.isoen_USen_US
dc.publisherFrontiersen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subjectBiomineralizationen_US
dc.subjectClimate changesen_US
dc.subjectMechanical propertiesen_US
dc.subjectBiofoulingen_US
dc.subjectCementen_US
dc.subjectAdhesive tenacityen_US
dc.subjectCalciteen_US
dc.subjectBalanusen_US
dc.titleAssessing the impacts of ocean acidification on adhesion and shell formation in the barnacle Amphibalanus amphitriteen_US
dc.typeArticleen_US
dc.typeTexten_US
prism.publicationNameFrontiers in Marine Scienceen_US
prism.volume5
prism.startingPage1
prism.endingPage13


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