Growth rate and age effects on Mya arenaria shell chemistry: Implications for biogeochemical studies

dc.contributor.author Strasser, Carly A.
dc.contributor.author Mullineaux, Lauren S.
dc.contributor.author Walther, Benjamin D.
dc.date.accessioned 2008-04-24T12:33:20Z
dc.date.available 2008-04-24T12:33:20Z
dc.date.issued 2008-01-30
dc.description This paper is not subject to U.S. copyright. The definitive version was published in Journal of Experimental Marine Biology and Ecology 355 (2008): 153-163, doi:10.1016/j.jembe.2007.12.022. en
dc.description.abstract The chemical composition of bivalve shells can reflect that of their environment, making them useful indicators of climate, pollution, and ecosystem changes. However, biological factors can also influence chemical properties of biogenic carbonate. Understanding how these factors affect chemical incorporation is essential for studies that use elemental chemistry of carbonates as indicators of environmental parameters. This study examined the effects of bivalve shell growth rate and age on the incorporation of elements into juvenile softshell clams, Mya arenaria. Although previous studies have explored the effects of these two biological factors, reports have differed depending on species and environmental conditions. In addition, none of the previous studies have examined growth rate and age in the same species and within the same study. We reared clams in controlled laboratory conditions and used solution-based inductively coupled plasma mass spectrometry (ICP-MS) analysis to explore whether growth rate affects elemental incorporation into shell. Growth rate was negatively correlated with Mg, Mn, and Ba shell concentration, possibly due to increased discrimination ability with size. The relationship between growth rate and Pb and Sr was unresolved. To determine age effects on incorporation, we used laser ablation ICP-MS to measure changes in chemical composition across shells of individual clams. Age affected incorporation of Mn, Sr, and Ba within the juvenile shell, primarily due to significantly different elemental composition of early shell material compared to shell accreted later in life. Variability in shell composition increased closer to the umbo (hinge), which may be the result of methodology or may indicate an increased ability with age to discriminate against ions that are not calcium or carbonate. The effects of age and growth rate on elemental incorporation have the potential to bias data interpretation and should be considered in any biogeochemical study that uses bivalves as environmental indicators. en
dc.description.sponsorship This work was supported by NSF project numbers OCE-0241855 and OCE-0215905. en
dc.format.mimetype application/pdf
dc.identifier.citation Journal of Experimental Marine Biology and Ecology 355 (2008): 153-163 en
dc.identifier.doi 10.1016/j.jembe.2007.12.022
dc.identifier.uri https://hdl.handle.net/1912/2175
dc.language.iso en_US en
dc.publisher Elsevier B.V. en
dc.relation.uri https://doi.org/10.1016/j.jembe.2007.12.022
dc.subject Bivalve shell en
dc.subject Carbonate chemistry en
dc.subject Element incorporation en
dc.subject Growth rate en
dc.subject Mya arenaria en
dc.title Growth rate and age effects on Mya arenaria shell chemistry: Implications for biogeochemical studies en
dc.type Article en
dspace.entity.type Publication
relation.isAuthorOfPublication 97ae02eb-b123-4e0f-a3ff-b98e2d697d2f
relation.isAuthorOfPublication 86a10919-a4eb-48b5-9661-c83604cba589
relation.isAuthorOfPublication b0d7c106-f800-4a0f-9e52-702197bb4ec4
relation.isAuthorOfPublication.latestForDiscovery 97ae02eb-b123-4e0f-a3ff-b98e2d697d2f
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