Relationship between water and aragonite barium concentrations in aquaria reared juvenile corals

dc.contributor.author Gonneea, Meagan E.
dc.contributor.author Cohen, Anne L.
dc.contributor.author DeCarlo, Thomas M.
dc.contributor.author Charette, Matthew A.
dc.date.accessioned 2017-08-16T14:52:04Z
dc.date.available 2017-08-16T14:52:04Z
dc.date.issued 2017-04-09
dc.description This paper is not subject to U.S. copyright. The definitive version was published in Geochimica et Cosmochimica Acta 209 (2017): 123-134, doi:10.1016/j.gca.2017.04.006. en_US
dc.description.abstract Coral barium to calcium (Ba/Ca) ratios have been used to reconstruct records of upwelling, river and groundwater discharge, and sediment and dust input to the coastal ocean. However, this proxy has not yet been explicitly tested to determine if Ba inclusion in the coral skeleton is directly proportional to seawater Ba concentration and to further determine how additional factors such as temperature and calcification rate control coral Ba/Ca ratios. We measured the inclusion of Ba within aquaria reared juvenile corals (Favia fragum) at three temperatures (∼27.7, 24.6 and 22.5 °C) and three seawater Ba concentrations (73, 230 and 450 nmol kg−1). Coral polyps were settled on tiles conditioned with encrusting coralline algae, which complicated chemical analysis of the coral skeletal material grown during the aquaria experiments. We utilized Sr/Ca ratios of encrusting coralline algae (as low as 3.4 mmol mol−1) to correct coral Ba/Ca for this contamination, which was determined to be 26 ± 11% using a two end member mixing model. Notably, there was a large range in Ba/Ca across all treatments, however, we found that Ba inclusion was linear across the full concentration range. The temperature sensitivity of the distribution coefficient is within the range of previously reported values. Finally, calcification rate, which displayed large variability, was not correlated to the distribution coefficient. The observed temperature dependence predicts a change in coral Ba/Ca ratios of 1.1 μmol mol−1 from 20 to 28 °C for typical coastal ocean Ba concentrations of 50 nmol kg−1. Given the linear uptake of Ba by corals observed in this study, coral proxy records that demonstrate peaks of 10–25 μmol mol−1 would require coastal seawater Ba of between 60 and 145 nmol kg−1. Further validation of the coral Ba/Ca proxy requires evaluation of changes in seawater chemistry associated with the environmental perturbation recorded by the coral as well as verification of these results for Porites species, which are widely used in paleo reconstructions. en_US
dc.description.sponsorship M.E.G. was supported by a NDSEG graduate fellowship. Funding for this research came from the NSF Chemical Oceanography program (OCE-0751525) and the Coastal Ocean Institute, the Ocean and Climate Change Institute and the Ocean Ventures Fund at Woods Hole Oceanographic Institution. en_US
dc.identifier.citation Geochimica et Cosmochimica Acta 209 (2017): 123-134 en_US
dc.identifier.doi 10.1016/j.gca.2017.04.006
dc.identifier.uri https://hdl.handle.net/1912/9163
dc.language.iso en_US en_US
dc.publisher Elsevier en_US
dc.relation.uri https://doi.org/10.1016/j.gca.2017.04.006
dc.subject Coral Ba/Ca en_US
dc.subject Barium en_US
dc.subject Aragonite en_US
dc.subject Distribution coefficient en_US
dc.subject Favia fragum en_US
dc.title Relationship between water and aragonite barium concentrations in aquaria reared juvenile corals en_US
dc.type Article en_US
dspace.entity.type Publication
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relation.isAuthorOfPublication.latestForDiscovery 8e0c3ecf-cf2d-4355-a41d-d55674ae6b6f
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