Ba/Ca of stylasterid coral skeletons records dissolved seawater barium concentrations
Kershaw, James; Stewart, Joseph A.; Strawson, Ivo; de Carvalho Ferreira, Maria Luiza; Robinson, Laura F.; Hendry, Katharine R. ORCID: https://orcid.org/0000-0002-0790-5895; Samperiz, Ana; Burke, Andrea; Rae, James W.B.; Day, Rusty D.; Etnoyer, Peter J.; Williams, Branwen; Häussermann, Vreni. 2023 Ba/Ca of stylasterid coral skeletons records dissolved seawater barium concentrations. Chemical Geology, 622, 121355. 15, pp. https://doi.org/10.1016/j.chemgeo.2023.121355
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© 2023 The Authors. Published by Elsevier B.V. 1-s2.0-S0009254123000554-main.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (9MB) | Preview |
Abstract/Summary
The concentration of dissolved barium in seawater ([Ba]SW) is influenced by both primary productivity and ocean circulation patterns. Reconstructing past subsurface [Ba]SW can therefore provide important information on processes which regulate global climate. Previous Ba/Ca measurements of scleractinian and bamboo deep-sea coral skeletons exhibit linear relationships with [Ba]SW, acting as archives for past Ba cycling. However, skeletal Ba/Ca ratios of the Stylasteridae – a group of widely distributed, azooxanthellate, hydrozoan coral – have not been previously studied. Here, we present Ba/Ca ratios of modern stylasterid (aragonitic, calcitic and mixed mineralogy) and azooxanthellate scleractinian skeletons, paired with published proximal hydrographic data. We find that [Ba]SW and sample mineralogy are the primary controls on stylasterid Ba/Ca, while seawater temperature exerts a weak secondary control. [Ba]SW also exerts a strong control on azooxanthellate scleractinian Ba/Ca. However, Ba-incorporation into scleractinian skeletons varies between locations and across depth gradients, and we find a more sensitive relationship between scleractinian Ba/Ca and [Ba]SW than previously reported. Paired Sr/Ca measurements suggest that this variability in scleractinian Ba/Ca may result from the influence of varying degrees of Rayleigh fractionation during calcification. We find that these processes exert a smaller influence on Ba-incorporation into stylasterid coral skeletons, a result consistent with other aspects of their skeletal geochemistry. Stylasterid Ba/Ca ratios are therefore a powerful, novel archive of past changes in [Ba]SW, particularly when measured in combination with temperature sensitive tracers such as Li/Mg or Sr/Ca. Indeed, with robust [Ba]SW and temperature proxies now established, stylasterids have the potential to be an important new archive for palaeoceanographic studies.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | https://doi.org/10.1016/j.chemgeo.2023.121355 |
ISSN: | 00092541 |
Additional Keywords: | Ba/Ca, Barium, Scleractinia, Stylasteridae, Coral |
Date made live: | 27 Feb 2023 11:43 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/534087 |
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