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Isotopic variability in the intertidal acorn barnacle Semibalanus balanoides: a potentially novel sea-level proxy indicator

By
K. F. Craven
K. F. Craven
School of Geography and Geosciences, University of St. Andrews, St. Andrews, Fife, KY16 9AJ, Scotland, UK (e-mail: Michael.bird@st-andrews.ac.uk)
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M. I. Bird
M. I. Bird
School of Geography and Geosciences, University of St. Andrews, St. Andrews, Fife, KY16 9AJ, Scotland, UK (e-mail: Michael.bird@st-andrews.ac.uk)
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W. E. N. Austin
W. E. N. Austin
School of Geography and Geosciences, University of St. Andrews, St. Andrews, Fife, KY16 9AJ, Scotland, UK (e-mail: Michael.bird@st-andrews.ac.uk)
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J. Wynn
J. Wynn
School of Geography and Geosciences, University of St. Andrews, St. Andrews, Fife, KY16 9AJ, Scotland, UK (e-mail: Michael.bird@st-andrews.ac.uk)Current address: Department of Geology, University of South Florida, 4202 E Fowler Ave, SCA 528, Tampa, FL 33620, USA
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Published:
January 01, 2008

Abstract

We report variations in the δ13C and δ18O values of barnacle skeletal carbonate as well as the δ13C and δ15N value of tissue from specimens of the acorn barnacle S. balanoides, as a function of elevation within its living range on the Isle of May, Scotland. Individuals were sampled over a 3.50 m range at 0.25 m intervals (1.00–4.50 m above ordnance datum). Carbonate δ18O values (2.44±0.13‰ [1σ], n=45) and tissue δ15N values (8.17±0.42‰, n=15) do not vary systematically with elevation. The δ13C value of shell carbonate increases with elevation by c. 1‰ (total range: −0.77‰ to +0.63‰), but the variability between samples at the same elevation suggests that this relationship will be of limited use in constraining palaeo-elevation. By contrast, tissue δ13C values show systematic variation with elevation, increasing by c. 8‰ (total range: −19.36‰ to −8.77‰) with increasing elevation.

These results suggest that there is potential to use the tissue δ13C values to determine the elevation of a Fixed Biological Indicator (FBI) such as S. balanoides within its living range. If this is also true of the organic matrix of the carbonate skeleton, and if this organic matrix is preserved in Holocene FBIs, then the potential exists to use carbon isotopes to more precisely constrain the palaeo-elevation of FBIs within their living range and hence palaeo sea-level. The small range of carbonate δ18O values suggests that oxygen isotopes in FBIs can be used to constrain water δ18O values if an independent estimate of temperature is available, or temperature if an independent estimate of salinity is available.

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Contents

Geological Society, London, Special Publications

Biogeochemical Controls on Palaeoceanographic Environmental Proxies

W. E. N. Austin
W. E. N. Austin
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R. H. James
R. H. James
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Geological Society of London
Volume
303
ISBN electronic:
9781862395510
Publication date:
January 01, 2008

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