Temperature dependence of oxygen-18 concentration in reef coral carbonates
- 20 January 1972
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 77 (3), 463-473
- https://doi.org/10.1029/jc077i003p00463
Abstract
Oxygen isotope ratios in the aragonite precipitated by the scleractinian reef-building corals indicate that the skeletal carbonate is not in isotopic equilibrium with the sea water of the reef environment in which the corals grew. Despite this apparent isotopic disequilibrium, values are temperature dependent. The $xsO versus temperature curves for various coral genera are parallel or nearly parallel to the isotopic 'paleotemperature scale' established by Epstein et aJ. (1953) but in each case the curves are displaced toward lower xsO/X60 ratios at a given temperature. Regression coefficients for 44 genera have been determined. These findings suggest that if skeletal carbonate is derived from both sea-water bicarbonate and metabolic carbon dioxide, the relative proportions contributed by each of these two sources of carbon and oxygen are essentially constant for a given genus, but are different from one genus to another. Thus it is possible that isotopic composition can indicate relative excretory efficiency and that stable isotope ratios can be of considerable value in elucidating some of the processes involved in reef coral development. Epstein et al. [1951, 1953] demonstrated that the skeletal carbonates of some marine invertebrates, molluscs for example, have the same oxygen isotopic composition as CaC08 precipitated inorganically from sea water at the same temperature and under conditions of isotopic equilibrium. Although the octocoral Heliopora and some hydrozoan corals appear to secrete calcium carbonate in isotopic equilibrium with sea water [Weber and Woodhead, 1971], the scleractinian corals have been found to have variable isotope ratios. Some unknown physiological process was proposed by Epstein et al. [1951] to account for the apparent isotopic disequilibrium. A model for carbon and oxygen isotope fractionation in the calcification of corals was developed by Weber and Woodhead [1970] to serve as a preliminary working hypothesis for explaining the variability of 8C/C and 0/60 ratios in a large collection of specimens from a single reef at Heron Island, Australia. Among the implications of the model is that the 80 of reef-building corals will be temperature dependent, despite apparent isoCopyright ¸ 1972 by the American Geophysical Union. topic disequilibrium between the skeletal carbonate and ambient sea water. The purpose of the study reported here is to verify this prediction with analyses of corals collected over a wide range of environmental temperatures. The significance of the results is then considered in terms of relative metabolic efficiency.Keywords
This publication has 12 references indexed in Scilit:
- The Last Interglacial: Paleotemperatures and ChronologyScience, 1971
- Incorporation of Metabolic CO2 into Coral SkeletonNature, 1970
- Mass spectrometer correction factors for the determination of small isotopic composition variations of carbon and oxygenInternational Journal of Mass Spectrometry and Ion Physics, 1970
- Carbon isotope fractionation during the precipitation of calcium carbonateEarth and Planetary Science Letters, 1970
- Abyssal carbon 13 in the South PacificJournal of Geophysical Research, 1970
- CALCIUM CARBONATE DEPOSITION BY CORALLINE ALGAE AND CORALS IN RELATION TO THEIR ROLES AS REEF‐BUILDERSAnnals of the New York Academy of Sciences, 1963
- Chapter 10: Carbonates and Carbon DioxidePublished by Geological Society of America ,1957
- REVISED CARBONATE-WATER ISOTOPIC TEMPERATURE SCALEGSA Bulletin, 1953
- CARBONATE-WATER ISOTOPIC TEMPERATURE SCALEGSA Bulletin, 1951
- On the Isotopic Chemistry of Carbonates and a Paleotemperature ScaleThe Journal of Chemical Physics, 1950