Penn Arts & Sciences Logo

Pre-treatment effects on coral skeletal delta C-13 and delta O-18

Authors: 
Grottoli, A. G., Rodrigues, L. J., Matthews, K. A., Palardy, J. E., Gibb, O. T.
Year: 
2 005
Source: 
Chemical Geology
Abstract: 
Pre-treatments are often used to remove organic "contaminant" material prior to isotopic analyses of coral skeletal samples. Here we conducted three experiments to test the pre-treatment effect of water, 30% hydrogen peroxide (H2O2), and household bleach [5.25% sodium hypochlorite (NaClO3) and 0.15% sodium hydroxide (NaOH)], on the stable isotopic composition of coral skeletal samples. First, using a mass balance approach we calculated the expected change in skeletal delta C-13 due to the removal of all organic carbon. The model showed that (1) the removal of organic carbon (which has a low delta C-13 value relative to skeletal delta C-13) from the skeletal sample should theoretically result in a higher delta C-13 value of the remaining organic-carbon-free carbonate, and that (2) only at the highest concentrations of skeletal organic carbon within the tissue layer of corals is the contribution of the organic carbon to the overall delta C-13 skeletal value potentially large enough to be detectable by mass spectrometry. We then conducted two sets of experiments to test the model where we pre-treated a large number of skeletal samples from five species of corals with water, H2O2, bleach, or no pre-treatment for 24 h. Skeletal delta C-13 generally decreased significantly with water, bleach, and H2O2 pre-treatments which is contrary to the model-predicted increase in delta C-13 following such pre-treatments. Thus, organic carbon within the skeleton is not a nets source of contamination to delta C-13 analyses. Skeletal delta O-13 decreased the most with water and bleach pre-treatments. In addition, the effect of H2O2 or bleach pre-treatments on either delta C-13 or delta O-18 was not consistent among species or locations. The direction of change in delta C-13 and delta O-18 with pre-treatments was no different for skeletal samples taken within or below the tissue layer. Based on our results, we suggest that pre-treatment is not necessary and recommend that pre-treatment not be performed on coral skeletal samples prior to stable isotope analysis to avoid any pre-treatment-induced variability that could significantly compromise inter-colony and inter-species comparisons. (c) 2005 Elsevier B.V. All rights reserved.
EES Authors: 
Lisa Rodrigues
Kathryn Matthews
Research Track Category: 

Department of Earth and Environmental Science / University of Pennsylvania, 251 Hayden Hall, 240 South 33rd Street, Philadelphia, PA 19104-6316