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MEPS 166:109-118 (1998)
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Abstract
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Seasonal variation in skeletal extension rate and stable isotopic (13C/12C and 18O/16O) composition in response to several environmental variables in the Caribbean reef coral Siderastrea siderea
Héctor M. Guzmán1,*, Alexander W. Tudhope2
1Smithsonian Tropical Research Institute, Unit 0948, APO. AA 34002-0948, USA 2Department of Geology and Geophysics, Edinburgh University, Edinburgh EH9 3JW, Scotland, UK
*E-mail: guzmanh@naos.si.edu

ABSTRACT: The potential of the massive reef building coral Siderastrea siderea to be a reliable archive of past environmental variations was investigated by means of a field experiment conducted on a fringing reef in Panama. Over a 14 mo experimental period,
5 closely spaced and shallow subtidal coral colonies were cored at 1 mo intervals. These cores were subsequently analysed to determine linear extension (growth) and the d13C and d18O of each monthly growth increment. Environmental conditions were recorded continuously by instruments deployed within a distance of 10 to 110 m from the corals. The environmental variables sea surface temperature (SST), salinity, wind, sun and rainfall
were all well correlated with one another, reflecting the dominant seasonal cycle in the region. Of the 3 skeletal attributes considered in this study, skeletal d18O showed the strongest correlation with this seasonal
cycle. The seasonal variations in skeletal d18O are attributed to changes in SST (accounting for ca 60% of the d18O signal) and inferred changes in water isotopic composition due
to rainfall and runoff (ca 40% of the d18O signal). Although these results indicate that this coral is capable of yielding high-resolution paleoenvironmental records from retrospective analysis of the skeleton, there
were significant and unexplained between-colony differences in mean d18O. Therefore, for this species of coral in this setting, great care must be taken before interpreting the regional environmental significance of
either gradual changes in mean d18O through the length of a single long coral core, or differences between modern and ancient (fossil) colonies. Although skeletal d13C and growth
rate did show some relatively weak but significant correlations with some of the environmental variables, especially when the records from all colonies were combined, it was concluded that these attributes have relatively low potential for regional
paleoenvironmental reconstruction.
KEY WORDS: Coral skeleton · Stable isotopes · Panama · Reefs

Published in MEPS Vol.
166
(1998) on May 28
ISSN: 0171-8630.
Copyright © Inter-Research, Oldendorf/Luhe, 1998
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