PALAIOS
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


PALAIOS; August 2008; v. 23; no. 8; p. 559-565; DOI: 10.2110/palo.2007.p07-056r
© 2008 SEPM Society for Sedimentary Geology
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Surge, D.
Right arrow Articles by Walker, K. J.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Isotope sclerochronology of Mercenaria mercenaria, M. Campechiensis, and their natural hybrid form: Does genotype matter?

Donna Surge*,1, Ginger Kelly1, William S. Arnold2, Stephen P. Geiger2, Ann E. Goewert1 and Karen Jo Walker3

1 University of North Carolina, Department of Geological Sciences, 104 South Road, Mitchell Hall, Campus Box 3315, Chapel Hill, North Carolina 27599, USA;
2 Fish and Wildlife Research Institute, 100 Eighth Avenue SE, St. Petersburg, Florida 33701, USA;
3 University of Florida, Florida Museum of Natural History, PO Box 117800, Gainesville, Florida 32611, USAdonna64{at}unc.edu

Isotopic variation in northern and southern hard clam (quahog) shells is used in studies including paleoecology, paleoclimatology, and archaeology. It is unknown, however, whether species-specific isotopic differences exist. Three genotypes—Mercenaria mercenaria, M. campechiensis, and their natural hybrid form—are found in coastal Florida waters and differentiation of genotypes can be difficult to determine morphologically. This issue may be problematic when using archaeological shells as paleoclimate archives, because genetic analysis cannot be done on such specimens. Their co-occurrence in coastal Florida waters provides a unique opportunity to study whether all three genotypes of modern individuals record the same environmental information preserved as variation in oxygen and stable carbon isotope ratios. A random sample of 49 individuals collected alive at the same time and from the same locality in Pine Island Sound were classified to genotype using allozyme electrophoresis. Three juveniles from each genotype were selected for isotopic analysis to control for ontogenetic effects. Timing of growth increment formation inferred from oxygen isotope ratios reveals similar overall patterns wherein dark (slow growth) increments formed in mid- to late spring and light (fast growth) increments formed in late fall. Results of the mixed model ANOVA (analysis of variance) indicate that no significant species-related differences exist in the variation of oxygen and carbon isotope ratios, although the Kolmogorov-Smirnov goodness-of-fit test detected a systematic difference among {delta}13C values of M. mercenaria and M. campechiensis comparison and M. mercenaria and the hybrid shell comparison. Any genotype or combination thereof is, thus, suitable for environmental and climate reconstruction using oxygen isotope ratios. The utility of carbon isotope ratios as an environmental proxy, however, remains questionable.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by the SEPM Society for Sedimentary Geology.