The Origin of Variations in the Isotopic Record of Scleractinian Corals: II. Carbon

Authors

Peter Koenraad Swart, University of Miami
J. J. Leder, University of Miami
Alina Szmant, University of Miami
Richard E. Dodge (editor), Nova Southeastern UniversityFollow

Document Type

Article

Publication Date

8-1996

Publication Title

Geochimica et Cosmochimica Acta

Keywords

Coral reefs, Montastraea annularis

ISSN

0016-7037

Volume

60

Issue/No.

15

First Page

2871

Last Page

2885

Abstract

This study examines the relationship between the δ¹³C of the skeleton of a zooxanthellate coral (Montastraea annularis) growing on the Florida Reef Tract and environmental variables (insolation and temperature), physiological variables (growth rate, respiration, calcification, and photosynthesis). Colonies of this species were grown in the field for a 2.5 year study period, during which the rates of photosynthesis, respiration, and calcification were measured on fifteen separate occasions, spaced approximately equally throughout the study period. The corals were stained with alizarin-red S within seven days after each set of physiological measurements. At the end of the period the corals were sacrificed and their skeletal extension, density, and skeletal δ¹³C determined. Despite substantial high-frequency variations, a strong seasonal cycle was evident in the skeletal δ¹³C records of all the corals throughout the experimental period. The skeletal δ¹³C and δ¹⁸O values varied approximately in phase, and showed a weak, but statistically significant positive relationship with each other. The δ¹³C of the coral skeletons, when corrected for changes in the δ¹³C of dissolved inorganic carbon (DIC), exhibited an inverse correlation with P/R, a finding opposite to what was expected based on current models of isotopic fractionation in coral skeletons. Although such findings tend to support the model of Erez (1978) that increases in photosynthesis act to isotopically deplete the δ¹³C of the coral skeleton, we note that the inverse association between δ¹³C and P/R arises because of a slight positive association between δ¹³C and respiration. We therefore believe that the association may be a result of seasonal variation in some parameters of the system which was not constrained in our study. Alternatives include (1) variations in the δ¹³C of the DIC which are translated into the δ¹³C of the food chain, (2) changes from heterotrophy to autotrophy, and (3) changes in the partitioning of δ¹³C between the zooxanthellae and the coral tissue. Based on previous studies which we have carried out we believe that changes in the skeletal δ¹³C are not related to sexual reproduction or growth rate. Contrary to previous work we were unable to measure any significant differences in the skeletal δ¹³C between the fast growing tops of the coral and the slower growing sides.

Comments

©1996 Elsevier Science Ltd.

Additional Comments

NSF grant #s: OCE-8900005, OCE-8907101

NSUWorks Citation

Swart, P. K., J. J. Leder, A. M. Szmant, and R. E. Dodge. "The origin of variations in the isotopic record of scleractinian corals: II. Carbon." Geochimica et Cosmochimica Acta 60, no. 15 (1996): 2871-2885.

DOI

10.1016/0016-7037(96)00119-6