Abstract
X-radiography and carbon and oxygen stable isotope analysis have been used to examine the effects of prolonged “bleaching” on the growth rate and chemical composition of the skeleton of the massive reef coral, Montastrea annularis. The post-bleaching linear growth of one colony that remained bleached for 10 to 12 months following the 1987 Caribbean-wide bleaching event was only 37% of mean annual growth from pre-bleaching years, and was manifest as a loss of the following year's low density band. Two colonies that did not bleach (normal) and two that bleached and regained their coloration (recovered) had linear growth rates over the same period that were 81 to 98% of mean pre-bleaching annual growth. Linear growth by a third recovered coral was 66% of pre-bleaching growth. No sub-annual stress bands were associated with the bleaching. The skeleton of the bleached colony had carbon and oxygen isotopic compositions that were reduced in range and enriched (increased) in both 13C and 18O in the post-bleaching year. The skeletons of two of the nine colonies, one bleached and one recovered, had depleted (reduced) δ18O values (-5.3 and -4.8%., respectively) during the bleaching episode that agree with the suggestion that positive temperature anomalies occurred during, and may have caused, the bleaching event. The range and values for all other normal and recovered corals, however, were not different between the post-bleaching year and previous years. Our data suggest that stress bands and isotopic analysis of coral skeletons may not always be reliable tools for examining the occurrence, cause or effects of certain discrete stress events that may interrupt skeletal growth.
Similar content being viewed by others
References
Aharon P (in press) Recorders of reef environment histories: stable isotopes in corals, giant clams, and calcareous algae. Coral Reefs
Barnes DJ, Taylor DL (1975) In situ studies of calcification and photosynthetic carbon fixation in the coral Montastrea annularis. Helgol Wiss Meeresunters 24:284–291
Buddemeier RW (1978) Coral growth: retrospective analysis. In: Stoddart DR, Johannes RE (eds) Coral reefs: research methods. UNESCO, pp 523–527
Buddemeier RW, Kinzie RA (1976) Coral growth. Oceanogr Mar Biol Annu Rev 14:183–225
Carriquiry JD, Risk MJ, Schwarcz HP (1988) Timing and temperature record from stable isotopes of the 1982–1983 El Nino warming event in Eastern Pacific corals. Palaios 3:359–369
Chalker BE (1981) Simulating light-saturation curves for photosynthesis and calcification for reef-building corals. Mar Biol 63:135–141
Chalker BE, Taylor DL (1978) Rhythmic variations in calcification and photosynthesis associated with the coral Acropora cervicornis (Lamarck). Proc R Soc London Ser B 201:179–189
Craig H (1957) Isotopic standards for carbon and oxygen and correction factors for mass-spectrometric analysis of carbon dioxide. Geochim Cosmochim Acta 12:133–149
Dodge RE, Lang JC (1983) Environmental correlates of hermatypic coral (Montastrea annularis) growth on the East Flower Gardens Bank, northwest Gulf of Mexico. Limnol Oceanogr 28:228–240
Emiliani C, Hudson JH, Shinn EA, George RY (1978) Oxygen and carbon isotopic growth record in a reef coral from the Florida Keys and a deep-sea coral from Blake Plateau. Science 202:627–629
Epstein S, Buchsbaum HA, Lowenstam HA, Urey HC (1953) Revised carbonate-water isotopic temperature scale. Geol Soc Am Bull 64:1315–1326
Fairbanks RG, Dodge RE (1979) Annual periodicity of the 18O/16O and 13C/12C ratios in the coral Montastrea annularis. Geochim Cosmochim Acta 3:1009–1020
Goreau TJ (1977a) Carbon metabolism in calcifying and photosynthetic organisms: theoretical models based on stable isotope data. Proc 3rd Int Coral Reef Symp 2:395–401
Goreau TJ (1977b) Seasonal variations of trace metals and stable isotopes in coral skeletons: physiological and environmental controls. Proc 3rd Int Coral Reef Symp 2:425–430
Goreau TJ, Macfarlane AH (1990) Reduced growth rate of Montastrea annularis following the 1987–1988 coral-bleaching event. Coral Reefs 8:211–215
Houck JE (1978) The potential utilization of coral skeletons in the study of marine environments. Ph D dissertation, University of Hawaii, Honolulu, 292 pp
Hudson JH (1981) Growth rates in Montastrea annularis: a recording of environmental change, Key Largo Coral Reef Marine Sanctuary, Florida. Bull Mar Sci 31:444–459
Hudson JH (1988) Coral bleaching at Looe Key National Marine Sanctuary, Florida. In: Ogden J, Wicklund R (eds) Mass bleaching of coral reefs in the Caribbean: a research strategy. NOAA National Undersea Research Program (Res Rept 88-2:22–23)
Hudson JH, Shinn EA, Halley RB, Lidz B (1976) Sclereochronology: a tool for interpreting past environments. Geology 4:361–364
Jaap WC (1985) An epidemic zooxanthellae expulsion during 1983 in the lower Florida Keys: hypothermic etiology. Proc 5th Int Coral Reef Symp 6:143–148
Jaap WC (1988) The 1987 zooxanthellae expulsion event at Florida reefs. In: Ogden J, Wicklund R (eds) Mass bleaching of coral reefs in the Caribbean: a research strategy. NOAA Nat Undersea Res Prog (Res Rept 88-2:24–29)
Jacques TG, Marshall N, Pilson MEQ (1983) Experimental ecology of the temperate scleractinian coral Astrangia danae. II. Effect of temperature, light intensity, and symbiosis with zooxanthellae. Mar Biol 76:136–148
Knutson DW, Buddemeier RW, Smith SV (1972) Coral chronometers: seasonal growth bands in reef corals. Science 177:270–272
Land LS, Lang JC, Barnes DJ (1975) Extension rate: a primary control on the isotopic composition of West Indian (Jamaican) scleractinian reef coral skeletons. Mar Biol 33:221–233
Land LS, Lang JC; Barnes DJ (1977) On the stable carbon and oxygen isotopic composition of some shallow water, ahermatypic, scleractinian coral skeletons. Geochim Cosmochim Acta 41:169–172
McConnaughey TA (1986) Oxygen and carbon isotope disequilibria in Galapagos corals: isotopic thermometry and calcification physiology. Ph D dissertation, University of Washington, 340 pp
McConnaughey TA (1989) 13C and 18O isotopic disequilibrium in biological carbonates. I. Patterns. Geochim Cosmochim Acta 53:151–162
Muscatine L, Porter JW, Kaplan IR (1989) Resource partitioning by reef corals as determined from stable isotope composition. I. δ13C of zooxanthellae and animal tissue vs depth. Mar Biol 110:185–193
Ogden J, Wicklund R (eds) (1988) Mass bleaching of coral reefs in the Caribbean: a research strategy. NOAA Nat Undersea Res Prog (Res Rept 88-2:1–9)
Porter JW, Fitt WK, Spero HJ, Rogers CS, White MW (1989) Bleaching in reef corals: physiological and stable isotopic responses. Proc Natl Acad Sci USA 86:9342–9346
Swart PK (1983) Carbon and oxygen isotope fractionation in scleractinian corals: a review. Earth-Sci Rev 19:51–80
Swart PK, Coleman ML (1980) Isotopic data for scleractinian corals explain their palaeotemperature uncertainty. Nature 283:557–559
Swart PK, Wilson AF, Jell JS (1983) Oxygen isotope variation on a lagoonal platform reef, Heron Island, Great Barrier Reef. Aust J Mar Freshwater Res 34:813–819
Swart PK, Sternberg L, Steinen R, Harrison SA (1989) Controls on the oxygen and hydrogen isotopic composition of waters from Florida Bay. Chem Geol (Isotope Geosci) 79:113–123
Swart PK, Burns SJ, Leder JJ (1991) Fractionation of carbon dioxide during the reaction of calcite with phosphoric acid as a function of temperature and technique. Chem Geol (Isotope Geosci) 86:89–96
Szmant AM, Gassman NJ (1990) The effects of prolonged “bleaching” on the tissue biomass characteristics and reproduction of the reef coral Montastrea annularis. Coral Reefs 8:217–224
Vaughan TW (1918) The temperature of the Florida coral-reef tract. Carnegie Institution of Washington, publ 213, papers from the Tortugas Lab 9:321–336
Weber JN, Woodhead PMJ (1970) Carbon and oxygen isotope fractionation on the skeletal carbonate of reef-building corals. Chem Geol 6:93–117
Weber JN, Woodhead PMJ (1972) Temperature dependence of oxygen-18 concentration in reef coral carbonates. J Geophys Res 77:463–474
Weber JN, Deines P, Weber PH, Baker PA (1976) Depth related changes in the 13C/12C ratio of skeletal carbonate by the Caribbean reef-frame-building coral Montastrea annularis: further implications for stable isotope fractionation by scleractinian corals. Geochim Cosmochim Acta 40:31–39
Weil SM, Buddemeier RW, Smith SV, Kroopnick PM (1981) The stable isotopic composition of coral skeletons: control by environmental variables. Geochim Cosmochim Acta 45:1147–1153
Williams EH, Goenaga C, Vincente V (1987) Mass bleaching on Atlantic coral reefs. Science 237:877–878
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Leder, J.J., Szmant, A.M. & Swart, P.K. The effect of prolonged “bleaching” on skeletal banding and stable isotopic composition in Montastrea annularis . Coral Reefs 10, 19–27 (1991). https://doi.org/10.1007/BF00301902
Accepted:
Issue Date:
DOI: https://doi.org/10.1007/BF00301902