Skip to main content
Log in

Growth rhythms recorded in stable isotopes and density bands in the reef coral Porites lobata (Cebu, Philippines)

  • Published:
Coral Reefs Aims and scope Submit manuscript

Abstract

Growth rhythms in the reef coral Porites lobata are revealed by X-radiography and stable carbon and oxygen isotopic analysis. High density increments were deposited during warm temperatures in summer and low density increments during winter. The seasonal temperature variations are reflected in the oxygen isotope ratios. The coral carbonate shows a constant depletion in 18O of −2.7%0 relative to calcite in equilibrium with the ambient seawater. The mean annual growth rate of the specimen studied was 1.3±0.3 cm/year.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Buddemeier RW (1978) Coral growth: retrospective analysis. In: Stoddart DR, Johannes RE (eds) Coral reefs: research methods. UNESCO, Monogr Oceanogr Methodol 5:551–571

  • Craig H, Gordon LI (1965) Deuterium and oxygen-18 variations in the ocean and the marine atmosphere. In: Tongiori E (ed) 2nd Conference Stable Isotopes in Oceanographic Studies and Paleotemperatures. Consiglio Nazionale delle Richerche, Roma, pp 9–130

    Google Scholar 

  • Dunbar R, Wefer G (1984) Stable isotope fractionation in benthic foraminifera from the Peruvian continental margin. Mar Geol 59 (in press)

  • Emiliani C, Hudson JH, Shinn EA, George RY (1978) Oxygen and carbon isotopic growth record in reef coral from the Florida Keys and a deep sea coral from the Blake Plateau. Science 202:627–629

    Google Scholar 

  • Epstein S, Buchsbaum R, Lowenstam HA, Urey HC (1953) Revised carbonate-water isotopic temperature scale. Geol Soc Am Bull 64:1315–1326

    Google Scholar 

  • Erez J (1977) Influence of symbiotic algae on the stable isotope composition of hermatypic corals: a radioactive tracer approach. Proc 3rd Int Coral Reef Symp 2:563–570

    Google Scholar 

  • Fairbanks RG, Dodge RE (1979) Annual periodicity of the 18O/16O and 13C/12C ratios in the coral Montastrea annularis. Geochim Cosmochim Acta 43:1009–1020

    Google Scholar 

  • Goreau TJ (1977) Seasonal variations of trace metals and stable isotopes in coral skeletons: physiological and environmental controls. Proc 3rd Int Coral Reef Symp 2:425–430

    Google Scholar 

  • Grobe H, Wefer G, Willkomm H (1984) Internal structure of the double reef of North Bohol and the Olango Reef Flat (Philippines). Philipp Sci 21 (in press)

  • Grossman EL (1982) Stable isotopes in live benthic foraminfera from the Southern California borderland. PhD dissertation, University of Southern California

  • Highsmith RC (1979) Coral growth rates and environmental control of density banding. J Exp Mar Biol Ecol 37:105–125

    Google Scholar 

  • Knutson DW, Buddemeier RW, Smith SV (1972) Coral chronometers: seasonal growth bands in reef corals. Science 177:270–272

    Google Scholar 

  • 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

    Google Scholar 

  • Macintyre IG (1978) A hand-operated submersible drill for coring reef substrata. In: Stoddart DR, Johannes RE (eds) Coral reefs: research methods. UNESCO, Monogr Oceanogr Methodol 5:75–80

  • Philippine Island Pilot (1978) 1 st edn. Hydrographer of the Navy, Taunton, Sommerset

  • Shinn EA (1966) Coral growth rate, an environmental indicator. J Paleontol 40:233–240

    Google Scholar 

  • Smith SV, Buddemeier RW, Redalje RC, Houck JE (1979) Strontium-calcium thermometry in coral skeletons. Science 204:404–407

    Google Scholar 

  • Tarutani T, Clayton RN, Mayeda TK (1969) The effect of polymorphism and magnesium substitution on oxygen isotope fractionation between calcium carbonate and water. Geochim Cosmochim Acta 33:987–996

    Google Scholar 

  • Urey HC, Lowenstam HA, Epstein S, McKinney CR (1951) Measurement of paleotemperatures and temperatures of the Upper Cretaceous of England, Denmark, and the southeastern United States. Bull Geol Soc Am 62:399–416

    Google Scholar 

  • Weber JN, Woodhead PMJ (1972) Temperature dependence of oxygen-18 concentration in reef coral carbonates. J Geophys Res 77:463–473

    Google Scholar 

  • Wefer G, Killingley JS, Lutze GF (1981) Stable isotopes in recent larger foraminifera. Palaeogeogr Palaeoclimatol Palaeoecol 33:253–270

    Google Scholar 

  • 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

    Google Scholar 

  • Wellington GM, Glynn PW (1983) Environmental influences on skeletal banding in Eastern Pacific (Panama) corals. Coral Reefs 1:215–222

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Pätzold, J. Growth rhythms recorded in stable isotopes and density bands in the reef coral Porites lobata (Cebu, Philippines). Coral Reefs 3, 87–90 (1984). https://doi.org/10.1007/BF00263758

Download citation

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF00263758

Keywords

Navigation