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Vol 59 Iss. 2
Pages:
26-32
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RUS
Article

Elements of the ecology of modern and paleoecology of fossil corals

Authors:
A. G. Kravtsov
Date submitted:
1970-08-28
Date accepted:
1970-10-25
Date published:
1971-04-06

Abstract

Optimal conditions for modern colonial six-beam corals of the scleractinids are well studied [Bogdanov, 1963; Carrington, 1964; Ommani, 1963; Ravikovich, 1954]. Their distribution is influenced by depth, temperature, salinity, water movement and oxygen supply, and soil composition. Corals reach their maximum development at depths of 20-40 m.

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References

  1. Bogdanov D. V. Geography of the blue continent. PH of the AS of the USSR, 1963.
  2. Zhuravlev A. I., Trostnikov V. N. Luminescence of living tiss.s. PH Nauka, 1966.
  3. Carrington R. Biography of the Sea. Hydrometeoizdat, 1964.
  4. Liozner L. D. Restoration of lost organs. PH of the AS USSR, 1962.
  5. Mechnikov I. I. Selected Biological Works. PH of the AS USSR, 1950.
  6. Ommani F. D. Ocean. Hydrometeoizdat, 1963.
  7. Ravikovich A. I. Modern and fossil reefs. PH of the AS USSR, 1954.
  8. Yakovlev N. N. Organism and environment. PH Nauka, 1964.
  9. Wells J. W. Mem. Geol. Soc. America, No. 67, 1967.

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