Elements of the ecology of modern and paleoecology of fossil corals
Authors:
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
- Bogdanov D. V. Geography of the blue continent. PH of the AS of the USSR, 1963.
- Zhuravlev A. I., Trostnikov V. N. Luminescence of living tiss.s. PH Nauka, 1966.
- Carrington R. Biography of the Sea. Hydrometeoizdat, 1964.
- Liozner L. D. Restoration of lost organs. PH of the AS USSR, 1962.
- Mechnikov I. I. Selected Biological Works. PH of the AS USSR, 1950.
- Ommani F. D. Ocean. Hydrometeoizdat, 1963.
- Ravikovich A. I. Modern and fossil reefs. PH of the AS USSR, 1954.
- Yakovlev N. N. Organism and environment. PH Nauka, 1964.
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