Ecology of beach rock fauna of the south Andaman Island, Bay of Bengal
The late Holocene microfauna from the beach-rock of the south Andaman Island has been investigated. The beach-rock fauna reflects the reefal environment of deposition. The occurrence of raised beaches and terraces has been attributed to the neotectonic activity in recent times. C-14 dates indicate t...
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Veröffentlicht in: | Current science (Bangalore) 2002-04, Vol.82 (7), p.881-885 |
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Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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Zusammenfassung: | The late Holocene microfauna from the beach-rock of the south Andaman Island has been investigated. The beach-rock fauna reflects the reefal environment of deposition. The occurrence of raised beaches and terraces has been attributed to the neotectonic activity in recent times. C-14 dates indicate that the Wandoor beach-rock is younger (1540–1350 years B.P.) than the Chidyatapu beach rock (4410–3900 years B.P.) indicating at least two phases of neotectonic activity. |
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ISSN: | 0011-3891 |