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Indian Gondwana palynochronology: relationships and chronocalibration
Content Provider | Birbal Sahni Institute of Paleobotany |
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Author | Tiwari, R.S. Kumar, Rajiv |
Abstract | The concept of Gondwana Sequence on the Indian Peninsula is discussed from the view point of time, geographical extent and environment. It has been ascertained that Talchir deposition began in the late Asselian (Early Permian) and not during the Permo-Carboniferous. The Karharbari succession is a distinct formation. The Barakar Formation should continue to be placed in the Lower Permian of the bipartite division of the Permian System. The Banspitali Nala section, in the south of Damodar River, Raniganj Coalfield, West Bengal, India, may be a suitable nonmarine reference section for the Permian-Triassic boundary. To determine the age-ranges of the palynozones through the Gondwana Sequence, there is a need for cross-correlation with sections in the Himalayan region and in other areas of Gondwanaland. |
Starting Page | 13 |
Ending Page | 30 |
File Format | |
Volume Number | 51 |
Language | English |
Publisher Date | 2002-01-01 |
Access Restriction | Open |
Subject Keyword | Palynology Gondwana Palynochronology Correlation India |
Content Type | Text |
Educational Use | Research Reading |
Resource Type | Article |
Education Level | Under Graduate Post Graduate |
Subject | Paleobotany; fossil microorganisms |