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Pillai, S. Suresh K.
- Evidence of Wildfires in the Late Permian (Changsinghian) Zewan formation of Kashmir, India
Abstract Views :257 |
PDF Views:134
Authors
Andre Jasper
1,
Dieter Uhl
1,
Deepa Agnihotri
2,
Rajni Tewari
2,
Sundeep K. Pandita
3,
Jose Rafael Wanderley Benicio
1,
Etiene Fabbrin Pires
4,
Atila Augusto Stock Da Rosa
5,
Gulam D. Bhat
6,
S. Suresh K. Pillai
2
Affiliations
1 Programa de Pos-Graduacao em Ambiente e Desenvolvimento, PPGAD. Centro Universitário Univates, Lajeado, BR
2 Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226 007, IN
3 Department of Geology, University of Jammu, Jammu 180 006, IN
4 Universidade Federal do Tocantins, Porto Nacional, BR
5 Universidade Federal de Santa Maria, Santa Maria, BR
6 Directorate of Geology and Mining, Jammu and Kashmir Government, Srinagar 190 002, IN
1 Programa de Pos-Graduacao em Ambiente e Desenvolvimento, PPGAD. Centro Universitário Univates, Lajeado, BR
2 Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226 007, IN
3 Department of Geology, University of Jammu, Jammu 180 006, IN
4 Universidade Federal do Tocantins, Porto Nacional, BR
5 Universidade Federal de Santa Maria, Santa Maria, BR
6 Directorate of Geology and Mining, Jammu and Kashmir Government, Srinagar 190 002, IN
Source
Current Science, Vol 110, No 3 (2016), Pagination: 419-423Abstract
The first record of palaeo-wildfire evidence in the form of charcoal is documented from the Late Permian Zewan Formation of the Kashmir region, northwest Himalaya. This evidence is in the form of fragments of tracheids that show homogenized cell walls, a characteristic feature of charcoal. Considering that palaeowildfire studies provide important palaeoecological information, the present study is significant, as it allows reconstructing new information about environmental conditions during the deposition of the sediments of the Late Permian Zewan Formation.Keywords
Charcoal, Gondwana, Himalayan Region, Late Palaeozoic, Marine Environment.Full Text
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