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Evidence of Wildfires in the Late Permian (Changsinghian) Zewan formation of Kashmir, India


Affiliations
1 Programa de Pos-Graduacao em Ambiente e Desenvolvimento, PPGAD. Centro Universitário Univates, Lajeado, Brazil
2 Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226 007, India
3 Department of Geology, University of Jammu, Jammu 180 006, India
4 Universidade Federal do Tocantins, Porto Nacional, Brazil
5 Universidade Federal de Santa Maria, Santa Maria, Brazil
6 Directorate of Geology and Mining, Jammu and Kashmir Government, Srinagar 190 002, India
 

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.
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  • Evidence of Wildfires in the Late Permian (Changsinghian) Zewan formation of Kashmir, India

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Authors

Andre Jasper
Programa de Pos-Graduacao em Ambiente e Desenvolvimento, PPGAD. Centro Universitário Univates, Lajeado, Brazil
Dieter Uhl
Programa de Pos-Graduacao em Ambiente e Desenvolvimento, PPGAD. Centro Universitário Univates, Lajeado, Brazil
Deepa Agnihotri
Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226 007, India
Rajni Tewari
Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226 007, India
Sundeep K. Pandita
Department of Geology, University of Jammu, Jammu 180 006, India
Jose Rafael Wanderley Benicio
Programa de Pos-Graduacao em Ambiente e Desenvolvimento, PPGAD. Centro Universitário Univates, Lajeado, Brazil
Etiene Fabbrin Pires
Universidade Federal do Tocantins, Porto Nacional, Brazil
Atila Augusto Stock Da Rosa
Universidade Federal de Santa Maria, Santa Maria, Brazil
Gulam D. Bhat
Directorate of Geology and Mining, Jammu and Kashmir Government, Srinagar 190 002, India
S. Suresh K. Pillai
Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226 007, India

Abstract


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.

References





DOI: https://doi.org/10.18520/cs%2Fv110%2Fi3%2F419-423