Chondrites isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular India
Rhythmic sandstone-mudstone-coal succession of the Barakar Formation (early Permian) manifests a transition from lower braided-fluvial to upper tide-wave influenced, estuarine setting. Monospecific assemblage of marine trace fossil Chondrites isp. in contemporaneous claystone beds in the upper Barak...
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2014-01-01
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Series: | The Scientific World Journal |
Online Access: | http://dx.doi.org/10.1155/2014/434672 |
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author | Biplab Bhattacharya Sudipto Banerjee |
author_facet | Biplab Bhattacharya Sudipto Banerjee |
author_sort | Biplab Bhattacharya |
collection | DOAJ |
description | Rhythmic sandstone-mudstone-coal succession of the Barakar Formation (early Permian) manifests a transition from lower braided-fluvial to upper tide-wave influenced, estuarine setting. Monospecific assemblage of marine trace fossil Chondrites isp. in contemporaneous claystone beds in the upper Barakar succession from two Gondwana basins (namely, the Raniganj Basin and the Talchir Basin) in eastern peninsular India signifies predominant marine incursion during end early Permian. Monospecific Chondrites ichnoassemblage in different sedimentary horizons in geographically wide apart (~400 km) areas demarcates multiple short-spanned phases of anoxia in eastern India. Such anoxia is interpreted as intermittent falls in oxygen level in an overall decreasing atmospheric oxygenation within the late Paleozoic global oxygen-carbon dioxide fluctuations. |
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institution | Kabale University |
issn | 2356-6140 1537-744X |
language | English |
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spelling | doaj-art-72bb58adc59442ecb749eb59d684aa0b2025-02-03T06:01:54ZengWileyThe Scientific World Journal2356-61401537-744X2014-01-01201410.1155/2014/434672434672Chondrites isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular IndiaBiplab Bhattacharya0Sudipto Banerjee1Department of Earth Sciences, Indian Institute of Technology Roorkee, Roorkee, Uttarakhand 247667, IndiaDepartment of Geology, Hooghly Mohsin College, Chinsurah, Hooghly, West Bengal 712101, IndiaRhythmic sandstone-mudstone-coal succession of the Barakar Formation (early Permian) manifests a transition from lower braided-fluvial to upper tide-wave influenced, estuarine setting. Monospecific assemblage of marine trace fossil Chondrites isp. in contemporaneous claystone beds in the upper Barakar succession from two Gondwana basins (namely, the Raniganj Basin and the Talchir Basin) in eastern peninsular India signifies predominant marine incursion during end early Permian. Monospecific Chondrites ichnoassemblage in different sedimentary horizons in geographically wide apart (~400 km) areas demarcates multiple short-spanned phases of anoxia in eastern India. Such anoxia is interpreted as intermittent falls in oxygen level in an overall decreasing atmospheric oxygenation within the late Paleozoic global oxygen-carbon dioxide fluctuations.http://dx.doi.org/10.1155/2014/434672 |
spellingShingle | Biplab Bhattacharya Sudipto Banerjee Chondrites isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular India The Scientific World Journal |
title | Chondrites isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular India |
title_full | Chondrites isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular India |
title_fullStr | Chondrites isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular India |
title_full_unstemmed | Chondrites isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular India |
title_short | Chondrites isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular India |
title_sort | chondrites isp indicating late paleozoic atmospheric anoxia in eastern peninsular india |
url | http://dx.doi.org/10.1155/2014/434672 |
work_keys_str_mv | AT biplabbhattacharya chondritesispindicatinglatepaleozoicatmosphericanoxiaineasternpeninsularindia AT sudiptobanerjee chondritesispindicatinglatepaleozoicatmosphericanoxiaineasternpeninsularindia |