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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Main Authors: Biplab Bhattacharya, Sudipto Banerjee
Format: Article
Language:English
Published: Wiley 2014-01-01
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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language English
publishDate 2014-01-01
publisher Wiley
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series The Scientific World Journal
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
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AT sudiptobanerjee chondritesispindicatinglatepaleozoicatmosphericanoxiaineasternpeninsularindia