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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Detalles Bibliográficos
Autores principales: Bhattacharya, Biplab, Banerjee, Sudipto
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Hindawi Publishing Corporation 2014
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3926327/
https://www.ncbi.nlm.nih.gov/pubmed/24616628
http://dx.doi.org/10.1155/2014/434672

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3926327/
https://www.ncbi.nlm.nih.gov/pubmed/24616628
http://dx.doi.org/10.1155/2014/434672

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