<i>Chondrites</i> isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular India

<table class="table-group" width="800px"><tr class="fig-image" id="a"><td><img alt="434672.fig.003a" src="https://static.hindawi.com/articles/tswj/volume-2014/434672/figures/434672.fig.003a.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(a) </b>Khudia Nala</td></tr></table></td></tr><tr class="fig-image" id="b"><td><img alt="434672.fig.003b" src="https://static.hindawi.com/articles/tswj/volume-2014/434672/figures/434672.fig.003b.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(b) </b>Kudaposi Nala</td></tr></table></td></tr></table>

<table>Vertical sedimentary logs of the upper Barakar succession in (a) Khudia Nala, Raniganj Basin, and (b) Kudaposi Nala, Talchir Basin. Note the occurrence of the claystone beds containing monospecific assemblage of <i>Chondrites</i> isp.</table>

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Figure 3

Figure 3: <i>Chondrites</i> isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular India 

The Scientific World Journal

Chondrites isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular India

Figure 3