Chondrites isp. Indicating Late Paleozoic Atmospheric Anoxia in Eastern Peninsular India
Figure 6
Claystone bedding surfaces within upper Barakar succession, showing associations of Chondrites patulus (Cp), Chondrites targionii (Ct), Chondrites affinis (Ca), and Chondrites recurvus (Cr). (a) and (b) are from Kudaposi Nala, Talchir Basin, and (c) is from Khudia Nala, Raniganj Basin. Diameter of the coin is 2.3 cm in (a) and (b) and 2.5 cm in (c).
