Microbially induced sedimentary textures are reported from the Neoarchaean Donimalai Formation (Dharwar Supergroup) of the Sandur Schist Belt in India. These occur in chert bands interlayered with banded iron formations (BIFs). The textures appear as interspersed carbonaceous specks lining flat or wavy laminae that build into a strand-like carbonaceous meshwork. Raman spectroscopy indicates the presence of organic carbon. Elemental mapping using field emission scanning electron microscopy with energy-dispersive X-ray (FE-SEM-EDAX) analyses supports a biogenic origin. The presence of syngenetic microbial mat textures in the BIFs of the Donimalai Formation suggests microbially mediated oxidation and deposition of Fe in the predominantly anoxic Neoarchaean Ocean. Yogmaya Shukla* [yogmayashukla@bsip.res.in], Mukund Sharma [sharmamukund1@rediffmail.com], Arif H. Ansari [a.h.ansari@bsip.res.in], Veeru Kant Singh [veerukantsingh@bsip.res.in], Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India; Nora Noffke [nnoffke@odu.edu], Old Dominion University, Oceanography & Physics Building, Norfolk, 23529, VA, USA.
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