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Carbon and oxygen isotope profiles from the terminal precambrian Marwar Supergroup, Rajasthan, India

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Abstract

Results of carbon and oxygen isotope studies from early Cambrian unfossiliferous carbonates belonging to the Marwar Supergroup, western Rajasthan, India are presented. The carbonates are enriched in “heavy” δ18O values (upto +6.50‰ PDB) and rules out the diagenetic modifications of isotope signals. The multiple, shortterm negative (upto −10.31‰ PDB) and positive (upto +2.80‰ PDB) carbon isotope oscillations observed in Marwar carbonates well matches with the lower Cambrian (Nemakit-Daldynian) carbonates reported world wide and these oscillations have been attributed to the result of climatic oscillations either from glaciations or from “cold house phases” that did not involve major glaciations.

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Authors and Affiliations

  1. Department of Geology, University of Rajasthan, Jaipur-4, India

    Anil Maheshwari

  2. NEG-LABISE, Dept. of Geology, Federal University of Pernambuco, C.P. 7852, 50,732-970, Recife, Brazil

    A. N. Sial

  3. Department of Geology, J.N.V. University, Jodhpur, India

    S. C. Mathur

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Maheshwari, A., Sial, A.N. & Mathur, S.C. Carbon and oxygen isotope profiles from the terminal precambrian Marwar Supergroup, Rajasthan, India. Carbonates Evaporites 18, 10–18 (2003). https://doi.org/10.1007/BF03178383

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