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Ichnological Significance of Upper Disang Formation and Lower Barail Formation (Late Eocene to Early Oligocene) of Nagaland, Northeast India, in the Indo-Myanmar Ranges

  • Research Article
  • Published:
Journal of the Geological Society of India

Abstract

The Upper Disang-Lower Barail Transition Sequences of Nagaland in northeast India, Indo-Myanmar Ranges (IMR) are found to preserve reasonably diverse biological sedimentary structures. Three ichnofacies were observed, Skolithos ichnofacies consisting of Bergaueria hemispherica, Gyrochorte comosa, Ophiomorpha nodosa, Skolithos linearis and Thalassinoides paradoxicus; Cruziana ichnofacies — Curvolithus simplex, Scolicia plana, Scolicia strozzii, Scolicia vertebralis, Treptichnus pedum, Taenidium diesingi and Palaeophycus tubularis; and Nereites ichnofacies — Chondrites targionii and Paleomeandron elegans. Presence of Skolithos and Cruziana ichnofacies suggest well oxidising, substrate rich depositional environment in the foreshoreface to offshore setting in general; and an overall possible fluctuation in the depositional bathymetry which is supported by the presence of Nereites ichnofacies in horizons alternating with Skolithos and Cruziana ichnofacies. The depositional system is proposed to be proximal to distal hyperpycnal-delta-fed turbidite system. Observation of sand spherules also suggests possibility of shoreline as one of the depositional environments.

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Authors and Affiliations

  1. Department of Geology, United College Lambung, Chandel, Lambung, 795 127, India

    H. S. Rajkumar

  2. Department of Earth Sciences, Manipur University, Canchipur, Imphal, 795 003, India

    I. Soibam & S. S. Sanasam

  3. Department of Geology, D.M. College of Science, Imphal, 795 001, India

    K. S. Khaidem

  4. Department of Geology, Nagaland University, Meriema, Aizawl, 797004, India

    Ch. M. Khuman

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  1. H. S. Rajkumar
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  2. I. Soibam
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  4. S. S. Sanasam
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  5. Ch. M. Khuman
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Rajkumar, H.S., Soibam, I., Khaidem, K.S. et al. Ichnological Significance of Upper Disang Formation and Lower Barail Formation (Late Eocene to Early Oligocene) of Nagaland, Northeast India, in the Indo-Myanmar Ranges. J Geol Soc India 93, 471–481 (2019). https://doi.org/10.1007/s12594-019-1202-0

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