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The Earliest Marine Transgression in Western India:New Insights from Calcareous Nannofossils from Lathi Formation, Jaisalmer Basin


Affiliations
1 Birbal Sahni Institute of Palaeosciences, 53, University Road, Lucknow 226 007, India
2 Geological Survey of India, Jaipur 302 004, India
 

We report the first record of an age-diagnostic, but depauperate assemblage of calcareous nannofossils, an exclusively marine phytoplankton group, from the Lathi Formation of Jaisalmer Basin, western India. The nannofossil evidence, precisely constrains the age of the Lathi Formation, traditionally considered to be a Bajocian (Middle Jurassic) continental deposit. Furthermore, the presence of several reworked nannofossil taxa of Pliensbachian, Toarcian and Aalenian ages suggests that the earliest epeiric sea transgressed western India during the Early Jurassic. Thick and luxuriant gymnosperm forests proliferated in the Jaisalmer Basin during this time. The presence of calcareous nannofossils in both the lower and upper members of the Lathi Formation (Odania and Thaiat members) points to intermittent coastal marine depositional environment.

Keywords

Calcareous Nannofossils, Early-Middle Jurassic, Jaisalmer Basin, Lathi Formation.
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  • Das Gupta, S. K., Revision of the Mesozoic–Tertiary stratigraphy of the Jaisalmer Basin Rajasthan. Indian J. Earth Sci., 1975, 2(10), 77–94.
  • Singh, N. P., Mesozoic lithostratigraphy of Jaisalmer Basin, Rajasthan. J. Palaeontol. Soc. India, 2006, 51(2), 53–56.
  • Pandey, D. K., Choudhary, S., Bahadur, T., Swami, N., Poonia, D. and Sha, J., A review of the Lower–lowermost Upper Jurassic facies and stratigraphy of the Jaisalmer Basin, western Rajasthan, India. Volumina Jurassica, 2012, X, 61–82.
  • Oldham, R. D., Preliminary notes on the Geology of Northern Jaisalmer. Rec. Geol. Surv. India, 1886, 19(3), 157–160.
  • Swaminathan, J., Krinshnamurthy, J. G., Verma, K. K. and Chandiak, G. J., General geology of Jaisalmer area, Rajasthan. In Proceedings of the symposium of development in petroleum resources of Asia and the Far East; Mineral Resources Development Series (10), Bangkok (ECAFE, UN), 1959.
  • Narayanan, K., Stratigraphy of the Rajasthan Shelf. In Proceedings of the Symposium on Problems of the Indian Arid Zones, Government of India publication, 1964, pp. 92–100.
  • Pandey, D. K., Sha, J. and Choudhary, S., Depositional history of the early part of the Jurassic succession on the Rajasthan Shelf, western India. In Natural Science, Special issue of IGCP 506 on the Jurassic Boundary Events, Beijing, 2006, 16, 176–185.
  • Pienkowski, G., Branski, P., Pandey, D. K., Schlog, J., Alberti, M. and Fursich, F. T., Dinosaur footprints from the Thaiat ridge and their palaeoenvironmental background, Jaisalmer Basin, Rajastan, India. Volumina Jurassica, 2015, XIII(1), 17–26.
  • Lukose, N. G., Palynological evidence on the age of Lathi Formation, Western Rajasthan, India. In Proceeding of Seminar on Palaeopalynology and Indian Stratigraphy, 1971, 1972, pp. 155–159.
  • Pareek, H. S., Geology of northwestern Rajasthan, Geology through pictures. Indian Mines, 1980, 33(4), 60–63.
  • Bown, P. R. and Young, J. R., Techniques. In Calcareous Nannofossil Biostratigraphy (ed. Bown, P. R.), British Micropalaeontological Society Series, Chapman & Hall, London, 1998, pp. 16–28.
  • Bown, P. R. and Cooper, M. K. E., Jurassic. In Calcareous Nannofossil Biostratigraphy (ed. Bown, P. R.), British Micropalaeontological Society Series, Chapman & Hall, London, 1998, pp. 34–54.
  • Pandey, D. K., Fürsich, F. T. and Alberti, M., Stratigraphy and palaeoenvironments of the Jurassic rocks of the Jaisalmer Basin–field guide. Beringeria, Special Issue, 2014, 9, 1–111.
  • Giraud, F., Pittet, B., Mattioli, E. and Audouin, V., Paleoenvironmental controls on the morphology and abundance of the coccolith Watznaueria britannica (Late Jurassic, southern Germany). Mar. Micropaleontol., 2006, 60, 205–225.
  • Rai, J. and Jain, S., Pliensbachian nannofossils from Kachchh: implications on the earliest Jurassic transgressive event on the western Indian margin. Zitteliana A, 2013, 53, 105–119.
  • von Salis, A. K. and Immenhauser, A., Mesozoic calcareous nannofossil from Masirah Island (Sultanat of Oman). J. Nannoplankton Res., 1997, 19, 95–101.
  • Kadar, A. P., Crittenden, S. and Karam, K. A., Middle Jurassic to Early Cretaceous calcareous nannofossils from Onshore North Kuwait: A new record. GeoArabia, 18(2), Late Jurassic Early Cretaceous Evaporite–Siliciclastic systems of the Arabian Plate, Abstracts of the EAGE’s Fourth Arabian Plate Geology Workshop, Abu Dhabi, United Arab Emirates, 2012, pp. 216–219.
  • Dera, G., Pellenard, P., Neige, P., Deconinck, J. F., Pueat, E. and Dommergues, J., Distribution of clay minerals in Early Jurassic Peritethyan seas: Palaeoclimatic significance inferred from multiproxy comparisons. Palaeogeogr., Palaeoclimatol., Palaeoecol., 2009, 271, 39–51.

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  • The Earliest Marine Transgression in Western India:New Insights from Calcareous Nannofossils from Lathi Formation, Jaisalmer Basin

Abstract Views: 516  |  PDF Views: 243

Authors

Jyotsana Rai
Birbal Sahni Institute of Palaeosciences, 53, University Road, Lucknow 226 007, India
Sunil Bajpai
Birbal Sahni Institute of Palaeosciences, 53, University Road, Lucknow 226 007, India
Ravindra Kumar
Geological Survey of India, Jaipur 302 004, India
Abha Singh
Birbal Sahni Institute of Palaeosciences, 53, University Road, Lucknow 226 007, India
Krishna Kumar
Geological Survey of India, Jaipur 302 004, India
Neeru Prakash
Birbal Sahni Institute of Palaeosciences, 53, University Road, Lucknow 226 007, India

Abstract


We report the first record of an age-diagnostic, but depauperate assemblage of calcareous nannofossils, an exclusively marine phytoplankton group, from the Lathi Formation of Jaisalmer Basin, western India. The nannofossil evidence, precisely constrains the age of the Lathi Formation, traditionally considered to be a Bajocian (Middle Jurassic) continental deposit. Furthermore, the presence of several reworked nannofossil taxa of Pliensbachian, Toarcian and Aalenian ages suggests that the earliest epeiric sea transgressed western India during the Early Jurassic. Thick and luxuriant gymnosperm forests proliferated in the Jaisalmer Basin during this time. The presence of calcareous nannofossils in both the lower and upper members of the Lathi Formation (Odania and Thaiat members) points to intermittent coastal marine depositional environment.

Keywords


Calcareous Nannofossils, Early-Middle Jurassic, Jaisalmer Basin, Lathi Formation.

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DOI: https://doi.org/10.18520/cs%2Fv111%2Fi10%2F1631-1639