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Spherules from the Late Cretaceous Phosphorite of the Fatehgarh Formation,Barmer Basin,India
Institution:1. Centre for Earth Sciences, Indian Institute of Science, Bangalore 560012, India;2. Department of Geology, University of Leicester, Leicester LE1 7RH, UK;3. Center for Global Tectonics, China University of Geosciences, 388 Lumo Road,Wuhan 430074, China;4. Départment de Sciences, de la Terre, Université de Toliara, BP.185, Toliara 601, Madagascar;5. Hiruzen Institute for Geology and Chronology Co. Ltd., 2-5 Nakashima, Naka-ku, Okayama 703-8252, Japan;6. Research Institute of Natural Sciences, Okayama University of Science, 1-1 Ridai-cho, Kita-ku, Okayama 700-0005, Japan
Abstract:A first report of discovery of spherules, glassy balls, highly magnetic fine dust and microbracciated matrix in the Fatehgarh Formation of Barmer Basin, Rajasthan, India is being presented in this paper. The Fatehgarh Formation is a mixed siliciclastic, carbonate and phosphorite formation of Cretaceous age in the Barmer Basin that comprises sediments of Middle Jurassic to Lower Eocene age. The phosphorite zone in the Fatehgarh Formation is ~8 metre-thick zone that comprises phosphatic sandstone, bone bed, bedded phosphorite and phosphatic and non phosphatic gastropod beds. The spherules occur in a thin phosphatic-clay mud and silt band of bone bed, which also yielded a very rich and diverse microvertebrate assemblage with a dominant Late Cretaceous (Maastrichtian) form of Igdabatis along with forms comprising of Semionodontid, Lapisosteum and Enchodontid. The end Cretaceous is marked for a mass extinction of numerous species including dinosaurs. An extraterrestrial impact is interpreted as the reason for this mass extinction. Whether these spherules are related to the volcanic source or K/T Boundary impact ejecta found at Caribbean and Gulf of Mexico region needs detailed chemical and age characterization for which study is in progress.
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