B
Bhawanisingh G. Desai
Researcher at Pandit Deendayal Petroleum University
Publications - 38
Citations - 344
Bhawanisingh G. Desai is an academic researcher from Pandit Deendayal Petroleum University. The author has contributed to research in topics: Geology & Trace fossil. The author has an hindex of 10, co-authored 28 publications receiving 249 citations. Previous affiliations of Bhawanisingh G. Desai include Maharaja Sayajirao University of Baroda.
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Animal-sediment relationship of the crustaceans and polychaetes in the intertidal zone around Mandvi, Gulf of Kachchh, Western India
TL;DR: In this paper, animal-sediment relationships of two benthic communities (Crustaceans and Polychaetes) were studied around Mandvi coast in the Gulf of Kachchh, Western India.
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Middle Jurassic Trace Fossils from Habo Dome, Mainland Kachchh, Western India
TL;DR: In this article, the authors described 30 ichnospecies of 23 ichnogenera and their preservational aspects, ecological observations, producers and behavioural aspects are discussed.
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Postrift deltaic sedimentation in western Kachchh Basin: insights from ichnology and sedimentology.
TL;DR: In this article, the authors address the older mid-Kimmeridgian to Tithonian "Jhuran Delta" and delineate the nature of the Jhuran delta using the ichnological and sedimentological parameters.
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Paleoecological significance of the trace fossils of Dhosa Oolite Member (Jumara Formation), Jhura dome, Mainland Kachchh, Western India
TL;DR: In this article, the authors describe a sequence of oolitic limestones and shales, exposed in Jhura dome of Mainland Kachchh, Western India, exhibiting a moderate diversity and behaviourally complex assemblage of ichnospecies.
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Significance of the trace fossil Balanoglossites Mägdefrau, 1932 from the Lower Cretaceous Guneri member (Bhuj formation) of the Guneri dome, Kachchh, India
TL;DR: In this paper, a detailed analysis of the trace fossil Balanoglossites along with lithofacies analysis suggests that it belongs to the Glossifungites ichnofacies surface and this trace fossil bearing surface corresponds to the Lower Cretaceous regressive phase that marks the unconformity of other parts of the Kachchhh basin.