Middle-Upper Jurassic Foraminifera from Jumara Hills, Kutch, India

Abstract

A prolific foraminiferal assemblage comprising 51 species is reported from Jurassic sediments of the Chari Formation, Jumara Hills, Kutch, India. The assemblage is dominated by the families Vaginulinidae and Nodosariidae. Sixteen species are reported for the first time from the Indian region including one new species. The foraminiferal assemblage suggests a Callovian to Oxfordian age for the studied sequence. The depositional environment of the studied sequence is interpreted based on foraminiferal evidence combined with lithology and megafauna which indicates that the sediments of the Chari formation exposed at Jumara Hills were deposited in a shallow-water, near shore, environment with fluctuating shoreline in a tectonically unstable shelf zone. The Jumara Hills foraminiferal assemblage exhibits close affinity with certain other Jurassic assemblages of the Tethyan Realm and helped in drawing palaeogeographic conclusions, suggesting that during the Middle and Late Jurassic epochs Kutch had close sea connections with Central Arabia, Afghanistan and Rajasthan on the one hand and Somalia and Malagasy on the other.