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Deshmukh, S.S., Sano, T., Fuji, T., Nair, K.K.K., Yedekar, D.B., Umino, S., Iwamori, H. and Aramaki, S. (1996) Chemical Stratigraphy and Geochemistry of the Basalt Flows from the Central and Eastern Parts of Deccan Volcanic Province of India. Gondwana Geological Magazine, Special Publication, 2, 145-170.

has been cited by the following article:

• TITLE: Cretaceous-Paleogene Transition of Reptilian Tetrapods across Deccan Volcanism in India

  AUTHORS: Dhananjay M. Mohabey, Bandana Samant

  KEYWORDS: Deccan Volcanism, Maastrichtian-Paleocene, Reptiles, Extinction

  JOURNAL NAME: Open Journal of Geology, Vol.9 No.10, September 24, 2019

  ABSTRACT: Eruptions of lava flows of Deccan large igneous province straddled the Cretaceous-Palaeogene boundary (K-Pg). Sediments associated at different stratigraphic levels within the lava piles of Deccan volcanic sequences (DVS) are mainly terrestrial. We studied the sediments of Eastern and Central Deccan Volcanic Province, and the Malwa Plateau for tracking changes in reptilian tetrapods across the volcanism. The reptiles are mainly represented by abelisaurid-titanosaurid dinosaurs, Alethinophidia madtsoiia snakes, Notosuchian crocodylomorph Simosuchus, bothremydid Kurmademydinae turtles and Anguimorph and Scincomorphs lizards. The evidences suggest that the non-avian dinosaurs were adversely affected by the arrival of the first volcanic flows locally in the province either within C30N or C29R Maastrichtian. The abelisaurid theropods became extinct whereas a single or two species of titanosauriforme dinosaurs survived but eventually became extinct at least 350 ky before the K-Pg boundary with increasing volcanism. The madtsooid snakes and crocodylimorphs were also adversely affected with decline in their diversity and abundance, whereas the Bothremydid turtles survived the initial onslaught of Deccan volcanism and continued across the K-Pg boundary.