Khosla, A. and Lucas, S.G., eds., 2016, Cretaceous Period: Biotic Diversity and Biogeography. New Mexico Museum of Natural History and Science Bulletin 71. 317 HISTORICAL BIOGEOGRAPHY OF THE LATE CRETACEOUS VERTEBRATES OF INDIA: COMPARISON OF GEOPHYSICAL AND PALEONTOLOGICAL DATA OMKAR VERMA1, ASHU KHOSLA2, FRANCISCO J. GOIN3 AND JASDEEP KAUR2 1Geology Discipline Group, School of Sciences, Indira Gandhi National Open University, New Delhi – 110 068, India, e-mail: omkarverma@ ignou.ac.in; 2Department of Geology, Centre for Advanced Studies, Panjab University, Sector-14, Chandigarh – 160014, India, e-mail:
[email protected], e-mail:
[email protected]; 3Consejo Nacional de Investigaciones Científicas y Técnicas and División Paleontología Vertebrados, Museo de Ciencias Naturales de La Plata, B1900FWA La Plata, Argentina, e-mail:
[email protected] Abstract—The Cretaceous was a special time for the Indian plate as it was separated from Gondwana landmasses and started its northward journey across the Tethys Sea towards the Equator. The northward movement of this plate implied shifting latitudes and climate belts, until it finally collided with Asia during the early Cenozoic. Geophysical data and plate tectonic models show that after splitting from Gondwana, the Indian plate remained as an isolated continent for more than 45 Ma during the Cretaceous; thus, it predicts a remarkable biotic endemism for the continent. Paleontological data on the Cretaceous vertebrates of India is best known for Maastrichtian time; in turn, the pre-Maastrichtian record is very poor—it contains very few fossils of fishes and marine reptiles. The Maastrichtian fossil record comprises vertebrates of Gondwana and Laurasian affinities and some endemic, ancient lineages as well.