A new Bartonian elasmobranch assemblage from the Kutch Basin, western India, and its significance in the context of paleoclimate change

Abstract

ABSTRACT The upper part of the Harudi Formation of the Kutch basin in Gujarat, western India, has recently yielded a heretofore undocumented assemblage of elasmobranchs, including extinct sand tiger sharks Brachycarcharias lerichei and Striatolamia macrota, extinct tiger sharks Galeocerdo eaglesomei and G. clarkensis, requiem shark Carcharhinus mancinae, as well as sawfish Pristis sp. A bony fish taxon represented by Trichiurus sp. was also recovered. After a 43-years gap, this study provides a taxonomic update on the middle Eocene sharks of Kutch. Their coexistence with the larger benthic foraminifera Nummulites obtusus and planktonic foraminifera Orbulinoides beckmanni dates this fish fauna to 40–41.03 Ma, which corresponds to the time frame of the Bartonian transgression and extreme warming event Middle Eocene Climatic Optimum (MECO). The MECO elasmobranch assemblage of Kutch comes from shelf settings with bathymetry of 30–60 m, and it differs from those associated with Paleocene–Eocene hyperthermal events and deposited in the bay complex. It seems that G. clarkensis and C. mancinae emerged in Kutch during MECO. The global stratigraphic distribution demonstrates that B. lerichei and S. macrota originated in North America, and their appearance in Kutch expands their geographic range into the eastern Tethys realm, possibly as a result of MECO-linked Bartonian/Kirther transgression.