EFFECT OF CLIMATIC SHIFT ON BIODIVERSITY OF BIVALVES: A CASE STUDY FROM LOWER MIOCENE OF KUTCH, INDIA
Our study primarily focuses on the shallow marine bivalve community from ten different localities representing two formations of Lower Miocene, namely, Khari Nadi formation (Aquitanian) and Chhasra formations (Burdigalian). We reconstructed the paleotemperature using the δ18O value analysed from accretionary growth sections of bivalve Ostrea angulate from the studied localities. On comparing the δ18O value of both the formations, we found a significant difference between the two; younger Chhasra formation revealed a much more negative value compared to those of older Khari Nadi formation. This indicates a climatic shift towards higher temperature in Lower Miocene of India. This climatic warming coincides with change in bivalve diversity and paleoecology of shallow marine deposits from this area. The rarefied family diversity of bivalves shows a decrease in overall diversity from Khari Nadi to Chhasra formation. While Khari Nadi formation is represented by families including Pectinidae, Ostreidae, Veneroidae, Tellinidae, Arcidae, Cardiidae, Plicatulidae, Glycymeridae, Chhasra formation only has Pectinidae, Ostreidae, Tellinidae, Cardiidae, Plicatulidae, Mellidae. The community structure also changes with nearly a four fold increase in the dominance of Ostreidae from Khari Nadi to Chhasra Formation. This coupling of decreasing diversity and increasing dominance could have been triggered by the change in temperature as indicated by the isotopic signature.