Cambay amber
The Cambay amber are deposits of amber that are located in Cambay, western India that dates back to the early Eocene epoch around 52-50 million years ago. It occurs in lignitic and muddy sediments concentrated by near-shore chenier systems.
The amber was being deposited during an important time in Earth's history as the peak of the Early Eocene Climatic Optimum was occurring. It was also deposited during a geologically and tectonically important time in the history of India. At this time, India was colliding into the continent of Asia undoubtably causing significant biotic interchange between both landmasses with India acting as a “biotic ferry”. This means that the Cambrey amber deposits could be helpful in aiding in the understanding of the biotic interchange between India and Asia during this time.
During India's drift northwards, it triggered extensive volcanism causing extinction events on the subcontinent. This is likely what lead to the disappearance of many lineages originating from Gondwana and explaining why many species originate from Laurasia.