A variety of trees, including cypress, maple, pine, poplar, and sequoia, produced copious quantities of resin which over millions of years fossilized into amber.
These resin-producing trees were particularly abundant during this period, and their resins were often buried underground, where they were preserved over time.
In addition, the climate during the Cretaceous period was generally warmer and more humid than it is today, which created ideal conditions for the formation of amber.