"Approximately 280 million years ago, during the late Permian period, the region now known as Gascoyne Junction was submerged under a vast, shallow sea. This marine environment provided ideal conditions for the growth and proliferation of crinoids. The sedimentary layers that formed during this period encapsulated the remains of these marine creatures, preserving them as fossils. The specific conditions of sedimentation, combined with mineralization processes over millions of years, have resulted in the exceptional preservation of Jimbacrinus crinoid fossils."
The Fossils of Jimbacrinus Crinoid: A Glimpse into Prehistoric Marine Life
The Fossils of Jimbacrinus Crinoid: A Glimpse into Prehistoric Marine Life