The Shaximiao Formation has produced mainly
sauropods, but has also held numerous other dinosaur types, such as
theropods and
stegosaurians amongst others. In total, over 8,000 pieces of bone have been unearthed from the area – amounting to nearly 40
tonnes. The site was unknown until the early 1970s, when a Chinese gas company unearthed
Gasosaurus in 1972. It would be the first of the many dinosaurs to be uncovered from the area. Most specimens found are held at the
Zigong Dinosaur Museum which has been placed on the area during the mid-1980s. The site is currently a frequented "dinosaur-quarry", but the Shaximiao Formation once hosted a lush
forest, evidenced by
fossilised wood found alongside the dinosaur remains.
Paleontologists speculate that the area also had a lake that was fed by a large river. Dinosaur remains would have been swept toward the lake over millions of years, thus accounting for the hundreds of specimens found. Based on
biostratigraphy, the Lower Shaximiao Formation has been usually seen to date to 168 to 161 million years old, between the
Bathonian to
Callovian stages of the Mid Jurassic, while the Upper Shaximiao was thought to be Oxfordian in age. A paper by Wang et al. (2018), (recalibrated dates reported in Moore et al. (2020)), reported a
zircon U-
Pb age of 160.4 ± 0.4 mya for the lower part of the Shaximiao Formation, suggesting that the Shaximiao Formation is younger than previously thought. Contradicting this, U-Pb dates from a
tuff bed supports traditional Middle Jurassic age for the lower part of the formation, with an average age of around 166.0 ± 1.5 Ma. The top of the Shaximiao Formation has been believed to be the end of the
Tithonian age. == Dong Zhiming's research ==