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The Hadrosaurus foulkii Leidy Site is a historic paleontological site in Haddonfield, Camden County, New Jersey.Now set in state-owned parkland, it is where the first relatively complete set of dinosaur bones were discovered in 1838, and then fully excavated by William Parker Foulke in 1858.
The fossil was being auctioned in the United States, and was returned to Mongolia in 2013. [22] The holotype specimen of the dinosaur Halszkaraptor had been obtained through the fossil trade by 2011. Due to its provenance, several scientists initially expressed concern that it was a hoax, but scanning suggests the specimen was not tampered with.
This list of fossil sites is a worldwide list of localities known well for the presence of fossils. Some entries in this list are notable for a single, unique find, while others are notable for the large number of fossils found there.
Author Rufus Johnson has described one Neogene marl pit near Aurora in Beaufort County as the most famous fossil site in the entire state. This single fossils site preserves a Neogene fauna that included coral, sand dollars , sea shells, sea urchins , fish remains, seals , sharks with huge teeth, and fossils from whales .
The Moroccan fossil trade is the large industry surrounding the excavation, preparation and international sale of fossils from Morocco. Morocco contains some of the world's richest fossil sites and has seen international interest from fossil collectors since the early 20th century.
Oklahoma was a terrestrial environment for most of the ensuing Mesozoic era. [3] The Late Triassic Dockum Group of western Oklahoma preserved remains of archosaurs and temnospondyls, although its fossil record is restricted to a narrow region of the panhandle and is far sparser than the equivalent records in Texas, New Mexico, and Arizona. [98]
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A study of fossil pollen showed that much of China was woody shrubland, with plants such as saltbush, mormon tea (Ephedra), and nitre bush (Nitraria), all adapted to arid environments. Trees were rare, and concentrated near groundwater. [51]
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