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Jorge
Velez Matthew Carrano, Ph.D. The fossils from Quarry Nine offer a unique window to the past; back to the real Jurassic Park |
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Paleoecology of the Late Jurassic
Morrison Formation based on microvertebrates from Quarry Nine The
paleoecology (ancient ecology) of the Late Jurassic (156 million years
ago) Morrison Formation is poorly understood, even though the formation
is one of the richest dinosaur-bearing rocks in the world. To be able
to understand this ancient ecosystem it is important to develop a
detailed study of the fossils found in the formation. For this study
the fossils collected from a quarry of the Morrison formation called
Quarry Nine were studied, highlighting the importance of the fossils
of small vertebrates as a tool for reconstructing the paleoecology.
The fossils collected from this quarry, yielded the single most important
collection of small vertebrate from the Late Jurassic. Therefore,
offering a unique insight into the Late Jurassic environment. Different
types of mammals, turtles, fishes, dinosaurs, frogs, salamanders,
lizards and crocodiles as well as freshwater snails and plants represent
the paleoenvironment from Quarry Nine. New additions to the list of
fossils vertebrates of Quarry Nine include one turtle, two fishes,
one lizard, one frog, one pterosaur (flying reptiles) and eight dinosaurs.
The occurrence of frogs and salamanders provide some evidence for
freshwater lacustrine conditions. This is also supported by the abundance
of turtle and crocodile remains and by the occurrence of freshwater
plant fossils. The Quarry Nine represented lacustrine environment
formed during seasonal wet and dry extremes, similar to the modern
environment in the Gran Chaco plain of central South America. This research was supported by a grant from the National Science Foundation Research Experiences for Undergraduates program, Award Number DBI-0243512. |