Green River Formation facts for kids
The Green River Formation is an Eocene rock formation on the eastern side of the Rocky Mountains. It records sediment from a group of intermountain lakes. Its fine fossils make this a lagerstätte, a place of exceptional preservation.
The various fossil beds of the Green River Formation span a 5 million year period, dating to between 53.5 and 48.5 million years ago (mya). During this period the climate moved from the moist early Eocene climate and the slightly drier mid-Eocene.
The sediments are deposited in very fine layers, in pairs: a dark layer from the growing season, and a light-hue inorganic layer in winter.
Each pair of layers is called a varve and represents one year. The sediments of the Green River Formation present a continuous record of six million years. The mean thickness of a varve here is 0.18 mm, with a minimum thickness of 0.014 mm and maximum of 9.8 mm.
The sedimentary layers were formed in a large area named after the present-day Green River, a tributary of the Colorado River. The formation is in three separate basins around the Uinta Mountains of northeastern Utah:
- an area in northwestern Colorado east of the Uintas
- a larger area in the southwest corner of Wyoming just north of the Uintas known as Lake Gosiute
- another area, in Fossil Butte National Monument, Lincoln County, Wyoming is Fossil Lake. It has exceptionally well preserved fish fossils. The most productive zone — the split fish layer — is a series of laminated or varved lime muds about 6 ft (1.8 m) thick. They contains abundant fish and other fossils. The rock is easily split along the layers to reveal the fossils. This thin zone took about 4000 years to deposit.
- the largest area, in northeastern Utah and western Colorado south of the Uintas, known as Lake Uinta
Conditions at the time
The formation has many evaporites – minerals formed by the evaporation of lakes. This suggests that high salinity was one of the causes of the superb fossilisation.
Another factor was the frequent ash falls from nearby volcanoes. Rapid burial also prevents normal decomposition.
Climate
Fossils preserved suggest that the region was a low, subtropical, freshwater basin when the sediments accumulated.
The Green River fossils show a transition between the moist early Eocene climate and the slightly drier mid-Eocene. The climate was moist and mild enough to support crocodiles, which do not tolerate frost, and the lakes were surrounded by sycamore forests. As the lake configurations shifted, each Green River location is distinct in character and time. The lake system formed over underlying river deltas and shifted in the flat landscape with slight tectonic movements
Oil shale
The Green River Formation contains the largest oil shale deposits in the world. The 213 billion tons of oil shale contain an estimated 2.38 × 10¹¹ m³ (1.5 trillion US barrels) of shale oil. This is a tribute to the high volume of organic material that was buried. The source of the organic material was probably cyanobacteria, which thrive in warm alkaline lake conditions.
Fossils
The lagerstätten formed in anoxic conditions in the fine carbonate muds that formed in the lakebeds. Lack of oxygen slowed bacterial decomposition and kept scavengers away. Leaves of palms, ferns and sycamores, some showing the insect damage got during their growth, were covered with fine-grained sediment and preserved. Insects were preserved whole, even delicate wing membranes and spider spinnerets.
The fauna included fish, alligators, bats, turtles, dog-sized horses, insects, and many other species of plants and animals
Images for kids
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Heliobatis radians (stingray), Green River Formation, Fossil Butte National Monument.
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Diplomystus (left) and Knightia (right), two fossil fish from one of the lake beds in the Green River Formation
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Crocodile lizard (Shinisauridae) preserved as a mineralized film; Parachute Creek Member in the Uintah Basin, Utah.
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Diplomystus dentatus from the Green River Formation Split Fish Layer
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Unidentified bird from the Green River Formation with preserved feathers
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Stromatolite fossil from the Eocene Lake Gosuite, Laney Member, Green River Formation of south-western Wyoming
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Oil Shale from the Mahogany Zone of the Green River Formation, Colorado. Weathered surface on right; fresh surface on left.
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Green River Formation Oil Gas Fields within the Uinta Basin and Piceance Basin
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Unnamed middle member, Green River Formation along U.S. Highway 191 near Indian Canyon Summit, Duchesne County, Utah.
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Unnamed upper member, saline facies, Green River Formation, along U.S. Highway 191 in lower Indian Canyon, Duchesne County, Utah. Left: typical exposure; right: exposure in roadcut.
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Transition facies, unnamed upper member of the Green River Formation along U.S. Highway 191, lower Indian Canyon, Duschesne County, Utah.
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Tranisition facies exposed in road cut along U.S. Highway 191, lower Indian Canyon, Duchesne County, Utah.
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See also
In Spanish: Formación Green River para niños
