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The Green River Formation is an Eocene rock formation on the eastern side of the Rocky Mountains.^[1] It gets 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 five million year period, between 53.5 and 48.5 million years ago (mya).^[2] 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.^[1]

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 many 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.^[3] 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.^[3]

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 show insect damage got during their growth. They 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

Reference

↑ ^1.0 ^1.1 Bradley W.H. 1929. The varves and climate of the Green River epoch: U.S. Geol. Survey, Professional paper #158, pp 87–110.
↑ Smith M.E; Singer B & Carroll, A. 2003. 40Ar/39Ar geochronology of the Eocene Green River Formation, Wyoming. Geological Society of America Bulletin, 115(5), 549-565.
↑ ^3.0 ^3.1 USGS Scientific Investigations Report 2005–5294, Geology and resources of some world oil-shale deposits