Green River Formation

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Green River Formation
Stratigraphic range: Eocene, 53.5–48.5Ma
Type Geological formation
Lithology
Primary varied
Other see text
Location
Region Rocky Mountains
Country United States
Type section
Named for Green River (Utah)

The Green River Formation is an Eocene geologic formation that records the sedimentation in a group of intermountain lakes in three basins along the present-day Green River in Colorado, Wyoming, and Utah. The sediments are deposited in very fine layers, a dark layer during the growing season and a light-hue inorganic layer in the dry season. 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 for the Green River, a tributary of the Colorado River. The three separate basins lie 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
  • the largest area, in northeastern Utah and western Colorado south of the Uintas, known as Lake Uinta

Fossil Butte National Monument in Lincoln County, Wyoming is in a part of the formation known as Fossil Lake because of its abundance of exceptionally well preserved fish fossils.

Lithology and formation[edit]

The formation of intermontane basin / lake environments during the Eocene resulted from mountain building and uplift of the Rocky Mountains (late Cretaceous Sevier orogeny and the Paleogene Laramide orogeny). Tectonic highlands supplied the Eocene sedimentary basins with sediment from all directions: the Uinta Mountains in the center; the Wind River Mountains to the north; the Front Range, Park Range and Sawatch Range of the Colorado Rockies to the east; the Uncompahgre Plateau and the San Juan Mountains to the south and finally, the Wasatch Mountains of Utah and the ranges of eastern Idaho to the west.

The lithology of the lake sediments is varied and includes sandstones, mudstones, siltstones, oil shales, coal beds, saline evaporite beds, and a variety of lacustrine limestones and dolostones. Volcanic ash layers within the various sediments from the then active Absaroka Volcanic field to the north in the vicinity of Yellowstone and the San Juan volcanic field to the southeast provide dateable horizons within the sediments.

The trona (hydrated sodium bicarbonate carbonate) beds of Sweetwater County, Wyoming are noted for a variety of rare evaporite minerals. The Green River Formation, is the type locality for eight rare minerals: bradleyite, ewaldite, loughlinite, mckelveyite-(Y), norsethite, paralabuntsovite-Mg, shortite and wegscheiderite. It also has a natural occurrence of moissanite (SiC) and 23 other valid mineral species.[2]

Cyclicity[edit]

The beds display a pronounced cyclicity, with the precession, obliquity, and eccentricity orbital components all clearly detectable. This enables the beds to be internally dated with a high degree of accuracy, and astrochronological dates agree very well with radiometric dates.[3]

Fossil zones[edit]

Diplomystus (left) and Knightia (right), two fossil fish from one of the lake beds in the Green River Formation

Within the Green River Formation of southwest Wyoming in the area known as Fossil Lake, two distinct zones of very fine-grained lime muds are particularly noted for preserving a variety of complete and detailed fossils. These layers are an Eocene Lagerstätte, a rare place where conditions were right for a rich accumulation of undisturbed fossils. The most productive zone—called the split fish layer—consists of a series of laminated or varved lime muds about 6 ft (1.8 m) thick, which contains abundant fish and other fossils. These are easily split along the layers to reveal the fossils. This thin zone represents some 4000 years of deposition. The second fossil zone, the 18 inch layer, is an unlaminated layer about 18 in (46 cm) thick that also contains abundant detailed fossils, but is harder to work because it is not composed of fissile laminae.

Diplomystus dentatus Prepared by Fossil Shack from the Green River Formation Split Fish Layer

The limestone matrix is so fine-grained that fossils include rare soft parts of complete insects and fallen leaves in spectacular detail. More than twenty-two orders of insects are represented in the Green River collection at the Smithsonian Institution in Washington, D.C., alone.

Fish fossils of Diplomystus and Knightia are found in Fossil Lake but not in Lake Gosiute. Only Lake Gosiute has fossils of catfish (Ictaluridae and Hypsidoridae) and suckers (Catostomidae). The catfish are found mostly in the deepest parts of the lake.[4][5]

Unidentified bird from the Green River Formation with preserved feathers
Stromatolite fossil from the Eocene Lake Gosuite, Laney Member, Green River Formation of south-western Wyoming

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 old.[6] This span of time includes the 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, receiving sediments from the Uinta highland and the Rocky Mountains to the east and north. 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, so leaves of palms, ferns and sycamores, some showing the insect damage they had sustained during their growth, were covered with fine-grained sediment and preserved. Insects were preserved whole, even delicate wing membranes and spider spinnerets.

Vertebrates were preserved too, including the scutes of Borealosuchus, the crocodile that was an early clue to the mild Eocene climate of Western North America. Fish are common. The fossils of the herring-like Knightia, sometimes in dense layers, as if a school had wandered into anoxic water levels and were overcome, are familiar to fossil-lovers and are among the most commonly available fossils on the commercial market. There was one indigenous freshwater stingray, Heliobatis. Approximately sixty vertebrate taxa in all have been found at Green River. Besides fishes they include at least eleven species of reptiles, and some birds and one armadillo-like mammal, Brachianodon westorum, with some scattered vertebrae of others, like the dog-sized Meniscotherium and Notharctus, one of the first primates. The earliest known bats (Icaronycteris index ,[7] and Onychonycteris finneyi[8]), already full-developed for flight, are found here. Even a snake, Boavus idelmani, found its way into a lake and was preserved in the mudstone.

Discovery of the fossil beds[edit]

The first documented records of (invertebrate) fossils from what is now called the Green River Formation are in the journals of early missionaries and explorers such as S. A. Parker, 1840, and J. C. Fremont, 1845.[9] Geologist Dr. John Evans collected the first fossil fish, described as Culpea humilis (later renamed Knightia eocaena), from the Green River beds in 1856.[10] Edward Drinker Cope collected extensively from the area and produced several publications on the fossil fish from 1870 onwards.[9] Ferdinand Vandeveer Hayden (geologist-in-charge of the United States Geological and Geographical Survey of the Territories, the forerunner of the United States Geological Survey) first used the name "Green River Shales" for the fossil sites in 1869.[9]

Millions of fish fossils have been collected from the area, commercial collectors operating from legal quarries on state and private land have been responsible for the majority of Green River vertebrate fossils in public and private collections all over the world. [11]

Oil shale[edit]

Oil Shale from the Mahogany Zone of the Green River Formation, Colorado. Weathered surface on right; fresh surface on left.

The Green River Formation contains the largest oil shale deposit in the world. It has been estimated that the oil shale reserves could be equal up to 3 trillion barrels (480 billion cubic metres) of shale oil, up to half of which may be recoverable by shale oil extraction technologies ("cooking" kerogen).[12][13][14][15][16] However, the above quoted estimate of 'recoverable' oil is in doubt, and challenged, by many renowned geologists because the technology for converting rock into an oil from the Green River shale deposit has not been developed, and it has never been profitably implemented at any significant scale.[17] While taking account the Green River oil shale the U.S. might indeed have greater oil resources than Saudi Arabia, U.S. conventional oil reserves (per the BP Statistical Review of World Energy) are only about 1/10th those of Saudi Arabia.[18]

Green River oil shale is lacustrine type which organic matter originates from the Eocene age blue-green algae (cyanobacteria).[13]

Notable mineral deposits[edit]

The unusual chemistry of the lakes in which it was deposited makes the Green River Formation a major source of sodium carbonate salts. In southwest Wyoming the formation contains the world's largest deposits of trona, and in Colorado, the world's largest deposits of nahcolite.[19] Another unusual mineral, currently only known from the Parachute Creek Member of this river formation[20] is the crystalline nickel porphyrin mineral abelsonite.

Notes[edit]

  1. ^ Bradley, W. H. The varves and climate of the Green River epoch: U.S. Geol. Survey Prof. Paper 158, pp 87–110, 1929.
  2. ^ Green River Formation locality data from Mindat, retrieved 11 June 2009 
  3. ^ Meyers, S. R. (2008), "Resolving Milankovitchian controversies: The Triassic Latemar Limestone and the Eocene Green River Formation", Geology 36 (4): 319–322, doi:10.1130/G24423A.1, retrieved 2008-04-24 
  4. ^ Morton, Glenn R., 2003, Creationist Misuse of the Green River Formation, accessed May 2, 2009
  5. ^ Grande, Lance; Paul Bucheim (1994), "Paleontological and Sedimentological Variation in Early Eocene Fossil Lake", Contributions to Geology, University of Wyoming 30: 45 
  6. ^ 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.
  7. ^ Jepsen, G. L. (1966), "Early Eocene bat from Wyoming", Science 154 (3754): 1333–9, Bibcode:1966Sci...154.1333J, doi:10.1126/science.154.3754.1333, PMID 17770307 
  8. ^ Nancy B. Simmons; Kevin L. Seymour; Jorg Habersetzer; Gregg F. Gunnell (2008), "Primitive Early Eocene bat from Wyoming and the evolution of flight and echolocation", Nature 451 (7180): 818–21, Bibcode:2008Natur.451..818S, doi:10.1038/nature06549, PMID 18270539 
  9. ^ a b c Lance Grande (1984), "Paleontology of the Green River Formation, with a review of the fish fauna", Bulletin of the Wyoming State Geological Survey (Laramie, WY), 63 2nd ed. 
  10. ^ J. Leidy (1856), "Notice of some remains of fishes discovered by Dr. John E. Evans", Proc. Acad. Nat. Sci. Phila.: 256 
  11. ^ Lance Grande (1984) Paleontology of the Green River Formation, with a review of the fish fauna. Geological Survey of Wyoming Bull. 63, p. 10
  12. ^ GAO: Unconventional Oil and Gas Production
  13. ^ a b Dyni, John R. (2006). Geology and resources of some world oil shale deposits. Scientific Investigations Report 2005–5294 (PDF). United States Department of the Interior, United States Geological Survey. Retrieved 2007-07-09. 
  14. ^ Annual Energy Outlook 2006 (PDF). Energy Information Administration. February 2006. p. 53. Retrieved 2008-04-18. 
  15. ^ Andrews, Anthony (2006-04-13). Oil Shale: History, Incentives, and Policy (PDF). Congressional Research Service. Retrieved 2007-06-25. 
  16. ^ NPR's National Strategic Unconventional Resource Model (PDF). United States Department of Energy. April 2006. Retrieved 2007-07-09. 
  17. ^ Pierrehumbert, Raymond. ""The Myth of "Saudi America"". Slate. Retrieved February 6, 2013. 
  18. ^ Rapier, Robert. "#1 - Does the U.S. Really Have More Oil than Saudi Arabia?". The Oil Drum. Retrieved January 3, 2013. 
  19. ^ George I. Smith and others (1973) Evaporites and brines, in United States Mineral Resources, US Geological Survey, Professional Paper 820, p. 206.
  20. ^ Mason, G. M.; Trudell, L. G.; Branthaver, J. F. (1989). "Review of the stratigraphic distribution and diagenetic history of abelsonite". Organic Geochemistry 14 (6): 585–594. doi:10.1016/0146-6380(89)90038-7.  (subscription required)

See also[edit]

References[edit]

External links[edit]