Golden Valley Formation
Stratigraphic range: Late Paleocene- Early Eocene ( Clarkforkian- Wasatchian) ~57–52  Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓
Type	Geological formation
Sub-units	Bear Den & Camels Butte Members
Underlies	White River Group
Overlies	Sentinel Butte Formation
Thickness	up to 122 metres (400 ft) [1]
Lithology
Primary	Claystone, mudstone, siltstone, sandstone
Other	Lignite, conglomerate
Location
Coordinates	48°30′N 102°42′W / 48.5°N 102.7°W / 48.5; -102.7
Approximate paleocoordinates	52°54′N 82°12′W / 52.9°N 82.2°W / 52.9; -82.2
Region	North Dakota
Country	United States
Extent	Williston Basin
Type section
Named for	Golden Valley, North Dakota
Named by	Benson & Laird [2]
Year defined	1947
Golden Valley Formation (the United States) Show map of the United States Golden Valley Formation (North Dakota) Show map of North Dakota

The Golden Valley Formation is a stratigraphic unit of Late Paleocene to Early Eocene age in the Williston Basin of North Dakota. ^[3] It is present in western North Dakota and was named for the city of Golden Valley by W.E. Benson and W.M. Laird in 1947. ^[2] It preserves significant assemblages of fossil plants ^[3] and vertebrates, ^[4] as well as mollusk and insect fossils. ^{[3] [4]}

Stratigraphy

The Golden Valley Formation is present as a series of outliers in western North Dakota. ^[5] It is underlain by the Sentinel Butte Formation and unconformably overlain by the White River Group. ^[1] It reaches thicknesses of up to 122 metres (400 ft) and is subdivided into two members: the Bear Den Member (lower) and the Camels Butte Member (upper). ^[1]

Lithologies

The base of the Bear Den Member consists of kaolinitic claystone, mudstone and sandstone that weather to white, light grey, orange, and purple. ^[1] These are overlain by grey or brownish carbonaceous sediments and, in some areas, a bed of lignite (the Alamo Bluff lignite). ^[3] In places the sequence is capped by a siliceous bed (the Taylor bed ^[3]) that represents a weathering surface or paleosol. ^[1] The Bear Den Member reaches a maximum thickness of about 15 metres (50 ft). ^[1]

The Camels Butte Member consists of montmorillonitic ^[3] and micaceous claystone, siltstone, lignite, poorly cemented sandstone and conglomerate. ^{[1] [3]} The upper part includes a massive fluvial sandstone that caps many of the major buttes in southwestern North Dakota. ^[1] The Camels Butte Member reaches a maximum thickness of about 107 metres (350 ft). ^[1]

Depositional environment

The Golden Valley Formation was deposited in a broad swampy lowland crossed by fluvial channels. ^[3] Deposition occurred during late Paleocene ( Clarkforkian) to early Eocene ( Wasatchian) time, ^[3] a period that spans the Paleocene-Eocene Thermal Maximum. ^[6]

Paleontology

Plant fossils collected from throughout the formation include floating and rooted aquatic plants such as Salvinia, Nelumbo and Isoetes, and lowland forest plants such as the ferns Onoclea and Osmunda, the conifers Glyptostrobus and Metasequoia, and the dicots Platanus and Cercidiphyllum. ^[3]

The vertebrate fossils have come primarily from the upper, early Eocene Camels Butte Member. They include the remains of mammals such as Coryphodon, Hyracotherium, Homogalax, Sinopa, Didymictis, Hyopsodus, Paramys and others; there are also remains of fish, amphibians, and reptiles such as Trionyx, Peltosaurus, and four genera of crocodilians. ^{[3] [4]}

Invertebrate fossils include shells of freshwater mollusks such as Viviparus, Unio, Hydrobia, and Planorbis, and the wing casing of a crabid beetle. ^{[3] [4]}

References

Bibliography

• Hickey, L. J. 1977. Stratigraphy and paleobotany of the Golden Valley Formation (Early Tertiary) of western North Dakota. Geological Society of America Memoir 150. 1–183. . ISBN  0-8137-1150-9