Buen Formation

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Sub-unitsUpper & lower members
Buen Formation
Stratigraphic range: Cambrian Series 2 (Atdabanian)
~520–513 Ma
TypeFormation
Unit ofSirius Passet
Sub-unitsUpper & lower members
UnderliesHans Tavsen icecap
OverliesPortfjeld Formation
ThicknessUp to 700 m (2,300 ft)
Lithology
PrimaryMudstone
OtherSandstone, shale
Location
Coordinates83°06′N 33°48′W / 83.1°N 33.8°W / 83.1; -33.8
Approximate paleocoordinates22°06′S 49°00′W / 22.1°S 49.0°W / -22.1; -49.0
RegionPeary Land
CountryGreenland
ExtentFranklinian Basin
Type section
LocationSouthern Peary Land
Buen Formation is located in Greenland
Buen Formation
Buen Formation
Buen Formation
Buen Formation
Buen Formation
Buen Formation
Buen Formation
Buen Formation (Greenland)

The Buen Formation is a geologic formation and Lagerstätte in Peary Land, North Greenland. The shale preserves fossils dating back to the Early Cambrian period (Atdabanian in the local timescale, about 520 to 513 Ma).[1]

Paleogeography

Geologic map of Sirius Passet with the Buen Formation shown in black

The oldest Cambrian series of the area was deposited in the Franklinian Basin and is poorly exposed in fragmentary, heavily metamorphosed outcrops in Peary Land. It was emplaced during the Ellesmerian orogeny.[2][3]

Cambrian paleogeography with the Buen Formation in orange

During the Cambrian, Greenland was located in the southern tropical to temperate region. The Buen Formation forms part of the southern shelf succession of the Franklinian Basin of North Greenland and the Canadian Arctic Islands. The formation, approximately 325 metres (1,066 ft) thick, consists of a lower, sand−dominated, member overlain by an upper member dominated by dark grey−green mudstones and siltstones in its type area in southern Peary Land. It thickens to around 700 metres (2,300 ft) in northern Peary Land where it comprises a mud−rich transitional succession into deep water trough deposits of the Polkorridoren Group. Dark grey to black mudstones form part of this transitional succession from the shelf to the slope. To the south they lie in faulted contact with pale dolomites of the underlying Portfjeld Formation, and to the north with bioturbated mudstones and sandstones of the Buen Formation.[4]

Fossil content

See also

References

Further reading

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