Cannabaceae

Gokwe Formation
Stratigraphic range: Early Cretaceous
TypeGeological formation
Sub-unitsWhite Sandstone Member
Lithology
PrimarySandstone
OtherLimestone
Location
Coordinates18°12′S 28°54′E / 18.2°S 28.9°E / -18.2; 28.9
Approximate paleocoordinates36°06′S 4°54′E / 36.1°S 4.9°E / -36.1; 4.9
RegionMidlands
Country Zimbabwe
Type section
Named forGokwe region
Gokwe Formation is located in Zimbabwe
Gokwe Formation
Gokwe Formation (Zimbabwe)

The Gokwe Formation is an Early Cretaceous geologic formation in Zimbabwe. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.[1] Sediments of the formation may have been laid down in a small shallow lake, carried by intermittent floods from a land surface surrounding the lake on which aeolian transport of sand took place. More likely the animals died on a dry lake bed, and their bones were exposed to a period of desiccation, later floods would scatter the fragments and incorporate them in sediment.[2]

See also

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References

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  1. ^ Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
  2. ^ Midlands at Fossilworks.org

Bibliography

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Further reading

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  • G. Bond and K. Bromley. 1970. Sediments with the remains of dinosaurs near Gokwe, Rhodesia. Palaeogeography, Palaeoclimatology, Palaeoecology 8:313-327

One thought on “Cannabaceae

  1. Well, that’s interesting to know that Psilotum nudum are known as whisk ferns. Psilotum nudum is the commoner species of the two. While the P. flaccidum is a rare species and is found in the tropical islands. Both the species are usually epiphytic in habit and grow upon tree ferns. These species may also be terrestrial and grow in humus or in the crevices of the rocks.
    View the detailed Guide of Psilotum nudum: Detailed Study Of Psilotum Nudum (Whisk Fern), Classification, Anatomy, Reproduction

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