Dinosaur Beds
Stratigraphic range:
TypeGeological formation
Unit ofLupata Group
Sub-unitsLower Member, Upper Member
UnderliesUnconformity with Pliocene Chiwondo Beds
OverliesPrecambrian metamorphic basement
ThicknessUpper member is 210 m (690 ft) thick in vicinity of CD-9 locality
Lithology
PrimarySandstone, siltstone, mudstone
Location
Coordinates10°17′S 34°02′E / 10.28°S 34.04°E / -10.28; 34.04
RegionNorthern Region
Country Malawi
ExtentKaronga District
Dinosaur Beds is located in Malawi
Dinosaur Beds
Dinosaur Beds (Malawi)

The Dinosaur Beds is a geological formation in Malawi whose strata date back to the Early Cretaceous. The age of the deposit is poorly constrained, but is likely to date from the Barremian to Aptian.[1] Dinosaurs, turtles and crocodylomorphs remains are among the fossils that have been recovered from the formation.[2] It is correlated with the Galula Formation in Tanzania. It consists of two members, a lower unfossiliferous member consisting of deep red stained sandstones, and an upper fossiliferous member consisting of white sands and grey to red mudstones and siltstones. The upper member is 210 m thick in the vicinity of the CD-9 locality.[3]

Vertebrate paleofauna

Invertebrate fauna

See also

References

  1. Widlansky, Sarah J.; Clyde, William C.; O'Connor, Patrick M.; Roberts, Eric M.; Stevens, Nancy J. (March 2018). "Paleomagnetism of the Cretaceous Galula Formation and implications for vertebrate evolution". Journal of African Earth Sciences. 139: 403–420. doi:10.1016/j.jafrearsci.2017.11.029. ISSN 1464-343X.
  2. Weishampel, David B; et al. (2004). "Dinosaur distribution (Early Cretaceous, Africa)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 571-573. ISBN 0-520-24209-2.
  3. WINKLER, DALE A.; GOMANI, ELIZABETH M.; JACOBS, LOUIS L. (2000). "COMPARATIVE TAPHONOMY OF AN EARLY CRETACEOUS SAUROPOD QUARRY, MALAWI, AFRICA". Paleont. Soc. Korea Special Publication. 4: 99–114.
  4. "Table 13.1," in Weishampel, et al. (2004). Page 269.
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