Sobral Formation Explained

Sobral Formation
Type:Geological formation
Age:Danian
~
Period:Danian
Prilithology:Siltstone, mudstone
Otherlithology:Concretion, sandstone
Region:Seymour Island, James Ross Island group
Country:Antarctica
Coordinates:-64.3°N -56.7°W
Paleocoordinates:-63.2°N -66.6°W
Underlies:Cross Valley & La Meseta Formations
Overlies:Lopez de Bertodano Formation
Unitof:Marambio Group
Thickness:250m (820feet)
Map:Geologic map of Seymour Island, Antarctica.png

The Sobral Formation is a palaeontological formation located in Antarctica. It dates to the Danian stage of the Lower Paleocene period.[1]

Spectacular fossils documenting marine and terrestrial ecosystems soon after the (non-avian) dinosaurs became extinct at the Cretaceous-Paleogene boundary are found in this formation.[2] One of the most significant sites is on Seymour Island.

See also

Further reading

Notes and References

  1. Bowman, V. . The Paleocene of Antarctica: Dinoflagellate cyst biostratigraphy, chronostratigraphy and implications for the palaeo-Pacific margin of Gondwana . 2016 . Gondwana Research . 38 . 132–148 . 10.1016/j.gr.2015.10.018 . Ineson, J. . Riding, J. . Crame, J. . Francis, J. . Condon, D. . Whittle, R. . Ferraccioli, F.. 2016GondR..38..132B . free .
  2. Crame, J.A. . The Early Origin of the Antarctic Marine Fauna and Its Evolutionary Implications . 2014 . PLOS ONE . 7 . 12 . e114743 . 10.1371/journal.pone.0114743 . Beu, A.G. . Ineson J.R. . Francis J.A. . Whittle R.J. . Bowman V.C.. 4262473 . 25493546. 2014PLoSO...9k4743C . free .