Sobral Formation

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Sobral Formation
Stratigraphic range: Danian
~66–61.6  Ma
O
S
D
C
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Pg
N
Type Geological formation
Unit of Marambio Group
Underlies Cross Valley & La Meseta Formations
Overlies Lopez de Bertodano Formation
Thickness250 m (820 ft)
Lithology
Primary Siltstone, mudstone
OtherConcretion, sandstone
Location
Coordinates 64°18′S56°42′W / 64.3°S 56.7°W / -64.3; -56.7
Approximate paleocoordinates 63°12′S66°36′W / 63.2°S 66.6°W / -63.2; -66.6
Region Seymour Island, James Ross Island group
Country Antarctica
Geologic map of Seymour Island, Antarctica.png
Geologic map of Seymour Island, Antarctica with the Sobral Formation in brown

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

Contents

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

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References

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

Further reading