Sobral Formation

Summary

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

Sobral Formation
Stratigraphic range: Danian
~66–61.6 Ma
TypeGeological formation
Unit ofMarambio Group
UnderliesCross Valley & La Meseta Formations
OverliesLopez de Bertodano Formation
Thickness250 m (820 ft)
Lithology
PrimarySiltstone, mudstone
OtherConcretion, sandstone
Location
Coordinates64°18′S 56°42′W / 64.3°S 56.7°W / -64.3; -56.7
Approximate paleocoordinates63°12′S 66°36′W / 63.2°S 66.6°W / -63.2; -66.6
RegionSeymour Island, James Ross Island group
CountryAntarctica

Geologic map of Seymour Island, Antarctica with the Sobral Formation in brown

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 edit

References edit

  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 edit

  • Baldoni M. A., Barreda V. D. (1986). "Estudio palinológico de las formaciones López de Bertodano y Sobral, Isla Vicecomodoro Marambio, Antártida". Boletín del IG-USP, Serie Científica. 17 (17): 89–98. doi:10.11606/issn.2316-8986.v17i0p89-96.
  • Filkorn H. F. (1994). "Fossil scleractinian corals from James Ross Basin, Antarctica". Antarctic Research Series. 65: 1–96.
  • Poole I., Mennega A. M. W., Cantrill D. J. (2003). "Valdivian ecosystems in the Late Cretaceous and Early Tertiary of Antarctica: further evidence from myrtaceous and eucryphiaceous fossil wood" (PDF). Review of Palaeobotany and Palynology. 124 (1–2): 9–27. doi:10.1016/s0034-6667(02)00244-0. hdl:1874/31608. S2CID 129281012.{{cite journal}}: CS1 maint: multiple names: authors list (link)