Hidden Lake Formation

Last updated
Hidden Lake Formation
Stratigraphic range: Coniacian [1]
Type Geological formation
Unit of Gustav Group
Underlies Santa Marta Formation
Overlies Whisky Bay Formation
Lithology
Primary Sandstone
Other Siltstone
Location
Coordinates 63°00′S57°00′W / 63.0°S 57.0°W / -63.0; -57.0
Approximate paleocoordinates 63°06′S63°54′W / 63.1°S 63.9°W / -63.1; -63.9
Region James Ross Island, James Ross Island group
Country Argentine Antarctica, British Antarctic Territory, Chilean Antarctic Territory
Type section
Named forHidden Lake
Wfm antarctic peninsula islands.png
Map of James Ross Island group
James Ross Island is number 2

The Hidden Lake Formation is a Late Cretaceous geologic formation in Antarctica. The sandstones and siltstones of the formation were deposited in a deltaic environment.

Contents

Indeterminate megalosaur remains have been recovered from it. [2] Also many plant fossils and ichnofossils of Planolites sp. and Palaeophycus sp. have been found in the formation. [3]

Paleofauna

Flora

See also

References

  1. Crame, J. A.; Pirrie, D.; Riding, J. B. (2006). "Mid-Cretaceous stratigraphy of the James Ross Basin, Antarctica" . Geological Society, London, Special Publications. 258 (1): 7–19. Bibcode:2006GSLSP.258....7C. doi:10.1144/GSL.SP.2006.258.01.02. ISSN   0305-8719.
  2. 1 2 Weishampel, et al. (2004). "Dinosaur distribution" pp. 517–607. in Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp.  ISBN   0-520-24209-2. " pp. 517–607.
  3. 1 2 3 Hidden Lake at Fossilworks.org
  4. Sakala, Jakub; Vodrážka, Radek (August 2014). "A new species of Antarctoxylon : a contribution to the early angiosperm ecosystem of Antarctica during the late Cretaceous". Antarctic Science. 26 (4): 371–376. Bibcode:2014AntSc..26..371S. doi: 10.1017/S095410201300076X . ISSN   0954-1020.
  5. 1 2 3 4 Kvaček, Jiří; Sakala, Jakub (2011-06-01). "Late Cretaceous flora of James Ross Island (Antarctica) – preliminary report". Czech Polar Reports. 1 (2): 96–103. doi: 10.5817/CPR2011-2-9 . ISSN   1805-0697.

Further reading