Mulichinco Formation Explained

Mulichinco Formation
Period:Valanginian
Age:Valanginian
~
Type:Geological formation
Prilithology:Mudstone, siltstone, sandstone
Otherlithology:Limestone
Unitof:Mendoza Group
Underlies:Agrio Formation
Overlies:Vaca Muerta
Thickness:200-
Coordinates:-38.5°N -70.2°W
Paleocoordinates:-37.8°N -33.5°W
Region:Neuquén Province
Country:Argentina
Extent:Neuquén Basin

The Mulichinco Formation is a geological formation in Argentina. It is Valanginian in age and is predominantly terrestrial, being deposited at a time of marine regression in the Neuquén Basin, and predominantly consists of siliciclastic rocks.[1]

Fossil content

Dinosaur remains have been found in the formation, including those of the dicraeosaurid Pilmatueia[2] and carcharodontosaurid Lajasvenator.[3] Flora recovered from the formation includes the tree fern Tempskya dernbachii and horsetail Equisetites.[4]

References

Bibliography

Notes and References

  1. Schwarz et al., 2005
  2. Coria et al., 2018
  3. Coria et al., 2019
  4. Martínez. Leandro C.A.. Olivo. Mariana S.. August 2015. Tempskya in the Valanginian of South America (Mulichinco Formation, Neuquén Basin, Argentina) — Systematics, palaeoclimatology and palaeoecology. Review of Palaeobotany and Palynology. en. 219. 116–131. 10.1016/j.revpalbo.2015.04.002. 2015RPaPa.219..116M . 11336/49538. free.