To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Portezuelo Formation

From Wikipedia, the free encyclopedia

Portezuelo Formation
Stratigraphic range: late Turonianearly Coniacian
~90.5–88.5 Ma
TypeGeological formation
Unit ofNeuquén Group
 Río Neuquén Subgroup
UnderliesLos Bastos Formation
OverliesLisandro Formation
Thickness95–130 m (312–427 ft)
Lithology
PrimarySandstone
OtherConglomerate, limestone
Location
Coordinates38°30′S 68°42′W / 38.5°S 68.7°W / -38.5; -68.7
Approximate paleocoordinates44°24′S 47°12′W / 44.4°S 47.2°W / -44.4; -47.2
RegionMendoza, Río Negro & Neuquén Provinces
CountryArgentina
ExtentNeuquén Basin
Type section
Named forSierra del Portezuelo
Portezuelo Formation (Argentina)

The Portezuelo Formation is a geologic formation of Late Cretaceous (Late Turonian to Early Coniacian) age, outcropping in the Mendoza, Río Negro and Neuquén provinces of Argentina.[1] It is the fourth-oldest formation in the Neuquén Group and the older of the two formations in the Río Neuquén Subgroup. Formerly, that subgroup was treated as a formation, and the Portezuelo Formation was known as the Portezuelo Member.[2]

Description

The type locality of the Portezuelo Formation is the mountain range known as Sierra del Portezuelo in Neuquén Province.[3] This formation conformably overlies the Lisandro Formation of the Río Limay Subgroup. In the top layers it grades into the Plottier Formation, the younger formation within the Río Neuquén Subgroup.

Sandstones and siltstones, probably deposited under fluvial conditions, make up the Portezuelo Formation. There are also occasional cemented claystone deposits, as well as numerous paleosols (fossil soils). The formation varies between 95 and 130 metres (312 and 427 ft) thick throughout its range.[2][4]

Fossil content

Megaraptor namunhuaiquii
Neuquenraptor argentinus

Many dinosaur fossils have recently been described from this formation, as well as remains of several other types of animals:

See also

References

  1. ^ a b Portezuelo Formation at Fossilworks.org
  2. ^ a b Sánchez et al., 2006
  3. ^ Wichmann, 1929
  4. ^ Leanza et al., 2004
  5. ^ a b c d Agnolin et al., 2006
  6. ^ Porfiri et al., 2007
  7. ^ Paulina-Carabajal and Currie, 2017
  8. ^ Baiano, Mattia A.; Pol, Diego; Bellardini, Flavio; Windholz, Guillermo J.; Cerda, Ignacio A.; Garrido, Alberto C.; Coria, Rodolfo A (2022-09-05). "Elemgasem nubilus: a new brachyrostran abelisaurid (Theropoda, Ceratosauria) from the Portezuelo Formation (Upper Cretaceous) of Patagonia, Argentina". Papers in Palaeontology. 8 (5): e1462. doi:10.1002/spp2.1462.

Bibliography

This page was last edited on 8 June 2023, at 18:12
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.