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Chachao Formation: Difference between revisions

Coordinates: 35°00′S 69°42′W / 35.0°S 69.7°W / -35.0; -69.7
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=== Bibliography ===
=== Bibliography ===
* {{citation |last1=Gómez Dacal |first1=Alejandro R. |last2=Gómez Peral |first2=Lucía E. |last3=Spalletti |first3=Luis A. |last4=Sial |first4=Alcides N. |last5=Siccardi |first5=Aron |last6=Poiré |first6=Daniel G. |year=2018 |title=First record of the Valanginian positive carbon isotope anomaly in the Mendoza shelf, Neuquén Basin, Argentina: palaeoclimatic implications |url=http://www.andeangeology.cl/index.php/revista1/article/view/V45n2-3059/pdf |journal=[[Andean Geology]] |volume=45 |issue=2 |pages=111–129 |doi=10.5027/andgeoV45n2-3059 |accessdate=2019-02-22|hdl=11336/64562 |hdl-access=free }}
* {{citation |last1=Gómez Dacal |first1=Alejandro R. |last2=Gómez Peral |first2=Lucía E. |last3=Spalletti |first3=Luis A. |last4=Sial |first4=Alcides N. |last5=Siccardi |first5=Aron |last6=Poiré |first6=Daniel G. |year=2018 |title=First record of the Valanginian positive carbon isotope anomaly in the Mendoza shelf, Neuquén Basin, Argentina: palaeoclimatic implications |url=http://www.andeangeology.cl/index.php/revista1/article/view/V45n2-3059/pdf |journal=[[Andean Geology]] |volume=45 |issue=2 |pages=111–129 |doi=10.5027/andgeoV45n2-3059 |accessdate=2019-02-22|hdl=11336/64562 |hdl-access=free }}
* {{citation |first1=R. M. |last1=Palma |first2=S. G. |last2=Lanes |year=2001 |title=Shell Bed Stacking Patterns in the Chachao Formation (Early Valanginian) in Malargüe Area, Mendoza Province, Neuquen Basin, Argintina |journal=[[Carbonates and Evaporites]] |volume=16 |issue=2 |pages=168–180|doi=10.1007/BF03175834 |bibcode=2001CarEv..16..168P }}
* {{citation |first1=R. M. |last1=Palma |first2=S. G. |last2=Lanes |year=2001 |title=Shell Bed Stacking Patterns in the Chachao Formation (Early Valanginian) in Malargüe Area, Mendoza Province, Neuquén Basin, Argentina |journal=[[Carbonates and Evaporites]] |volume=16 |issue=2 |pages=168–180|doi=10.1007/BF03175834 |bibcode=2001CarEv..16..168P }}
* {{citation |first1=M. B. |last1=Aguirre Urreta |first2=P. P. |last2=Álvarez |year=1999 |title=The Berriasian genus ''Groebericeras'' in Argentina and the problem of its age |journal=[[Scripta Geologica]] |volume=3 |issue=Special Issue|pages=15–29}}
* {{citation |first1=M. B. |last1=Aguirre Urreta |first2=P. P. |last2=Álvarez |year=1999 |title=The Berriasian genus ''Groebericeras'' in Argentina and the problem of its age |journal=[[Scripta Geologica]] |volume=3 |issue=Special Issue|pages=15–29}}
* {{citation |first1=R. M. |last1=Palma |first2=M. P. |last2=Angeleri |year=1992 |title=Early Cretaceous serpulid limestones: Chachao Formation, Neuquen basin, Argentina |journal=[[Facies (journal)|Facies]] |volume=27 |issue=1 |pages=175–178|doi=10.1007/BF02536810 |bibcode=1992Faci...27..175P }}
* {{citation |first1=R. M. |last1=Palma |first2=M. P. |last2=Angeleri |year=1992 |title=Early Cretaceous serpulid limestones: Chachao Formation, Neuquen basin, Argentina |journal=[[Facies (journal)|Facies]] |volume=27 |issue=1 |pages=175–178|doi=10.1007/BF02536810 |bibcode=1992Faci...27..175P }}

Latest revision as of 15:26, 24 December 2024

Chachao Formation
Stratigraphic range: Valanginian
~140–136 Ma
TypeGeological formation
Unit ofMendoza Group
UnderliesAgrio Formation
OverliesVaca Muerta
Lithology
PrimaryLimestone
OtherMudstone
Location
Coordinates35°00′S 69°42′W / 35.0°S 69.7°W / -35.0; -69.7
Approximate paleocoordinates33°48′S 33°00′W / 33.8°S 33.0°W / -33.8; -33.0
RegionMendoza Province
CountryArgentina
ExtentNeuquén Basin
Chachao Formation is located in Argentina
Chachao Formation
Chachao Formation (Argentina)

The Chachao Formation is a geological formation in the Mendoza Province in northern Patagonian Argentina. It is Valanginian in age and is predominantly marine, being deposited at a time of marine transgression in the Neuquén Basin, and predominantly consists of carbonate rocks.

The formation belongs to the Mendoza Group, sediments deposited on the Mendoza Shelf. The formation overlies the Vaca Muerta and is overlain by the Agrio Formation.

Description

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A typical feature of the Chachao Formation is the dominance of oysters, many of them quite large e.g. Aetostreon latissimun, and others small, e.g. Ceratostreon minos. Different kinds of semi-infaunal soft bottom dwellers and swimming bivalves were recognized. Additional forms are represented by gastropods, ammonites (Olcostephanus curacoensis), and ichnofossils such as Thalassinoides sp. Serpulids are represented by the colonial Sarcinella sp., and the solitary form Parsimonia sp. The highly diverse fauna of the analyzed succession, made up with numerous stenohaline elements such as echinoderm, bryozoa, ammonite as well as serpulids and typical marine pelecypods indicate a fully marine environment.[1]

Fossil content

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The formation has provided the following fossils:[2]

References

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Bibliography

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  • Gómez Dacal, Alejandro R.; Gómez Peral, Lucía E.; Spalletti, Luis A.; Sial, Alcides N.; Siccardi, Aron; Poiré, Daniel G. (2018), "First record of the Valanginian positive carbon isotope anomaly in the Mendoza shelf, Neuquén Basin, Argentina: palaeoclimatic implications", Andean Geology, 45 (2): 111–129, doi:10.5027/andgeoV45n2-3059, hdl:11336/64562, retrieved 2019-02-22
  • Palma, R. M.; Lanes, S. G. (2001), "Shell Bed Stacking Patterns in the Chachao Formation (Early Valanginian) in Malargüe Area, Mendoza Province, Neuquén Basin, Argentina", Carbonates and Evaporites, 16 (2): 168–180, Bibcode:2001CarEv..16..168P, doi:10.1007/BF03175834
  • Aguirre Urreta, M. B.; Álvarez, P. P. (1999), "The Berriasian genus Groebericeras in Argentina and the problem of its age", Scripta Geologica, 3 (Special Issue): 15–29
  • Palma, R. M.; Angeleri, M. P. (1992), "Early Cretaceous serpulid limestones: Chachao Formation, Neuquen basin, Argentina", Facies, 27 (1): 175–178, Bibcode:1992Faci...27..175P, doi:10.1007/BF02536810
  • Aguirre Urreta, M.B (1989), "The Cretaceous decapod Crustacea of Argentina and the Antarctic Peninsula", Palaeontology, 32: 499–552