Santa Cruz Formation
{{Short description|Geological formation in Patagonia}}
{{other uses}}
{{Infobox rockunit
| name = Santa Cruz Formation
| period = Miocene
| age = Burdigalian-Langhian
(Santacrucian-Friasian)
~{{fossil range|18|15.2}}
| image =Santa Cruz Formation strata.jpg
| imagesize =
| caption =
| type = Geological formation
| prilithology = *Tuff, claystone, mudstone (Estancia La Costa Member)
- Claystone, mudstone, sandstone (Estancia La Angelina Member)
| otherlithology =
| unitof =
| subunits = Estancia La Costa Member, Estancia La Angelina Member (coastal section)
| underlies = Cerro Boleadoras Formation
| overlies = Monte Léon Formation
| thickness = Over 295 metres
| area =
| map =Santa Cruz in Argentina (+Falkland hatched).svg
| map_caption =
Santa Cruz Province in Argentina, where the majority of the formation of exposed
| location =
| coordinates =
| region =
| extent = Austral Basin
| namedfor =
| namedby = Furque & Camacho
| year_ts = 1972
| location_ts = near Lago Argentino
| coordinates_ts =
| paleocoordinates_ts =
| region_ts =
| country_ts =
| thickness_ts =
}}
The Santa Cruz Formation is a geological formation in the Magallanes/Austral Basin in southern Patagonia in Argentina and adjacent areas of Chile. It dates to the late Early Miocene epoch, and is contemporaneous with the eponymous Santacrucian age of the SALMA (South American land mammal age) timescale.{{Cite book |last1=Matheos |first1=Sergio D. |title=Sedimentology and paleoenvironment of the Santa Cruz Formation |date=2012-10-11 |url=https://www.cambridge.org/core/product/identifier/9780511667381%23c19461-4-1/type/book_part |work=Early Miocene Paleobiology in Patagonia |pages=59–82 |editor-last=Vizcaíno |editor-first=Sergio F. |edition=1 |publisher=Cambridge University Press |doi=10.1017/cbo9780511667381.005 |isbn=978-0-511-66738-1 |access-date=2022-11-06 |last2=Raigemborn |first2=M. Sol |editor2-last=Kay |editor2-first=Richard F. |editor3-last=Bargo |editor3-first=M. Susana}}{{Cite journal |last1=Cuitiño |first1=José I. |last2=Vizcaíno |first2=Sergio F. |last3=Bargo |first3=M. Susana |last4=Aramendía |first4=Inés |date=2019-05-31 |title=Sedimentology and fossil vertebrates of the Santa Cruz Formation (early Miocene) in Lago Posadas, southwestern Patagonia, Argentina |url=http://www.andeangeology.cl/index.php/revista1/article/view/V46n2-3128 |journal=Andean Geology |language=en |volume=46 |issue=2 |pages=383–420 |doi=10.5027/andgeoV46n2-3128 |issn=0718-7106 |doi-access=free|hdl=11336/96343 |hdl-access=free }} The Santa Cruz Formation is known for its abundance of vertebrate fossils, including South American native ungulates (astrapotheres, litopterns, notoungulates),{{Cite book |last1=Cassini |first1=Guillermo H. |title=Paleobiology of Santacrucian native ungulates (Meridiungulata: Astrapotheria, Litopterna and Notoungulata) |date=2012 |url=https://www.cambridge.org/core/books/early-miocene-paleobiology-in-patagonia/paleobiology-of-santacrucian-native-ungulates-meridiungulata-astrapotheria-litopterna-and-notoungulata/85776FBE33085A8959D44D7331D5900E |chapter=Early Miocene Paleobiology in Patagonia: High-Latitude Paleocommunities of the Santa Cruz Formation |pages=243–286 |editor-last=Bargo |editor-first=M. Susana |place=Cambridge |publisher=Cambridge University Press |isbn=978-0-521-19461-7|last2=Cerdeño |first2=Esperanza |last3=Villafañe |first3=Amalia L. |last4=Muñoz |first4=Nahuel A. |editor2-last=Kay |editor2-first=Richard F. |editor3-last=Vizcaíno |editor3-first=Sergio F.}} as well as rodents, xenarthrans (armadillos, sloths, anteaters), and metatherians.
The formation extends from the Andes to the Atlantic coast. In its coastal section it is divided into two members, the lower, fossil rich Estancia La Costa Member, which consists predominately of tuffaceous deposits and fine grained mudrock, and the upper fossil-poor Estancia La Angelina Member, which consists of sedimentary rock, primarily mudrock, and sandstone. The environment of deposition was mostly fluvial, with the lowermost part of the Estancia La Costa Member being transitional between fluvial and marine conditions. The environment of the Estancia La Costa Member is thought to have been relatively warm and humid, but likely became somewhat cooler and drier towards the end of the sequence.
Stratigraphy
The Santa Cruz Formation is exposed in isolated outcrops across the Magallanes/Austral Basin extending from the Atlantic coast to the Andes, especially along the Santa Cruz River, as well as along the southern coastline of Santa Cruz Province.{{Cite journal |last1=Cuitiño |first1=José I. |last2=Sol Raigemborn |first2=M. |last3=Susana Bargo |first3=M. |last4=Vizcaíno |first4=Sergio F. |last5=Muñoz |first5=Nahuel A. |last6=Kohn |first6=Matthew J. |last7=Kay |first7=Richard F. |date=2021-04-07 |title=Insights on the controls on floodplain-dominated fluvial successions: a perspective from the Early–Middle Miocene Santa Cruz Formation in Río Chalía (Patagonia, Argentina) |url=https://pubs.geoscienceworld.org/jgs/article-abstract/178/4/jgs2020-188/595176/Insights-on-the-controls-on-floodplain-dominated|journal=Journal of the Geological Society |volume=178 |issue=4 |doi=10.1144/jgs2020-188 |bibcode=2021JGSoc.178..188C |s2cid=233779691 |issn=0016-7649|url-access=subscription }} While primarily located in Argentina, small outcrops are also found in Chile.Raúl Ugalde , Enrique Bostelmann , Karina E. Buldrini , and José Luis Oyarzún [https://www.researchgate.net/publication/282652427 Lithofacies, architecture, and depositional environments of the Santa Cruz Formation in Chilean Patagonia] (2015) XIV Congreso Geológico Chileno The base of the formation is defined by a marine regression event transitioning from the marine environment of the underlying Monte Léon Formation, which formed when large areas of Patagonia were submerged as a part of the Patagoniense Transgression.
The main source of sediment input to the basin was from the Andean orogeny to the west. The formation reaches a maximum thickness of over 295 meters, though the total thickness of the formation is strongly controlled by subsequent erosion and the 295 meters likely does not represent a complete sequence. The formation primarily consists of floodplain deposits. The lower parts of the formation have an abundance of tuffs and tuffaceous sediments. These likely originated from distant eruptions that were transported into the basin by aerial fallout, wind and/or river transport. The formation likely spans an approximately 3 million year interval in the late Early Miocene around 18 to 15.2 million years ago, during the Burdigalian and Langhian stages.
Paleoenvironment
The environment of the Santa Cruz Formation is thought to have been relatively warm and humid, including a mix of open savanna, gallery forests and semi-deciduous forests. Permanent bodies of water such as lakes, ponds and streams are likely to have been present.{{Cite journal |last1=Kay |first1=Richard F. |last2=Vizcaíno |first2=Sergio F. |last3=Bargo |first3=M. Susana |last4=Spradley |first4=Jackson P. |last5=Cuitiño |first5=José I. |date=August 2021 |title=Paleoenvironments and paleoecology of the Santa Cruz Formation (early-middle Miocene) along the Río Santa Cruz, Patagonia (Argentina) |journal=Journal of South American Earth Sciences |language=en |volume=109 |pages=103296 |doi=10.1016/j.jsames.2021.103296|s2cid=233693434 |doi-access=free |bibcode=2021JSAES.10903296K }}
Paleoflora
Paleofauna
= Invertebrates =
= Amphibians =
= Birds =
= Squamates =
class="wikitable" align="center" width="75%" |
Name
! Species ! Locality ! Material ! Notes ! Image |
---|
Pristidactylus{{Cite journal |last1=Albino |first1=Adriana |last2=Brizuela |first2=Santiago |last3=Vizcaíno |first3=Sergio |date=2017 |title=The southernmost fossil record of Squamates |url=https://brill.com/view/journals/amre/38/1/article-p15_2.xml |journal=Amphibia-Reptilia |volume=38 |issue=1 |pages=15–30 |doi=10.1163/15685381-00003078 |issn=0173-5373|hdl=11336/55451 |hdl-access=free }}
| rowspan="4" |Indeterminate | rowspan="2" |La Cueva | rowspan="2" |Fragmentary jaw bones | rowspan="2" |Originally assigned to the dubious genus "Erichosaurus" | |
Pleurodonta
| |
Tupinambis
|Monte León |Fragmentary dentaries and maxilla |A teiid lizard | |
Colubridae
|Cerro Observatorio |Partial trunk vertebrae |A snake | |
= Mammals =
== Meridiungulates ==
=== Astrapotheres ===
=== Litopterns ===
=== Notoungulates ===
== Xenarthrans ==
=== Pilosa ===
=== Cingulata ===
== Metatherians ==
== Rodents ==
class="wikitable" align="center" width="75%" |
Name
! Species ! Locality ! Material ! Notes ! Image |
---|
Acarechimys
|A. minutus A. minutissmus A. constans A. gracilis | | |A member of Octodontoidea | |
Acaremys{{Cite journal |last1=Arnal |first1=Michelle |last2=Pérez |first2=María Encarnación |last3=Deschamps |first3=Cecilia |date=2019-12-20 |title=Revision of the Miocene caviomorph rodents from the Río Santa Cruz (Argentinean Patagonia).|url=https://www.peapaleontologica.org.ar/index.php/peapa/article/view/299 |journal=Publicación Electrónica de la Asociación Paleontológica Argentina |language=en |volume=19 |issue=2 |doi=10.5710/PEAPA.25.09.2019.299 |issn=2469-0228|doi-access=free|hdl=11336/175184 |hdl-access=free }}
|A. murinus A. messor | | |A member of Acaremyidae (Octodontoidea) | |
Adelphomys
|A. candidus | | |A member of Octodontoidea | |
Dudumus
|Indeterminate, potentially new species | | |A member of Octodontoidea | |
Eocardia
|E. montana "E". excavata "E". fissa | | |A member of Cavioidea |
Neoreomys
|N. australis | | |A member of Cavioidea | |
Perimys
|P. erutus P. onustus P. incavatus | | |A member of Chinchilloidea |
Phanomys
|P. mixtus P. vetulus | | |A member of Cavioidea | |
Pliolagostomus
|P. notatus | | |A member of Chinchilloidea | |
Prolagostomus
|P. pusilllus | | |A member of Chinchilloidea | |
Prospaniomys
|Indeterminate, potentially new species | | |A member of Octodontoidea | |
Pseudoacaremys
|P. kramarzi | | |A member of the family Acaremyidae (Octodontoidea) | |
Schistomys
|S. erro | | |A member of Cavioidea | |
Sciamys
|S. principalis S. varians S. latidens | | |A member of the family Acaremyidae (Octodontoidea) | |
Scleromys
|S. angustus | | |A member of Chinchilloidea | |
Spaniomys
|S. riparius S. regularis | | |A member of Octodontoidea | |
Steiromys
|S. dentatus S. duplicatus | | |A member of Erethizontoidea | |
== Primates ==
== Meridiolestida ==
class="wikitable"
|+ !Name !Species !Locality !Material !Notes !Image |
Necrolestes{{Cite web |title=Fossilworks: Necrolestes patagonensis |url=https://paleobiodb.org/classic/checkTaxonInfo?taxon_no=244538 |access-date=2022-11-25 |website=Paleobiology Database}}
|N. patagonicus | |Skull and postcranial remains |A mole-like meridiolestidan, youngest known member of the group |
References
{{reflist}}
{{SALMA}}
Category:Geologic formations of Argentina
Category:Geologic formations of Chile
Category:Miocene Series of South America
Category:Fossiliferous stratigraphic units of South America
Category:Paleontology in Argentina
Category:Tuff formations of Argentina
Category:Geology of Santa Cruz Province, Argentina
Category:Austral or Magallanes Basin