Santa Cruz Formation - Biblioteka.sk

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Santa Cruz Formation
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Santa Cruz Formation
Stratigraphic range: Burdigalian-Langhian
(Santacrucian-Friasian)
~18–15.2 Ma
TypeGeological formation
Sub-unitsEstancia La Costa Member, Estancia La Angelina Member (coastal section)
UnderliesCerro Boleadoras Formation
OverliesMonte Léon Formation
ThicknessOver 295 metres
Lithology
Primary
Location
CountryArgentina, Chile
ExtentAustral Basin
Type section
Named byFurque & Camacho
Locationnear Lago Argentino
Year defined1972

Santa Cruz Province in Argentina, where the majority of the formation of exposed

The Santa Cruz Formation is a geological formation in the Magallanes/Austral Basin in southern Patagonia in Argentina and in adjacent areas of Chile. It dates to the late Early Miocene epoch, and is contemporaneous with eponymous Santacrucian SALMA.[1][2] 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 has a lithology predominantly consisting of tuffaceous deposits and fine grained sedimentary claystone and mudstone, and the upper fossil-poor Estancia La Angelina Member, which consists of sedimentary rock, primarily claystone, mudstone, and sandstone. The environment of deposition is interpreted to have been 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.[1] The Santa Cruz Formation is known for its abundance of South American native ungulates (astrapotheres, litopterns, notoungulates),[3] as well as an abundance of rodents, xenarthrans (armadillos, sloths, anteaters), and metatherians.

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.[4] While primarily located in Argentina, small outcrops are also present in adjacent areas of Chile.[5] The base of the formation is defined by a marine regression event transitioning from the marine environment of the underlying Monte Léon Formation, during which time 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 at any one locality of over 295 metres, though the total thickness of the formation is strongly controlled by subsequent erosion and the 295 metres 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 or river transport. The formation is suggested to span 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.[4]

Paleoenvironment

The environment of the Santa Cruz Formation is thought to have been relatively warm and humid, to have included a mix of open savannah, gallery forests and semi-deciduous forests. Permanent bodies of water such as lakes, ponds and streams are likely to have been present in some areas.[6]

Paleoflora

Name Species Locality Material Notes Image
Nothofagus[7] Indeterminate Rincón del Buque, Punta Sur Leaves, wood
Araucaria[7] Indeterminate Punta Sur Twig Morphologically similar to A. marensii from the Eocene of Antarctica
Lauraceae[7] Indeterminate Punta Sur Wood Assigned to form genus Laurinoxylon
Myrceugenia[7] M. chubutense Punta Sur Wood A member of the family Myrtaceae
Eucryphiaceoxylon[7] E. eucryphioides Punta Sur Wood Wood probably belonging to the genus Eucryphia
Faboideae[7] Indeterminate Punta Sur Wood Possible affinities to Sophora (Fabaceae)
Doroteoxylon[7] D. vicenti-perezii Punta Sur Wood Wood with affinities to the subfamily Caesalpinioideae
Akanioxylon[8] A. santacrucensis Punta Sur Wood A member of the family Akaniaceae
Chloridoideae[7] Indeterminate Phytoliths Grass
Panicoideae[7]
Danthonioideae[7]
Pooideae[7]

Paleofauna

Invertebrates

Name Species Material Notes Image
Crassostrea[9] C. orbignyi Numerous individuals in large beds at the base of the formation A marine true oyster
Diplodon[10] D. cf. colhuapiensis A freshwater bivalve belonging to Hyriidae
Stephadiscus[11] Indeterminate A terrestrial gastropod belonging to Charopidae
Gastrocopta[12] G.patagonica A terrestrial gastropod belonging to Vertiginidae
?Scolodonta [12] Indeterminate A terrestrial gastropod belonging to Scolodontidae
Punctum[12] P. patagonicum A terrestrial gastropod belonging to Punctidae
Zilchogyra[12] Z. miocenica A terrestrial gastropod belonging to Charopidae
Patagocharopa[12] P. enigmatica A terrestrial gastropod of uncertain affinities, possibly a member of Charopidae
Porifera[7] Unspecified Spicules Freshwater sponge
Bacillariophyceae[7] Unspecified Frustules Freshwater diatoms
Chrysophyceae[7] Unspecified Freshwater algae

Amphibians

Name Species Locality Material Notes Image
Calyptocephalella[13][14] C. cf. canqueli Estancia La Costa, Rinconada de los López Skull and jaw fragments A calyptocephalellid frog
Neobatrachia[13] Indeterminate Estancia La Costa Skull fragments and presacral vertebrate A frog originally assigned to "Leptodactylidae", but requires further investigation

Birds

Name Species Locality Material Notes Image
Anisolornis[15] A. excavatus A bird of uncertain affinities, authors have varyingly suggested affinities to trumpeters or limpkins
Ankonetta[15] A. larriestrai Partial tarsometatarsus A basal member of Anatidae
Badiostes[15] B. patagonicus A member of the family Falconidae
Brontornis[15] B. burmeisteri Controversial taxonomic position, either considered a terror bird or an anserimorph
Dryornis[16][17] D. pampeanusD. hatcheri Two partial left humerus A New World vulture.
Eutelornis[15] E. patagonicus

E. australis

Limb fragments A member of Anseriformes, relationships of the species to each other or to other Ansiferiformes is uncertain
Liptornis[15] L. hesternus A member of Anhingidae
Macranhinga[15] Indeterminate A member of Anhingidae
Miocariama[15][18] M. santacrucensis Partial cranium and tibiotarsi fragments A seriema
Nothurinae[15] 2 Indeterminate species Tinamou
Opisthodactylus[15] O. patagonicus Limb, vertebra and skull fragments A member of Rheidae
Patagornis [15] P. marshi A terror bird
Phorusrhacos[19] P. longissimus Partial skulls A terror bird
Protibis[15] P. cnemialis distal end of tibiotarsus Potentially a spoonbill
Psilopterus[15] P. lemoinei

P. bachmanni

A terror bird
Thegornis[15] T. musculosus

T. debilis

A member of the family Falconidae
Archaeopsophia[20] A. aoni A member of the family Psophiidae (trumpeters)
Chehuenia[20] C. facongrandei A roller
Kaikenia[20] K. mourerchauvirea An anatid belonging to the subfamily Tadorninae
Peioa[20] P. australis A member of Anseriformes. Zdroj:https://en.wikipedia.org?pojem=Santa_Cruz_Formation
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