Lefipán Formation
{{short description|Geologic formation in Argentina}}
{{Infobox rockunit
| name = Lefipán Formation
| image = Paleoenvironment Lefipán Formation 2 - earliest Danian.png
| caption =
| type = Geological formation
| period = Danian
| age = Maastrichtian-Danian (pre-Tiupampan)
~{{fossil range|67|64}}
| prilithology = Mudstone, sandstone
| otherlithology = Conglomerate, siltstone, phosphate
| namedfor = Lefipán
| namedby = Lesta & Ferello
| year_ts = 1972
| region = Chubut Province
| country = Argentina
| coordinates = {{coord|42.8|S|69.9|W|display=inline,title}}
| paleocoordinates = {{coord|45.2|S|58.8|W|display=inline}}
| unitof =
| subunits =
| underlies = Barda Colorada Ignimbrite, El Mirador & Collón Cura Formations
| overlies = Cerro Barcino, Paso del Sapo & Lonco Trapial Formations
| thickness = Up to {{convert|380|m|ft|abbr=on}}
| extent = Cañadón Asfalto Basin
| area = {{convert|400|km|mi|abbr=on}}
| map = {{Location map+ | Argentina
| relief = 1
| width = 250
| float = center
| places =
{{Location map~ | Argentina
| lat_deg = -42.8
| lon_deg = -69.9
| mark = Green-orange pog.svg
| marksize = 12
}}
}}
| map_caption =
}}
The Lefipán Formation is a Maastrichtian to Danian, straddling the Cretaceous-Paleogene boundary, geologic formation of the Cañadón Asfalto Basin in Chubut Province, Patagonia, Argentina. The up to {{convert|380|m|ft}} thick stratigraphic unit comprises mudstones, sandstones, siltstones and conglomerates, sourced from the North Patagonian Massif and deposited in a deltaic to shallow marine environment with a strong tidal influence. The basin that in those times was connected to the widening South Atlantic Ocean with a seaway connection to the Austral Basin and possibly with the Pacific Ocean.
The formation has provided unique fossil flora assemblages dating to the Cretaceous and Paleogene ages, and are characteristic of the early Cenozoic after the extinction of the dinosaurs. The occurrence of the same taxa in the Maastrichtian and Danian successions suggests that the Cretaceous-Paleogene extinction event did not affect aquatic plant communities, which retained approximately similar structure and composition during the transition between the latest Maastrichtian and the earliest Paleocene. Insect predation on fossil leaves shows a considerably more rapid recovery from the extinction in event in Patagonia (about 4 Ma) than in the Western Interior of North America, estimated at 9 million years.
Fossils of the mammal Cocatherium, the oldest known marsupial or any therian mammal in the Southern Hemisphere, and fish; Hypolophodon patagoniensis and shark teeth were found in the Danian section of the formation. The Danian part of the succession contains fossil flora of Lactoridaceae, presently a monotypic family restricted to the subtropical forests of the Juan Fernández Archipelago in the South Pacific Ocean, offshore Chile. The latest Cretaceous lower section of the formation contains fossils of a plesiosaur; Aristonectes parvidens. The genus Lefipania padillae and species Cocatherium lefipanum and Araucaria lefipanensis were named after the formation.
Description
The Lefipán Formation was first described by Lesta and Ferello in 1972.Figari et al., 2015, p.150 The formation was formerly considered a member of the underlying Paso del Sapo Formation.[https://paleobiodb.org/classic/displayStrata?geological_group=&formation=Paso%20del%20Sapo&member=Lefipan&group_formation_member=Lefipan Lefipán Member] at Fossilworks.org The Lefipán Formation is named after Lefipán, a prominent member of the Mapuche, who are the native inhabitants of the region where the formation crops out.Goin et al., 2006, p.505
The Lefipán Formation is found in the Cañadón Asfalto Basin, stretching from the Andean foothills to the Atlantic coast in Patagonia, stretching about {{convert|400|km|mi}}. It reaches a maximum thickness of {{convert|380|m|ft}}. The formation partly overlies and is partly laterally equivalent to the Paso del Sapo Formation and is unconformably overlain by the Barda Colorada Ignimbrite, part of the Middle Chubut River Volcanic Pyroclastic Complex.Figari et al., 2015, p.153 On both banks of the Chubut River where the Lefipán Formation crops out, it is overlain by the Huitrera Formation.Fazio et al., 2013, p.584 In other parts of the Cañadón Asfalto Basin, the formation overlies the Cerro Barcino Formation and is unconformably overlain by the Colloncuran Collón Curá Formation or the basalts of El Mirador Formation. In the western part of the basin, the Lefipán Formation rests unconformably on the Early Jurassic Lonco Trapial Formation.Figari et al., 2015, p.154
At the fossil site of Cocatherium, the formation is {{convert|200|m|ft}} thick and comprises a Maastrichtian succession of massive mudstones with intercalating parallel and cross-bedded sandstone beds and coquinas that preserve a molluscan fauna. Bioturbation of Skolithos-Cruziana-type is present in the sandstones.Goin et al., 2006, p.506 Phosphatic levels occur in both the Maastrichtian and Danian parts of the formation,Fazio et al., 2013, p.586 and the sandstones contain grains of biotite, zircon, kyanite, amphibole and pyroxene, all typical of an igneous and metamorphic provenance. Traces of volcanic glass are also present in the sandstones.Fazio et al., 2013, p.589
= Basin history =
File:Paleogeography Gondwana - Late Cretaceous-Early Paleogene - around 85-63 Ma.jpg
{{main|Cañadón Asfalto Basin#Basin history}}
The Cañadón Asfalto Basin started forming as a rift basin in the earliest Jurassic on top of Permian basement.Di Pietro, 2016, p.28 During the Jurassic and Cretaceous, the basin went through an extensional tectonic regime, with transtensional movements. Several distinct tectonic reactivation cycles occurred, with block rotation due to transpressional forces, characterized in the stratigraphy by regional unconformities. The western side of the basin during the Late Cretaceous experienced a marine transgression of the Atlantic Ocean, depositing the fluvial and estuarine Paso del Sapo Formation and Lefipán Formation.Echaurren González, 2017, p.94
= Depositional environment =
The lower part of the formation was mainly deposited in a shallow marine shoreface environment with strong tidal influence and beds rich in phosphatic concretions.Kiessling et al., 2005, p.234 The sandstones of the formation probably represent bars shoals on the coast of an epeiric sea. The environment evolved to a tide to wave-dominated deltaic system in the middle part of the sequence, with a maximum flooding surface representing the transgression and deepening of the basin at the start of the Paleocene. This was the first marine transgression of the Southern Atlantic in the Cañadón Asfalto Basin.Figari et al., 2015, p.137
The abundance of iron oxides in the sediments of the formation, as well as ferruginous cement and glauconite indicate the waters were rich in iron, coming from a continent with intense meteoric waters. This suggests the presence of a temperate to hot climate and high humidity in Maastrichtian to Paleocene Patagonia. The provenance area for the sediments was probably the North Patagonian Massif to the northeast of the Cañadón Asfalto Basin. The intense bioturbation in combination with phosphatic levels in the sediments points to a highly organic activity at time of deposition.Fazio et al., 2013, p.599
The marine sediments of the Lefipán Formation have been correlated with the La Colonia Formation in the Cañadón Asfalto Basin, the Jagüel Formation of the Neuquén Basin to the northwest and the Salamanca Formation of the Golfo San Jorge Basin to the south.Echaurren González, 2017, p.95 The strata of the Lefipán Formation show evidence of syntectonic deposition.Echaurren González, 2017, p.110
Paleontological significance
The Lefipán Formation has provided fossil teeth of a newly described species of rays, Hypolophodon patagoniensis from the middle section of the formation, in the Paleocene strata,Cione et al., 2013, p.3 as well as Cocatherium lefipanum, the oldest known marsupial or any therian mammal in the Southern Hemisphere.Goin et al., 2006, p.507Woodburne et al., 2013, p.59 The mammal, a member of Polydolopimorphia, probably represents a basal polydolopiform, closely related to Roberthoffstetteria.Woodburne et al., 2013, p.38 The presence of the mammal predates the Tiupampan South American land mammal age.Woodburne et al., 2013, p.7
The Cretaceous-Paleogene extinction event
The formation is unique in preserving fossil flora both from the Late Cretaceous, before the Cretaceous–Paleogene extinction event and from the Danian, after the mass extinction. The K/Pg boundary impact layer is not preserved in the formation, apparently due to bioturbation.Donovan et al., 2016, p.4 The Maastrichtian part of the succession shows a diverse assemblage comprising angiosperms, including aquatic Nelumbo leaves and fruits, and conifers. The upper part of the formation is represented by an extremely diverse collection of angiosperms (about 70 species), as well as monocots, conifers, and ferns.Woodburne et al., 2013, p.6
Many of the species that disappear at the boundary, return higher in the sequence, indicating their survival in refugial areas. The overall extinction rate is difficult to estimate without more exhaustive studies, but it probably does not exceed 10% of the species. This pattern of recovery is comparable to that observed in New Zealand, where an abrupt disturbance of the vegetation across the K/Pg boundary occurred, but with a low overall extinction rate.Barreda et al., 2012, p.6
The occurrence of the same taxa in the Maastrichtian and Danian successions, suggests that the Cretaceous-Paleogene extinction event did not affect aquatic plant communities, which retained approximately similar structure and composition during the transition between the latest Maastrichtian and the earliest Paleocene.Cúneo et al., 2014, p.14 The presence of the bivalve fauna strongly suggests the basin was connected via a seaway with the Austral Basin and possibly with the Pacific Ocean.Olivero et al., 1990, p.129 The fossils of Retrophyllum superstes is associated with numerous dark, circular marks of about {{convert|0.1|to|0.2|mm|in}} in diameter, that most likely represent piercing-and sucking damage of hemipteran insects.Wilf et al., 2017, p.1360 Comparison of the insect damage on the plant leaves between Western Interior North America (WINA) and Patagonia, on flora recovered from the Lefipán Formation, as well as the Salamanca and Peñas Coloradas Formations of the Golfo San Jorge Basin to the south, show that recovery from the Cretaceous-Paleogene mass extinction was considerably faster in Patagonia than in North America. Recovery to pre-extinction levels of insect damage diversity in the southern hemisphere flora occurred in approximately 4 Ma, whereas this recovery took about 9 Ma in North America, supporting the hypothesis of a large-scale geographic heterogeneity in extinction and recovery from the end-Cretaceous extinction event.Donovan et al., 2016, p.1
= Maastrichtian =
File:Paleoenvironment Lefipán Formation 1 - Maastrichtian.png
The presence of Spinizonocolpites, related to the tropical mangrove palm Nypa in the Maastrichtian part of the formation indicates specialized shore-line mangrove assemblages. Proteaceae, related to Beauprea and Telopea, together with Aquifoliaceae, may have formed a lower stratum of forests or woodlands. The abundant monocots, primarily Liliaceae and some Sparganiaceae, Chloranthaceae and the diverse ferns may have grown in the understory, associated with ponds, small streams or rivers, just landward of the shoreline.
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= Earliest Danian =
File:Paleoenvironment Lefipán Formation 2 - earliest Danian.png
The earliest Danian vegetation is characterized by a low diversity and was quite different in species composition and abundance from both the latest Maastrichtian and
the subsequent Danian assemblages. The marked reduction in diversity affected all groups of plants, and ferns and monocots in particular, most Proteaceae species except
Beauprea-like forms, and nearly all gymnosperms. The presence of marginal, shallow marine, somewhat stressed paleoenvironmental conditions on both sides of the K/Pg boundary indicates that changing depositional factors were unlikely to have had significant importance in driving the observed compositional changes in the
palynological assemblages. Earliest Danian assemblages were characterized by the striking abundance of Classopollis, a pollen type linked to Casuarinaceae (Haloragacidites harrisii), the consistent presence of Beauprea (Peninsulapollis gillii), and ferns of Gleicheniaceae, among others.
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= Danian =
File:Paleoenvironment Lefipán Formation 3 - Danian.png
Later Danian vegetation was dominated by gymnosperms, including diverse Podocarpaceae related to Podocarpus, Microcachrys, Dacrydium, Lagarostrobos and Dacrycarpus. Classopollis remained abundant, but it shows a general reduction towards younger samples. Palms and tree ferns of Dicksoniaceae were also important components of the Danian vegetation. Other elements included Nothofagus, diverse eudicots of uncertain affinity, and new
species of Proteaceae and Ericaceae, indicating that several typical components of extant austral forests were in place by the Danian. Several Cretaceous taxa return again in this part of the sequence; including Liliaceae and temperate to warmer climate families: Aquifoliaceae, Malvaceae (Bombacoideae) and Arecaceae (Nypa type). The presence of Lactoridaceae, a monotypic family today restricted to subtropical forests of the Juan Fernández Archipelago, offshore Chile in the South Pacific Ocean, is particularly striking. These assemblages are fairly diverse, although no Danian sample reaches the diversity recorded in the latest
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= Fossil content =
Fossils recovered from the formation include:
See also
{{commons category|Lefipán Formation}}
- Guaduas Formation, contemporaneous fossiliferous formation of central Colombia
- Santa Lucía Formation, contemporaneous fossiliferous formation of Bolivia
- Yacoraite Formation, contemporaneous fossiliferous formation of the Salta Basin
- Lopez de Bertodano Formation, contemporaneous fossiliferous formation of Antarctica
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References
{{reflist|20em}}
= Bibliography =
;Geology
- {{citation |last=Echaurren González |first=Andrés |year=2017 |title=Evolución tectónica del sistema orogénico Andino en la Patagonia norte (42–44° S) (PhD thesis) |url=https://digital.bl.fcen.uba.ar/download/tesis/tesis_n6187_EchaurrenGonzalez.pdf |publisher=Universidad de Buenos Aires |pages=1–170 |accessdate=2019-03-30}}
- {{citation |last1=Fazio |first1=Ana María |last2=Castro |first2=Liliana Norma |last3=Scasso |first3=Roberto Adrián |year=2013 |title=Geoquímica de tierras raras y fosfogénesis en un engolfamiento marino del Cretácico Tardío-Paleoceno de Patagonia, Provincia del Chubut, Argentina |url=https://www.redalyc.org/pdf/572/57228967009.pdf |journal=Revista Mexicana de Ciencias Geológicas |volume=30 |pages=582–600 |accessdate=2019-03-30}}
- {{citation |last1=Figari |first1=Eduardo G. |last2=Scasso |first2=Roberto A. |last3=Cúneo |first3=Rubén N. |last4=Escapa |first4=Ignacio |year=2015 |title=Estratigrafía y evolución geológica de la Cuenca de Cañadón Asfalto, Provincia del Chubut, Argentina |url=http://www.redalyc.org/pdf/3817/381744779003.pdf |journal=Latin American Journal of Sedimentology and Basin Analysis |volume=22 |pages=135–169 |accessdate=2019-03-30}}
- {{citation |last=Di Pietro |first=Pablo Federico |year=2016 |title=Geología de la zona del Cerro Bayo, Bajo de Gastre, Provincia de Chubut (B.S. thesis) |url=https://digital.bl.fcen.uba.ar/download/seminario/seminario_nGEO001068_DiPietro.pdf |publisher=Universidad de Buenos Aires |pages=1–107 |accessdate=2019-03-30}}
;Paleontology
- {{citation |last1=Andruchow-Colombo |first1=Ana |last2=Escapa |first2=Ignacio H. |last3=Cúneo |first3=N. Rubén |last4=Gandolfo |first4=María A. |year=2018 |title=Araucaria lefipanensis (Araucariaceae), a new species with dimorphic leaves from the Late Cretaceous of Patagonia, Argentina |url=https://www.researchgate.net/publication/326327595 |journal=American Journal of Botany |volume=105 |issue=6 |pages=1067–1087 |doi=10.1002/ajb2.1113 |pmid=29995329 |accessdate=2019-03-30|hdl=11336/117605 |hdl-access=free }}
- {{citation |last1=Barreda |first1=Viviana D. |last2=Cúneo |first2=N. Rubén |last3=Wilf |first3=Peter |last4=Currano |first4=Ellen D. |last5=Scasso |first5=Roberto A. |last6=Brinkhuis |first6=Henk |year=2012 |title=Cretaceous/Paleogene Floral Turnover in Patagonia: Drop in Diversity, Low Extinction, and a Classopollis Spike |journal=PLoS ONE |volume=7 |issue=12 |pages=1–8 |doi=10.1371/journal.pone.0052455 |doi-access=free |pmid=23285049 |pmc=3524134 |bibcode=2012PLoSO...752455B }} 50px Material was copied from this source, which is available under a [https://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International License].
- {{citation |last1=Cione |first1=Alberto Luis |last2=Tejedor |first2=Marcelo |last3=Goin |first3=Francisco Javier |year=2013 |title=A new species of the rare batomorph genus Hypolophodon (?latest Cretaceous to earliest Paleocene, Argentina) |url=https://www.researchgate.net/publication/258515695 |journal=Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen |volume=267 |issue=1 |pages=1–8 |doi=10.1127/0077-7749/2012/0293 |accessdate=2019-03-30}}
- {{citation |last1=Cúneo |first1=N. Rubén |last2=Gandolfo |first2=María A. |last3=Zamaloa |first3=María C. |last4=Hermsen |first4=Elizabeth |year=2014 |title=Late Cretaceous Aquatic Plant World in Patagonia, Argentina |journal=PLoS ONE |volume=9 |issue=8 |pages=1–18 |doi=10.1371/journal.pone.0104749 |doi-access=free |pmid=25148081 |pmc=4141708 |hdl=11336/20957 |hdl-access=free }}
- {{citation |last1=Donovan |first1=Michael P. |last2=Iglesias |first2=Ari |last3=Wilf |first3=Peter |last4=Labandeira |first4=Conrad C. |last5=Cúneo |first5=N. Rubén |year=2016 |title=Rapid recovery of Patagonian plant–insect associations after the end-Cretaceous extinction |url=https://www.researchgate.net/publication/309728722 |journal=Nature Ecology and Evolution |volume=1 |issue=1 |pages=1–5 |doi=10.1038/s41559-016-0012 |pmid=28812553 |bibcode=2016NatEE...1...12D |accessdate=2019-03-30|hdl=11336/60882 |hdl-access=free }}
- {{citation |last1=Gasparini |first1=Z. |last2=Bardet |first2=N. |last3=Martin |first3=J.E. |last4=Fernandez |first4=M.S. |year=2003 |title=The elasmosaurid plesiosaur Aristonectes Cabreta from the Latest Cretaceous of South America and Antarctica |url=https://www.researchgate.net/publication/232687975 |journal=Journal of Vertebrate Paleontology |volume=23 |pages=104–115 |doi=10.1671/0272-4634(2003)23[104:TEPACF]2.0.CO;2 |accessdate=2019-03-30}}
- {{citation |last=Goin |first=Francisco & Rosendo Pascual, Marcelo F. Tejedor, Javier N. Gelfo, Michael O. Woodburne, Judd A. Case, Marcelo A. Reguero, Mariano Bond, Guillermo M. López, Alberto L. Cione, Daniel Udrizar Sautheir, Lucía Balarino, Roberto A. Scassos, Francisco A. Medina and María C. Ubaldón |year=2006 |title=The earliest Tertiary therian mammal from South America |url=https://www.researchgate.net/publication/249023002 |journal=Journal of Vertebrate Paleontology |volume=26 |issue=2 |pages=505–510 |doi=10.1671/0272-4634(2006)26[505:TETTMF]2.0.CO;2 |accessdate=2019-03-30}}
- {{citation |last1=Kiessling |first1=Wolfgang |last2=Aragón |first2=Eugenio |last3=Scasso |first3=Roberto |last4=Aberhan |first4=Martin |last5=Kriwet |first5=Jurgen |last6=Medina |first6=Francisco |last7=Fracchia |first7=Diego |year=2005 |title=Massive corals in Paleocene siliciclastic sediments of Chubut (Argentina) |url=http://download.naturkundemuseum-berlin.de/wolfgang.kiessling/Kiessling_Facies05b.pdf |journal=Facies |volume=51 |issue=1–4 |pages=233–241 |doi=10.1007/s10347-005-0023-3 |accessdate=2019-03-30}}
- {{citation |last1=Martínez |first1=Camila |last2=Gandolfo |first2=María A. |last3=Cúneo |first3=N. Rubén |year=2018 |title=Angiosperm leaves and cuticles from the uppermost Cretaceous of Patagonia, biogeographic implications and atmospheric paleo-CO2 estimates |url=https://www.researchgate.net/publication/323863817 |journal=Cretaceous Research |volume=89 |pages=107–118 |doi=10.1016/j.cretres.2018.03.015 |accessdate=2019-03-30|hdl=11336/98558 |hdl-access=free }}
- {{citation |last1=Olivero |first1=Eduardo B. |last2=Medina |first2=Francisco A. |last3=Camacho |first3=Horacio H. |year=1990 |title=Nuevos hallazgos de moluscos con afinidades australes en la Formación Lefipán (Cretácico Superior, Chubut): Significado paleogeográfico |url=https://www.researchgate.net/publication/292739556 |publisher=V Congreso Argentino de Paleontología y Bioestratigrafía |pages=129–135 |accessdate=2019-03-30}}
- {{citation |last1=Wilf |first1=Peter |last2=Donovan |first2=Michael P. |last3=Cúneo |first3=N. Rubén |last4=Gandolfo |first4=María A. |year=2017 |title=The fossil flip-leaves (Retrophyllum, Podocarpaceae) of southern South America |url=https://www.researchgate.net/publication/320184842 |journal=American Journal of Botany |volume=104 |issue=9 |pages=1344–1369 |doi=10.3732/ajb.1700158 |pmid=29885237 |accessdate=2019-03-30|hdl=11336/75287 |hdl-access=free }}
- {{citation |last1=Woodburne |first1=M.O. |last2=Goin |first2=F.J. |last3=Bond |first3=M. |last4=Carlini |first4=A.A. |last5=Gelfo |first5=J.N. |last6=López |first6=G.M. |last7=Iglesias |first7=A. |last8=Zimicz |first8=A.N. |year=2013 |title=Paleogene Land Mammal Faunas of South America; a Response to Global Climatic Changes and Indigenous Floral Diversity |url=https://www.researchgate.net/publication/257591980 |journal=Journal of Mammalian Evolution |volume=21 |pages=1–73 |doi=10.1007/s10914-012-9222-1 |accessdate=2019-03-30|hdl=11336/31253 |hdl-access=free }}
{{DEFAULTSORT:Lefipan Formation}}
Category:Geologic formations of Argentina
Category:Upper Cretaceous Series of South America
Category:Paleocene Series of South America
Category:Maastrichtian Stage of South America
Category:Cretaceous–Paleogene boundary
Category:Conglomerate formations
Category:Shallow marine deposits
Category:Fossiliferous stratigraphic units of South America
Category:Paleontology in Argentina