Gaiman Formation
{{Short description|Geologic formation in Chubut Province, Argentina}}
{{Infobox rockunit
| name = Gaiman Formation
| image = Cerro Castillo stratigraphy.png
| caption = Gaiman Formation stratigraphy at Cerro Castillo
| type = Geological formation
| period = Burdigalian
| age = Burdigalian (Colhuehuapian)
~{{fossil range|19.8|17.5}}
| prilithology = Mudstone, sandstone
| otherlithology = Tuff, phosphate
| namedfor = Gaiman
| namedby = Mendía & Bayarsky
| year_ts = 1981
| region = Chubut Province
| country = Argentina
| coordinates = {{coord|43.3|S|65.3|W|display=inline,title}}
| paleocoordinates = {{coord|44.0|S|59.2|W|display=inline}}
| unitof =
| subunits =
| underlies = Puerto Madryn Formation
| overlies = Sarmiento Formation
| thickness = {{convert|70|m|ft|abbr=on}}
| extent = Peninsula Valdés Basin
| area =
| map = {{Location map+ | Argentina
| relief = 1
| width = 250
| float = center
| places =
{{Location map~ | Argentina
| lat_deg = -43.3
| lon_deg = -65.3
| mark = Yellow pog.svg
| marksize = 12
}}
}}
| map_caption =
}}
The Gaiman Formation ({{langx|es|Formación Gaiman}}), in older literature also referred to as Patagonian Marine Formation ({{langx|es|Formación Patagonia Marino}}, Patagoniense), is a fossiliferous geologic formation of the Peninsula Valdés Basin in the eastern Chubut Province of northwestern Patagonia, eastern Argentina.
The {{convert|70|m|ft}} thick formation overlies the Sarmiento Formation and is overlain by the Puerto Madryn Formation and comprises grey and white tuffaceous mudstones and sandstones, deposited in a shallow marine environment.
The Gaiman Formation has provided fossils of many extinct penguins, among which five species in the genus Palaeospheniscus, as well as whales and dolphins, most notably Aondelphis talen, Prosqualodon australis, Idiorophus patagonicus and Argyrocetus patagonicus, indeterminate seal and turtle fossils, shark and other fossils. The richness of the formation, and the other formations in the area, such as the underlying Sarmiento Formation, led to the establishment of the {{ill|Bryn Gwyn Paleontological Park|es|Parque paleontológico Bryn Gwyn}}, with a Welsh name, reflecting the number of Welsh settlers in the region.
Description
File:Peninsula Valdés Basin map - Puerto Madryn, Gaiman, Sarmiento Formations, Argentina.jpg
The Gaiman Formation was first defined by Mendía & Bayarsky in 1981,Cione et al., 2010, p.434 and further described by Mendía in 1983, taking its name from Gaiman in Chubut Province, eastern Patagonia.Rodríguez, 2015, p.198 Gaiman in the local language of the native Tehuelche people means "rocky point".{{in lang|es}} [http://www.agenciacna.com/2/nota_1.php?noticia_id=38125 Significado de los nombres de los Municipios de Chubut] The formation crops out in the lower course of the Chubut River,Noriega & Tambussi, 2008, p.272 and overlies the continental Trelew Member of the Sarmiento Formation and is overlain by the Late Miocene Puerto Madryn Formation. The formation is {{convert|70|m|ft}} thick, and comprises marine tuffs, tuffaceous mudstones, sandstones and coquinas.
The Gaiman Formation is correlated with the Chenque Formation of the Golfo San Jorge Basin and the Monte León Formation of the Austral Basin to the south, the Saladar Member of the lower Gran Bajo del Gualicho Formation of the Colorado Basin to the north and the Vaca Mahuida Formation of the Neuquén Basin to the northwest.Reichler, 2018, p.185
= Depositional environment =
The basal stratum of the Gaiman Formation is a thin transgressive lag with some gravels, bones and teeth from marine vertebrates. The unit displays a concentration of phosphatic concretions, ooids, bones and teeth.Cione et al., 2011, p.424 The marine sediments overlying this basal stratum are composed of white, tuffaceous, thoroughly bioturbated mudstones and fine sandstones with occasional mollusk molds and thin oyster horizons, deposited in a shallow shelf environment.Viglino et al., 2018, p.263
The marine transgression leading to the deposition of the Gaiman Formation is the first of two major South Atlantic transgressions of the Miocene, the second causing the deposition of the overlying Puerto Madryn Formation.Cuitiño, 2017, p.47
Facies analysis shows that the formation represents a transgressive-regressive stratigraphic cycle, with palaeoenvironments including coastal, storm-dominated shoreface, inner shelf embayment and open inner shelf.Cuitiño et al., 2019
The age of the Gaiman Formation is established on stratigraphic correlations to other absolutely-dated sections in Patagonia and biostratigraphic data and dates to the Early Miocene (Burdigalian, or Colhuehuapian in the SALMA classification).
Paleontological significance
File:Estacion de campo Bryn Gwyn (4).JPG
The Gaiman Formation has provided several fossil penguins, of which nine are assigned to specific species and include five species of the genus Palaeospheniscus. Also, shark teeth, fossils of indeterminate seals and turtles, and several dolphins, baleen and toothed whales have been found in the formation. Argentine paleontologist Florentino Ameghino described an isolated tooth from the formation first as an ichthyodectiform fish, Portheus patagonicus in 1901, however this fossil was assigned to a delphinoid cetacean of the family Kentriodontidae by Cione and Cozzuol in 1990.Cione & Cozzuol, 1990, p.451 Fish recorded from the formation are hexanchiform hexanchids, lamniform isurids, odontaspidids, cetorhinids, carcharhiniform carcharhinids, heterodontiform heterodontids, squatiniform squatinids myliobatiform myliobatids, perciform oplegnathids and labrids, and tetraodontiform molids.Cione et al., 2010, p.443 Rays are abundant in the formation.Cione et al., 2010, p.429 The lack of somatic remains of most molluscs, bryozoans, polychaetes and cirripeds in the formation is attributed to the high-energy and corrosive environment at time of deposition, as well as diagenesis after the formation was deposited.Cione et al., 2010, p.450
The bird species Eretiscus tonnii solely occurs in the Gaiman Formation.Chávez Hoffmeister, 2008, p.82 Bite marks on several of the penguin bones are attributed to terrestrial mammals such as didelphid or hathliacyniid sparassodont marsupials, common in Patagonia during the Miocene.Cione et al., 2010, p.437 Other ichnofossils found on the bones are presumably caused by dental erosion by regular echinoids,Cione et al., 2010, p.439 and bite marks by sharks, as Galeocerdo aduncus.Cione et al., 2010, p.441
The paleontological richness of the formation, as well as the more fossiliferous underlying Sarmiento Formation, led to the establishment of the {{ill|Bryn Gwyn Paleontological Park|es|Parque paleontológico Bryn Gwyn}}.{{in lang|es}} [http://www.cpatagonia.com/gaiman/parque.htm Parque paleontológico Bryn Gwyn]
= Fossil content =
The formation has provided the following fossils:[https://paleobiodb.org/classic/displayCollResults?collection_no=47303 Cerro del Castillo, Trelew] at Fossilworks.org[https://paleobiodb.org/classic/displayCollResults?collection_no=45886 Bryn Gwyn] at Fossilworks.org[https://paleobiodb.org/classic/displayCollResults?collection_no=74645 Patagonian] at Fossilworks.org[https://paleobiodb.org/classic/displayCollResults?collection_no=142513 Gaiman (marine vertebrates)] at Fossilworks.org[https://paleobiodb.org/classic/displayCollResults?collection_no=80914 Playa Santa Isabel, south] at Fossilworks.org
See also
- South American land mammal ages
- Uitpa Formation, contemporaneous fossiliferous formation of the Cocinetas Basin, Colombia
- Castillo Formation, contemporaneous fossiliferous formation of the Falcón Basin, Venezuela
- Biblián Formation, contemporaneous fossiliferous formation of Ecuador
- Bahía Inglesa Formation, contemporaneous fossiliferous formation of Chile
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References
{{reflist|20em}}
= Bibliography =
;Geology
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- {{citation |last=Rodríguez |first=Karina M |year=2015 |title=Análisis de los rasgos geomorfológicos del paleovalle Simpson (Provincia de Chubut) mediante técnicas de procesamiento digital de imágenes LANDSAT7 ETM+ |url=https://aacyg.files.wordpress.com/2017/04/actas-vi-cacyg-2015.pdf |publisher=VI Congreso Argentino de Cuaternário y Geomorfología |pages=198–199 |access-date=2019-04-05 |archive-date=2020-02-15 |archive-url=https://web.archive.org/web/20200215002814/https://aacyg.files.wordpress.com/2017/04/actas-vi-cacyg-2015.pdf |url-status=dead }}
;Paleontology
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- {{citation |last=Chávez Hoffmeister |first=Martín Felipe |year=2008 |title=La ornitofauna de la Formación Bahía Inglesa, Caldera, Chile (BSc. thesis) |url=http://cybertesis.uach.cl/tesis/uach/2008/fcc512o/doc/fcc512o.pdf |publisher=Universidad Austral de Chile |pages=1–165 |access-date=2019-04-05}}
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- {{citation |last=Tonni |first=Eduardo P |year=1979 |title=Un Nuevo Anseriforme de Sedimentos Marinos Terciarios de Chubut, Argentina |url=http://digital.bl.fcen.uba.ar/Download/008_ElHornero/008_ElHornero_v012_n01_articulo011.pdf |journal=Hornero |volume=12 |issue=1 |pages=11–15 |doi=10.56178/eh.v12i1.1212 |access-date=2019-04-05}}
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- {{citation |last1=Viglino |first1=Mariana |last2=Buono |first2=Mónica R. |last3=Gutstein |first3=Carolina S. |last4=Cozzuol |first4=Mario A. |last5=Cuitiño |first5=José I. |year=2018 |title=A new dolphin from the early Miocene of Patagonia, Argentina: Insights into the evolution of Platanistoidea in the Southern Hemisphere |url=https://app.pan.pl/archive/published/app63/app004412017.pdf |journal=Acta Palaeontologica Polonica |volume=63 |issue=2 |pages=261–277 |doi=10.4202/app.00441.2017 |access-date=2019-04-05}}
Further reading
- {{citation |last=Cabrera |first=Ángel |year=1926 |title=Cetaceos fósiles del Museo de La Plata |journal=Revista del Museo de La Plata |volume=29 |pages=363–411}}
- {{citation |last=Lydekker |first=Richard |year=1894 |title=Cetacean skulls from Patagonia |journal=Anales del Museo de la Plata |volume=II |pages=1–13}}
- {{citation |last=Simpson |first=George Gaylord |year=1946 |title=Fossil Penguins |journal=Bulletin of the American Museum of Natural History |volume=87 |pages=1–100}}
Category:Geologic formations of Argentina
Category:Miocene Series of South America