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Escucha Formation

Escucha Formation
Stratigraphic range: Late Aptian-mid Albian
~117–103 Ma
View of Escucha and surrounding rocks
TypeGeological formation
Sub-unitsE1 to E3
UnderliesUtrillas Formation
OverliesCastrillo de la Reina, Benassal & Oliete Formations
Thickness~70 m (230 ft)
Lithology
PrimarySiltstone, mudstone (E1, E3) sandstone (E2)
OtherCoal (E1) siltstone (E2), amber
Location
Coordinates42°36′N 2°42′W / 42.6°N 2.7°W / 42.6; -2.7
Approximate paleocoordinates30°24′N 1°24′E / 30.4°N 1.4°E / 30.4; 1.4
RegionTeruel, Aragón
La Rioja
Country Spain
ExtentCameros, Maestrazgo & Oliete Basins
Type section
Named forEscucha, Teruel
Escucha Formation is located in Spain
Escucha Formation
Escucha Formation
Escucha Formation (Spain)

The Escucha Formation is a geological formation in La Rioja and Teruel provinces of northeastern Spain whose strata date back to the late Aptian to middle Albian stages of the Early Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.[1]

The approximately 70 m (230 ft) thick formation underlies the Utrillas Formation and overlies Castrillo de la Reina, Benassal & Oliete Formations. The Escucha Formation comprises siltstones, mudstones, sandstones, coal, siltstones and amber, in which several fossil insects were found. The formation was deposited in a variety of continental to paralic (deltaic) environments.[2]

Fossil content

The Escucha Formation has provided the following fossils, among others:[3]

Dinosaurs

Dinosaurs
Taxa Location Notes Images
Europelta carbonensis La Rioja [4]
Proa valdearinnoensis La Rioja [5]
Other dinosaurs
Reptiles
Fish
Crustaceans

Insects

Insects
Taxa Location/site Notes Images
Alavaraphidia Peñacerrada I amber [8]
Amarantoraphidia Peñacerrada I amber [8]
Microcostaphron parvus Peñacerrada I amber [9]
Radiophron ibericus Peñacerrada I amber [10]
Styporaphidia? hispanica Peñacerrada I amber [8]
Other arthropods
Invertebrates
Flora

Correlation

Early Cretaceous stratigraphy of Iberia
Ma Age Paleomap \ Basins Cantabrian Olanyà Cameros Maestrazgo Oliete Galve Morella South Iberian Pre-betic Lusitanian
100 Cenomanian
La Cabana Sopeira Utrillas Mosquerela Caranguejeira
Altamira Utrillas
Eguino
125 Albian Ullaga - Balmaseda Lluçà Traiguera
Monte Grande Escucha Escucha Jijona
Itxina - Miono
Aptian Valmaseda - Tellamendi Ol Gp. - Castrillo Benassal Benassal Olhos
Font En Gp. - Leza Morella/Oliete Oliete Villaroya Morella Capas
Rojas
Almargem
Patrocinio - Ernaga Senyús En Gp. - Jubela Forcall Villaroya Upper
Bedoulian
Figueira
Barremian Vega de Pas Cabó Abejar Xert Alacón Xert Huérguina Assises
Prada Artoles Collado Moutonianum Papo Seco
Rúbies Tera Gp. - Golmayo Alacón/Blesa Blesa Camarillas Mirambel
150 Hauterivian Ur Gp. - Pinilla Llacova Castellar Tera Gp. - Pinilla Villares Porto da
Calada
hiatus
Huerva Gaita
Valanginian Villaro Ur Gp. - Larriba Ped Gp. - Hortigüela
Ped Gp. - Hortigüela Ped Gp. - Piedrahita
Peñacoba Galve Miravetes
Berriasian Cab Gp. - Arcera Valdeprado hiatus Alfambra
TdL Gp. - Rupelo Arzobispo hiatus Tollo
On Gp. - Huérteles
Sierra Matute
Tithonian Lastres Tera Gp. - Magaña Higuereles Tera Gp. - Magaña Lourinhã
Arzobispo
Ágreda
Legend Major fossiliferous, oofossiliferous, ichnofossiliferous, coproliferous, minor formation
Sources


See also

References

  1. ^ Weishampel, et al., 2004
  2. ^ Peyrot et al., 2007
  3. ^ Escucha Formation at Fossilworks.org
  4. ^ Kirkland et al., 2013
  5. ^ McDonald et al., 2012
  6. ^ Pérez García et al., 2020
  7. ^ a b Ossó, À.; Charbonnier, S.; Hyžný, M.; van Bakel, B. W. M.; Devillez, J.; Bover-Arnal, T.; Moreno-Bedmar, J. A. (2024). "Decapod assemblages from the Aptian-Albian transition of the eastern Maestrat Basin (Iberian Chain)". Geologica Acta. 22: 1–35. doi:10.1344/GeologicaActa2024.22.7.
  8. ^ a b c Pérez de la Fuente et al., 2012
  9. ^ Ortega Blanco et al., 2010, p.272
  10. ^ Ortega Blanco et al., 2010, p.267
  11. ^ a b Sánchez-García, A.; Palencia, L.; Delclòs, X.; Peñalver, E. (2024). "False scorpions (Arachnida, Pseudoscorpiones) from Lower Cretaceous Spanish amber". Papers in Palaeontology. 10 (6). e1608. doi:10.1002/spp2.1608.

Bibliography

Further reading

  • L. Alcalá, E. Espílez, L. Mampel, J. I. Kirkland, M. Ortiga, D. Rubio, A. González, D. Ayala, A. Cobos, R. Royo-Torres, F. Gascó and M. D. Pesquero. 2012. A new Lower Cretaceous vertebrate bonebed near Arino (Tereul, Aragon, Spain); found and managed in a joint collaboration between a mining company and a palaeontological park. Geoheritage 4:275-286
  • J. I. Canudo, A. Cobos, C. Martín-Closas, X. Murelaga, X. Pereda-Suberbiola, R. Royo-Torres, J. I. Ruiz-Omeñaca and L. M. Sender. 2005. Sobre la presencia de dinosaurios ornitópodos en la Formación Escucha (Cretácico Inferior, Albiense): redescubierto “Iguanodon” en Utrillas (Teruel) [On the presence of ornithopod dinosaurs in the Escucha Formation (Lower Cretaceous, Albian): redescribing “Iguanodon” in Utrillas (Teruel)]. Fundamental 6:51-56
  • E. Peñalver, D. A. Grimaldi, and X. Delclos. 2006. Early Cretaceous spider web with its prey. Science 312:1761