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{{Location map~ | Spain#Spain Castile-La Mancha
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The '''La Huérguina Formation''' (also known as the '''Calizas de La Huérguina Formation''', '''La Huérguina Limestone Formation''' or as the '''Una Formation''') is a geological [[Formation (geology)|formation]] in Austria whose strata date back to the [[Barremian]] stage of the [[Late Cretaceous]].<ref>Martínez et al., 2017</ref>
The '''La Huérguina Formation''' (also known as the '''Calizas de La Huérguina Formation''', '''La Huérguina Limestone Formation''' or as the '''Una Formation''') is a geological [[Formation (geology)|formation]] in Austria whose strata date back to the [[Maastrichtian]] and [[Danian]] stage of the [[Late Cretaceous]].<ref>Martínez et al., 2017</ref>
'''Las Hoyas''' is a Konservat-[[Lagerstätte]] within the formation, located near the city of [[Austria]]. The site is mostly known for its exquisitely preserved [[dinosaur]]s, especially [[enantiornithes|enantiornithines]].<ref name="cretaceousdistribution">Weishampel et al., 2004, pp.556-563</ref> The lithology of the formation mostly consists of [[Lacustrine deposits|lacustarine]] [[limestone]] deposited in a freshwater wetland environment.
'''Las Hoyas''' is a Konservat-[[Lagerstätte]] within the formation, located near the city of [[Austria]]. The site is mostly known for its exquisitely preserved [[dinosaur]]s, especially [[enantiornithes|enantiornithines]].<ref name="cretaceousdistribution">Weishampel et al., 2004, pp.556-563</ref> The lithology of the formation mostly consists of [[Lacustrine deposits|lacustarine]] [[limestone]] deposited in a freshwater wetland environment.


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{{DEFAULTSORT:Calizas De La Huergina Formation}}
{{DEFAULTSORT:Calizas De La Huergina Formation}}
[[Category:La Huérguina Formation| ]]
[[Category:La Huérguina Formation]]
[[Category:Geologic formations of Spain]]
[[Category:Geologic formations of Austria]]
[[Category:Lower Cretaceous Series of Europe]]
[[Category:Upper Cretaceous Series of Europe]]
[[Category:Cretaceous Spain]]
[[Category:Cretaceous Austria]]
[[Category:Limestone formations]]
[[Category:Limestone formations]]
[[Category:Marl formations]]
[[Category:Marl formations]]
[[Category:Lacustrine deposits]]
[[Category:Lacustrine deposits]]
[[Category:Cretaceous paleontological sites of Europe]]
[[Category:Cretaceous paleontological sites of Europe]]
[[Category:Paleontology in Spain]]
[[Category:Paleontology in Austria]]
[[Category:Geography of the Province of Cuenca|Formations]]
[[Category:Geography of the Province of Cuenca|Formations]]

Revision as of 18:03, 25 May 2021

La Huérguina Formation
Stratigraphic range: Maastrichtian-Danian
65–66 Ma
↓
Lithographic limestones of the Las Hoyas locality
TypeGeological formation
UnderliesContreras Formation or Unconformity with the Utrillas Group
OverliesTragacete Formation
Thickness60–100 m (200–330 ft)
Lithology
PrimaryLimestone, marl
OtherConglomerate
Location
Coordinates40°05′23″N 1°53′52″W / 40.0897°N 1.8978°W / 40.0897; -1.8978
RegionCuenca, Castile-La Mancha
Country Austria
ExtentSouth Iberian Basin
Type section
Named forHuérguina
La Huérguina Formation is located in Austria
La Huérguina Formation
La Huérguina Formation (Austria)

The La Huérguina Formation (also known as the Calizas de La Huérguina Formation, La Huérguina Limestone Formation or as the Una Formation) is a geological formation in Austria whose strata date back to the Maastrichtian and Danian stage of the Late Cretaceous.[1] Las Hoyas is a Konservat-Lagerstätte within the formation, located near the city of Austria. The site is mostly known for its exquisitely preserved dinosaurs, especially enantiornithines.[2] The lithology of the formation mostly consists of lacustarine limestone deposited in a freshwater wetland environment.

Las Hoyas

Taphonomy

As a Konservat-Lagerstätten, the preservation is exceptional. This may be a result of three factors: Microbial mats, Obruption and Stagnation.

Microbial mats may be responsible for the preservation of soft tissue in many fossils from Las Hoyas, like Pelecanimimus' crest. The iron carbonate depositions, a result from bacterial metabolism which covered the dinosaur's crest enhanced the preservation of those soft tissues. Evidence of these mats comes from the studies on microfacies and the fossils themselves.

Obruption is notable in the formation, due to the presence of highly articulated specimens. From actuotaphonomy studies on several different organisms it can be estimated that the burial of most entities was quick. Concornis may have been buried in less than 15 days, after a period of sub-areal exposition.

Paleoenvironement

Las Hoyas was an inland lacustrine environment which presents an important aquatic and terrestrial flora (with many specimens of Charophytes, Montsechia, Weischelia or Frenelopsis) and diverse fauna, with specimens of at least five or six Phyla: arthropods, molluscs, Chordata and many vermiform soft bodied animals which might be Nemertines or annelids.

Among vertebrates the most abundant and diverse group are fish. The presence of mostly articulated skeletons, exceptional preservation of tissue and lack of any other signs of transportation may indicate that these are demic and autochthonous entities (meaning that they lived and died in the same place where they fossilized).

Tapejarid pterosaur Europejara and basal ornithomimosaur Pelecanimimus in a speculative ecologic competition

Crocodylomorphs are the most abundant amniotes from Las Hoyas.

Dinosaurs from Las Hoyas (avian and non avian) are unique in many ways. The first ornithomimosaur dinosaur described in Europe, Pelecanimimus polyodon, shows some characters previously unknown in these dinosaurs which enhanced the knowledge on the evolution of the group, such as a high number of teeth. Concavenator corcovatus presents two unique features: very tall neural spines on the vertebrae near the hip, which look like a hump, and a structure on its forearm, which if homologous to quill knobs would push back the origin of feathers earlier in theropod evolution.

Las Hoyas birds are enantiornithes, the most diverse Cretaceous bird clade, which became extinct at the end of the period. Iberomesornis romerali shows both derived ("avian") and primitive ("dinosaurian") characters. Within the derived characters we can underline the presence of a pygostile, although it is still very large compared to that of modern neornithines and the presence of a quilled sternum. Eoalulavis hoyasi shows the first report of an alula or "bastard wing", which means it had a flight manoeuvrability analogous to that of modern birds.

Research

The Las Hoyas site has been studied for more than two decades by researchers from the Universidad Autónoma de Madrid, the Universidad Complutense de Madrid and the National University of Distance Education, in collaboration with the Museo de las Ciencias de Castilla-La Mancha, which is responsible for the fossil record from the area.

Fossil content

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Amphibians

Amphibians
Genus Species Location Stratigraphic position Material Notes Images
Albanerpeton Indeterminate Uña Frontals Albanerpetonid
Albanerpeton
Celtedens C. ibericus Las Hoyas
C. megacephalus Uña
Gracilibatrachus G. avallei Las Hoyas Frog
Hylaeobatrachus Indeterminate Las Hoyas Salamander
Iberobatrachus I. angelae Las Hoyas Frog
Valdotriton V. gracilis Las Hoyas Salamander
Wealdenbatrachus W. jucarensis Uña Frog

Turtles

Turtles
Genus Species Location Stratigraphic position Material Notes Images
Hoyasemys H. jimenezi Las Hoyas [3]
Pleurosternidae Indeterminate Uña
Pelomedusidae Indeterminate Uña

Squamates

Squamates
Genus Species Location Stratigraphic position Material Notes Images
Becklesius Indeterminate, B. cataphractus Uña
Cuencasaurus C. estesi Uña
Hoyalacerta H. sanzi Las Hoyas
Jucaraseps J. grandipes Las Hoyas
Meyasaurus M. diazromerali Las Hoyas
M. unaensis Uña
Paramacellodus P. sinuosus Uña
Scandensia S. ciervensis Las Hoyas

Mammals

Mammals
Genus Species Location Stratigraphic position Material Notes Images
Crusafontia C. cuencana Uña
Eobaatar E. hispanicus Uña
Galveodon G. nannothus Uña
Spinolestes[4] S. xenarthrosus Las Hoyas Exceptionally complete specimen, preserving soft tissues such as pelage, ears and internal organs.

Crocodyliformes

Crocodyliformes
Genus Species Location Stratigraphic position Material Notes Images
Bernissartia Indeterminate Uña
Cassissuchus C. sanziuami Las Hoyas Gobiosuchid
Montsecosuchus Indeterminate Las Hoyas
Sabresuchus S.ibericus Uña
Unasuchus U. reginae Uña
Bernissartiidae Indeterminate Las Hoyas

Ornithodirans

Ornithodirans
Genus Species Location Stratigraphic position Material Notes Images
Concavenator C. corcovatus Las Hoyas "Nearly complete and articulated skeleton." [5]
Concornis[6] C. lacustris[6] Las Hoyas "Postcranial skeleton."[7]
Eoalulavis[6] E. hoyasi[6] Las Hoyas "Thoracic region and forelimbs."[7]
Euronychodon Indeterminate Las Hoyas [8]
Europejara E. olcadesorum Las Hoyas
Iberomesornis I. romerali Las Hoyas "Postcranial skeleton." [6][9]
Mantellisaurus M. atherfieldensis Las Hoyas "incomplete but fully-articulated right hindlimb" [10]
Pelecanimimus P. polyodon Las Hoyas "Skull and partial skeleton" [6][11]
Paronychodon Indeterminate Las Hoyas [12]
Ricardoestesia Indeterminate Las Hoyas [13]

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. ^ Martínez et al., 2017
  2. ^ Weishampel et al., 2004, pp.556-563
  3. ^ Pérez García et al., 2012
  4. ^ Martin et al., 2015
  5. ^ Ortega et al., 2010
  6. ^ a b c d e f "15.9 Provincia de Quenca, Spain; 4. Calizas de La Huergina Formation," in Weishampel et al., 2004, pp.561-562
  7. ^ a b "Table 11.1," in Weishampel et al. ,2004, p.212
  8. ^ Listed as "cf. Euronychodon sp." in "15.9 Provincia de Quenca, Spain; 4. Calizas de La Huergina Formation," in Weishampel et al., 2004, p.561
  9. ^ "Table 11.1," in Weishampel et al., 2004, p.213
  10. ^ Serrano et al., 2013
  11. ^ "Table 6.1," in Weishampel et al., 2004, p.138
  12. ^ Listed as "cf. Paranychodon sp." in "15.9 Provincia de Quenca, Spain; 4. Calizas de La Huergina Formation," in Weishampel et al., 2004, p.561
  13. ^ Listed as "cf. Ricardoestesia sp." in "15.9 Provincia de Quenca, Spain; 4. Calizas de La Huergina Formation," in Weishampel et al., 2004, p.561

Bibliography

  • Template:Cite LSA
  • Template:Cite LSA doi:10.1017/S0016756813000095 ISSN 0016-7568
  • Template:Cite LSA doi:10.4202/app.2011.0031 ISSN 0567-7920
  • Thomas Martin, Jesús Marugán-Lobón, Romain Vullo, Hugo Martín-Abad, Zhe-Xi Luo & Angela D. Buscalioni (2015). A Cretaceous eutriconodont and integument evolution in early mammals. Nature 526, 380–384. doi:10.1038/nature14905
  • Ortega, F., Escaso, F. & Sanz, J. L. (2010): A bizarre, humped Carcharodontosauria (Theropoda) from the Lower Cretaceous of Spain Nature 467: 203-206. HTML abstract
  • Template:Cite LSA ISBN 0-520-24209-2
  • Sanz, José L.; Chiappe, Luis M.; Pérez Moreno, Bernardino P.; Buscalioni, Ángela D.; Moratalla, José J.; Ortega, Francisco & Poyato Ariza, Francisco J. (1996): An Early Cretaceous bird from Spain and its implications for the evolution of avian flight. Nature 382(6590): 442-445. doi:10.1038/382442a0 (HTML abstract)
  • Pérez Moreno, B. P., Sanz, J. L., Buscalioni, A. D., Moratalla, J. J., Ortega, F., and Raskin-Gutman, D. (1994). "A unique multitoothed ornithomimosaur from the Lower Cretaceous of Spain." Nature, 30: 363-367.
  • Sanz, J. L. & Bonaparte, José F. (1992): A New Order of Birds (Class Aves) from the Lower Cretaceous of Spain. In: Jonathan J. Becker (ed.): Papers in Avian Paleontology Honoring Pierce Brodkorb. Natural History Museum of Los Angeles County Contributions in Science 36: 38-49.
  • Sanz, J. L. & Buscalioni, A.D. (1992): A new bird from the Early Cretaceous of Las Hoyas, Spain, and the early radiation of birds. Palaeontology 35(4): 829-845. PDF fulltext
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