La Huérguina Formation
La Huérguina Formation | |
---|---|
Stratigraphic range: Late Barremian | |
Type | Geological formation |
Underlies | Contreras Formation or Unconformity with the Utrillas Group |
Overlies | Tragacete Formation |
Thickness | 60–100 m (200–330 ft) |
Lithology | |
Primary | Limestone, marl |
Other | Conglomerate |
Location | |
Coordinates | 40°05′23″N 1°53′52″W / 40.0897°N 1.8978°W |
Region | Cuenca, Castile-La Mancha |
Country | Spain |
Extent | South Iberian Basin |
Type section | |
Named for | Huérguina |
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 Spain whose strata date back to the Barremian stage of the Early Cretaceous.[1] Las Hoyas is a Konservat-Lagerstätte within the formation, located near the city of Cuenca, Spain. 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).
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
|
Notes Uncertain or tentative taxa are in small text; |
Amphibians
Amphibians | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Albanerpeton | Indeterminate | Uña | Frontals | Albanerpetonid | ||
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
See also
- List of dinosaur-bearing rock formations
- Paja Formation, contemporaneous Lagerstätte of Colombia
- Yixian Formation, contemporaneous Lagerstätte of China
References
- ^ Martínez et al., 2017
- ^ Weishampel et al., 2004, pp.556-563
- ^ Pérez García et al., 2012
- ^ Martin et al., 2015
- ^ Ortega et al., 2010
- ^ 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
- ^ a b "Table 11.1," in Weishampel et al. ,2004, p.212
- ^ 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
- ^ "Table 11.1," in Weishampel et al., 2004, p.213
- ^ Serrano et al., 2013
- ^ "Table 6.1," in Weishampel et al., 2004, p.138
- ^ 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
- ^ 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
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- 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