Rocha-Pelejón, RPAH (Galve syncline): Late/Upper Hauterivian, Spain

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Reptilia
Mesosuchia indet. Huxley 1875
    = Mesoeucrocodylia indet. Whetstone and Whybrow 1983
Ruiz-Omeñaca et al. 2004
Neosuchia indet. Clark 1988
Ruiz-Omeñaca et al. 2004
Reptilia - Goniopholididae
Goniopholis cf. crassidens Owen 1842
1 specimen
Reptilia
Theriosuchus sp. Owen 1878
Ruiz-Omeñaca et al. 2004
    = aff. Theriosuchus sp. Owen 1878
Tennant et al. 2016
cf. Goniopholis sp. Owen 1842
1 specimen
    = Bernissartia sp. Dollo 1883
Ruiz-Omeñaca et al. 2004
Reptilia - Testudines
Testudines indet. Batsch 1788
Ruiz-Omeñaca et al. 2004
see common names

Geography
Country:Spain State/province:Teruel
Coordinates: 40.7° North, 0.7° West (view map)
Paleocoordinates:31.0° North, 9.0° East
Basis of coordinate:based on political unit
Geographic resolution:outcrop
Time
Period:Cretaceous Epoch:Early/Lower Cretaceous
Stage:Hauterivian 10 m.y. bin:Cretaceous 2
Key time interval:Late/Upper Hauterivian
Age range of interval:132.60000 - 125.77000 m.y. ago
Stratigraphy
Formation:El Castellar
Local section:Galve Local bed:250 m
Local order:bottom to top
Stratigraphic resolution:group of beds
Stratigraphy comments: Can't find reference to "Unit 3/4" in Diaz and Yebenez 1987. Comments below refer to units 3 and 4.
Lithology and environment
Primary lithology: sandy "siliciclastic"
Secondary lithology: "mixed carbonate-siliciclastic"
Lithology description: Unit 3: Formed predominately of red limes, with rare thick lenses of terrigenous deposits (Molina and Yebenes 1987). "The coarser terrigenous material (fine to medium sand) is not typically channelized, but most frequently occurs in lenticular bedding and isolated dunes (Diaz et al. 1984)." Unit 4: "formed by sequences composed of marls and micrites. Carbonate nodules frequently occur within the marls, and the micrites reveal desiccation features." (Diaz et al. 1984) See also Molina and Yebenes 1987.
Environment:deltaic indet.
Geology comments: "Unit 3 is characterized by the disappearance of the carbonate facies and predominance of mudstones. This is interpreted as a muddy intertidal flat deposit...Despite a large discontinuity existing within unit 3, or at its upper or lower boundaries, the intertidal facies can be integrated withing[sic].." terregenous delta-derived material prograding into a shallow lagoon (Diaz et al. 1987). Unit 4: "This facies correspond to shallow coastal lagoon deposits, formed in fresh to brackish water (Diaz et al. 1987)"
Taphonomy
Modes of preservation:body,trace
Size of fossils:macrofossils,mesofossils
Disassociated major elements:many
Disassociated minor elements:many
Fragmentation:frequent
Collection methods and comments
Collection excludes:all microfossils,some genera,some macrofossils,ichnofossils
Collection methods:field collection
Reason for describing collection:taxonomic analysis
Collection method comments: Material is in the J. M. Herrero collection (Galve).

Unit 4: abundant Charophytes, Bivalves, Gastropods, fish teeth and vertebrate remains.
Metadata
Also known as:Rocha Pelejon, Teruel, Spain
Database number:36378
Authorizer:J. Alroy, M. Carrano, P. Mannion Enterer:R. Whatley, P. Mannion, M. Carrano
Modifier:M. Carrano Research group:vertebrate
Created:2004-01-27 12:58:29 Last modified:2007-01-25 16:42:08
Access level:the public Released:2004-01-27 12:58:29
Creative Commons license:CC BY
Reference information

Primary reference:

7243.5% 17900A. D. Buscalioni and J. L. Sanz. 1987. Cocodrilos del Cretacico Inferior de Galve (Teruel, España). Estudios Geologicos (Madrid) extr.:23-43 [J. Alroy/R. Whatley/J. Alroy]

Secondary references:

72425% 24760M. Diaz, A. Yébenes, A. Goy and J. L. Sanz. 1984. Landscapes inhabited by Upper Jurassic/Lower Cretaceous archosaurs (Galve, Teruel, Spain). In W.-E. Reif & F. Westphal (ed.), Third Symposium on Mesozoic Terrestrial Ecosystems, Short Papers 67-72 [J. Alroy/R. Whatley/M. Uhen]
72405% 17900M. D. Molina and A. Yébenes. 1987. La sedimentacion litoral y continental durante el Cretacico Inferior. Sinclinal de Galve, Teruel. Estudios Geologicos (Madrid) extr.:3-21 [J. Alroy/R. Whatley/J. Alroy]
19754ETE J. I. Ruiz-Omeñaca, J. I. Canudo, M. Aurell, B. Bádenas, J. L. Barco, G. Cuenca-Bescós, and J. Ipas. 2004. Estado de las investigaciones sobre los vertebrados del Jurásico Superior y Cretácico Interior de Galve (Teruel) [State of the investigations into the vertebrates of the Upper Jurassic and Lower Cretaceous of Galve (Teruel)]. Estudios Geológicos 60:179-202 [M. Carrano/M. Carrano]
32167ETE B. Sánchez-Hernández, M. J. Benton, and D. Naish. 2007. Dinosaurs and other fossil vertebrates from the Late Jurassic and Early Cretaceous of the Galve area, NE Spain. Palaeogeography, Palaeoclimatology, Palaeoecology 249:180-215 [R. Butler/R. Butler/M. Carrano]
59838 J. P. Tennant, P. D. Mannion, and P. Upchurch. 2016. Evolutionary relationships and systematics of Atoposauridae (Crocodylomorpha: Neosuchia): implications for the rise of Eusuchia. Zoological Journal of the Linnean Society 177:854-936 [P. Mannion/P. Mannion]