Praia do Guincho tracksite: Early Barremian, Portugal
collected 2011
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Reptilia
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Figueiredo et al. 2020 | 1 specimen | |||||||||
fragment of vertebral process | ||||||||||
Reptilia
- Iguanodontipodidae
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1 specimen | ||||||||||
footprint cast (CPGP.3.11.1) | ||||||||||
see common names |
Geography
Country: | Portugal | State/province: | Lisboa |
Coordinates: | 38.5° North, 9.2° West (view map) | ||
Paleocoordinates: | 28.8° North, 15.0° East (Wright 2013) | ||
Basis of coordinate: | stated in text | ||
Geographic resolution: | small collection |
Time
Period: | Cretaceous | Epoch: | Early Cretaceous |
Stage: | Barremian | 10 m.y. bin: | Cretaceous 2 |
Key time interval: | Early Barremian | ||
Age range of interval: | 125.77 - 121.4 m.y. ago |
Stratigraphy
Formation: | Papo Seco |
Stratigraphic resolution: | bed |
Lithology and environment
Primary lithology: | "cross stratification",medium,coarse sandstone |
Secondary lithology: | fine,gypsiferous,gray,white silty sandstone |
Includes fossils? | Y |
Lithology description: footprint: "small coarse-grained limestone block" "a meter thick, white or grey, fine-grained silty sandstones, with gypsum and thin organic laminae. The organic laminae frequently highlight distinct erosive-based sets with cross-stratification and, sometimes, parallel stratification. These sediments are interbedded with up to three layers of trough cross-stratified, moderately sorted, medium to coarse feldspathic sandstones. In general, these coarser grained layers are less than 0.80 m thick, wedging out laterally into the fine-grained deposits. Channel-shaped beds of fining upward coarse to medium-grained sandstone with scattered pebbles occasionally occur. Cross stratification and the geometry of the channel-shape beds indicates a general W to SW direction of the palaeocurrents. This mostly siliciclastic interval passes upwards to mudstone-marl layers with carbonate nodules. | |
Environment: | coarse channel fill |
Geology comments: "The coarser grained units, which texturally resemble the tridactyl footprint sediment cast, probably represent deposition in distributary channels within the coastal plain. The thicker and coarser sandstone bed may be attributed to a larger channel" |
Taphonomy
Modes of preservation: | body,cast,trace |
Size of fossils: | macrofossils,mesofossils |
Spatial orientation: | life position |
Fragmentation: | occasional |
Temporal resolution: | snapshot |
Spatial resolution: | autochthonous |
Collection methods and comments
Collection methods: | surface (float),surface (in situ),observed (not collected) |
Reason for describing collection: | taxonomic analysis | Collection dates: | 2011 |
Metadata
Also known as: | Cabo Espichel | ||
Database number: | 217238 | ||
Authorizer: | M. Carrano | Enterer: | M. Carrano |
Modifier: | M. Carrano | ||
Created: | 2021-02-01 15:24:15 | Last modified: | 2025-02-22 15:12:02 |
Access level: | the public | Released: | 2021-02-01 15:24:15 |
Creative Commons license: | CC0 |
Reference information
Primary reference:
79841. | S. Figueiredo, P. Dinis, P. Rosina and I. Bachtsevanidou Strantzali. 2017. A new record of a possible ornithopod footprint from the Lower Cretaceous of Cabo Espichel (Sesimbra, Portugal). Bollettino della Società Paleontologica Italiana 56(2):217-231 [M. Carrano/M. Carrano] |
Secondary references:
75421 | S. D. Figueiredo, C. N. d. Carvalho, P. P. Cunha and I. S. Carvalho. 2021. New dinosaur tracks from the lower Barremian of Portugal (Areia do Mastro Formation, Cape Espichel). Journal of Geoscience and Environment Protection 9:84-96 [M. Carrano/M. Carrano] | |
86555 | S. D. Figueiredo, I. S. Carvalho, X. Pereda-Suberbiola, P. P. Cunha, V. Antunes and I. Díaz-Martínez. 2022. New ornithopod footprints from the Areia do Mastro Formation (Lower Cretaceous), Espichel Cape (Portugal, Western Iberia) and their context in the Iberian ichnological ornithopod record. Cretaceous Research 131:105069 [M. Carrano/M. Carrano] | |
81822 | S. D. Figueiredo, P. P. Cunha, X. Pereda Suberbiola, C. N. Carvalho, I. S. Carvalho, E. Buffetaut, H. Tong, M. Fernanda Sousa, V. Antunes and R. Anastácio. 2022. The dinosaur tracksite from the lower Barremian of Areia do Mastro Formation (Cabo Espichel, Portugal): implications for dinosaur behavior. Cretaceous Research 137:105219 [M. Carrano/M. Carrano] | |
75850 | S. D. Figueiredo, X. Pereda-Suberbiola, P. P. Cunha, F. Sousa, and P. Rosina. 2020. A brief approach about the ornithopod dinosaurs from the Papo-Seco Formation (Cabo Espichel, western central Portugal). Boletim do Centro Português de Geo-História e Pré-História 2(1):59-63 [M. Carrano/M. Carrano] |