|Imagens do artigo por Gasca et al. (2017)|
Só dentro desta unidade, na área de Ladruñán, na província de Teruel, foram reconhecidos 31 locais contendo fósseis de variados vertebrados e trilhos de dinossauros.
O registro de dinossauros identificado inclui ornitópodes, terópodes e saurópodes; os trilhos permitem concluir que estes frequentavam zonas costeiras de lagos, planícies aluviais e cursos fluviais. Os fragmentos de cascas de ovos são frequentes em toda a unidade, mas são claramente mais comuns em depósitos lacustres.
O resumo, em inglês, é o seguinte:
The Barremian Mirambel Formation (Maestrazgo Basin, Iberian Chain, NE Spain) preserves different types of dinosaur and other vertebrate fossils (skeletal, eggshell and ichnological remains). A total of 31 vertebrate fossil sites and tracksites have been recognized within this unit in the Ladruñán area (Teruel province). Detailed stratigraphic, sedimentological and micropalaeontological analyses have also been performed in the unit. A vertical sedimentary trend from alluvial-dominated facies (meandering river and related overbank areas) to palustrine-lacustrine facies and back has been defined for the Mirambel Formation in this area. The depositional system was located close to the coastline, as indicated by sporadic marine input in the lower part of the unit.
Most fossil remains were recovered by surface collection as well as by the usual techniques used for macrovertebrate excavations. The dinosaur record identified comprises ornithopods, theropods and sauropods. Four distinct track-bearing horizons have been identified. The heterolithic nature and aggradation characteristic of the Mirambel Formation are favourable factors for track formation and preservation. The dinosaur tracks consist of convex hyporeliefs or concave epireliefs that record the trackmakers as they frequented lakeshores, alluvial floodplains and fluvial courses. Macrovertebrate bonebeds occur in alluvial settings (poorly-drained floodplains and “ponds”). Microvertebrate concentrations are located in shallow lacustrine deposits. Isolated skeletal elements can be found in a great variety of deposits. Attritional accumulation in a low-energy depositional context is the general pattern of origin for the bone-bearing fossil sites of the Mirambel Formation. As regards the genetic framework, the resulting skeletal assemblages are predominantly the result of physical factors, with sedimentology as a key factor, rather than biological phenomena. Eggshell fragments are frequent throughout the unit but are clearly more common in palustrine-lacustrine deposits. These can be taken to be parautochthonous bioclasts from nearby areas and might be indicative of the preferential affinity of the egg-layers for wetlands and lakeshores.
A referência completa do artigo é:Gasca, J. M., Moreno-Azanza, M., Bádenas, B., Díaz-Martínez, I., Castanera, D. , Canudo, J. I., Aurell, M. 2017. Integrated overview of the vertebrate fossil record of the Ladruñán anticline (Spain): Evidence of a Barremian alluvial-lacustrine system in NE Iberia frequented by dinosaurs, Palaeogeography, Palaeoclimatology, Palaeoecology, Volume 472: 192-202