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  • Cenozoic Macrovertebrates (Betic and Iberic Basins). Taphonomy, Systematics, Biostratigraphy and Biogeography of large vertebrates are studied. Work is currently underway in various localities ranging from the upper Miocene to the Pleistocene (Crevillent 2, Alicante; Venta del Moro, Valencia; Puerto de la Cadena and Quibas, Murcia).
  • Study of Mio-Pliocene boundary in continental facies in Valencian Community. Several outcrops in CV containing paleontological sites from the upper Miocene-lower Pliocene (5-6 ma) are studied, which record the so-called Salinity Crisis of the Messinian, which led to the drying up of the Mediterranean and a faunal exchange between Africa and the Iberian Peninsula.
  • Study of Miocene vertebrate faunas from the Iberian Peninsula. In the Morteral (Magro) and Araia (Ribesalbes-Alcora) area, high-resolution series of small Aragonian mammals have been studied. The results allow to show paleontological information hitherto unknown and of great interest in the temporal context under study.
  • Study of Tertiary and Quaternary faunas from Ecuador. A very few Neogene deposits in Ecuador harbor a rich and spectacular fauna of micro and macrovertebrates (Eocene Cetaceans, Pleistocene Megafauna). The data from these enclaves should allow us to delve into the origin of cetaceans and the extinction of the South American megafauna.
  • Isotopic analysis of micromammalian fossil remains. The bones and teeth are the only remains found in paleontological contexts. The analysis of its chemical composition allows us to understand the paleobiology, paleoecology and habitat use of these organisms, reflecting the environmental parameters and paleoclimatic conditions .
  • GIS in palaeoclimatic and palaeoenvironmental reconstruction based on microvertebrates fossil remains. Microvertebrates are distributed according to a few bioclimatic variables, and these conditions can be characterized according to the area occupied by their populations. The GIS allows to relate the area of ​​distribution and the bioclimatic variables, which allows to know the real conditions of the past.
  • Both application of GIS and Image Analysis in form study in Palaeontology. The use of image analysis tools and GIS allows to recognize the shape of the remains of the cranial and postcranial skeleton of vertebrates. The vectorial analysis of the form, direct or based on statistical analysis, allows to approach a novel form of the theoretical study of the form.