0000000000277138
AUTHOR
Carlos De Santisteban
showing 7 related works from this author
Cazuma 1, nueva localidad de micromamíferos (Mammalia, Rodentia) del Aragoniense superior en la cuenca de Quesa - Bicorp (prov. Valencia)
2021
En el presente trabajo se describe la asociación de Megacricetodon crusafonti (Freudenthal, 1963), Megacricetodon sp. y Heteroxerus aff. grivensis (Forsyth Major, 1893) de Cazuma 1, localidad situada en el sector de Bicorp, en la cuenca terciaria de Quesa - Bicorp (Prov. Valencia). La edad atribuida a esta localidad es Aragoniense Superior. Hasta el momento, con ésta, ya son cinco las localidades conocidas de mamíferos en el Aragoniense de la cuenca de Quesa - Bicorp (Cazuma 1, Quesa 0, Quesa 2, Quesa 3 y Quesa 6).
Age determination of the Arcillas de Morella Formation (Maestrazgo Basin, Spain)
2014
New palynological analysis of the Arcillas de Morella Formation provides data for determinations of age of the Lower Cretaceous strata in the Ermita Sant Antoni de la Vespa section located in the d...
Dolomitization as an eventualdetermining factor in the colour alteration index (CAI)
1993
Abstract The Colour Alteration Index of conodonts (CAI) is indicative of the degree of alteration of organic material that exists in the interior of the conodonts. This CAI is used ordinarily in the determination of paleotemperatures. More frequent findings of abnormally high CAI values, equivalent to paleotemperatures that are not compatible with temperatures obtained by other more trustworthy methods, has taken us to use values not superior to 6 for the establishment of paleotemperatures. The CAI values measured in specimens proceding from dolostones in the Iberian Range (Spain) show in this way a certain degree of incompatibility with geological data. These anomalous values are the conse…
A new styracosternan hadrosauroid (Dinosauria: Ornithischia) from the Early Cretaceous of Portell, Spain
2021
A new styracosternan ornithopod genus and species is described based on the right dentary of a single specimen from the Mirambell Formation (Early Cretaceous, early Barremian) at the locality of Portell, (Castellón, Spain).Portellsaurus sosbaynatigen. et sp. nov. is diagnosed by two autapomorphic features as well as a unique combination of characters. The autapomorphies include: the absence of a bulge along the ventral margin directly ventral to the base of the coronoid process and the presence of a deep oval cavity on the medial surface of the mandibular adductor fossa below the eleventh-twelfth tooth position. Phylogenetic analyses reveal that the new Iberian form is more closely related …
New rodent faunas from Middle Miocene and Mio- Pliocene in the Cabriel Basin (Valencia, Spain)
2011
Five new localities with micromammal remains have been located in the Cabriel Basin. These localities are situated in the eastern area of the Cabriel Basin, in the Juan Vich ravine, where the oldest deposits of this basin crop out. The localities JV2, JV3 and JV6 are of Middle Miocene age, JVTLI1 of Middle Miocene or Late Miocene age and JVTS1 of Late Miocene or Early Pliocene age. The beginning of the sedimentary history of the basin was attributed to Late Turolian (Late Miocene). The new sedimentary record from the Juan Vich ravine and the mammalian findings extend the stratigraphic and paleontological knowledge of the Basin.
Neogene and Quaternary fan-delta deposits in southeastern Spain. Field Guide.
1991
[EN] A guided field-trip througIt tIta basins of Fortuna, Carrascoy-Murcia, Lower Segura and Cope. with detailed sections, interpretation of rock bodies and sedientary models.
Revisión de la sección del yacimiento del Mas de la Chimenea Alta (Formación Arcillas de Morella, Castellón) y significado en el contexto paleoambien…
2012
Desde los primeros estudios estratigráficos y paleontológicos, que datan de principios del siglo XX, la Fm Morella se ha caracterizado por su coloración rojiza y su contenido fósil. La mayor parte de sus depósitos se han interpretado como continentales, aunque con intercalaciones locales de materiales marinos. En esta unidad se da la paradoja de que muchos de los lugares descritos con fauna de vertebrados continentales se encuentran en depósitos interpretados como ambientes marinos poco profundos y de transición. La sección del Mas de la Chimenea Alta es un ejemplo. Ésta contiene yacimientos con fósiles de vertebrados que son claramente alóctonos, pero también otros, con icnitas que permite…