0000000000656862

AUTHOR

Jan Van Der Made

showing 3 related works from this author

Early Pliocene continental vertebrate fauna at Puerto de la Cadena (SE Spain) and its bearing on the marine-continental correlation of the Late Neoge…

2017

In this paper, we synthesize sedimentological, magnetostratigraphic and paleontological data from the continental vertebrate site of Puerto de la Cadena (Murcia, SE Spain), in order to clarify its age. The study site is located on the northern edge of the Carrascoy mountain range, in the upper part of the Cigarrón Unit. The end-Messinian discontinuity has been detected at the base of this unit, which indicates it has an early Pliocene age. Abundant remains of small and large vertebrates, including rodents, lagomorphs, primates, carnivorans, perissodactyls, artiodactyls, proboscideans, testudines, squamats, and crocodiles, have been found in this area. Some of these elements are of African o…

010506 paleontologyMessinian salinity crisisFaunaEstratigrafíaLate MioceneBiostratigraphy010502 geochemistry & geophysicsOceanographyNeogene01 natural sciencesPaleontologybiology.animalSivatheriumEcology Evolution Behavior and SystematicsMagnetostratigraphy0105 earth and related environmental sciencesEarth-Surface ProcessesMammalsbiologyEcologyMagnetostratigraphyPaleontologyVertebrateReptilesBiostratigraphybiology.organism_classificationHipparionGeologyIberian Peninsula
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La Cova de Dalt del Tossal de la Font

2014

Estado de las excavaciones y estudios realizados en La Cova de Dalt del Tossal de la Font (Castellón).

UNESCO::HISTORIA:HISTORIA [UNESCO]
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Une faune très diversifiée du Pléistocène inférieur de la Sierra de Quibas (province de Murcia, Espagne)

2001

The Quaternary karstic site of Sierra de Quibas (Abanilla, province of Murcia, Spain) has provided a wide faunal list with more than 60 species. The assemblage of the taxa Arvicola deucalion, Castillomys rivas rivas, Eliomys intermedius, Equus altidens, Capra sp. aff. C. alba and cf. Praeovibos allows the correlation with other Spanish Lower Pleistocene sites in the Betic Cordillera, as Plines 1, Orce 3 and Venta Micena. Therefore Quibas can be located between 1.3 and 1.0 Ma. The palaeoenvironmental features of the area around the karstic cavity and the palaeoclimatic regime are inferred.

biologyPleistoceneOcean EngineeringBiostratigraphybiology.organism_classificationArchaeologyEquusGeographyBiochronologyArvicolaEliomysQuaternaryCenozoicEcology Evolution Behavior and SystematicsComptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science
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