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General palaeontology, systematics and evolution (Vertebrate palaeontology) Early Late Miocene insectivores (Eulipotyphla, Mammalia) from the Cañada section (Province of Zaragoza, east Central Spain).

dc.contributor.authorHoek Ostende, L. W. van den
dc.contributor.authorLópez Guerrero, Paloma
dc.contributor.authorPeláez-Campomanes de Labra, Pablo
dc.contributor.authorÁlvarez Sierra, María De Los Ángeles
dc.contributor.authorGarcía Paredes, Israel
dc.date.accessioned2023-06-20T03:42:43Z
dc.date.available2023-06-20T03:42:43Z
dc.date.issued2012
dc.description.abstractVallesian (early Late Miocene) strata from the recently introduced Ca˜nada section (province of Zaragoza, east Central Spain) have yielded fairly large insectivore assemblages. These show that, after the generally dry Aragonian, the Vallesian gave rise to more humid conditions that were favourable to insectivores, both in number of taxa, and in overall number of specimens. The assemblage of Ca˜nada 8 (Biozone H) is dominated by shrews, whereas the assemblage of Ca˜nada 10 (uppermost Biozone H) contains the oldest record of Desmanella in the area. This seems to signify a bioevent in which after millions of years of absence, talpids return to the area. In addition to the Vallesian assemblages, a small Turolian insectivore fauna has been recovered. On the basis of the rodents, Ca˜nada 12 was assigned to Biozone L, and the insectivore assemblage is very similar to the assemblages from the Teruel basin of that zone. This implies that the discovery of Postpalerinaceus in Ca˜nada 12 is the youngest published record of this large spiny hedgehog.
dc.description.abstractLes niveaux Vallésiens récemment présentés de la section de la Ca˜nada ont livré de relativement grands assemblages d’insectivores. Ces derniers attestent que les conditions climatiques, alors relativement sèches à l’Aragonien, deviennent plus humides au Vallésien, qu’un environnement favorable aux insectivores se développe, ces derniers étant, par comparaison, bien mieux représentés autant par le nombre de taxa que par l’abondance relative des spécimens présents dans les assemblages. L’assemblage Ca˜nada 8 (Biozone H) est dominé par les musaraignes, tandis que l’assemblage Ca˜nada 10 (partie supérieur de la Biozone H) contient le plus ancien Desmanella de la région. Cette découverte semble marquer un événement durant lequel, après des millions d’années d’absence, les talpidés ré-immigrent en Espagne du centre-est. En plus des assemblages vallésiens, une faunule turolienne est décrite.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/26248
dc.identifier.doidx.doi.org/10.1016/j.crpv.2012.06.003
dc.identifier.issn1631-0683
dc.identifier.officialurlhttp://www.journals.elsevier.com/comptes-rendus-palevol/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/44298
dc.journal.titleComptes rendus. Palévol
dc.language.isoeng
dc.page.final506
dc.page.initial495
dc.publisherEd. scientifiques et médicales Elsevier
dc.rights.accessRightsopen access
dc.subject.cdu569(460.27)
dc.subject.keywordVallesian
dc.subject.keywordBiostratigraphy
dc.subject.keywordPalaeoecology
dc.subject.keywordDesmanella
dc.subject.keywordPostpalerinaceus
dc.subject.keywordVallésien
dc.subject.keywordBiostratigraphie
dc.subject.keywordPaléoecologie
dc.subject.ucmPaleontología
dc.subject.unesco2416 Paleontología
dc.titleGeneral palaeontology, systematics and evolution (Vertebrate palaeontology) Early Late Miocene insectivores (Eulipotyphla, Mammalia) from the Cañada section (Province of Zaragoza, east Central Spain).
dc.title.alternativeInsectivores (Eulipotyphla, Mammalia) du Miocène Supérieur de la section de la Cañada (Prov. de Zaragoza, centre-est de l’Espagne)
dc.typejournal article
dc.volume.number11
dspace.entity.typePublication
relation.isAuthorOfPublication0352da50-3a05-49d4-b2a2-81cbe14d4992
relation.isAuthorOfPublication.latestForDiscovery0352da50-3a05-49d4-b2a2-81cbe14d4992

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