Abstract
A new species of Deinsdorfia is defined using new material coming from the karstic fissure infilling of Almenara-Casablanca 4 (Castelló, Spain), which shows important differences with the rest of the previously known species of the genus. The definition of a new species is supported by the characters found in extra material coming from the localities of Valdeganga, in the Albacete Province (Spain). The stratigraphical occurrence of this genus of pigmented-toothed shrews reinforces the idea of the Iberian Peninsula as a sink area during the Pliocene, where some Central-European soricids expanded their distribution. Most of those migrations or distributional expansions coincide with moments of climatic changes in the northern hemisphere. © 2008 Académie des sciences.
Original language | English |
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Pages (from-to) | 347-359 |
Journal | Comptes Rendus - Palevol |
Volume | 7 |
Issue number | 6 |
DOIs | |
Publication status | Published - 1 Aug 2008 |
Keywords
- Almenara-Casablanca
- Deinsdorfia doukasi nov. sp.
- Pliocene glaciation
- Spain
- Valdeganga