[EN] During recent years the comparison and synchronisation of several high-resolution climate archives (ice-cores, deep sea cores and terrestrial sequences) has repeatedly shown that Late Glacial climatic oscillations were firstly very rapid and secondly, at least in the northern hemisphere, more or less simultaneous events. This database has made it possible to establish a broad spectrum of parameters which can be used to model the essential mechanisms of European Late Glacial climatic change. During phases when northern and north-western Europe lay for longer periods of time outside the direct influence of the North Atlantic Current (Gulf Stream) the tail of the current switched directly to the latitude of the Iberian Peninsula. Here, climate change had a far less severe impact on the flora and fauna than in the more northern regions, although the pattern of oscillations is the same as in Greenland or the North Atlantic. Nevertheless, several pleniglacial climatic events allowed characteristic species to reach the northern edge of the Iberian Peninsula and, during certain time-slices, to penetrate even further to the south. This paper discusses the chronological significance of typical Cold Fauna elements from specific Late Glacial sites, as represented by both skeletal remains and mobiliary and parietal art. Finally, we discuss the absolute age of the Cantabrian "Magdaleniense con Tri?ngulos" relative to the cold climate faunal data.

[ES] Durante las ?ltimas d?cadas se ha venido demostrando la existencia de oscilaciones clim?ticas ocurridas durante del Tardiglaciar en el Hemisferio Norte por medio de correlaciones entre los diferentes tipos de archivos (sondeos glaciares y marinos y secuencias terrestres). Esto ha permitido detectar un amplio espectro de par?metros que nos ayuda a comprender mejor los cambios clim?ticos ocurridos en Europa. Mientras los territorios situados en el Norte y Noroeste de Europa se ven privados de la influencia directa de la Corriente del Golfo durante el Tardiglaciar, la P. Ib?rica est? situada en estos momentos al Este de la parte norte de dicha Corriente Noratl?ntica. Aqu?, los cambios acaecidos parecen haber influido menos en la flora y fauna que en los territorios situados m?s al Norte. Sin embargo, de forma epis?dica, estas condiciones del M?ximo Glaciar pudieron penetrar dentro de la franja norte de la P. Ib?rica vi?ndose afectadas tambi?n las regiones del centro de este territorio. En este art?culo se analizan diferentes datos de Fauna Fr?a (representaciones parietales, mobiliares y restos faun?sticos) de determinados yacimientos peninsulares durante el Tardiglaciar, discuti?ndose sus fechas absolutas y relacion?ndolas con las del "El Magdaleniense con Tri?ngulos".