摘要：En 2010 y 2011, el ¨¢rea del sondeo en el cual niveles solutrenses hab¨ªan sido expuestos en la Cueva del Mir¨®n fu¨¦ duplicada. Estos dep¨®sitos, en contraste marcado con los niveles del Magdaleniense Inicial e Inferior superyacentes (que yacen casi horizontalmente y que son extraordinaria- mente ricos en materia org¨¢nica y toda clase de residuos culturales¨Cartefactos de todo tipo, estructuras y restos de fauna¡ªindicativos de importantes ocupaciones residenciales repetidas y multifuncionales de la cueva), siguen la pendiente de 15 grados de la cara erosiva del relleno aluvial del in- terior de la cueva y son culturalmente bastante pobres. Los niveles solutrenses est¨¢n datados por el radiocarbono entre 19,230 y 18,390 BP (sin ca- librar), aunque el nivel m¨¢s alto (121) es amb¨ªguo debido a la ausencia de puntas solutrenses al menos en la peque.a ¨¢rea (ahora 4 m 2 ) que ha sido excavada. Los otros niveles solutrenses (122-127) son particularmente ricos en fragmentos de puntas foliadas y de muesca de diversos tipos (in- cluyendo a las de base c¨®ncava) y deshecho l¨ªtico, pero con relativamente pocos otros utensilios retocados, lo cual sugiere unas expediciones de caza en el interior monta.oso del Este de Cantabria en parte en momentos de amelioraci¨®n clim¨¢tica durante el Ultimo M¨¢ximo Glacial (sensu lato¨C justo despu¨¦s del Evento Heinrich 2, durante o poco despu¨¦s del Interestadio Greenland 2), cuando, sin embargo, los glaciares todav¨ªa recubr¨ªan las laderas superiores de la vecina Cordillera. Otros indicios de la caza incluyen a unas azagayas de asta, algunas de las cuales tienen formas y de- coraciones grabadas t¨ªpicas del Solutrense cant¨¢brico. Por otro lado estos niveles son extraordinariamente ricos en conchas marinas (de diversas especies), muchas de las cuales est¨¢n perforadas. Estas est¨¢n acompa.adas por otros objetos perforados (caninos de ciervo, huesos y piedras ta- llados en forma de caninos), asi confimando el patr¨®n revelado en el sondeo excavado en 1998 y 2000. Los restos de fauna est¨¢n presentes, pero no son abundantes, lo cual podria sugerir o que los reses fueron descuartizados y depositados en otra(s) parte(s) de la cueva o llevados a otros si- tios para su consumo, tal vez en la parte baja y as¨ª m¨¢s habitable del valle del R¨ªo As¨®n
其他摘要：In 2010 and 2011, the area of the test pit in which Solutrean levels originally had been exposed in El Mir¨®n Cave was doubled. These deposits, in sharp contrast with the overlying Initial and Lower Magdalenian levels (which lie relatively flat and are extraordinarily rich in organic matter and all man- ner of cultural debris¨Cartifacts of many types, features and faunal remains¨Cindicative of major, repeated, multi-functional, residential occupations of the cave), follow the 15 degree slope of the erosional face of the alluvial fill of the inner cave and are culturally rather poor. The Solutrean levels are ra- diocarbon dated between 19,230 and 18,390 BP (uncal.), although the topmost level (121) is ambiguous due to the lack of Solutrean points in the small area (now 4 m 2 ) in which it has been dug. The other Solutrean levels (122-127) are particularly rich in foliate and shouldered point fragments of diverse types (including concave base points) and lithic d¨¦bitage, but relatively few other retouched tools, suggesting that the successive occupa- tions may have been related to brief hunting expeditions in the montane interior of eastern Cantabria in part during times of slight climatic ameliora- tion within the Last Glacial Maximum (sensu lato¨C specifically soon after Heinrich Event 2, during or immediately after Greenland Interstadial 2), when ice sheets nonetheless still covered the upper slopes of the adjacent Cordillera. Other indicators of hunting include broken antler points (sagaies), some of which are shaped and decorated in ways that are classic for this period in Cantabria. On the other hand, these levels are unusually rich in marine shells (of diverse species), many of which are perforated. These are accompanied by other perforated objects (red deer canines, bones and stones fashioned to resemble such canines), confirming the pattern observed in the initial test pit. Faunal remains are present, but are not very abun- dant, suggesting that carcasses were either butchered and the bones deposited elsewhere in the cave or removed for consumption at other sites, perhaps in the more habitable lower reaches of the As¨®n River valley
关键词：Solutre aldia; Cueva del Mir¨®n; Azken Maximo Glaziarra
其他关键词：Solutrean; El Mir¨®n Cave; Cantabria; Last Glacial Maximum
