Introduction and objectivesAlthough the Iberian Peninsula is a key area for understanding the Middle to Upper Paleolithic transition and the demise of the Neandertals, valuable evidence for these debates remains scarce and problematic in its interior regions. Sparse data supporting a late Neandertal persistence in the Iberian interior have been recently refuted and hence new evidence is needed to build new models on the timing and causes of Neandertal disappearance in inland Iberia and the whole peninsula. In this study we provide new evidence from Los Casares, a cave located in the highlands of the Spanish Meseta, where a Neandertal-associated Middle Paleolithic site was discovered and first excavated in the 1960’s. Our main objective is twofold: (1) provide an updated geoarcheological, paleoenvironmental and chronological framework for this site, and (2) discuss obtained results in the context of the time and nature of the last Neandertal presence in Iberia.MethodsWe conducted new fieldwork in an interior chamber of Los Casares cave named ‘Seno A’. Our methods included micromorphology, sedimentology, radiocarbon dating, Uranium/Thorium dating, palinology, microfaunal analysis, anthracology, phytolith analysis, archeozoology and lithic technology. Here we present results on site formation processes, paleoenvironment and the chronological setting of the Neandertal occupation at Los Casares cave-Seno A.Results and discussionThe sediment sequence reveals a mostly in situ archeological deposit containing evidence of both Neandertal activity and carnivore action in level c, dated to 44,899–42,175 calendar years ago. This occupation occurred during a warm and humid interval of Marine Isotopic Stage 3, probably correlating with Greenland Interstadial 11, representing one of the latest occurrences of Neandertals in the Iberian interior. However, overlying layer b records a deterioration of local environments, thus providing a plausible explanation for the abandonment of the site, and perhaps for the total disappearance of Neandertals of the highlands of inland Iberia during subsequent Greenland Stadials 11 or 10, or even Heinrich Stadial 4. Since layer b provided very few signs of human activity and no reliable chronometric results, and given the scarce chronostratigrapic evidence recorded so far for this period in interior Iberia, this can only be taken as a working hypothesis to be tested with future research. Meanwhile, 42,000 calendar years ago remains the most plausible date for the abandonment of interior Iberia by Neandertals, possibly due to climate deterioration. Currently, a later survival of this human species in Iberia is limited to the southern coasts.

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Los resultados de las excavaciones realizadas entre 1968 y 1984 en la Cova de Hort de Cortés- Volcán del Faro quedaron limitados a identificar materiales solutrenses, magdalenienses y neolíticos-calcolíticos. Una lectura crítica de la Memoria de excavaciones, publicada en 2003, permitió plantear la posibilidad de la presencia de ocupaciones anteriores, posiblemente gravetienses. En 2018 se iniciaron nuevos trabajos en el yacimiento, dentro de un proyecto que pretende recuperar información a partir de los cortes de las antiguas excavaciones. Los datos obtenidos en el área más externa (corte frontal posterior, cuadrícula O4) han permitido retomar la discusión sobre la existencia de los niveles presolutrenses. Los primeros resultados, sobre los trabajos realizados en el perímetro del sector A de las antiguas excavaciones, así como los datos geoaqueológicos, radiocarbónicos e industriales plantean una serie de alternativas sobre la formación y conservación del depósito que supone un punto de partida para la comprensión de un yacimiento complejo.

4077 Several murine models resembling multiple myeloma have been developed in the last years: the subcutaneous plasmocytoma model and the disseminated model, based on the iv or intracardiac injection of MM cells, have been widely used to test the efficacy of novel agents. Nevertheless, it is well known the crucial role that the interaction between MM plasma cells and the bone marrow microenvironment plays in MM pathogenesis as well as in the proliferation of MM cells and drug resistance; however, unfortunately, most murine models do not recapitulate these interactions. In order to overcome this caveat, other models such as the SCIDhu or the SCIDrab have been developed. However, in these models, the induced microenvironmental milleu is derived from a fetus and a rabbit respectively, which can be relatively different from that found in an adult patient with MM. We have developed a novel model of a human disseminated MM with the presence of human adult microenvironment. For this purpose, CB17-SCID mice, which lack B and T lymphocytes, were anesthetized and a human bone chip obtained from a healthy adult patient undergoing a hip replacement due to a non-malignant fracture, was subcutaneously implanted in the back of the mice. In the same day 3×106 MM1S-Luc cells were iv injected through the tail vein. Two groups were also included as controls in the study, one with MM1S-Luc cells without the bone chip, and the other with only the human bone chip (without MM cells). Luciferase activity was measured three times per week using a Xenogen-IVIS 50 system after ip injection of 0,15 mg/Kg luciferin. Mice were sacrificed when they developed signs associated with advanced disease, such as body weight loss or back limb paralysis. Although the group of mice receiving MM1S-Luc without bone, did develop a disseminated myeloma, this was much more precocious in the group of mice with a human bone subcutaneous implant. In fact, in mice with human bone and MM1S-Luc cells, the luciferase activity was detectable a median of 9 days after the injection of the cells whereas it was necessary 16 days for obtaining the same effect in mice without the bone chip. This is pointing out that the bone chip in these mice induces a favourable environment for myeloma growth and could be appropriate model to study the interactions of MM cells with human stroma. The increase of tumour growth rate also correlated with a decrease in survival. Median survival (CI 95%) of 64 (47-80) days for mice without bone vs 48 (45-50) days for mice with human bone (Log Rank=0.004). Regarding the sites of infiltration, luminescence images showed a disseminated involvement in all skeletal regions, and this was confirmed by histopathology, as there was a general infiltration of spine, femora, tibia and cranium of these mice. By contrast we did not find infiltration of extra-skeletal regions such as heart, lung or spleen in any mice and only unclear infiltrates were observed in the kidney and liver of some mice. In order to validate the suitability of this model for testing the in vivo antimyeloma activity of novel drugs in the presence of a human microenvironment, 6 mice bearing this novel model were randomized to receive: bortezomib (0.5 mg/Kg ip five days per week) + dexamethasone (0.5 mg/Kg 2 days per week) or vehicle control. A second group of the same number of mice with MM1S-Luc but without the bone chip were randomized in the same way and used as control. Bortezomib + dex significantly decreased tumour growth in both groups of mice without any clear differences in activity between both models, suggesting that this combination overcomes the influence of the microenvironment. In summary we have developed a murine model of MM that may allows us to 1) gain insights into the role of the BM microenvironment interactions in MM pathogenesis. 2) Evaluate the in vivo activity of different anti-MM agents in the presence of human microenvironment. 3) Potentially, this model could also contribute to analyze the effect of different agents in the myeloma bone disease. Disclosures: No relevant conflicts of interest to declare.