Climatic and stratigraphic paleoindicators from the Canary Island

[EN] The last 5 Myr  are characterized by cliamatic variations globally and are reflected in ancient fossiliferous marine deposits visible in the Canary Islands. The fossils contained are identificated as paleoecological and paleoclimatic indicators. The Mio-Pliocene Transit is represented by the coral Siderastrea micoenica Osasco, 1897; the gastropods Rothpletzia rudista Simonelli, 1890; Ancilla glandiformis (Lamarck, 1822); Strombus coronatus Defrance, 1827 and Nerita emiliana Mayer, 1872 and the bivalve Gryphaea virleti Deshayes, 1832 as most characteristic fossils  and typical of a very warm climate and littoral zone. Associated  lava flows  have been dated radiometrically  and provides a range between  8.9 and about 4.2 Kyr. In the mid-Pleistocene, about 400,000 years ago, the called Marine Isotope Stage 11, a strong global warming that caused a sea level rise happens. Remains of the MIS 11  are preserved on the coast of Arucas (Gran Canaria), and associated with a tsunami in Piedra Alta (Lanzarote). These fossilifeorus  deposits contains the bivalve Saccostrea cucullata (Born, 1780), the gastropod Purpurellus gambiensis (Reeve, 1845) and the corals Madracis pharensis (Heller, 1868) and Dendrophyllia cornigera (Lamarck, 1816). Both sites have been dated by K-Ar on pillow lavas (approximately 420,000 years) and by Uranium Series on corals (about 481,000 years) respectively. The upper Pleistocene starts with another strong global warming known as the last interglacial or marine isotope  stage (MIS) 5.5, about 125,000 years ago, which also left marine  fossil deposits exposed in parallel to current in Igueste of San Andrés (Tenerife),  El Altillo, the  city of Las Palmas de Gran Canaria  and Maspalomas (Gran Canaria),  Matas Blancas, the Playitas and Morrojable (Fuerteventura ) and in Playa Blanca and Punta Penedo (Lanzarote ). The fossil coral Siderastrea radians (Pallas , 1766 ) currently living in the Cape Verde Islands , the Gulf of Guinea and the Caribbean has allowed Uranium series dating. The gastropods Strombus bubonius Lamarck, 1822 and Harpa doris (Röding , 1798 ) currently living in the Gulf of Guinea. Current biogeography using synoptic data obtained through satellites provided by the ISS Canary Seas provides data of Ocean Surface Temperature (SST) and Chlorophyll a (Chlor a) . This has allowed the estimation of these sea conditions during interglacials compared to today .

¿Centros de poder? Sociedad y poblamiento en la Meseta Norte española (ca. 800-400 a.C.)

[ES]La aparición de los primeros centros fortificados en la Meseta Norte durante la Primera Edad del Hierro es un proceso cuya comprensión se encuentra aún en sus inicios. No obstante, los resultados de las investigaciones arqueológicas más recientes proporcionan una imagen considerablemente mejorada sobre el desarrollo de estos sitios autosuficientes, algunos de los cuales se aglomeraron formando grupos mayores y más complejos al final del período. La configuración de asentamientos y comunidades, la interpretación sociológica de sus correspondientes necrópolis y los patrones regionales de poblamiento nos acercan a la organización social de las gentes que habitaron la Meseta en aquel período. [EN] The appearance of the first fortified settlements in the Northern Plateau (Spain) during the Early Iron Age is a process whose understanding is still far from resolved. We know when some small settlements were founded, but the evolution of these communities into other ones that were somewhat larger and more complex is not clear. However, the results of the latest archaeological research provide significantly improved image on the development of these sites, some of which were nucleated into larger and more complex groups at the end of this period. The configuration of settlements and communities, the sociological interpretation of their cemeteries and the regional settlement patterns reveal the social organisation of the people who inhabited the plateau in that period.

Face recognition from a tabula rasa perspective

[EN]In this paper a system for face recognition from a tabula rasa (i.e. blank slate) perspective is described. A priori, the system has the only ability to detect automatically faces and represent them in a space of reduced dimension. Later, the system is exposed to over 400 different identities, observing its recognition performance evolution. The preliminary results achieved indicate on the one side that the system is able to reject most of unknown individuals after an initialization stage.