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 .

La historiografía obrera italiana (1900-1981)

[ES] Este artículo estudia la evolución de la historiografía obrera italiana, que surge del marxismo y vinculada al PCI. Esta historiografía militante se caracterizó por la recopilación de fuentes documentales y el estudio del movimiento organizado, al tiempo que se debatía sobre cuestiones socio-económicas. En una segunda fase, a partir de 1956, la historiografía obrera italiana avanzó en pos de un mayor rigor científico, propósito que se concretó en una mayor apertura de los archivos y en la ampliación de la investigación a temáticas políticamente sensibles. Posteriormente, al calor de los cambios experimentados por el país en los años sesenta y setenta, y favorecida por los contactos con historiografías foráneas, la historiografía obrera italiana perdió progresivamente su carácter militante y se renovó con nuevas interrogantes y metodologías. [EN] This article looks at the evolution of labour historiography in Italy, a movement that emerged from Marxism and was linked to the PCI. This militant historiography was characterized by the compilation of documentary sources and the study of the organised movement, while general socio-economic issues were under discussion. The second phase, from 1956 onward, saw Italian labour historiography making advances in achieving greater thoroughness, involving the opening of more archives and expanding the research to politically sensitive issues. Subsequently, in the light of changes experienced by the country in the 1960s and 1970s, and thanks to foreign historiographies, the Italian labour historiography lost its militant nature in a progressive way and developed new queries and methodologies.