Extreme pointer years in tree-ring records of central Spain as evidence of climatic events and the eruption of the Huaynaputina Volcano (Peru, 1600 AD)

The study of pointer years of numerous tree-ring chronologies of the central Iberian Peninsula (Sierra de Guadarrama) could provide complementary information about climate variability over the last 405 yr. In total, 64 pointer years have been identified: 30 negative (representing minimum growths) and 34 positive (representing maximum growths), the most significant of these being 1601, 1963 and 1996 for the negative ones, and 1734 and 1737 for the positive ones. Given that summer precipitation was found to be the most limiting factor for the growth of Pinus in the Sierra de Guadarrama in the second half of the 20th century, it is also an explanatory factor in almost 50% of the extreme growths. Furthermore, these pointer years and intervals are not evenly distributed throughout time. Both in the first half of the 17th and in the second half of 20th, they were more frequent and more extreme and these periods are the most notable for the frequency of negative pointer years in Central Spain. The interval 1600–1602 is of special significance, being one of the most unfavourable for tree growth in the centre of Spain, with 1601 representing the minimum index in the regional chronology. We infer that this special minimum annual increase was the effect of the eruption of Huaynaputina, which occurred in Peru at the beginning of 1600 AD. This is the first time that the effects of this eruption in the tree-ring records of Southern Europe have been demonstrated.

Representacion hecha á S. M. C. el señor Don Fernando VII, en defensa de las Cortes

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Conciliación político-cristiana del sí y el no : dialogo entre ... Joaquin Lorenzo Villanueva, diputado en Cortes, el doctor Luceredi y Don Joaquin Lorenzo Villanueva, calificador del Santo Oficio y doctoral ... que vivia por ...

Segun Palau VII, p. 703 Doctor Luceredi es seudónimo de Miguel Elizalde Urdioz, que también firmo con el anagrama Diaz Luzeredi, Guillermo

Representacion y manifiesto que algunos diputados a las cortes ordinarias firmaron en los mayores apuros de su opresion en Madrid para que la magestad del señor Don Fernando el VII ... se penetrase del estado de la nacion ... [Texto impreso]

Precede al título : "J. M. J."

The MIS 5 palaeoenvironmental record in the SE Mediterranean coast of the Iberian Peninsula (Río Antas, Almería, Spain)

Se realiza un estudio detallado del episodio cálido MIS 5 en la zona sureste de la Península Ibérica. Se realiza la reconstrucción paleoambiental a partir del estudio polínico y biomarcadores de un sondeo perforado en la costa de Almería. La cronología se estableció a partir del método de racemizaciónd e aminoácidos.Landwards of a MIS5 bar, a borehole core (SRA) was analyzed to establish the relationship between the lagoonal record and the raised beach deposits in the surroundings of the Antas river mouth and to reconstruct the Pleistocene palaeoenvironmental evolution 5 of the southern Mediterranean coast of the Iberian Peninsula. 63 samples were recovered for amino acid racemization dating, 86 samples for sedimentological and paleontological determination, 37 samples for pollen identification and 54 for biomarker analysis. AAR revealed that the borehole record contains MIS11, MIS6 and MIS5 deposits, the latter extensively represented. During the end of MIS6 and MIS5, a sand 10 barrier developed and created a shallow lagoon with alternating terrestrial inputs this process being common in other Mediterranean realms. Litho- and biofacies allowed the identification of distinct paleoenvironments through time, with the presence of a lagoonal environment alternating with alluvial fan progradation. Biomarkers indicated constant input from terrestrial plants, together with variable development of aquatic 15 macrophytes. The palynological content allowed the reconstruction of the paleoclimatological conditions during MIS6 and 5, with evidence of seven scenarios characterized by alternating arid and relatively humid conditions

Rafèlo de Picasent ignora la novetat del dia 21 de chuliol añ 1813, y Tòni de Alcácer li explica el per qué y la causa del bullisio y la alegría de la Ciutat de Valencia [Texto impreso]

Hay un ejemplar encuadernado con: Relacion de la entrada que hizieron en la ciudad de Denia, Reyno de Valencia, las armas de la Magestad Catolica, del Rey nuestro Señor Carlos IIJ [sic] ... el dia 18 de agosto de 1705. (XVIII/1688).