Origen y distribución de los pesticidas organoclorados (OCPs) en sedimentos actuales de la Laguna de El Hito (Cuenca, España Central)

Se llevó a cabo el estudio del estado ambiental actual de la Laguna de El Hito basado en el análisis y cuantificación de 24 pesticidas organoclorados (OCPs): hexaclorobenceno, hexaclorociclohexanos, diclorodifenil-tricloroetano sus homólogos y metabolitos (DDTs), y ciclodienos (aldrín, dieldrín, endrín, endrín aldehido, endrín cetona, ?-clordano, ?-clordano, endosulfán I, endosulfán II, endosulfán sulfato, heptacloro, heptacloro epóxido B y metoxicloro). Algunos compuestos superaron los Niveles Genéricos de Referencia (NGR) para la salud humana y los ecosistemas del R.D.09/2005. Se determinó su origen a partir de diversos índices interpretándose tanto aplicaciones históricas como más recientes. Se obtuvieron los mapas de distribución de los índices y de las concentraciones de OCPs.Environmental evaluation of the current state of El Hito Lake referred to 24 organochlorine pesticides (OCPs) was carried out: hexachlorobenzene, hexachlorocyclohexanes, dichlorodiphenyltrichloroethane their homologs and metabolites (DDTs), and cyclodienes (aldrin, dieldrin, endrin, endrin aldehyde, endrin ketone, α- chlordane, γ- chlordane, endosulfan I, endosulfan II, endosulfan sulphate, heptachlor, heptachlor epóxide B and metoxichlor). Some of these compounds showed concentrations above the Soil Screening Levels (SSLs) for human health and ecosystems as is established in R.D.09/2005. Different indexes were used to determine their origin. Both historical and recent applications sources were interpreted. Distribution maps for concentrations and indexes were plotted

Protein diagenesis in Patella shells: implications for amino acid racemisation dating

Se analiza la racemización de aminoácidos en proteínas inter e intracristalinas en conchas de Patella y su utilización como herramienta geocronológica, fundamentalmente empleadas en yacimientos arqueológicos.The inter- and intra-crystalline fractions of Patella vulgata limpets recovered from archaeological sites in Northern Spain (covering Neolithic, Mesolithic, Magdalenian, Solutrean, and Aurignacian periods) were examined for amino acid composition and racemisation over time. The calcitic apex and rim areas of the shells were found to probably be composed of similar proteins, as the D/L values and amino acids were comparable and varied in the same way with increasing age; however, the mineral structures present in these areas differed. The aragonitic intermediate part of the shell showed a distinctly different amino acid composition and mineral structure. The main protein leaching from the inter-crystalline fraction occurred within the first 6000 yr after the death of the organism. In contrast, the intra-crystalline fraction — comprised of a different protein composition than the inter-crystalline fraction — appeared to behave as a closed system for at least 34 ka, as reflected by the lack of a significant decrease in the amino acid content; however, changes in the amino acid percentages occurred during this period. The concentration of aspartic acid remained almost constant with age both in inter- and intra-crystalline proteins, and its contribution to the total amino acid content increased with age at the expense of other amino acids such as glutamic acid, serine, glycine and alanine. Temperature is thought to play a key role in the amino acid racemisation of P. vulgata and could explain why in the localities belonging to the Gravettian and Solutrean period, which formed during relatively cold conditions, D/L values were similar to those detected in shells from sites formed during the Magdalenian.

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

[Altar de los Trinitarios Descalzos] [Material gráfico]

Resumen: Descripción: en la parte central, San José, Virgen de los Desamparados, San Fermin, San Juan de la Mata y San Felix Valois.; sobre ellos, la Beatísima Trinidad. En la parte superior, escudo de la Congregación

Estudio de la movilidad que presenta el diésel en un suelo contaminado empleando surfactantes

La contaminación de suelos con hidrocarburos de petróleo en México es un problema que se ha vuelto muy común en nuestros días, debido principalmente a derrames, así como a las actividades propias de la industria petrolera. Algunos suelos contaminados, principalmente en el sureste de México, contienen concentraciones de hidrocarburos hasta de 450,000 mg/kg. Por dichas razones, una de las preocupaciones de las autoridades ambientales es el desarrollo de tecnologías eficientes y económicamente factibles que permitan la eliminación de este tipo de contaminantes. El saneamiento del sitio se puede lograr a través de diversos procedimientos, como son la aplicación de métodos físicos, químicos y biológicos (o combinaciones de ellas). La elección de un método depende de la naturaleza del contaminante, su estado físico, concentración, tipo de suelo, espacio físico disponible, tiempo destinado para su tratamiento, así como de los recursos económicos disponibles. Previa a la aplicación de la tecnología es necesario la realización de un diagnóstico de la contaminación del suelo, con el fin de conocer el tipo, concentración y distribución de los contaminantes presentes, así como el volumen de suelo a tratar, las condiciones climáticas de la zona, y características físicas del lugar (vías de acceso y servicios, entre otros). En la presente tesis, el empleo de surfactantes, se ha propuesto como una técnica para incrementar la movilidad de contaminantes orgánicos hidrofóbicos (HOCs) como hidrocarburos totales del petróleo (HTPs), bifenilos policlorados (PCBs), Benceno, Tolueno, Xilenos, explosivos, clorofenoles, pesticidas, entre otros, y así facilitar su degradación. Los surfactantes debido a que reducen la tensión superficial del agua, son moléculas formadas por grupos polares hidrofílicos y largas cadenas carbonadas hidrofóbicas. Sus grupos polares forman puentes hidrógeno con las moléculas de agua, mientras que las cadenas carbonadas se asocian a los hidrocarburos debido a interacciones hidrofóbicas que estos presentan. En soluciones acuosas, los surfactantes forman estructuras esféricas organizadas llamadas micelas. La solubilización de los contaminantes se lleva a cabo solamente cuando se forma la fase micelar, la cual se obtiene cuando la concentración del surfactante es superior a la concentración micelar crítica (CMC), es decir, arriba de la concentración de la cual el monómero se comienza a auto-agregar. La eficiencia de desorción de diésel por un surfactante depende de su naturaleza, de la dosis empleada, de la hidrofobicidad del contaminante, de la interacción surfactante-suelo y del tiempo de contacto surfactante-suelo. Sin embargo, la mejor eficiencia de desorción no está siempre relacionada con la mejor eficiencia de movilidad o solubilidad, debido principalmente a que el empleo de una alta concentración de surfactante puede inhibir la movilización. De acuerdo con información proporcionada por la Procuraduría Federal de Protección al Ambiente (PROFEPA), a la fecha no se ha llevado a cabo en México ninguna restauración de sitios específicamente contaminados con diésel, la técnica de lavado de suelos. Por lo anterior existe la necesidad de emplear la técnica de lavado de suelos ex situ. Específicamente en el suelo extraído de la ex refinería 18 de marzo ubicada en el Distrito Federal México y empleando una solución de surfactantes con agua desionizada, la cual consiste ponerlos en contacto con el suelo contaminado con diésel por medio de columnas de lavado cilíndricas, para lograr la remoción del contaminante. Se emplearon como surfactantes el lauril sulfato de sodio, lauril éter sulfato de sodio y Glucopon AV-100 a diferentes concentraciones de 0.5 a 4.0 [g/L], lográndose obtener una eficiencia del 80 % con este último surfactante. El lavado de suelos contaminados con diésel empleado surfactantes, es una tecnología que requiere que se profundice en el estudio de algunas variables como son el tipo de surfactante, concentración, tiempo de lavado, fenómenos de difusión, desorción, propiedades termodinámicas, entre otros. Los cuales determinarán el éxito o fracaso de la técnica empleada. Nowadays, soil pollution with oil in Mexico is a very common issue due mainly to both oil spill and oil activities. For example, mainly in the southeast area of Mexico, polluted soil contains high concentrations of hydrocarbons, up to 450,000 mg/kg. For these reasons, enviromental authorities have the concern in developing economically feasible and efficient technology that allow the elimination of these type of contaminants. The sanitation in sites can be achieved through several procedures such as physical, chemical and biological methods (or a combination among them). The choice of a method depends on the nature and physical state of the contaminant, the concentration, type of soil, physical space available, time consumption and financial resources. Before any technological application, a diagnostic of the polluted soil is necessary in order to know the type, concentration and distribution of contaminants as well as the soil volume, climatic conditions and physical features of the place (access routes and services, among others). In this thesis, surfactants has been proposed as a technique to increase the mobility of hydrophobic-organic contaminants (HOCs), e.g. total hydrocarbons of petroleum, polychlorinated biphenyls, benzene, toluene, xylenes, explosives, chlorophenols, pesticides, among others, and, hence, to facilitate degradation. Since surfactants reduce the water surface tension, they are molecules comprised of hydrophilic polar groups and long-hydrophobic carbon chains. Surfactant’s polar groups form hydrogen bonding with water molecules while carbon chains, i.e. hydrocarbon chains, have hydrophobic interactios. In aqueous solutions, surfactants form self-organised spherical structures called micelles. The solubilisation of contaminants is carried out only when the micellar phase is formed. This is obtained when the surfactant concentration is higher than the crítical micelle concentration (CMC), i.e. above the concentration where the surfactant monomer begins to self-aggregate. The diesel efficiency desorption by surfactants depends on their nature, the dose use, the contaminant hydrophobicity, the surfactant-soil interaction and the contact time with surfactant soil. However, the best desorption is not always related with the best either mobility or solubility efficiency since high concentration of surfactant can inhibit mobilisation. According to information of the Federal Bureau of Environmental Protection (PROFEPA), up today, there is not any restauration of diesel-polluted sites using the washing-soil technique. Due to the above, there exist the necessity of employing the waching-soil technique ex situ. More specifically, a sample soil from the oil-refinery of “18 de marzo” in Mexico city was extracted and a surfactant solution with deionised water was put in contact with the diesel contaminated soil by means of cylindrical waching columns in order to remove the contaminant. The surfactants employed in this work were sodium lauryl sulfate, sodium lauryl ether sulfate and Glucopon AV-100 at different concentrations of 0.5 to 4 [g/L], obtaining a efficiency of 80 % with this last surfactant. The washing of diesel-polluted soil using surfactants is a technology which requires a deeper study of some variables such as the type of surfactant, concentration, washing time, difusión phenomena, desorption, thermodynamic properties, among others. These parameters determine the succes or failure of the employed technique.

Evolución paleoambiental de la Península Ibérica desde hace 1 Ma a partir de los biomarcadores del registro de la Turbera de Padul (Granada)

La Turbera de Padul, en la Provincia de Granada, ofrece unas posibilidades de estudio muy atractivas desde el punto de vista de la reconstrucción paleoambiental. Se trata de una fosa tectónica subsidente de naturaleza detrítica, a cuyo techo aparecen alternantes niveles de turba. El sondeo, de 107 metros, se realizó en un punto donde los estratos de turba aparecen a mayor profundidad, lo que permite obtener un registro geoquímico orgánico con mucho detalle con una antigüedad de hasta 1Ma. Se tomaron muestras cada 20 cm para el análisis de biomarcadores. Estos biomarcadores se obtuvieron mediante extracción Soxhlet, posterior separación de fracciones de diferente polaridad mediante Cromatografía en Columna, con Gel de Sílice y Alúmina, y posteriormente el análisis e identificación por Cromatografía de Gases - Espectrometría de masas, con confirmación de los compuestos químicos identificados por comparación con Bibliotecas de Espectros de Masas. La datación del sondeo se realizó utilizando distintos métodos como datación por 14C, U/Th, y datación por racemización de aminoácidos. Los resultados dataron el muro del sondeo con una antigüedad de 1 millón de años. El estudio de los biomarcadores ha permitido identificar episodios con distintas características en un escenario complejo, como es la Turbera de Padul, donde el aporte de agua por fusión nival complica la interpretación paleoambiental, y es la responsable de la existencia de la lámina de agua en la turbera en periodos secos con temperaturas elevadas. Se han identificado series de n-alcanos, de n-metilcetonas y series de nalcanoles, que han permitido identificar la aportación de materia orgánica de distintas fuentes al sedimento y por tanto la interpretación paleoambiental. La identificación de diterpenoides fenólicos (cis-Totatol, trans-Totarol y Ferruginol) han permitido identificar episodios de clima templado y húmedo con proliferación de cupresáceas, y precipitaciones abundantes. Por otro lado, se han identificado triterpenoides como el Friedelan-3-ona (Friedelin) y el A-norfriedel-8en-10-ona, cuya relación como precursor (Friedelin) y producto (A-norfriedel-8en-10-ona) ha permitido identificar episodios con fluctuaciones del espesor de la lámina de agua y aporte de material vegetal. ABSTRACT The Bog of Padul, in the province of Granada, offers very attractive possibilities for the study of paleoenvironmental reconstruction. It is a subsiding graben of detrital nature, whose upper part appear alternating peat levels. The core of 107 meters, obtained from a borehole drilled in a place where the layers of peat appear deeper, allowing to obtain organic geochemist information along the last 1 million years. Every 20 cm samples for biomarkers analysis were taken. These biomarkers were obtained by Soxhlet extraction, subsequent separation of fractions of different polarity by column chromatography with silica gel and alumina, and then analyzed and identified by gas chromatography - mass spectrometry, with confirmation of the chemicals identified by comparison to mass spectral libraries. The dating of the core was conducted using different methods such as 14C dating, U/Th, and amino acid racemization dating. The results dated the base of the core to be 1 million years old. The study has identified biomarkers episodes with different characteristics in a complex scenario, such as the Bog of Padul, where the contribution of snowmelt water complicates the paleoenvironmental interpretation, and is responsible for the existence of a sheet of water in dry periods with high temperatures. There have been identified series of n-alkanes, n-methyl ketones and series of n-alkanols that have shown the contribution of different organic matter sources to the sediment and therefore allowed to paleo interpretation. The identification of phenolic diterpenoids (cis-Totatol, trans-Totarol and Ferruginol) have identified episodes of mild and humid climate with proliferation of Cupressaceae, and abundant rainfall. In addition, triterpenoids have been identified, as the friedelan-3-one (friedelin) and the A-norfriedel-8en-10-one, whose relationship as precursor (friedelin) and product (A-norfriedel-8en-10-one) has identified episodes with fluctuations on the thickness of the sheet of water and supply of plant material debris.

Lipid biomarkers in the Enol Lake (Asturias, Northern Spain): coupled natural and human induced environmental history

The lipid content of three cores from Lake Enol (Picos de Europa National Park, Asturias, Northern Spain) was studied. The n-alkane profiles indicated a major input from terrigenous plants [predominance of high molecular weight (HMW) alkanes] since ca. 1695 AD to the water body, although the uppermost cm revealed a predominance of organic matter (OM) derived from algae, as the most abundant alkane was C17. Three units revealing different environmental conditions were defined. Unit A (ca. 1695–1860 AD) in the lowermost parts of ENO13-10 (< 12 cm) and ENO13-15 (< 28 cm) was identified and was characterized by higher OM input and evidence of minimal degradation (high CPI values, predominance of HMW n-alkanoic acids and good correspondence between the predominant n-alkane and n-alkanoic acid chains). These findings could be linked to the Little Ice Age, when cold and humid conditions may have favored an increase in total organic carbon (TOC) and n-alkane and n-alkanoic acid content (greater terrigenous OM in-wash), and may have also reduced bacterial activity. In Unit B (ca. 1860–1980 AD) the lack of correspondence between the n-alkane and n-alkanoic acid profiles of ENO13-10 (12–4 cm) and ENO13-15 (28–8 cm) suggested a certain preferential microbial synthesis of long chain saturated fatty acids from primary OM and/or bacterial activity, coinciding with a decrease in OM input, which could be linked to the global warming that started in the second half of the 19th century. In ENO13-7 the low OM input (low TOC) was accompanied by some bacterial degradation (predominance ofHMWn-alkanoic acids but with a bimodal distribution) in the lowermost 16–5 cm. Evidence of considerable phytoplankton productivity and microbial activity was especially significant in Unit C (ca. 1980–2013 AD) identified in the uppermost part of all three cores (5 cm in ENO13-7, 4 cm in ENO13-10 and 8 cm in ENO13-15), coinciding with higher concentrations of n-alkanes and n-alkanoic acids, which were considered to be linked to warmer and drier conditions, as well as to greater anthropogenic influence in modern times. Plant sterols, such as b-sitosterol, campesterol and stigmasterol, were significantly present in the cores. In addition, fecal stanols, such as 24-ethylcoprostanol from herbivores, were present, thereby indicating a continuous and significant pollution input derived from these animals since the 17th century, being more important in the last 20 years.

Amino acid epimerization dating of coastal neotectonic processes in southeastern Iberian Peninsula: the region between Aguas and Antas river mouths

The coastal area between the mouths of the Aguas and Antas Rivers presents a deformed system of raised marine deposits, some of which have been strongly affected by active tectonics. The use of amino acid epimerization dating of Glycymeris shells from raised coastal deposits allowed determining the age of these marine deposits, all of them linked to highstand sea levels in the Mediterranean realm, with ages between MIS 11 and MIS 1. These results allowed corroborating the age of some previously studied sites, and using new sampling sites, the general aminostratigraphy for the Quaternary raised marine deposits on the Mediterranean coast was confirmed. The main deformation event took place after MIS 11 and continued until MIS 5, and was linked to the activity of the Palomares Faul

Biomarkers and inorganic proxies in the paleoenvironmental reconstruction of mires: The importance of landscape in Las Conchas (Asturias, Northern Spain)

We determined the lipid distributions (n-alkanes, n-alkan-2-ones, n-alkanoic acids), total organic carbon (TOC), total nitrogen (TN), Ca/Mg and ash content in Las Conchas mire, a 3.2 m deep bryophyte-dominated mire in Northern Spain covering 8000 cal yr BP. Bog conditions developed in the bottom 20 cm of the profile, and good preservation of organic matter (OM) was inferred from n-alkanoic acid distribution, with the exception of the uppermost 20 cm (last ca. 200 yr). Microbial synthesis of long chain saturated fatty acids from primary OM likely produced a dominance of short chain n-alkanoic acids with a bimodal distribution, as well as the lack of correspondence between the n-alkane and n-alkanoic acid profiles in the upper 20 cm. This was accompanied by an increase in ash content, a decrease in TOC and variation in n-alkane ratios, thereby suggesting significant changes in the mire, namely drainage and transformation to a meadow, in the last ca. 200 yr. The distribution of n-alkan-2-ones indicated an increase in bacterial source from the bottom of the record to 94 cm, whereas their distribution in the upper part could be attributed mainly to plant input and/or the microbial oxidation of n-alkanes. The different n-alkane proxies showed variations, which we interpreted in terms of changes in vegetation (Sphagnum vs. non-Sphagnum dominated phases) during the last 8000 cal yr BP. C23 was the most abundant homolog throughout most of the record, thereby suggesting dominant humid conditions alternating with short drier phases. However, such humid conditions were not linked to paleoclimatic variation but rather to geomorphological characteristics: Las Conchas mire, at the base of the Cuera Range, receives continuous runoff—even during drier periods—which is not necessarily accompanied by additional mineral input to peat, producing the development of Sphagnum moss typical of waterlogged ecotopes and damp habitats. Thus, although geochemical proxies indicated an ombrotrophic regime in the mire, geomorphological characteristics may make a considerable contribution to environmental conditions.

[Colección de fotografías sobre la ciudad de Valencia (1914 a 1930) [ [Material gráfico].]

[27]. Pasadizo que une la Catedral con el Palacio Arzobispal de Valencia en la calle de la Barcella, 1917 (1 par estereoscópico) (1 fot.) -- [28]. Puerta románica de la Catedral de Valencia, 1917 (1 par estereoscópico) (1 fot.) -- [29-30]. Fuente monumento al Márques de Campo situado en la plaza Emilio Castelar, 1917 (3 pares estereoscópicos) (2 fot.) -- [31]. Patio interior sin identificar, un hombre y un policia (1 par estereoscópico) (1 fot.) -- [32]. Estatua ecuestre de Don Jaime I El Conquistador en el Parterre, 1917 (1 par estereoscópico) (1 fot.) -- [32 A y B]. Máximo López Roglá en el Parterre (2 par estereoscópico) (2 fot.) -- [33-35]. Nieve en Valencia, en la alameditas de Serranos, niños jugando con la nieve en la Glorieta, 30-12-1917 (3 pares estereoscópicos) (3 fot.) -- [36-38]. Claustro del Patriarca con la escultura del Beato Juan de Ribera, en una de las fotos un grupo de seminaristas, 1917 (5 pares estereoscópicos) (3 fot.) -- [39-40]. Museo del Patriarca de Valencia, relicarios, Cruz Patriarcal (2 pares estereoscópicos) (2 fot.) -- [41-48]. Antiguo Hospital Padre Jofré, acceso desde la calle, patio de entrada y estatua del Padre Jofré, pórtico del Real Monasterio de la Santísima Trinidad, miembros de la Congregación de la Inmaculada y San Luís, los congregantes con los enfermos en el patio del hospital, 1913 (8 pares estereoscópicos) (8 fot.) -- [49]. Estandarte de la Academia Valencianista del Centro Escolar y Mercantil, 1917 (1 par estereoscópico) (1 fot.) -- [50-51].Miembros de la Congregación de la Inmaculada y San Luís y de la Academia Valencianista del Centro Escolar y Mercantil (calle libreros 2) junto a la falla, en una de las fotos llevan el estandarte de la Academia (2 pares estereoscópicos) (2 fot.) -- [52]. Sede de la Academia Valencianista del Centro Escolar y Mercantil (2 pares estereoscópicos) (1 fot.) -- [53-69]. Fallas, año 1917 (21 pares estereoscópicos) (14 fot.) -- [70]. Mercado de Colón, carruaje con caballo junto a la puerta principal, 1917 (1 par estereoscópico) (1 fot.) -- [71]. Palacio de la Exposición, 1917 (1 par estereoscópico) (1 fot.) -- [72-87]. Los Jardines de Viveros: ruinas en primer plano al fondo la torre del Palacio de Ripalda, jaulas de los pájaros, Francisco Roglá López en Viveros, Isabel Orrico Vidal con sus hijos y las niñeras en Viveros en distintos situaciones y contemplando el estanque con el Museo de San Pío V al fondo, 1922 (19 pares estereoscópicos) (17 fot.) -- [88-90]. La Hípica (5 pares estereoscópicos) (3 fot.) -- [91-94]. Jugando al tenis en un campo habilitado para el tenis entre pinos (8 pares estereoscópicos) (4 fot.) -- [95-97]. El Puerto de Valencia, 1921 (4 pares estereoscópicos) (3 fot.) -- [98-104]. Llegada al puerto de Valencia de cuatro submarinos, entre ellos el submarino Monturiol, escoltados por torpederos y acompañados por el buque de salvamento Canguro, 8 de septiembre de 1921 (7 pares estereoscópicos) (7 fot.) -- [105-107A-D]. Playa y Balneario de las Arenas: un hombre y tres mujeres patinando en las Arenas; Isabel Orrico Vidal (izquierda), Ignacio Roglá Orrico (bebe) en brazos de Pilar (la niñera de Chiva), Manolo Orrico Vidal con su mujer Mercedes Gay, la niñera con Luisito Roglá Orrico, los niños más mayores son Merceditas Orrico Gay y Paquito Roglá Orrico; en las Arenas a la izquierda de la foto Ignacio Roglá Orrico (bebe), Ana María Rodríguez Gay, Paquito Roglá Orrico, Manolo Orrico Vidal, Merceditas Orrico Gay, en el centro Mercedes Gay Lloveras (sentada) y Gonzalo Rodríguez Gay, a la derecha Gonzalo Rodríguez, Ana Gay Lloveras, Isabel Orrico Vidal con Luisito Roglá Orrico y Francisco Roglá López (6 pares estereoscópicos) (6 fot.) -- [109]. En la playa de la Malvarrosa barca tirada por bueyes, 1922 (1 pares estereoscópicos) (1 fot.) -- [110-117]. Fiesta de la Virgen de los Desamparados, tapíz de flores con la imagen de la Virgen colocada en el retablo de flor, salida de la Virgen de la Basílica en el traslado a la Catedral, salida de la Virgen de la Catedral para la procesión de la tarde (9 pares estereoscópicos) (7 fot.) -- [118-120]. Carroza del MArqués de Llanera (actualmente en el Museo Nacional de Cerámica y Artes Suntuarias "González Martí" por la calle Carniceros esquina con la calle Arolas, vista lateral de la carroza, procesión del Corpus? (5 pares estereoscópicos) (3 fot.) -- [121-122]. Gigantes y Cabezudos junto a la Catedral, Fiesta del Corpus (2 pares estereoscópicos) (2 fot.) -- [123]. Isabel Orrico Vidal en el balcón del nº 11 de la calle de la Paz (1 par estereoscópico) (1 fot.) -- [124]. Procesión del domingo de Ramos (1 par estereoscópico) (1 fot.) -- [125-136]. Desfile del cortejo fúnebre por la calle (de la Paz?) de los restos de Sorolla el 13 de agosto de 1923 (16 pares estereoscópicos) (10 fot.) -- [137]. Detalle de la fuente de la Alameda (1 par estereoscópico) (1 fot.) -- [138-139]. Francisco Roglá López con su caballo en la Alameda, carruaje por la Alameda (2 pares estereoscópicos) (2 fot.) -- [140-143]. Jura de bandera en la Alameda (4 pares estereoscópicos) (4 fot.) -- [144A, B, C, D, E]. Fuente con estatua de la Alameda, José Roglá López leyendo el periódico junto a la fuente, con un grupo de amigos, grupo de amigos y un barquillero en el Paseo de la Alameda, José Roglá López con unos amigos en una fuente de la Alameda que ahora está en el barrio del Carmen (5 fot.) -- [145]. Grupo de coches de la época en la plaza de la Virgen (1 fot.) -- [146A, B]. Pareja de novios saliendo de la Basílica de la Virgen? (2 pares estereoscópicos) (2 fot.) -- [147-148]. Niños de la Asociación de San Vicente Ferrer que representan los milagros en los altares (2 pares estereoscópicos) (2 fot.) -- [149-150]. Actos festivos, dos mujeres llevando una bandera con gente alrededor (2 fot.) -- [151-152]. Plaza de toros de Valencia, 1930 (2 fot.) -- [153]. Rosalía Roglá López con su abuela materna en el piso de la calle Liñán nº 3, a través de los cristales se ve el edificio de la Lonja (1 par estereoscópico) (1 fot.) -- [154]. Rosalía Roglá López en el balcón de su piso de la calle Liñán nº 3, al fondo a la izquierda se ve la plaza del mercado y la Lonja (1 par estereoscópico) (1 fot.) -- [155]. José Roglá López de pié junto a la ventana leyendo un periódico (1 fot.) -- [156-157]. Isabel Orrico Vidal en la Alameditas de Serranos, al fondo el Museo San Pío V (2 fot.) -- [158-159]. Ignacio Roglá Orrico, Luís Roglá Orrico y Francisco Roglá Orrico sentados en un banco en la Glorieta, los tres niños junto al monumento al Dr. Gómez Ferrer de la Glorieta, 1928 (2 fot.) -- [160-161]. Ignacio Roglá Orrico, Luís Roglá Orrico en el jardín de los Viveros, los dos niños con Paco bebiendo en una fuente de Viveros junto al estanque, 1929 (2 fot.) -- [162]. Grupo familiar sentado en el jardín de los Viveros, Manolo Orrico Gay, Manolo Orrico Vidal, Luís Roglá Orrico, Isabel Orrico Vidal, Mercedes Gay Lloveras y Mercedes Orrico Gay, 1930 (1 par estereoscópico) (1 fot.) -- [163]. Isabel Orrico Vidal junto a Luís Roglá Orrico en bicicleta en el jardín de los Viveros, 1930 (1 par estereoscópico) (1 fot.) -- [164]. Manolo Orrico Gay y Luís Roglá Orrico (detrás) en bicicleta por el jardín de los Viveros (1 par estereoscópico) (1 fot.)

Palaeoenvironmental reconstruction of Las Conchas Mire (Asturias, N. Spain) from the ketone and fatty acid record= reconstrucción paleoambiental de la Turbera de las Conchas (Asturias, N. España)a partir del registro de cetonas y ácidos grasos

Se han estudiado los biomarcadores, principalmente cetonas y ácidos, preservados en el registro de 3.2 m de la Turbera de Las Conchas. Las cetonas reflejan cierta actividad bacteriana desde 94 cm hasta la base del registro, Los ácidos grasos reflejan una buena preservación de la materia orgánica, salvo en los 20 cm superiores en los que hay indicios de oxidación microbiana de alcanos .The biomarkers, mainly ketones and fally aclds, preserved In 3.2 m deep Las Conchas Mire have been studied, Kelones reflect certain bacterial activity from 94 cm to the bottom of the record. Falty aclds indlcate a good preservation of the organlc matter, wlth the exception of the uppermost 20 cm In whlch mlcroblal oxldation of alkanes are likely to occur

NA PALMA DA MÃO: A difusão de celulares e smartphones e possibilidades para o ensino-aprendizagem no Brasil

A pesquisa considera a difusão de celulares e smartphones e as consequências deste fato em possibilidades para o ensino-aprendizagem. Aparatos de comunicação sempre estiveram ligados ao processo de ensino-aprendizagem. Entretanto, com o desenvolvimento mais intenso, nas últimas décadas, das Tecnologias de Informação e Comunicação (TIC), essa relação vem ganhando novos contornos. Surge a Internet, a evolução das máquinas computacionais e, recentemente, a explosão dos dispositivos móveis, fornecendo novos produtos e serviços convergentes. Nesse contexto, celulares e smartphones tem sido utilizados e recomendados para apoio e complemento do processo de ensino-aprendizagem: a chamada Aprendizagem Móvel. Esse ramo cresce devido à rápida expansão e barateamento dessas tecnologias na sociedade. Para verificar cientificamente essa relação foi realizada uma pesquisa de natureza qualitativa, do tipo exploratória, com dois projetos de Aprendizagem Móvel em andamento no Brasil, o Palma – Programa de Alfabetização na Língua Materna e o Escola Com Celular – ECC. Assim, a partir dos dados provenientes da pesquisa, identificamos alguns aspectos relacionados ao uso de celulares e smartphones para o processo de ensino-aprendizagem que contribuem na compreensão desse campo ainda em construção no Brasil. O uso desses dispositivos como suporte para processos de ensino-aprendizagem nos projetos estudados é delineado pelos aspectos tecnologia, dispositivo, público e contexto e novas tecnologias e Aprendizagem Móvel. O aspecto dispositivo desdobra-se em dimensões como disseminação, multifuncionalidade e acessibilidade que embasam os projetos, ainda favorece características apontadas como importantes para o processo de ensino-aprendizagem na atualidade, como mobilidade e portabilidade. Os projetos pesquisados demonstram potencial e metodologia adequada aos contextos para os quais foram criados e aplicados. Entretanto, a pesquisa indicou que ao mesmo tempo em que celulares e smartphones representam o ápice da convergência tecnológica e são considerados extremamente populares e acessíveis na sociedade contemporânea, com possibilidades concretas como nos projetos estudados, não conseguiram conquistar uma posição sólida como suporte para o ensino-aprendizagem. Tal indicação se deve, de acordo com o corpus, à carência de alguns fatores, como: fomento, as práticas se mostram extremamente dependentes da iniciativa pública ou privada para sua extensão e continuidade; sensibilização para o uso de tecnologias disponíveis, não consideram o aparelho dos próprios alunos e um planejamento que inclua, capacite e incentive o uso desses dispositivos. Além disso, a pesquisa também destaca a necessidade de uma visão crítica do uso e papel da tecnologia nesses processos.

Tomato Flower Abnormalities Induced by Low Temperatures Are Associated with Changes of Expression of MADS-Box Genes1

Flower and fruit development in tomato (Lycopersicon esculentum Mill.) were severely affected when plants were grown at low temperatures, displaying homeotic and meristic transformations and alterations in the fusion pattern of the organs. Most of these homeotic transformations modified the identity of stamens and carpels, giving rise to intermediate organs. Complete homeotic transformations were rarely found and always affected organs of the reproductive whorls. Meristic transformations were also commonly observed in the reproductive whorls, which developed with an excessive number of organs. Scanning electron microscopy revealed that meristic transformations take place very early in the development of the flower and are related to a significant increase in the floral meristem size. However, homeotic transformations should occur later during the development of the organ primordia. Steady-state levels of transcripts corresponding to tomato MADS-box genes TM4, TM5, TM6, and TAG1 were greatly increased by low temperatures and could be related to these flower abnormalities. Moreover, in situ hybridization analyses showed that low temperatures also altered the stage-specific expression of TM4.

Interface between culturally based preferences and genetic preferences: female mate choice in Poecilia reticulata.

The relative contribution of genetic and socio-cultural factors in the shaping of behavior is of fundamental importance to biologists and social scientists, yet it has proven to be extremely difficult to study in a controlled, experimental fashion. Here I describe experiments that examined the strength of genetic and cultural (imitative) factors in determining female mate choice in the guppy, Poecilia reticulata. Female guppies from the Paria River in Trinidad have a genetic, heritable preference for the amount of orange body color possessed by males. Female guppies will, however, also copy (imitate) the mate choice of other females in that when two males are matched for orange color, an "observer" female will copy the mate choice of another ("model") female. Three treatments were undertaken in which males differed by an average of 12%, 24%, or 40% of the total orange body color. In all cases, observer females viewed a model female prefer the less colorful male. When males differed by 12% or 24%, observer females preferred the less colorful male and thus copied the mate choice of others, despite a strong heritable preference for orange body color in males. When males differed by 40% orange body color, however, observer females preferred the more colorful male and did not copy the mate choice of the other female. In this system, then, imitation can "override" genetic preferences when the difference between orange body color in males is small or moderate, but genetic factors block out imitation effects when the difference in orange body color in males is large. This experiment provides the first attempt to experimentally examine the relative strength of cultural and genetic preferences for a particular trait and suggests that these two factors moderate one another in shaping social behavior.