Always looking on the bright side of life? : Exploring optimism and health in three UK post-industrial urban settings

The survey was jointly funded by NHS Health Scotland and the Glasgow Centre for Population Health.

Comparing time and risk preferences across three post-industrial UK cities

Date of Acceptance: 10/07/2015 The Chief Scientist Office of the Scottish Government Health and Social Care Directorates funds HERU. The survey was jointly funded by NHS Health Scotland and the Glasgow Centre for Population Health. The views expressed in this paper are those of the authors only and not those of the funding bodies. The investigator team for the overall survey comprises David Walsh, Gerry McCartney, Sarah McCullough, Marjon van der Pol, Duncan Buchanan and Russell Jones.

Always looking on the bright side of life? : Exploring optimism and health in three UK post-industrial urban settings

The survey was jointly funded by NHS Health Scotland and the Glasgow Centre for Population Health.

Comparing time and risk preferences across three post-industrial UK cities

Date of Acceptance: 10/07/2015 The Chief Scientist Office of the Scottish Government Health and Social Care Directorates funds HERU. The survey was jointly funded by NHS Health Scotland and the Glasgow Centre for Population Health. The views expressed in this paper are those of the authors only and not those of the funding bodies. The investigator team for the overall survey comprises David Walsh, Gerry McCartney, Sarah McCullough, Marjon van der Pol, Duncan Buchanan and Russell Jones.

Always looking on the bright side of life? : Exploring optimism and health in three UK post-industrial urban settings

The survey was jointly funded by NHS Health Scotland and the Glasgow Centre for Population Health.

Acerca de las relaciones entre la ciencia y la política

La ponencia que aquí presentamos constituye una reflexión en torno al libro de Shapin y Schaffer, "El Leviathan y la bomba de vacío. Hobbes, Boyle y la vida experimental", libro que saldrá en breve editado por la Universidad Nacional de Quilmes. No constituye una reflexión genérica sobre este texto, sino que apunta a elucidar la tesis fundamental del mismo. La misma, contextualizada en una investigación histórica acerca de las investigaciones sobre la presión del aire realizadas por Robert Boyle hacia 1660 y sus debates con Thomas Hobbes, sugiere que las soluciones al problema del conocimiento están embebidas dentro de las soluciones prácticas dadas al problema del orden social, y que diferentes soluciones prácticas al problema del orden social involucran soluciones prácticas distintas al problema del conocimiento. La ponencia reconstruye los principales momentos del texto de referencia para discutir después la tesis sociológica de más vasto alcance. Se argumenta que si bien la generalización que realizan los autores posee dificultades metodológicas, en un plano argumental más vasto posee elementos especialmente interesantes a la hora de concebir la articulación existente entre conocimiento y sociedad

Acerca de las relaciones entre la ciencia y la política

La ponencia que aquí presentamos constituye una reflexión en torno al libro de Shapin y Schaffer, "El Leviathan y la bomba de vacío. Hobbes, Boyle y la vida experimental", libro que saldrá en breve editado por la Universidad Nacional de Quilmes. No constituye una reflexión genérica sobre este texto, sino que apunta a elucidar la tesis fundamental del mismo. La misma, contextualizada en una investigación histórica acerca de las investigaciones sobre la presión del aire realizadas por Robert Boyle hacia 1660 y sus debates con Thomas Hobbes, sugiere que las soluciones al problema del conocimiento están embebidas dentro de las soluciones prácticas dadas al problema del orden social, y que diferentes soluciones prácticas al problema del orden social involucran soluciones prácticas distintas al problema del conocimiento. La ponencia reconstruye los principales momentos del texto de referencia para discutir después la tesis sociológica de más vasto alcance. Se argumenta que si bien la generalización que realizan los autores posee dificultades metodológicas, en un plano argumental más vasto posee elementos especialmente interesantes a la hora de concebir la articulación existente entre conocimiento y sociedad

Acerca de las relaciones entre la ciencia y la política

La ponencia que aquí presentamos constituye una reflexión en torno al libro de Shapin y Schaffer, "El Leviathan y la bomba de vacío. Hobbes, Boyle y la vida experimental", libro que saldrá en breve editado por la Universidad Nacional de Quilmes. No constituye una reflexión genérica sobre este texto, sino que apunta a elucidar la tesis fundamental del mismo. La misma, contextualizada en una investigación histórica acerca de las investigaciones sobre la presión del aire realizadas por Robert Boyle hacia 1660 y sus debates con Thomas Hobbes, sugiere que las soluciones al problema del conocimiento están embebidas dentro de las soluciones prácticas dadas al problema del orden social, y que diferentes soluciones prácticas al problema del orden social involucran soluciones prácticas distintas al problema del conocimiento. La ponencia reconstruye los principales momentos del texto de referencia para discutir después la tesis sociológica de más vasto alcance. Se argumenta que si bien la generalización que realizan los autores posee dificultades metodológicas, en un plano argumental más vasto posee elementos especialmente interesantes a la hora de concebir la articulación existente entre conocimiento y sociedad

Cadmium analytical results from sediment and foraminifera shells

There has been a major contradiction between benthic foraminiferal Cd/Ca and d13C data concerning the labile nutrient chemistry of the Southern Ocean during the Last Glacial Maximum (LGM). Cd data indicates that LGM South Atlantic nutrient concentrations were as low as they are today, indicative of a persistent influx of nutrient-depleted North Atlantic Deep Water (NADW). d13C data indicates that LGM South Atlantic nutrient concentrations were much higher than at present (even higher than anywhere else in the ocean at that time), and these data have been interpreted as signifying the complete shutdown ofthe export of NADW into the global ocean. This paper examines both true geochemical differences and various confounding foraminiferal artifacts for both tracers. While many different processes and artifacts affect both tracers in the margin, we conclude the discrepancy is mainly due to the "Mackensen Effect" of low foraminiferal d13C as a result of high carbon flux to the sediments, and that LGM Atlantic Sector Southern Ocean nutrient concentrations remained similar to the levels encountered today.

(Table 1) Age determination of North Atlantic sediment cores

Stable isotope, trace metal, alkenone paleothermometry, and radiocarbon methods have been applied to sediment cores in the western subpolar North Atlantic between Hudson Strait and Cape Hatteras to reveal the history of climate in that region over the past ~11 kyr. We focus on cores from the Laurentian Fan, which is known to have rapid and continuous accumulation of hemipelagic sediment. Although results among our various proxy data are not always in agreement, the weight of the evidence (alkenone sea surface temperature (SST), d18O and abundance of Globigerinoides ruber) indicates a continual cooling of surface waters over Laurentian Fan, from about 18°C in the early Holocene to about 8°C today. Alternatively, Mg/Ca data on planktonic foraminifera indicate no systematic change in Holocene SST. The inferred long-term decrease in SST was probably driven by decreasing seasonality of Northern Hemisphere insolation. Two series of proxy data show the gradual cooling was interrupted by a two-step cold pulse that began 8500 years ago, and lasted about 700 years. Although this event is associated with the final deglaciation of Hudson Bay, there is no d18O minimum anywhere in the Labrador Sea, yet there is some evidence for it as far south as Cape Hatteras. Finally, although the 8200 year B.P. event has been implicated in decreasing North Atlantic ventilation, and hence widespread temperature depression on land and at sea, we find inconsistent evidence for a change at that time in deep ocean nutrient content at ~4 km water depth.

(Table 1) Age control and temporal resolution of paleoceanographic records of the North Atlantic

Short-term changes in sea surface conditions controlling the thermohaline circulation in the northern North Atlantic are expected to be especially efficient in perturbing global climate stability. Here we assess past variability of sea surface temperature (SST) in the northeast Atlantic and Norwegian Sea during Marine Isotope Stage (MIS) 2 and, in particular, during the Last Glacial Maximum (LGM). Five high-resolution SST records were established on a meridional transect (53°N-72°N) to trace centennial-scale oscillations in SST and sea-ice cover. We used three independent computational techniques (SIMMAX modern analogue technique, Artificial Neural Networks (ANN), and Revised Analog Method (RAM)) to reconstruct SST from planktonic foraminifer census counts. SIMMAX and ANN reproduced short-term SST oscillations of similar magnitude and absolute levels, while RAM, owing to a restrictive analog selection, appears less suitable for reconstructing "cold end" SST. The SIMMAX and ANN SST reconstructions support the existence of a weak paleo-Norwegian Current during Dansgaard-Oeschger (DO) interstadials number 4, 3, 2, and 1. During the LGM, two warm incursions of 7°C water to occurred in the northern North Atlantic but ended north of the Iceland Faroe Ridge. A rough numerical estimate shows that the near-surface poleward heat transfer from 53° across the Iceland-Faroe Ridge up to to 72° N dropped to less than 60% of the modern value during DO interstadials and to almost zero during DO stadials. Summer sea ice was generally confined to the area north of 70°N and only rarely expanded southward along the margins of continental ice sheets. Internal LGM variability of North Atlantic (>40°N) SST in the GLAMAP 2000 compilation (Sarnthein et al., 2003, doi:10.1029/2002PA000771; Pflaumann et al., 2003, doi:10.1029/2002PA000774) indicates maximum instability in the glacial subpolar gyre and at the Iberian Margin, while in the Nordic Seas, SST was continuously low.

(Table T2) Biogenic opal in Palmer Deep sediments at ODP Site 178-1098

High-resolution records of sedimentary proxies provide insights into fine-scale geochemical responses to climatic forcing. Gamma-ray attenuation (GRA) bulk-density data and magnetic stratigraphy records from Palmer Deep, Site 1098, show variability close to the same scale as ice cores, making this site ideal for high-resolution geochemical investigations. In conjunction with shipboard geophysical measurements, silica records allow high-resolution evaluation of the frequencies and amplitudes of biogenic variability. This provides investigators additional data sets to evaluate the global extent of climatic events that are presently defined by regional oceanic data sets (e.g., Younger Dryas in the North Atlantic) and to evaluate the potential mechanisms that link biological productivity and climate in the Southern Ocean. In addition, because of the observed links between diatom blooms and export productivity (Michaels and Silver, 1988, doi:10.1016/0198-0149(88)90126-4), biogenic silica may be an indicator of the efficiency of the biological pump (removal of organic carbon from the euphotic zone and burial within the sediments). Because the net removal of CO2 (on short time scales up to millennial, the balance between upwelled CO2, carbon fixation, and the removal of organic carbon from the surface ocean) can determine the atmospheric concentration; proxies that allow us to quantify export production yield insights into carbon cycle responses. In today's ocean, diatoms are integrally linked with new production (production based on the use of nitrate and molecular nitrogen rather than ammonium, which is generated by the microbial degradation of organic carbon) (Dugdale and Goering, 1967). Thus, as with nutrient utilization proxies, biogenic silica may be a good indicator of export production. The difficulties lie in translating the biogenic opal burial records to export production. Numerous factors control the preservation of sedimentary biogenic silica, including depth of the water column, water temperature, trace element chemistry, grazing pressure, bloom structure, and species composition of the diatom assemblage (Nelson et al., 1995, doi:10.1029/95GB01070). In addition, several recent investigations have noted additional complications. Iron limitation increases the uptake of Si relative to carbon (Hutchins et al., 1998, ; Takeda, 1998, doi:10.1038/31674). In the Southern Ocean, iron limitation could produce more robust, and thus better preserved, diatoms; thus, the burial record may be a record of iron limitation rather than of the export of organic carbon (Boyle, 1998). In addition, laboratory experiments show that bacteria accelerate the dissolution of biogenic silica (Bidle and Azam, 1999, doi:10.1038/17351). Both the species composition and temperature seem to influence the amount of dissolution. Evidence of recycling of silicic acid within the photic zone (Brzezinski et al., 1997) suggests that the silica pump (removal from the euphotic zone of silica relative to nitrogen and phosphorus) may work with variable efficiency. This becomes an issue when trying to reconstruct the removal of organic carbon from sedimentary biogenic silica records. In fact, there is a wide range in the Si:Corganic molar ratio in the Southern Ocean (0.18-0.81) (Nelson et al., 1995; Ragueneau et al., 2000, doi:10.1016/S0921-8181(00)00052-7). Thus, the presence (or absence) of biogenic silica alone may tell us little about the export productivity, complicating the interpretation of age-related trends. One recent assessment has added some hope to links between productivity and opal burial in the Southern Ocean (Pondaven et al., 2000). Quantitative comparison of different productivity proxies will greatly aid in this evaluation.

El periodismo deportivo condicionado por la gestión comunicativa de los clubes de fútbol: el caso del FC Barcelona

Las relaciones entre los gabinetes de Comunicación de los clubes de fútbol y los periodistas deportivos se enmarcan en el modelo de Gieber y Johnson (1961) por el que el hecho de que ambos compartan objetivos comunes, donde los gabinetes de Comunicación necesitan que los medios publiquen determinadas informaciones y los periodistas precisan de noticias que publicar, provoca una pérdida de independencia por parte de los periodistas, ya que necesitan a esos departamentos como fuentes. En la actualidad, los departamentos de Comunicación de los clubes de fútbol, como el del FC Barcelona, se han constituido en gatekeepers. Esto ha acentuado las históricas diferencias que existen entre los periodistas y los profesionales de la comunicación corporativa, incrementado por el control informativo de estos departamentos lo que provoca constantes tensiones entre ambos.