Ferroviarios y Zapleros en Jujuy : De la seguridad social a la inestabilidad laboral

El presente trabajo propone un recorrido analítico y comparativo conducente a identificar e interpretar cómo las transformaciones de Ferrocarriles Argentinos (FA) y Altos Hornos Zapla (AHZ) a principios de la década de 1990 afectaron las condiciones de trabajo de sus hasta entonces empleados, tanto en el aspecto material como en el simbólico-identitario. Para ello, en un primer momento, se reconstruye, brevemente, la historia de ambas empresas haciendo foco en el empleo y las condiciones laborales antes y durante los procesos de privatización o desmantelamiento, según el caso. Luego se analizan las condiciones laborales de los ahora ex empleados y se intenta identificar sus nuevas inserciones ocupacionales y las características de las mismas. En las conclusiones se recuperan las similitudes y divergencias entre ambos casos. Se observa que en su situación actual parece jugar de manera diferenciada el rol del sindicato (en el caso de FA) y el de la empresa (en AHZ), dando lugar a distinta capacidad de respuestaante la desaparición de la fuente de trabajo. Entre las conclusiones también se destaca el hecho de que, en su mayoría, los ex empleados de fa y de ahz en Jujuy no han logrado reinsertarse laboralmente en una situación similar a la que tenían en dichas empresas, generando no solo consecuencias en el plano material (para la subsistencia de ellos y sus familias) sino también en la construcción y valorización de sus identidades sociolaborales

El sector industrial en Jujuy : Un análisis desde la teoría de la localización y la problemática del medio ambiente

La estructura productiva de Jujuy en los últimos cincuenta años se ha caracterizado por la transición desde una economía centrada en la producción primaria (predominante hasta comienzos de la década de 1960) hacia otra con preeminencia creciente del sector terciario (desde mediados de la década de 1970 hasta la actualidad). El sector secundario nunca llegó a ser el más importante en el contexto económico provincial. Sin embargo, en una desagregación mayor, es la industria uno de los sectores que más aporta al producto bruto geográfico en los últimos quince años, con la particularidad de encontrarse concentrada en unas pocas localidades de la provincia. En ese marco, el presente trabajo se propone comprender la ubicación de las industrias en el territorio jujeño a partir de las teorías de la localización, con un análisis particular del caso de Palpalá (por su diseño de parques industriales destinado a aprovechar las economías de escala) y de la problemática ambiental generada por el sector. Se pretende responder a algunos de los siguientes interrogantes: ¿Qué criterios fueron tomados en cuenta para decidir la ubicación de cada fábrica? ¿Cómo incidieron los cambios políticos en la radicación industrial en territorio jujeño? ¿Qué reconversiones se fueron logrando a partir de una industria básica como la siderúrgica? ¿Cómo fue resolviéndose la demanda de bienes finales e intermedios ante el crecimiento poblacional y la inserción/reinserción de la mano de obra? ¿Qué vinculaciones se observan entre la provincia y la región desde el punto de vista de la ocupación del espacio económico? ¿Qué problemas sobre los recursos naturales suscita la industrialización? ¿Cómo responden el Estado y la actividad privada en la prevención y solución de los inconvenientes ambientales? El análisis se realiza sobre la base de la transferencia de teoría a la situación real, entrevistas a informantes especializados y relevamiento de información en organismos estatales (para interiorizarse de aspectos político/económicos), interpretándose luego de modo interdisciplinar los datos relevados. Las respuestas a los distintos interrogantes van elaborándose a medida que se encuentran las relaciones entre las razones que la historia reciente registra y la respuesta social y productiva de los actores económicos de la provincia. En ese sentido, entre las conclusiones se destaca la escasez de aportes foráneos en la construcción del sector industrial local, la necesidad de políticas que incentiven al sector manufacturero a nivel regional, así como la importancia de que se desplieguen acciones con respecto al control de la contaminación, su prevención y la restauración de recursos naturales: agua, suelo, atmósfera y biomas

Ferroviarios y Zapleros en Jujuy : De la seguridad social a la inestabilidad laboral

El presente trabajo propone un recorrido analítico y comparativo conducente a identificar e interpretar cómo las transformaciones de Ferrocarriles Argentinos (FA) y Altos Hornos Zapla (AHZ) a principios de la década de 1990 afectaron las condiciones de trabajo de sus hasta entonces empleados, tanto en el aspecto material como en el simbólico-identitario. Para ello, en un primer momento, se reconstruye, brevemente, la historia de ambas empresas haciendo foco en el empleo y las condiciones laborales antes y durante los procesos de privatización o desmantelamiento, según el caso. Luego se analizan las condiciones laborales de los ahora ex empleados y se intenta identificar sus nuevas inserciones ocupacionales y las características de las mismas. En las conclusiones se recuperan las similitudes y divergencias entre ambos casos. Se observa que en su situación actual parece jugar de manera diferenciada el rol del sindicato (en el caso de FA) y el de la empresa (en AHZ), dando lugar a distinta capacidad de respuestaante la desaparición de la fuente de trabajo. Entre las conclusiones también se destaca el hecho de que, en su mayoría, los ex empleados de fa y de ahz en Jujuy no han logrado reinsertarse laboralmente en una situación similar a la que tenían en dichas empresas, generando no solo consecuencias en el plano material (para la subsistencia de ellos y sus familias) sino también en la construcción y valorización de sus identidades sociolaborales

Calcium carbonate content and concentration of phosphorus components in sediments of ODP Leg 171B sites

Quantifying phosphorus (P) concentrations in marine sediments is necessary for constraining the oceanic record of phosphorus burial and helps to constrain P sedimentary geochemistry. To understand P geochemistry in the sediments, we must determine the geochemical forms of P as well as the transformations occurring between these P components with depth and age. Although several records now exist of P geochemistry in the western and eastern equatorial Pacific (Filippelli and Delaney, 1995, doi:10.2973/odp.proc.sr.138.144.1995; 1996, doi:10.1016/0016-7037(96)00042-7), the western equatorial Atlantic (Delaney and Anderson, 1997, doi:10.2973/odp.proc.sr.154.124.1997), the California Current (Delaney and Anderson, in press), and the Benguela Current (Anderson et al., 2001, doi:10.1029/2000GB001270), most of these are Neogene records. Relatively little data exist from sediments of the Paleogene or Cretaceous, time periods when carbon isotope records indicate major carbon shifts and when the nature of P geochemistry has not been well constrained. Samples from several sites at various water depths, oceanographic regions, and ages are needed to understand how P geochemistry and burial in sediments reflect ocean history. We determined P geochemistry and reactive P concentrations in Atlantic sediments of Eocene to Cretaceous age. These are the first records of P geochemistry with good age control from this period. Blake Nose sites are ideal for investigating P geochemistry, as the sediments are shallowly buried at a range of water depths and sedimentation rates. We determined P concentrations and geochemistry, along with calcium carbonate contents, in mid-Cretaceous to upper Eocene sediments drilled on Blake Nose (Ocean Drilling Program Leg 171B) in a depth transect of four sites (Sites 1052, 1051, 1050, and 1049; water depths: 1345, 1983, 2300, and 2656 m, respectively).

El sector industrial en Jujuy : Un análisis desde la teoría de la localización y la problemática del medio ambiente

La estructura productiva de Jujuy en los últimos cincuenta años se ha caracterizado por la transición desde una economía centrada en la producción primaria (predominante hasta comienzos de la década de 1960) hacia otra con preeminencia creciente del sector terciario (desde mediados de la década de 1970 hasta la actualidad). El sector secundario nunca llegó a ser el más importante en el contexto económico provincial. Sin embargo, en una desagregación mayor, es la industria uno de los sectores que más aporta al producto bruto geográfico en los últimos quince años, con la particularidad de encontrarse concentrada en unas pocas localidades de la provincia. En ese marco, el presente trabajo se propone comprender la ubicación de las industrias en el territorio jujeño a partir de las teorías de la localización, con un análisis particular del caso de Palpalá (por su diseño de parques industriales destinado a aprovechar las economías de escala) y de la problemática ambiental generada por el sector. Se pretende responder a algunos de los siguientes interrogantes: ¿Qué criterios fueron tomados en cuenta para decidir la ubicación de cada fábrica? ¿Cómo incidieron los cambios políticos en la radicación industrial en territorio jujeño? ¿Qué reconversiones se fueron logrando a partir de una industria básica como la siderúrgica? ¿Cómo fue resolviéndose la demanda de bienes finales e intermedios ante el crecimiento poblacional y la inserción/reinserción de la mano de obra? ¿Qué vinculaciones se observan entre la provincia y la región desde el punto de vista de la ocupación del espacio económico? ¿Qué problemas sobre los recursos naturales suscita la industrialización? ¿Cómo responden el Estado y la actividad privada en la prevención y solución de los inconvenientes ambientales? El análisis se realiza sobre la base de la transferencia de teoría a la situación real, entrevistas a informantes especializados y relevamiento de información en organismos estatales (para interiorizarse de aspectos político/económicos), interpretándose luego de modo interdisciplinar los datos relevados. Las respuestas a los distintos interrogantes van elaborándose a medida que se encuentran las relaciones entre las razones que la historia reciente registra y la respuesta social y productiva de los actores económicos de la provincia. En ese sentido, entre las conclusiones se destaca la escasez de aportes foráneos en la construcción del sector industrial local, la necesidad de políticas que incentiven al sector manufacturero a nivel regional, así como la importancia de que se desplieguen acciones con respecto al control de la contaminación, su prevención y la restauración de recursos naturales: agua, suelo, atmósfera y biomas

Ferroviarios y Zapleros en Jujuy : De la seguridad social a la inestabilidad laboral

El presente trabajo propone un recorrido analítico y comparativo conducente a identificar e interpretar cómo las transformaciones de Ferrocarriles Argentinos (FA) y Altos Hornos Zapla (AHZ) a principios de la década de 1990 afectaron las condiciones de trabajo de sus hasta entonces empleados, tanto en el aspecto material como en el simbólico-identitario. Para ello, en un primer momento, se reconstruye, brevemente, la historia de ambas empresas haciendo foco en el empleo y las condiciones laborales antes y durante los procesos de privatización o desmantelamiento, según el caso. Luego se analizan las condiciones laborales de los ahora ex empleados y se intenta identificar sus nuevas inserciones ocupacionales y las características de las mismas. En las conclusiones se recuperan las similitudes y divergencias entre ambos casos. Se observa que en su situación actual parece jugar de manera diferenciada el rol del sindicato (en el caso de FA) y el de la empresa (en AHZ), dando lugar a distinta capacidad de respuestaante la desaparición de la fuente de trabajo. Entre las conclusiones también se destaca el hecho de que, en su mayoría, los ex empleados de fa y de ahz en Jujuy no han logrado reinsertarse laboralmente en una situación similar a la que tenían en dichas empresas, generando no solo consecuencias en el plano material (para la subsistencia de ellos y sus familias) sino también en la construcción y valorización de sus identidades sociolaborales

Phosphorus components and barite in untreated and in carbonate-free sediments of ODP Hole 199-1221C

We determined changes in equatorial Pacific phosphorus (µmol P/g) and barite (BaSO4; wt%) concentrations at high resolution (2 cm) across the Paleocene/Eocene (P/E) boundary in sediments from Ocean Drilling Program (ODP) Leg 199 Site 1221 (153.40 to 154.80 meters below seafloor [mbsf]). Oxide-associated, authigenic, and organic P sequentially extracted from bulk sediment were used to distinguish reactive P from detrital P. We separated barite from bulk sediment and compared its morphology with that of modern unaltered biogenic barite to check for diagenesis. On a CaCO3-free basis, reactive P concentrations are relatively constant and high (323 µmol P/g or ~1 wt%). Barite concentrations range from 0.05 to 5.6 wt%, calculated on a CaCO3-free basis, and show significant variability over this time interval. Shipboard measurements of P and Ba in bulk sediments are systematically lower (by ~25%) than shore-based concentrations and likely indicate problems with shipboard standard calibrations. The presence of Mn oxides and the size, crystal morphology, and sulfur isotopes of barite imply deposition in sulfate-rich pore fluids. Relatively constant reactive P, organic C, and biogenic silica concentrations calculated on a CaCO3-free basis indicate generally little variation in organic C, reactive P, and biogenic opal burial across the P/E boundary, whereas variable barite concentrations indicate significant changes in export productivity. Low barite Ba/reactive P ratios before and immediately after the Benthic Extinction Event (BEE) may indicate efficient nutrient burial, and, if nutrient burial and organic C burial are linked, high relative organic C burial that could temporarily drawdown CO2 at this site. This interpretation requires postdepositional oxidation of organic C because organic C to reactive P ratios are low throughout the section. After the BEE, higher barite Ba/reactive P ratios combined with higher barite Ba concentrations may imply that higher export productivity was coupled with unchanged reactive P burial, indicating efficient nutrient and possibly also organic C recycling in the water column. If the nutrient recycling is decoupled from organic C, the high export production could be indicative of drawdown of CO2. However, the observation that organic C burial is not high where barite burial is high may imply that either C sequestration was restricted to the deep ocean and thus occurred only on timescales of the deep ocean mixing or that postdepositional oxidation (burn down) of organic matter affected the sediments. The decoupling of barite and opal may result from low opal preservation or production that is not diatom based.

Phosphorus components, CaCO3 and biogenic opal in sediments from ODP Leg 167 sites

The ocean history of reactive phosphorus (P) (i.e., dissolved P available to fuel oceanic primary productivity) is of interest because of the role of P as a biolimiting nutrient, and knowledge of P burial in marine sediments is key to testing hypotheses about temporal changes in P input or output fluxes. Our understanding of the history of the P cycle over the Cenozoic has increased substantially with temporal records of reactive P mass accumulation rates from open-ocean Pacific and Atlantic equatorial sites. However, questions about the relative importance of nutrient burial in ocean-margin sediments relative to burial in open-ocean sediments and about the extent of P remobilization in organic-rich, reducing environments characteristic of margin sediments remain unresolved. Nutrient burial in oceanic boundary current systems has been suggested to have a controlling role in oceanic nutrient budgets in certain time intervals (Vincent and Berger, 1985, doi:10.1029/GM032p0455), with higher sediment accumulation rates balancing the limited spatial extent of these sediments. Some investigators suggest that remobilization of P from reducing sediments in margin settings is a significant positive feedback to primary productivity (e.g., Van Cappellan and Ingall, 1994, doi:10.1029/94PA01455), whereas other results indicate that both P uptake and P release may occur in these settings depending on the balance of organic carbon and iron supply to the sediments and on the oxygenation of bottom waters (McManus et al., 1997, doi:10.1016/S0016-7037(97)00138-5). It is important to quantitatively understand the geochemistry of reactive P in margin sediments, where productivity and delivery of organic-rich material to the sediments in relatively shallow-water settings is often sufficient to promote anoxia in interstitial waters. To address these questions, we determined the P concentrations and geochemistry in sediment samples from eight sites drilled during Ocean Drilling Program (ODP) Leg 167, California margin (Sites 1010-1012, 1014, 1016-1017, and 1021-1022). These results are the first records of reactive P concentrations on long time scales-required for the calculation of P accumulation rates-for sediments from a highly productive eastern boundary current setting. In addition, we determined calcium carbonate contents and biogenic silica concentrations to define the environments of sedimentary production, burial, and diagenesis.

Zeolite and silica diagenesis and sandstone petrography at DSDP Sites 57-438 and 57-439

We detected authigenic clinoptilolites in two core samples of tuffaceous, siliceous mudstone in the lower Miocene section of Hole 439. They occur as prismatic and tabular crystals as long as 0.03 mm in various voids of dissolved glass shards, radiolarian shells, calcareous foraminifers, and calcareous algae. They are high in alkalies, especially Na, and in silica varieties. There is a slight difference in composition among them. The Si : (Al+ Fe3+) ratio is highest (4.65) in radiolarian voids, intermediate (4.34) in dissolved glass voids, and lowest (4.26) in voids of calcareous organisms. This difference corresponds to the association of authigenic silica minerals revealed by the scanning electron microscope: There are abundant opal-CT lepispheres in radiolarian voids, low cristobalite and some lepispheres in dissolved glass voids, and a lack of silica minerals in the voids of calcareous organisms. Although it contains some silica from biogenic opal and alkalies from trapped sea water, clinoptilolite derives principally from dissolved glass. Although they are scattered in core samples of Quaternary through lower Miocene diatomaceous and siliceous deposits, acidic glass fragments react with interstitial water to form clinoptilolite only at a sub-bottom depth of 935 meters at approximately 25°C. Analcimes occur in sand-sized clasts of altered acidic vitric tuff in the uppermost Oligocene sandstones. The analcimic tuff clasts were probably reworked from the Upper Cretaceous terrain adjacent to Site 439. Low cristobalite and opal-CT are found in tuffaceous, siliceous mudstone of the middle and lower Miocene sections at Sites 438 and 439. Low cristobalite derives from acidic volcanic glass and opal-CT from biogenic silica. Both siliceous organic remains and acidic glass fragments occur in sediments from the Quaternary through lower Miocene sections. However, the shallowest occurrence is at 700 meters subbottom in Hole 438A, where temperature is estimated to be 21°C. The d(101) spacing of opal-CT varies from 4.09 to 4.11 Å and that of low cristobalite from 4.04 to 4.06 Å. Some opal-CT lepispheres are precipitated onto clinoptilolites in the voids of radiolarian shells at a sub-bottom depth of 950 meters in Hole 439. Sandstone interlaminated with Upper Cretaceous shale is chlorite- calcite cemented and feldspathic. Sandstones in the uppermost Oligocene section are lithic graywacke and consist of large amounts of lithic clasts grouped into older sedimentary and weakly metamorphosed rocks, younger sedimentary rocks, and acidic volcanic rocks. The acidic volcanic clasts probably originated from the volcanic high, which supplied the basal conglomerate with dacite gravels. The older sedimentary and weakly metamorphosed rocks and green rock correspond to the lithologies of the lower Mesozoic to upper Paleozoic Sorachi Group, including the chert, limestone, and slate in south-central Hokkaido. However, the angular shape and coarseness of the clasts and the abundance of carbonate rock fragments indicate a nearby provenance, which is probably the southern offshore extension of the Sorachi Group. The younger sedimentary rocks, including mudstone, carbonaceous shale, and analcime-bearing tuff, correspond to the lithologies of the Upper Cretaceous strata in south-central Hokkaido. Their clasts were reworked from the southern offshore extension of the strata. Because of the discontinuity of the zeolite zoning due to burial diagenesis, an overburden several kilometers thick must have been denuded before the deposition of sediments in the early Oligocene.

Rare earth and other element contents in surface layer bottom sediments and ferromanganese nodules along the Transatlantic profile

Behavior of rare earth elements (REE) and Th is studied along the Transatlantic transect at 22°N. It is shown that both REE and Th contents relative to Al (the most lithogenic element) increase toward the pelagic region. The increasing trend becomes more complicated due to variations in content of biogenic calcium carbonate that acts as a diluting component in sediments. REE composition varies symmetrically relative to the Mid-Atlantic Ridge (MAR) emphasizing weak hydrothermal influence on sediments of the ridge axis, although the well-known criteria for hydrothermal contribution, such as Al/(Al+Mn+Fe) and (Fe+Mn)/Ti, do not reach critical values. Variations in REE content and composition allowed to distinguish the following five sediment zones in the transect: (I) terrigenous sediments of the Nares abyssal plain; (II) pelagic sediments of the North American Basin; (III) carbonate ooze of the MAR axis; (IV) pelagic sediments of the Canary Basin; and (V) terrigenous clay and calcareous mud of the African continental slope and slope base. Ferromanganese nodules of the hydrogenous type with extremely high Ce (up to 1801 ppm) and Th (up to 138 ppm) contents occur in pelagic sediments. It is ascertained that P, REE, and Th contents depend on Fe content in Atlantic sediments. Therefore, one can suggest that only minor amount of phosphorus is bound with bone debris. Low concentration of bone debris phosphorus is a result of relatively high sedimentation rates in the Atlantic Ocean, as compared with those in pelagic regions of the Pacific Ocean.

Silicate content in sediment ofthe Santa Monica Basin, California

Seafloor recycling of organic materials in Santa Monica Basin, California was examined through in situ benthic chamber experiments, shipboard whole-core incubations and pore water studies. Mass balance calculations indicate that the data are internally consistent and that the estimated benthic exchange rates compare well with those derived from deep, moored conical sediment traps and hydrographic modeling. Pore water and benthic flux observations indicate that the metabolizable organic matter at the seafloor must be composed of at least two fractions of very different reactivities. While the majority of reactive organic compounds degrade quickly, with a half-life of <=6.5 years, 1/4 of the total metabolizable organic matter appears to react more slowly, with a half-life on the order of 1700 years. Down-core changes in pore water sulfate and titration alkalinity are not explained by stoichiometric models of organic matter diagenesis and suggest that reactions not considered previously must be influencing the pore water concentrations. Measured recycling and burial rates indicate that 43% of the organic carbon reaching the basin seafloor is permanently buried. The results for Santa Monica Basin are compared to those reported for other California Borderland Basins that differ in sedimentation rate and bottom water oxygen content. Organic carbon burial rates for the Borderland Basins are strongly correlated with total organic carbon deposition rate and bulk sedimentation rate. No significant correlation is observed between carbon burial and bottom water oxygen, extent of oxic mineralization and sediment mixing. Thus, for the California Borderlands, it appears that carbon burial rates are primarily controlled by input rates and not by variations in preservation.

Spatiotemporal monitoring of water quality in coral reefs of Tayrona National Natural Park, Colombian Caribbean, 2011-2013

Tayrona National Natural Park (TNNP; 11°17' - 11°22' N and 73°53' - 74°12' W) is a hotspot of coral reef biodiversity in the Colombian Caribbean, located between the city of Santa Marta (>455,000 inhabitants) and several smaller river mouths (Rio Piedras, Mendihuaca, Guachaca). The region experiences a strong seasonal variation in physical parameters (temperature, salinity, wind, and water currents) due to alternating dry seasons with coastal upwelling and rainy seasons. Here, a range of water quality parameters relevant for coral reef functioning is provided. Water quality was measured directly above local coral reefs (~10 m water depth) by a monthly monitoring for up to 25 months in the four TNNP bays (Chengue, Gayraca, Neguanje, and Cinto) and at sites with different degree of exposition to winds, waves and water currents (exposed vs. sheltered sites) within each bay. The water quality parameters include: inorganic nutrient (nitrate, nitrite and soluble reactive phosphorus), chlorophyll a, particulate organic carbon and nitrogen concentrations (with a replication of n=3) as well as oxygen availability, biological oxygen demand, seawater pH, and water clarity (with a replication of n=4). This is by far the most comprehensive coral reefs water quality dataset for the region. A detailed description of the methods can be found within the referenced publications.

Fatty acid composition, and bacteria and meiofauna abundance in sediment cores PS71/013 and PS71/085 during POLARSTERN cruise ANT-XXIV/2

During the RV Polarstern ANT XXIV-2 cruise to the Southern Ocean and the Weddell Sea in 2007/2008, sediment samples were taken during and after a phytoplankton bloom at 52°S 0°E. The station, located at 2960 m water depth, was sampled for the first time at the beginning of December 2007 and revisited at the end of January 2008. Fresh phytodetritus originating from the phytoplankton bloom first observed in the water column had reached the sea floor by the time of the second visit. Absolute abundances of bacteria and most major meiofauna taxa did not change between the two sampling dates. In the copepods, the second most abundant meiofauna taxon after the nematodes, the enhanced input of organic material did not lead to an observable increase of reproductive effort. However, significantly higher relative abundances of meiofauna could be observed at the sediment surface after the remains of the phytoplankton bloom reached the sea floor. Vertical shifts in meiofauna distribution between December and January may be related to changing pore-water oxygen concentration, total sediment fatty acid content, and pigment profiles measured during our study. Higher oxygen consumption after the phytoplankton bloom may have resulted from an enhanced respiratory activity of the living benthic component, as neither meiofauna nor bacteria reacted with an increase in individual numbers to the food input from the water column. Based on our results, we infer that low temperatures and ecological strategies are the underlying factors for the delayed response of benthic deep-sea copepods, in terms of egg and larval production, to the modified environmental situation.

(Appendix) Recent surface areas and historical lengths of glaciers from Patagonia and Tierra del Fuego, South America

Fluctuations in the length of 72 glaciers in the Northern and Southern Patagonia Icefield (NPI and SPI, respectively) and the Cordillera Darwin Icefield (CDI) were estimated between 1945 and 2005. The information obtained from historical maps based on 1945 aerial photographs was compared to ASTER and Landsat satellite images and to information found in the literature. The majority of glaciers have retreated considerably, with maximum values of 12.2 km for Marinelli Glacier in the CDI, 11.6 km for O'Higgins Glacier in the SPI and 5.7 km for San Rafael Glacier in the NPI. Among the 20 glaciers that have retreated the most relative to their size, small (less than 50 km**2) and medium (between 50 and 200 km**2) glaciers are the most affected. However, no direct relation between glacier retreat and size was found for the 72 glaciers studied. The highest percentage retreat in the CDI was by the CDI-03 Glacier (37.9%) and Marinelli Glacier (37.6%). In the SPI, relative retreats were heterogeneous and fluctuated between 27.2% (Amelia Glacier) and 0.4% (Viedma Glacier). In the NPI, relative retreat was very high for Strindberg and Cachet glaciers (35.9% and 27.6%, respectively) but for the remaining glaciers in this icefield it ranged between 11.8% (Piscis Glacier) and 3.6% (San Quintin Glacier). In addition to surface area, the surface slope (calculated on the basis of the DEM SRTM) was also related to the relative retreat and no straightforward relation was found. From a global point of view, we suggest that glacier retreat in the region is controlled firstly by atmospheric warming, as it has been reported in this area. Besides the general increase in temperature observed, no signal of a geographical pattern for the fluctuations in glacier length was found. Consequently, glaciers appear to initially react to local conditions most probably induced by their exposition, geometry and hypsometry. The heterogeneity of rates of retreat suggests that differences in basin geometry, glacier dynamics and response time are key features to explain fluctuations of each glacier.

Organic carbon flux through the benthic community in the temperate abyssal Northeast Atlantic

In order to assess the carbon flux through the deep-sea benthic boundary layer, sediment community oxygen consumption (SCOC) was measured in different months and years at the BIOTRANS area in the abyssal northeastern Atlantic. SCOC varied seasonally with a maximum in July/August. Evidence is given for a direct coupling between a substantial sedimentation of phytodetritus and the seasonal increase in SCOC. Rapid colonization, growth and decomposition rates indicate that the deep-sea benthic microbial and protozoan biota can react quickly to substantial falls of particulate organic matter. They seem to be the most important groups to generate seasonal changes in deep-sea benthic carbon flux rates.