Sedimentation rate calculations and isotopic analysis on sediment cores along the IODP Expedition 311 transect

The oceanographic and tectonic conditions of accretionary margins are well-suited for several potential processes governing methane generation, storage and release. To identify the relevant methane evolution pathways in the northern Cascadia accretionary margin, a four-site transect was drilled during Integrated Ocean Drilling Program Expedition 311. The d13C values of methane range from a minimum value of -82.2 per mil on an uplifted ridge of accreted sediment near the deformation front (Site U1326, 1829 mbsl, meters below sea level) to a maximum value of -39.5 per mil at the most landward location within an area of steep canyons near the shelf edge (Site U1329, 946 mbsl). An interpretation based solely on methane isotope values might conclude the 13C-enrichment of methane indicates a transition from microbially- to thermogenically-sourced methane. However, the co-existing CO2 exhibits a similar trend of 13C-enrichment along the transect with values ranging from -22.5 per mil to +25.7 per mil. The magnitude of the carbon isotope separation between methane and CO2 (Ec = 63.8 ± 5.8) is consistent with isotope fractionation during microbially mediated carbonate reduction. These results, in conjunction with a transect-wide gaseous hydrocarbon content composed of > 99.8% (by volume) methane and uniform dDCH4 values (-172 per mil ± 8) that are distinct from thermogenic methane at a seep located 60 km from the Expedition 311 transect, suggest microbial CO2 reduction is the predominant methane source at all investigated sites. The magnitude of the intra-site downhole 13C-enrichment of CO2 within the accreted ridge (Site U1326) and a slope basin nearest the deformation front (Site U1325, 2195 mbsl) is ~ 5 per mil. At the mid-slope site (Site U1327, 1304 mbsl) the downhole 13C-enrichment of the CO2 is ~ 25 per mil and increases to ~ 40 per mil at the near-shelf edge Site U1329. This isotope fractionation pattern is indicative of more extensive diagenetic alteration at sites with greater 13C-enrichment. The magnitude of the 13C-enrichment of CO2 correlates with decreasing sedimentation rates and a diminishing occurrence of stratigraphic gas hydrate. We suggest the decreasing sedimentation rates increase the exposure time of sedimentary organic matter to aerobic and anaerobic degradation, during burial, thereby reducing the availability of metabolizable organic matter available for methane production. This process is reflected in the occurrence and distribution of gas hydrate within the northern Cascadia margin accretionary prism. Our observations are relevant for evaluating methane production and the occurrence of stratigraphic gas hydrate within other convergent margins.

Statistics of the National soil test database of France

In France, farmers commission about 250,000 soil-testing analyses per year to assist them managing soil fertility. The number and diversity of origin of the samples make these analyses an interesting and original information source regarding cultivated topsoil variability. Moreover, these analyses relate to several parameters strongly influenced by human activity (macronutrient contents, pH...), for which existing cartographic information is not very relevant. Compiling the results of these analyses into a database makes it possible to re-use these data within both a national and temporal framework. A database compilation relating to data collected over the period 1990-2009 has been recently achieved. So far, commercial soil-testing laboratories approved by the Ministry of Agriculture have provided analytical results from more than 2,000,000 samples. After the initial quality control stage, analytical results from more than 1,900,000 samples were available in the database. The anonymity of the landholders seeking soil analyses is perfectly preserved, as the only identifying information stored is the location of the nearest administrative city to the sample site. We present in this dataset a set of statistical parameters of the spatial distributions for several agronomic soil properties. These statistical parameters are calculated for 4 different nested spatial entities (administrative areas: e.g. regions, departments, counties and agricultural areas) and for 4 time periods (1990-1994, 1995-1999, 2000-2004, 2005-2009). Two kinds of agronomic soil properties are available: the firs one correspond to the quantitative variables like the organic carbon content and the second one corresponds to the qualitative variables like the texture class. For each spatial unit and temporal period, we calculated the following statistics stets: the first set is calculated for the quantitative variables and corresponds to the number of samples, the mean, the standard deviation and, the 2-,4-,10-quantiles; the second set is calculated for the qualitative variables and corresponds to the number of samples, the value of the dominant class, the number of samples of the dominant class, the second dominant class, the number of samples of the second dominant class.

Eocene to Early Miocene palaeoclimate of Saxony, Germany (Table 4)

In the present study, proxy data concerning changes in atmospheric CO2 and climatic conditions from the Late Eocene to the Early Miocene were acquired by applying palaeobotanical methods. Fossil floras from 10 well-documented locations in Saxony, Germany, were investigated with respect to (1) stomatal density/index of fossil leaves from three different taxa (Eotrigonobalanus furcinervis, Laurophyllum pseudoprinceps and Laurophyllum acutimontanum), (2) the coexistence approach (CA) based on nearest living relatives (NLR) and (3) leaf margin analysis (LMA). Whereas the results of approach (1) indicate changes in atmospheric CO2 concentration, approaches (2) and (3) provide climate data. The results of the analysis of stomatal parameters indicate that the atmospheric CO2 concentration was higher during the Late Eocene than during the Early Oligocene and increased towards the Late Oligocene. A lower atmospheric pCO2 level after the Late Eocene is also suggested by an increase in marine palaeoproductivity at this time. From the Late Oligocene onwards, no changes in atmospheric CO2 concentration can be detected with the present data. For the considered sites, the results of the coexistence approach and of the leaf margin analysis document a significant cooling event from the Late Eocene to the Early Oligocene. The pCO2 decrease from the Late Eocene to the Early Oligocene indicated by the stomatal data raised in this study was thus coupled to a temperature decrease which is reflected by the present datasets. From the Early Oligocene onwards, however, no further fundamental climate change can be inferred for the considered locations. The pCO2 increase from the Early Oligocene to the Late Oligocene, which is indicated by the present data, is thus not accompanied by a climate change at the considered sites. A warming event during the Late Oligocene is, however, recorded by marine climate archives. According to the present data, no change in pCO2 occurred during the cooling event at the Oligocene/Miocene boundary, which is also indicated by marine data. The quality and validity of stomatal parameters as sensors for atmospheric CO2 concentration are discussed.

Sporomorphs and quantitative analysis of the Eocene record from IODP Hole 318-U1356A

The early Eocene epoch was characterized by extreme global warmth, which in terrestrial settings was characterized by an expansion of near-tropical vegetation belts into the high latitudes. During the middle to late Eocene, global cooling caused the retreat of tropical vegetation to lower latitudes. In high-latitude settings, near-tropical vegetation was replaced by temperate floras. This floral change has recently been traced as far south as Antarctica, where along the Wilkes Land margin paratropical forests thrived during the early Eocene and temperate Nothofagus forests developed during the middle Eocene. Here we provide both qualitative and quantitative palynological data for this floral turnover based on a sporomorph record recovered at Integrated Ocean Drilling Program (IODP) Site U1356 off the Wilkes Land margin. Following the nearest living relative concept and based on a comparison with modern vegetation types, we examine the structure and diversity patterns of the Eocene vegetation along the Wilkes Land margin. Our results indicate that the early Eocene forests along the Wilkes Land margin were characterized by a diverse canopy composed of plants that today occur in tropical settings; their richness pattern was similar to that of present-day forests from New Caledonia. The middle Eocene forests were characterized by a canopy dominated by Nothofagus and exhibited richness patterns similar to modern Nothofagus forests from New Zealand.

Movilidad social de ingresos

Este trabajo procura aportar una dimensión adicional al análisis de la evolución del bienestar de una sociedad basado en la dinámica de ingresos, mediante la metodología "The Nearest Neighbour Matching". El objetivo no es sólo considerar el ranking o dispersión de ingresos en un momento determinado, sino también abordar su evolución. Particularmente, consiste en determinar cómo los individuos se "mueven" en el Gran Mendoza durante los años 2003 y 2013.

Physicochemical and photosynthetic characteristics of water samples obtained during a CCGS Amundsen cruise in 2008

During summer 2008, as part of the Circumpolar Flaw Lead system study, we measured phytoplankton photosynthetic parameters to understand regional patterns in primary productivity, including the degree and timescale of photoacclimation and how variability in environmental conditions influences this response. Photosynthesis-irradiance measurements were taken at 15 sites primarily from the depth of the subsurface chlorophyll a (Chl a) maximum (SCM) within the Beaufort Sea flaw lead polynya. The physiological response of phytoplankton to a range of light levels was used to assess maximum rates of carbon (C) fixation (P*m), photosynthetic efficiency (alpha*), photoacclimation (Ek), and photoinhibition (beta*). SCM samples taken along a transect from under ice into open water exhibited a >3-fold increase in alpha* and P*m, showing these parameters can vary substantially over relatively small spatial scales, primarily in response to changes in the ambient light field. Algae were able to maintain relatively high rates of C fixation despite low light at the SCM, particularly in the large (>5 µm) size fraction at open water sites. This may substantially impact biogenic C drawdown if species composition shifts in response to future climate change. Our results suggest that phytoplankton in this region are well acclimated to existing environmental conditions, including sea ice cover, low light, and nutrient pulses. Furthermore, this photoacclimatory response can be rapid and keep pace with a developing SCM, as phytoplankton maintain photosynthetic rates and efficiencies in a narrow ''shade-acclimated'' range.

Stable carbon isotope in bottom water and Cibicidoides wuellerstorfi on the Ontong Java Plateau and Emperor Seamount

We have measured the carbon isotopic composition of dissolved inorganic carbon in bottom waters of the Ontong Java Plateau (western equatorial Pacific) and on the northern Emperor Seamounts (northwest Pacific). Each of these locations is several hundred miles from the nearest Geochemical Ocean Sections Study (GEOSECS) stations, and the observed delta13C values at each site differ substantially from regionally averaged GEOSECS delta13C profiles. We discuss the possible causes of these differences, including horizontal variability, near-bottom effects, and problems with the Pacific GEOSECS delta13C data. We also measured the isotopic composition (C and O) of core top C. wuellerstorfi from a depth transect of cores at each location. The delta18O data are used to verify that our samples are Holocene. Comparison of foraminiferal and bottom water delta13C values shows that this species faithfully records bottom water delta13C at both sites and demonstrates that there is no depth-related artifact in the dissolved inorganic carbon-C. wuellerstorfi delta13C relationship at these sites.

Poderes locales y gobierno central ante el cambio de régimen en Buenos Aires : Cartas de ciudadanía, cargos públicos y práctica de oficios, 1812-1815

En la presente ponencia nos proponemos analizar la situación jurídica y política de algunos extranjeros que ocupaban cargos públicos o realizaban oficios civiles en el Rio de la Plata. En este contexto, los criterios para definir quién era un vecino-ciudadano dependían de la posibilidad de mantener o perder cargos públicos, o de ejercer ciertos oficios en los pueblos de la campaña. Se estudiarán dos casos en los cuales se presentaron situaciones análogas para los que no eran reconocidos pertenecientes a la comunidad política, es decir para los extranjeros. Aquellos que no lograban la obtención de una carta de ciudadanía se veían obligados a dejar sus cargos u oficios. Sin embargo, los reglamentos y las decisiones del gobierno en estos casos se vieron superados por las prácticas y situaciones concretas. Otro de los casos estudiados en esta ponencia se corresponde con un litigio en Chascomús un fuerte y pueblo de la campaña de Buenos Aires, en la frontera con el mundo indígena. Allí, un hombre de origen catalán le es impedido ejercer su oficio de panadero, limitándolo a la producción de pastelería fina. La decisión fue tomada por el comandante del fuerte ante un pedido de un grupo de panaderas que se consideraban 'patricias', señalando el origen español de dicho panadero para limitarlo en el ejercicio del oficio. El conflicto nos ofrece varias aristas interesantes sobre los mecanismos del ejercicio del poder que estamos viendo en otros trabajos, pero aquí nos detendremos en la definición del grupo de pertenencia y en la utilización de los conceptos de patria y patriotas

La jerarquía de vínculos socioafectivos en Ilíada XXIII.1-256

El artículo analiza las relaciones entre Aquiles y sus camaradas en la primera parte del canto XXIII (vv. 1-256), sobre la base de una mirada lingüístico-poética y un enfoque ético-pedagógico. Aquiles tiene dos comportamientos diferentes: como amigo y como caudillo. A Patroclo le dedica sus mejores manifestaciones de ternura y afecto. Como jefe, se dirige primero a sus camaradas más próximos, los mirmidones, y luego, según avanza el canto, a Agamenón, los nobles, las tropas, la comitiva más circunscripta de deudos y, finalmente, a los panaqueos en tanto cuerpo militar completo. Para una mayor comprensión de estas vinculaciones, se examina la autoridad y sus grados, a partir del grupo sémico correspondiente

Rendición o Resistencia? : El primer discurso latino

En la segunda mitad del siglo IV a. C. Roma ocupa la Italia central y se orienta al dominio de la región meridional en colisión posible con griegos y cartagineses; su influjo se extiende incluso al Jónico cuando varias ciudades de la Magna Grecia solicitan su protección, no así Tarento, que al anclar una escuadra romana en su puerto, reaccionó atacando las naves y una guarnición romana próxima. Tarento, ante una guerra inevitable, pidió apoyo al rey Pirro de Epiro, quien vio la oportunidad de extender hacia occidente las conquistas que Alejandro dejó inconclusas; su invasión de Italia generó fuerte resistencia, pero no le impidió victorias costosas ni su avance hacia el norte; propuso por intermedio de un embajador la rendición y condiciones gravosas para los romanos que estuvieron a punto de ceder. Allí surge Appio Claudia el Ciego, anciano senador ya retirado, que con un discurso breve, preciso y muy logrado produjo un giro en las decisiones de los patricios. Analizamos el discurso conservado por Plutarco en la Vida de Pirro y lo ubicamos dentro de su contexto histórico y político; gracias a él, Roma conservó sus fronteras itálicas y preparó su futura expansión.

Late Pliocene carbonate mineralogy of ODP Hole 133-818B

Shedding of shallow carbonate material toward the deep slopes and basin floors is clearly tied to the position of the carbonate bank tops relative to the photic zone. The onset of bank shedding in periplatform sediments can record either the flooding of the bank tops within the photic zone during a rise in sea level following a period of exposure, referred to in the literature as the "highstand shedding" scenario, or the reentry of the bank tops into the photic zone during a lowering of sea level following a period of drowning, referred to as the "lowstand shedding" scenario. Results from Leg 133 post-cruise research on the Pliocene sequences, drilled in six sites within different slope settings of the Queensland Plateau, seem to point out that the latter "lowstand shedding" scenario can be applied to this particular carbonate system. At the Queensland Plateau sites, the early Pliocene (5.2-3.5 Ma) and the earliest part of the late Pliocene (3.5-2.9 Ma) age sequences were characterized, especially in the ôdeepö Sites 811 and 817, by pelagic sediments (foraminifers and coccoliths) and by typically pelagic sedimentation rates not exceeding 20 mm/k.y. The earliest part of the late Pliocene age section was characterized by well-developed hardgrounds in the "shallow" Sites 812 and 814 and by normal pelagic sediments mixed with reworked phosphatized planktonic foraminifers in Site 813. Finally, the early part of the late Pliocene (2.9-2.4 Ma) section was characterized by high sedimentation rates, related to the shedding and admixture into the pelagic sediments of bank-derived materials. These bank-derived materials consist of either diagenetically unaltered fine aragonite with traces of dolomite in Site 818 or micritic calcite resulting from seafloor and/or shallow burial alteration in the deepest Sites 817 and 811. The highest sedimentation rates (163 mm/k.y.) were recorded in Site 818, drilled nearest the modern carbonate bank of Tregrosse Reef. The sedimentation rates decrease with increasing distance from Tregrosse Reef - 120 mm/k.y. in Site 817 and 47.5 mm/k.y. in Site 811. The initial appearance of fine aragonite in Site 818, corresponding to the transition from pelagic to periplatform sedimentation rates, has been dated at 2.9 Ma. This Pliocene sediment pattern on the Queensland Plateau is different from the pattern observed in sediments from two earlier ODP legs (i.e., Leg 101 in the Bahamas and in Leg 115 in the Maldives), where aragonite-rich sediments, characterized by high periplatform sedimentation rates, were observed in the lower Pliocene section (5.2-3.5 Ma), whereas the upper Pliocene (3.5-1.6 Ma) sediments are more pelagic in nature and are characterized by low sedimentation rates or major hiatuses. These Pliocene periplatform sequences in the Bahamas and in the Maldives and late Quaternary age periplatform sequences worldwide have pointed out that "highstand shedding" was the typical response of carbonate platforms to fluctuations in sea level, just opposite to a "lowstand shedding" response to sea-level fluctuations, typical of siliciclastic shelves. Assuming that the envelope of Haq et al.'s (1987) sea-level curve, showing a well-defined lowering of sea level between 3.5 and 2.9 Ma, can also be applied to the southwest Pacific Ocean, based on a high-resolution Pliocene d18O record from the Ontong Java Plateau recently published by Jansen et al. (1993, doi:10.2973/odp.proc.sr.130.028.1993), the Pliocene periplatform sequences on the Queensland Plateau would have recorded the reentry of the bank tops into the photic zone during a general lowering of sea level, following an interval characterized by high sea level, during which the shallow carbonate system on the Queensland Plateau was drowned. The early Pliocene age (5.2-3.5 Ma) sediments deposited on the Queensland Plateau, an established interval of eustatic sea-level highstand, are typically pelagic in character. In addition, relatively cold surface temperatures (estimated to have ranged from 18° to 20°C by Isern et al. [this volume]) might have also stressed the reefs during early Pliocene time and contributed to the drowning of the Queensland Plateau carbonate system during the late Miocene and early Pliocene. Differential and relatively high subsidence rates, inferred by variations in paleodepth of water (based upon benthic foraminifer assemblages; Katz and Miller, this volume) may also have influenced the drowning of the carbonate bank tops on the Queensland Plateau during the late Miocene and early Pliocene. The sediments of early late Pliocene age (2.9-2.4 Ma), a well-established interval of lowering of sea level, are clearly periplatform and cyclic in nature. High-frequency (~40 k.y.) aragonite cycles, well-developed between 2.9 and 2.45 Ma, correlate with the planktonic high-resolution Pliocene d18O record from the Ontong Java Plateau, a good sea-level proxy (Jansen et al., in press). Contrary to late Quaternary age aragonite cycles from the Bahamas, the Nicaragua Rise, the Maldives, and the Queensland Plateau, the late Pliocene aragonite cycles in Hole 818B display high levels of aragonite during glacial stages and, therefore, lowstands of sea level. In addition, sediments deposited during the earliest part of the late Pliocene (3.5-2.9 Ma), transition between the early Pliocene highstand and the late Pliocene lowering in sea level, have recorded the first evidence of a fall in sea level, by (1) the occurrence of synchronous submarine hardgrounds in the two shallowest sites (Sites 812 and 814), (2) the deposition of reworked material from the shallower part of the slope into the intermediate Sites 813 and 818, and (3) the deposition of pelagic sediments in the deepest Sites 817 and 817. In summary, contrary to previous findings, the Pliocene periplatform sediments on the Queensland Plateau appear to have recorded a regional shedding of shallow carbonate bank tops during an interval of sea-level lowering, a good illustration of the "carbonate lowstand shedding" scenario, occurring during the reentry of previously drowned carbonate bank tops into the photic zone related to a decrease in sea level.

La jerarquía de vínculos socioafectivos en Ilíada XXIII.1-256

El artículo analiza las relaciones entre Aquiles y sus camaradas en la primera parte del canto XXIII (vv. 1-256), sobre la base de una mirada lingüístico-poética y un enfoque ético-pedagógico. Aquiles tiene dos comportamientos diferentes: como amigo y como caudillo. A Patroclo le dedica sus mejores manifestaciones de ternura y afecto. Como jefe, se dirige primero a sus camaradas más próximos, los mirmidones, y luego, según avanza el canto, a Agamenón, los nobles, las tropas, la comitiva más circunscripta de deudos y, finalmente, a los panaqueos en tanto cuerpo militar completo. Para una mayor comprensión de estas vinculaciones, se examina la autoridad y sus grados, a partir del grupo sémico correspondiente

Rendición o Resistencia? : El primer discurso latino

En la segunda mitad del siglo IV a. C. Roma ocupa la Italia central y se orienta al dominio de la región meridional en colisión posible con griegos y cartagineses; su influjo se extiende incluso al Jónico cuando varias ciudades de la Magna Grecia solicitan su protección, no así Tarento, que al anclar una escuadra romana en su puerto, reaccionó atacando las naves y una guarnición romana próxima. Tarento, ante una guerra inevitable, pidió apoyo al rey Pirro de Epiro, quien vio la oportunidad de extender hacia occidente las conquistas que Alejandro dejó inconclusas; su invasión de Italia generó fuerte resistencia, pero no le impidió victorias costosas ni su avance hacia el norte; propuso por intermedio de un embajador la rendición y condiciones gravosas para los romanos que estuvieron a punto de ceder. Allí surge Appio Claudia el Ciego, anciano senador ya retirado, que con un discurso breve, preciso y muy logrado produjo un giro en las decisiones de los patricios. Analizamos el discurso conservado por Plutarco en la Vida de Pirro y lo ubicamos dentro de su contexto histórico y político; gracias a él, Roma conservó sus fronteras itálicas y preparó su futura expansión.

Poderes locales y gobierno central ante el cambio de régimen en Buenos Aires : Cartas de ciudadanía, cargos públicos y práctica de oficios, 1812-1815

En la presente ponencia nos proponemos analizar la situación jurídica y política de algunos extranjeros que ocupaban cargos públicos o realizaban oficios civiles en el Rio de la Plata. En este contexto, los criterios para definir quién era un vecino-ciudadano dependían de la posibilidad de mantener o perder cargos públicos, o de ejercer ciertos oficios en los pueblos de la campaña. Se estudiarán dos casos en los cuales se presentaron situaciones análogas para los que no eran reconocidos pertenecientes a la comunidad política, es decir para los extranjeros. Aquellos que no lograban la obtención de una carta de ciudadanía se veían obligados a dejar sus cargos u oficios. Sin embargo, los reglamentos y las decisiones del gobierno en estos casos se vieron superados por las prácticas y situaciones concretas. Otro de los casos estudiados en esta ponencia se corresponde con un litigio en Chascomús un fuerte y pueblo de la campaña de Buenos Aires, en la frontera con el mundo indígena. Allí, un hombre de origen catalán le es impedido ejercer su oficio de panadero, limitándolo a la producción de pastelería fina. La decisión fue tomada por el comandante del fuerte ante un pedido de un grupo de panaderas que se consideraban 'patricias', señalando el origen español de dicho panadero para limitarlo en el ejercicio del oficio. El conflicto nos ofrece varias aristas interesantes sobre los mecanismos del ejercicio del poder que estamos viendo en otros trabajos, pero aquí nos detendremos en la definición del grupo de pertenencia y en la utilización de los conceptos de patria y patriotas

Strontium isotopes in pore waters of east equatorial Pacific sediments

Pore-water samples from the equatorial sedimentary bulge area show reversals in depth profiles of 87Sr/86Sr ratios at the sediment/basement interface. Results of this work support inferences made from previous pore-water data (from DSDP drilling in the area) that large-scale horizontal advection of seawater has occurred through the basement underlying the thick sedimentary sequence in this region. The area of apparent advection includes the eastern part of the equatorial high-productivity zone and part of the Guatemala Basin. We attempted to find links between the observed near-basement reversals in pore-water chemistry and sedimentary thickness, age, and topography of the area. Most of the sites that show horizontal advection have disturbed basement topography or outcrops within 10 to 20 km, suggesting that the cooling effects of outcrops may extend for at least 20 km horizontally. Heat-flow data from the area were compared to determine whether sites showing near-bottom chemistry reversals were consistent with areas of low conductive heat flow. This was generally true for the area of the sedimentary bulge and Guatemala Basin. Not enough pore-water data from the Nazca Plate were available to establish any reliable systematics. Because the high-productivity area is well-sealed from hydrothermal circulation, the missing heat must be lost by horizontal advective heat transport. From profiles of strontium isotopes and other elements that show departure from seawater values with increasing depth in the sediments, but return to seawater values near the basement, it appears that water flows relatively freely through much of the oceanic crust, even when sealed by considerable sedimentary cover.