Relaciones ciudad-aldea en Trasmiera y la zona Oriental de Cantabria : Linajes, parentelas y clientelas en el marco del señorío de los Condestables (siglos XIV-XVI)

El presente artículo tiene como objetivo analizar la dinámica que adquieren las relaciones de dominio señorial al interior del señorío de la Casa de los Velasco, Condestables hereditarios del reino de Castilla, partiendo de la forma que adopta la intrincada red de agentes y administradores señoriales a su servicio ubicados en el nivel de las aldeas y villas que forman parte de la zona oriental de Cantabria entre los siglos XIV al XVI. Para ello, estableceremos los diversos mecanismos de solidaridad, dependencia y sujeción de los cuales se vale el señor para ejercer su jurisdicción y poder de mando sobre este conjunto plural de comunidades y hombres. Es decir, nuestra intención es estudiar el proceso de construcción del poder señorial a partir de una imagen dinámica que le brinde dimensión y profundidad y que, al mismo tiempo, permita entender la constitución del dominio político señorial no sólo como una imposición de arriba hacia abajo, sino también como un espacio de negociación en permanente rearticulación que involucra tanto al señor, su parentela y clientela, como a las comunidades jerarquizadas, tanto rurales como urbanas, que se encuentran sometidas a su poder

Sobre tensiones, transición y transformación en el territorio de una ciudad andina : San Juan. Argentina

El trabajo que se presenta se referencia en una serie de propuestas de ordenamiento territorial desarrolladas de manera conjunta entre municipios de la provincia de San Juan, Argentina y la Universidad Nacional de San Juan. Se trata de propuestas que abordan múltiples desafíos, los que no por recurrentes minimizan su complejidad. Por el contrario señalan la transición hacia la construcción de territorios más sostenibles en este contexto particular, enfrentan el desafío que supone la disputa por el suelo urbano, las tensiones derivadas del avance de la urbanización y la expectativa de valorización inmobiliaria por parte de sectores del periurbano. Se propone una transformación del propio territorio, sostenida en la construcción de capacidades locales, en el afianzamiento de redes, y en la concienciación sobre las propias capacidades. Los resultados alcanzados desde lo 'tangible' refieren a propuestas orientadas en tres direcciones principales: reestructuración espacial y funcional, reestructuración socio-productiva y gestión integrada de recursos patrimoniales. Más allá de estos resultados, vinculados al diseño de estrategias de ocupación y manejo sustentable del territorio se destacan diversas construcciones, como el reconocimiento e incorporación de nuevos actores, el fortalecimiento de lazos entre actores locales y externos a la comunidad: Universidad, Gobierno provincial, Municipios; la continuidad de proyectos, la socialización de resultados con otros municipios, los proyectos en marcha. En este sentido, actualmente se trabaja en la construcción del Plan para el Area Metropolitana de San Juan, en una conjunción de voluntades políticas, sociales y técnicas, involucrando a seis municipios de la provincia. Indudablemente, se trata de procesos que requieren complementariamente o simultáneamente de aquellos 'microprocesos' a escala de las comunidades, que se transformen en 'micrologros', en una estrategia que integre procesos 'top down' y 'bottom up'. Éste es un camino que se comienza a recorrer. Concluyendo, se valora especialmente, el rol dinamizador que los procesos desarrollados han provocado en el entorno local, generando nuevas propuestas, atrayendo programas y acciones concretas hacia el territorio. Se comienza a transitar de una manera sostenida, la incorporación del tema planificación en la agenda de gobierno, la construcción de microprocesos en distintas comunidades, y la Universidad recuperando su rol, no sólo como consultor de referencia en estas temáticas, sino esencialmente como 'caja de resonancia' de las necesidades y deseabilidades de esta comunidad. En síntesis, se espera que estos procesos de transición alcancen la necesaria escala de transformación

Relaciones ciudad-aldea en Trasmiera y la zona Oriental de Cantabria : Linajes, parentelas y clientelas en el marco del señorío de los Condestables (siglos XIV-XVI)

El presente artículo tiene como objetivo analizar la dinámica que adquieren las relaciones de dominio señorial al interior del señorío de la Casa de los Velasco, Condestables hereditarios del reino de Castilla, partiendo de la forma que adopta la intrincada red de agentes y administradores señoriales a su servicio ubicados en el nivel de las aldeas y villas que forman parte de la zona oriental de Cantabria entre los siglos XIV al XVI. Para ello, estableceremos los diversos mecanismos de solidaridad, dependencia y sujeción de los cuales se vale el señor para ejercer su jurisdicción y poder de mando sobre este conjunto plural de comunidades y hombres. Es decir, nuestra intención es estudiar el proceso de construcción del poder señorial a partir de una imagen dinámica que le brinde dimensión y profundidad y que, al mismo tiempo, permita entender la constitución del dominio político señorial no sólo como una imposición de arriba hacia abajo, sino también como un espacio de negociación en permanente rearticulación que involucra tanto al señor, su parentela y clientela, como a las comunidades jerarquizadas, tanto rurales como urbanas, que se encuentran sometidas a su poder

Sobre tensiones, transición y transformación en el territorio de una ciudad andina : San Juan. Argentina

El trabajo que se presenta se referencia en una serie de propuestas de ordenamiento territorial desarrolladas de manera conjunta entre municipios de la provincia de San Juan, Argentina y la Universidad Nacional de San Juan. Se trata de propuestas que abordan múltiples desafíos, los que no por recurrentes minimizan su complejidad. Por el contrario señalan la transición hacia la construcción de territorios más sostenibles en este contexto particular, enfrentan el desafío que supone la disputa por el suelo urbano, las tensiones derivadas del avance de la urbanización y la expectativa de valorización inmobiliaria por parte de sectores del periurbano. Se propone una transformación del propio territorio, sostenida en la construcción de capacidades locales, en el afianzamiento de redes, y en la concienciación sobre las propias capacidades. Los resultados alcanzados desde lo 'tangible' refieren a propuestas orientadas en tres direcciones principales: reestructuración espacial y funcional, reestructuración socio-productiva y gestión integrada de recursos patrimoniales. Más allá de estos resultados, vinculados al diseño de estrategias de ocupación y manejo sustentable del territorio se destacan diversas construcciones, como el reconocimiento e incorporación de nuevos actores, el fortalecimiento de lazos entre actores locales y externos a la comunidad: Universidad, Gobierno provincial, Municipios; la continuidad de proyectos, la socialización de resultados con otros municipios, los proyectos en marcha. En este sentido, actualmente se trabaja en la construcción del Plan para el Area Metropolitana de San Juan, en una conjunción de voluntades políticas, sociales y técnicas, involucrando a seis municipios de la provincia. Indudablemente, se trata de procesos que requieren complementariamente o simultáneamente de aquellos 'microprocesos' a escala de las comunidades, que se transformen en 'micrologros', en una estrategia que integre procesos 'top down' y 'bottom up'. Éste es un camino que se comienza a recorrer. Concluyendo, se valora especialmente, el rol dinamizador que los procesos desarrollados han provocado en el entorno local, generando nuevas propuestas, atrayendo programas y acciones concretas hacia el territorio. Se comienza a transitar de una manera sostenida, la incorporación del tema planificación en la agenda de gobierno, la construcción de microprocesos en distintas comunidades, y la Universidad recuperando su rol, no sólo como consultor de referencia en estas temáticas, sino esencialmente como 'caja de resonancia' de las necesidades y deseabilidades de esta comunidad. En síntesis, se espera que estos procesos de transición alcancen la necesaria escala de transformación

Carbon/Nitrogen ratio of plant tissues and biomass of belowground consumers after 11 years of experimental treatment, Toolik lake

Theory and observation indicate that changes in the rate of primary production can alter the balance between the bottom-up influences of plants and resources and the top-down regulation of herbivores and predators on ecosystem structure and function. The Exploitation Ecosystem Hypothesis (EEH) posited that as aboveground net primary productivity (ANPP) increases, the additional biomass should support higher trophic levels. We developed an extension of EEH to include the impacts of increases in ANPP on belowground consumers in a similar manner as aboveground, but indirectly through changes in the allocation of photosynthate to roots. We tested our predictions for plants aboveground and for phytophagous nematodes and their predators belowground in two common arctic tundra plant communities subjected to 11 years of increased soil nutrient availability and/or exclusion of mammalian herbivores. The less productive dry heath (DH) community met the predictions of EEH aboveground, with the greatest ANPP and plant biomass in the fertilized plots protected from herbivory. A palatable grass increased in fertilized plots while dwarf evergreen shrubs and lichens declined. Belowground, phytophagous nematodes also responded as predicted, achieving greater biomass in the higher ANPP plots, whereas predator biomass tended to be lower in those same plots (although not significantly). In the higher productivity moist acidic tussock (MAT) community, aboveground responses were quite different. Herbivores stimulated ANPP and biomass in both ambient and enriched soil nutrient plots; maximum ANPP occurred in fertilized plots exposed to herbivory. Fertilized plots became dominated by dwarf birch (a deciduous shrub) and cloudberry (a perennial forb); under ambient conditions these two species coexist with sedges, evergreen dwarf shrubs, and Sphagnum mosses. Phytophagous nematodes did not respond significantly to changes in ANPP, although predator biomass was greatest in control plots. The contrasting results of these two arctic tundra plant communities suggest that the predictions of EEH may hold for very low ANPP communities, but that other factors, including competition and shifts in vegetation composition toward less palatable species, may confound predicted responses to changes in productivity in higher ANPP communities such as the MAT studied here.

Isotopic composition of ground ice, ebullition gases and thermokarst lake water, North America

Thermokarst lakes are thought to have been an important source of methane (CH4) during the last deglaciation when atmospheric CH4 concentrations increased rapidly. Here we demonstrate that meltwater from permafrost ice serves as an H source to CH4 production in thermokarst lakes, allowing for region-specific reconstructions of dD-CH4 emissions from Siberian and North American lakes. dD CH4 reflects regionally varying dD values of precipitation incorporated into ground ice at the time of its formation. Late Pleistocene-aged permafrost ground ice was the dominant H source to CH4 production in primary thermokarst lakes, whereas Holocene-aged permafrost ground ice contributed H to CH4 production in later generation lakes. We found that Alaskan thermokarst lake dD-CH4 was higher (-334 ± 17 per mil) than Siberian lake dD-CH4 (-381 ± 18 per mil). Weighted mean dD CH4 values for Beringian lakes ranged from -385 per mil to -382 per mil over the deglacial period. Bottom-up estimates suggest that Beringian thermokarst lakes contributed 15 ± 4 Tg CH4 /yr to the atmosphere during the Younger Dryas and 25 ± 5 Tg CH4 /yr during the Preboreal period. These estimates are supported by independent, top-down isotope mass balance calculations based on ice core dD-CH4 and d13C-CH4 records. Both approaches suggest that thermokarst lakes and boreal wetlands together were important sources of deglacial CH4.

Mesozooplankton biomass data from the Kapisigdlit an inner fjord branch of the Godthaabsfjord system, West Greenland, 2010

Sampling was conducted from March 24 to August 5 2010, in the fjord branch Kapisigdlit located in the inner part of the Godthåbsfjord system, West Greenland. The vessel "Lille Masik" was used during all cruises except on June 17-18 where sampling was done from RV Dana (National Institute for Aquatic Resources, Denmark). A total of 15 cruises (of 1-2 days duration) 7-10 days apart was carried out along a transect composed of 6 stations (St.), spanning the length of the 26 km long fjord branch. St. 1 was located at the mouth of the fjord branch and St. 6 was located at the end of the fjord branch, in the middle of a shallower inner creek . St. 1-4 was covering deeper parts of the fjord, and St. 5 was located on the slope leading up to the shallow inner creek. Mesozooplankton was sampled by vertical net tows using a Hydrobios Multinet (type Mini) equipped with a flow meter and 50 µm mesh nets or a WP-2 net 50 µm mesh size equipped with a non-filtering cod-end. Sampling was conducted at various times of day at the different stations. The nets were hauled with a speed of 0.2-0.3 m s**-1 from 100, 75 and 50 m depth to the surface at St. 2 + 4, 5 and 6, respectively. The content was immediately preserved in buffered formalin (4% final concentration). All samples were analyzed in the Plankton sorting and identification center in Szczecin (www.nmfri.gdynia.pl). Samples containing high numbers of zooplankton were split into subsamples. All copepods and other zooplankton were identified down to lowest possible taxonomic level (approx. 400 per sample), length measured and counted. Copepods were sorted into development stages (nauplii stage 1 - copepodite stage 6) using morphological features and sizes, and up to 10 individuals of each stage was length measured.

Geochemical studies of the Cretaceous-Tertiary boundary in ODP Holes 113-689B and 113-690C

In a study of ODP Hole 689B no iridium (Ir) anomaly was found in Sections 1 through 6 of Core 25X or in Core 26X from the top down to section 2, 3-12 cm. The background Ir abundance averaged 11 parts per trillion (ppt) and a clay-enriched region had nearly the same average, 26 ± 12 ppt. If the Cretaceous-Tertiary (K-T) contact is in the region studied, then sedimentation was not continuous, and the K-T boundary was probably either not deposited or it was eroded away. In a study of Cores 15X and 16X of ODP Hole 690C, an iridium peak with a maximum abundance of 1566 ± 222 ppt was found in Section 4 of Core 15X at 39-40 cm with a half-width of 6.6 cm. Background abundances were ~15 ppt and distinctly higher Ir abundances were observed from 119 cm below to 72 cm above the main peak. The Ir distribution below the main peak is attributed to bioturbation by organisms with burrows extending at least 0.4 m. The Ir distribution above the main peak may be due to the same cause but other explanations may be significant. There are variable enrichments of clay in the mainly CaCO3 sediment of Core 15X, and the stratigraphically lowest part of the most abundant clay deposits is found (within 2 cm) in the same position as the main Ir peak. The clay deposit, which is estimated to be about 50% of the sediment, extends upward ~19 cm and then slowly decreases to a background level of 10% over 1 m. The degree of homogeneity of the clay-rich interval suggests it was not due to episodic volcanism but may have been due to a decrease of the CaCO3 deposition rate which was possibly triggered by the impact of a large asteroid or comet on the Earth.

Seawater carbonate chemistry during experiments with Patella vulgata, 2010

The effect of short-term (5 days) exposure to CO2-acidified seawater (year 2100 predicted values, ocean pH = 7.6) on key aspects of the function of the intertidal common limpet Patella vulgata (Gastropoda: Patellidae) was investigated. Changes in extracellular acid-base balance were almost completely compensated by an increase in bicarbonate ions. A concomitant increase in haemolymph Ca2+ and visible shell dissolution implicated passive shell dissolution as the bicarbonate source. Analysis of the radula using SEM revealed that individuals from the hypercapnic treatment showed an increase in the number of damaged teeth and the extent to which such teeth were damaged compared with controls. As radula teeth are composed mainly of chitin, acid dissolution seems unlikely, and so the proximate cause of damage is unknown. There was no hypercapnia-related change in metabolism (O2 uptake) or feeding rate, also discounting the possibility that teeth damage was a result of a CO2-related increase in grazing. We conclude that although the limpet appears to have the physiological capacity to maintain its extracellular acid-base balance, metabolism and feeding rate over a 5 days exposure to acidified seawater, radular damage somehow incurred during this time could still compromise feeding in the longer term, in turn decreasing the top-down ecosystem control that P. vulgata exerts over rocky shore environments.

Seafloor hydrothermal activity in sediment core MV0502-15JC

A large diameter piston core containing 8.35 m of metalliferous sediment has been recovered from a small abyssal valley in the remote Southwest Pacific Basin (31°42.194'S, 143°30.331'W; 5082 m water depth), providing unique insight into hydrothermal activity and eolian sedimentation there since the early Oligocene. A combination of fish-teeth Sr-isotope stratigraphy and INAA geochemical data reveals an exponentially decreasing hydrothermal flux 31 Ma to the present. Although hydrothermal sedimentation related to seafloor spreading explains this trend, a complex history of late Eocene/early Oligocene ridge jumps, propagating rifts and plate tectonic reorganization of South Pacific seafloor could have also played a role. A possible hiatus in deposition, as recorded by changes in core composition just below 2 m depth, is beyond the resolution of the fish teeth Sr isotope dating method employed here; however, the timing of this interval may be coincident with extinction of the Pacific-Farallon Ridge at ~20 Ma. A low flux eolian component accumulating at this site shows an increase relative to the hydrothermal component above 2 m depth, consistent with dust-generating continental sources far to the west (Australia/New Zealand). This is the first long-term paleoceanographic record obtained from within the South Pacific "bare zone" (Rea et al., 2006), an anomalous region where Pacific seafloor has largely escaped sediment accumulation since the Late Cretaceous.

Seawater carbonate chemistry, thickness and carbonate elemental composition of the test of juvenile sea urchins in a laboratory experiment

Continuous anthropogenic CO2 emissions to the atmosphere and uptake by the oceans will cause a reduction of seawater pH and saturation state (Omega) of CaCO3 minerals from which marine calcifiers build their shells and skeletons. Sea urchins use the most soluble form of calcium carbonate, high-magnesium calcite, to build their skeleton, spines and grazing apparatus. In order to highlight the effects of increased pCO2 on the test thickness and carbonate elemental composition of juvenile sea urchins and potential differences in their responses linked to the diet, we performed a laboratory experiment on juvenile Paracentrotus lividus, grazing on calcifying (Corallina elongata) and non-calcifying (Cystoseira amentacea, Dictyota dichotoma) macroalgae, under different pH (corresponding to pCO2 values of 390, 550, 750 and 1000 µatm). Results highlighted the importance of the diet in determining sea urchin size irrespectively of the pCO2 level, and the relevance of macroalgal diet in modulating urchin Mg/Ca ratio. The present study provides relevant clues both in terms of the mechanism of mineral incorporation and in terms of bottom-up processes (algal diet) affecting top-down ones (fish predation) in rocky subtidal communities

Juvenile sea stars exposed to acidification decrease feeding and growth with no acclimation potential

Ocean acidification has the potential to affect growth and calcification of benthic marine invertebrates, particularly during their early life history. We exposed field-collected juveniles of Asterias rubens from Kiel Fjord (western Baltic Sea) to 3 seawater CO2 partial pressure (pCO2) levels (ranging from around 650 to 3500 µatm) in a long-term (39 wk) and a short-term (6 wk) experiment. In both experiments, survival and calcification were not affected by elevated pCO2. However, feeding rates decreased strongly with increasing pCO2, while aerobic metabolism and NH4+ excretion were not significantly affected by CO2 exposure. Consequently, high pCO2 reduced the scope for growth in A. rubens. Growth rates decreased substantially with increasing pCO2 and were reduced even at pCO2 levels occurring in the habitat today (e.g. during upwelling events). Sea stars were not able to acclimate to higher pCO2, and growth performance did not recover during the long-term experiment. Therefore, the top-down control exerted by this keystone species may be diminished during periods of high environmental pCO2 that already occur occasionally and will be even higher in the future. However, some individuals were able to grow at high rates even at high pCO2, indicating potential for rapid adaption. The selection of adapted specimens of A. rubens in this seasonally acidified habitat may lead to higher CO2 tolerance in adult sea stars of this population compared to the juvenile stage. Future studies need to address the synergistic effects of multiple stressors such as acidification, warming and reduced salinity, which will simultaneously impact the performance of sea stars in this habitat.

Remote Effects of Hippocampal Sclerosis on Effective Connectivity during Working Memory Encoding: A Case of Connectional Diaschisis?

Accumulating evidence suggests a role for the medial temporal lobe (MTL) in working memory (WM). However, little is known concerning its functional interactions with other cortical regions in the distributed neural network subserving WM. To reveal these, we availed of subjects with MTL damage and characterized changes in effective connectivity while subjects engaged in WM task. Specifically, we compared dynamic causal models, extracted from magnetoencephalographic recordings during verbal WM encoding, in temporal lobe epilepsy patients (with left hippocampal sclerosis) and controls. Bayesian model comparison indicated that the best model (across subjects) evidenced bilateral, forward, and backward connections, coupling inferior temporal cortex (ITC), inferior frontal cortex (IFC), and MTL. MTL damage weakened backward connections from left MTL to left ITC, a decrease accompanied by strengthening of (bidirectional) connections between IFC and MTL in the contralesional hemisphere. These findings provide novel evidence concerning functional interactions between nodes of this fundamental cognitive network and sheds light on how these interactions are modified as a result of focal damage to MTL. The findings highlight that a reduced (top-down) influence of the MTL on ipsilateral language regions is accompanied by enhanced reciprocal coupling in the undamaged hemisphere providing a first demonstration of “connectional diaschisis.”

A study of set-sharing analysis via cliques

We study the problem of efñcient, scalable set-sharing analysis of logic programs. We use the idea of representing sharing information as a pair of abstract substitutions, one of which is a worst-case sharing representation called a clique set, which was previously proposed for the case of inferring pair-sharing. We use the clique-set representation for (1) inferring actual set-sharing information, and (2) analysis within a topdown framework. In particular, we define the abstract functions required by standard top-down analyses, both for sharing alone and also for the case of including freeness in addition to sharing. Our experimental evaluation supports the conclusión that, for inferring set-sharing, as it was the case for inferring pair-sharing, precisión losses are limited, while useful efñciency gains are obtained. At the limit, the clique-set representation allowed analyzing some programs that exceeded memory capacity using classical sharing representations.

An integration of partial evaluation in a generic abstract interpretation framework

Information generated by abstract interpreters has long been used to perform program specialization. Additionally, if the abstract interpreter generates a multivariant analysis, it is also possible to perform múltiple specialization. Information about valúes of variables is propagated by simulating program execution and performing fixpoint computations for recursive calis. In contrast, traditional partial evaluators (mainly) use unfolding for both propagating valúes of variables and transforming the program. It is known that abstract interpretation is a better technique for propagating success valúes than unfolding. However, the program transformations induced by unfolding may lead to important optimizations which are not directly achievable in the existing frameworks for múltiple specialization based on abstract interpretation. The aim of this work is to devise a specialization framework which integrates the better information propagation of abstract interpretation with the powerful program transformations performed by partial evaluation, and which can be implemented via small modifications to existing generic abstract interpreters. With this aim, we will relate top-down abstract interpretation with traditional concepts in partial evaluation and sketch how the sophisticated techniques developed for controlling partial evaluation can be adapted to the proposed specialization framework. We conclude that there can be both practical and conceptual advantages in the proposed integration of partial evaluation and abstract interpretation.