A mutation in hairless dogs implicates FOXI3 in ectodermal development

Mexican and Peruvian hairless dogs and Chinese crested dogs are characterized by missing hair and teeth, a phenotype termed canine ectodermal dysplasia (CED). CED is inherited as a monogenic autosomal semidominant trait. With genomewide association analysis we mapped the CED mutation to a 102-kilo-base pair interval on chromosome 17. The associated interval contains a previously uncharacterized member of the forkhead box transcription factor family (FOXI3), which is specifically expressed in developing hair and teeth. Mutation analysis revealed a frameshift mutation within the FOXI3 coding sequence in hairless dogs. Thus, we have identified FOXI3 as a regulator of ectodermal development.

Apoyando innovaciones locales: Un instrumento para el fortalecimiento de innovaciones locales y la promoción del desarrollo rural sostenible: Experiencias de dos talleres pilotos de MASAL y CDE realizados en laprovincia de Cuzco, Perú

Local communities have often underestimated their endogenous potentials for innovation – potentials that could help them adapt to changing socio-cultural, political, economic and environmental conditions, to improve their livelihoods, develop their own visions, and negotiate their own priorities. While the significance of local innovation potentials for sustainable development is now increasingly acknowledged, projects and development plans rarely attempt to explicitly develop these potentials; nor do they try to disseminate local innovations within and among communities. Based on the conceptual framework of “social learning”, CDE has developed an instrument to promote existing local potential for innovation. The instrument is based on social learning processes involving different stakeholder groups in local contexts. It was successfully tested during two pilot workshops in a rural development context in the Peruvian highland. The present paper reports on the experience of these two workshops held in April and May 2004 in the communities of Tungasuca in the Cuzco Province. The paper describes the context of innovations and the methodology applied, followed by a detailed description of the contents and outcomes of the workshops, as well as the experience gained in the process. Finally it draws a set of conclusions and presents the lessons learnt.

Large-scale land acquisitions in Peru: Land (re)-concentration, agrarian change and reactions from rural communities

More than 40 years after the agrarian reform, Peru is experiencing a renewed process of concentration of land ownership in the hands of large-scale investors, favoring the development of a sugar cane production cluster along the northern coast. The expansion of the agricultural frontier by means of large irrigation projects – originally developed to benefit medium- and small-scale farmers – is carried out today in order to be sold to large-scale investors for the production of export crops. In the region of Piura the increasing presence of large-scale biofuel investors puts substantial pressure on land and water resources, not only changing the use of and access to land for local communities, but also generating water shortages vis-à-vis the multiple water demands of local food producers. The changes in land relations and the agro-ecosystem, the altering food production regime as well as the increasing proletarization of smallholders, is driving many locals – even those which (initially) welcomed the investment – into resistance activities against the increasing control of land, water and other natural resources in the hands of agribusinesses. The aim of this presentation is to discuss the contemporary political, social and cultural dynamics of agrarian change along the northern Peruvian coast as well as the «reactions from below» emanating from campesino communities, landless laborers, brick producers, pastoralists as well as other marginalized groups. The different strategies, forms and practices of resistance with the goal of the «protection of the territory» shall be explored as well as the reasons for their rather scattered occurrence and the lack of alliances on the land issue. This input shall make a contribution to the on-going debate on individual and communal property rights and the question of what is best in terms of collective defense against land grabbing.

Trace Elements in the Statoliths of Jumbo Flying Squid Off the Exclusive Economic Zones of Chile and Peru

Ontogenetic variation in 4 trace element ((88)Sr, (137)Ba, (24)Mg, (23)Na) concentrations and their ratios to Ca were measured in statoliths of the jumbo flying squid Dosidicus gigas off the Exclusive Economic Zone of Chilean and Peruvian waters using laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). The element compositions of statoliths showed no significant differences between females and males. All of the elements in different growth zones showed significant variations, except for Mg. Sr:Ca and Mg:Ca were good indicators for distinguishing squid from autumn and winter spawning seasons. Sr:Ca and Ba:Ca distribution patterns in statoliths confirmed that paralarvae and juvenile squid inhabit surface waters, while subadult squid migrate into deeper waters. An increasing Sr: Ca ratio of subadult squid could be explained by declining temperature gradients from northern to southern sampling locations, although no significant Sr: Ca differences were observed (p > 0.05). Mg:Ca ratios decreased progressively from the nucleus to the peripheral zone, which might be correlated with statolith growth rates. Na:Ca ratios slightly declined from paralarvae to the subadult phase. Quantitative relationships between statolith trace elements and environmental conditions under different growth stages are needed to improve our understanding of life history of D. gigas.

Methane concentration in sediment cores during METEOR cruise M92

We studied the concurrence of methanogenesis and sulfate reduction in surface sediments (0-25 cm below sea floor, cmbsf) at six stations (70, 145, 253, 407, 770 and 1024 m) along the Peruvian margin (12° S). This oceanographic region is characterized by high carbon export to the seafloor, creating an extensive oxygen minimum zone (OMZ) on the shelf, both factors that could favor surface methanogenesis. Sediments sampled along the depth transect traversed areas of anoxic and oxic conditions in the bottom-near water. Net methane production (batch incubations) and sulfate reduction (35S-sulfate radiotracer incubation) were determined in the upper 0-25 cmbsf of multicorer cores from all stations, while deep hydrogenotrophic methanogenesis (> 30 cmbsf, 14C-bicarbonate radiotracer incubation) was determined in two gravity cores at selected sites (78 and 407 m). Furthermore, stimulation (methanol addition) and inhibition (molybdate addition) experiments were carried out to investigate the relationship between sulfate reduction and methanogenesis. Highest rates of methanogenesis and sulfate reduction in the surface sediments, integrated over 0-25 cmbsf, were observed on the shelf (70-253 m, 0.06-0.1 and 0.5-4.7 mmol m-2 d-1, respectively), while lowest rates were discovered at the deepest site (1024 m, 0.03 and 0.2 mmol m-2 d-1, respectively). The addition of methanol resulted in significantly higher surface methanogenesis activity, suggesting that the process was mostly based on non-competitive substrates, i.e., substrates not used by sulfate reducers. In the deeper sediment horizons, where competition was probably relieved due to the decline of sulfate, the usage of competitive substrates was confirmed by the detection of hydrogenotrophic activity in the sulfate-depleted zone at the shallow shelf station (70 m). Surface methanogenesis appeared to be correlated to the availability of labile organic matter (C / N ratio) and organic carbon degradation (DIC production), both of which support the supply of methanogenic substrates. A negative correlation of methanogenesis rates with dissolved oxygen in the bottom-near water was not obvious, however, anoxic conditions within the OMZ might be advantageous for methanogenic organisms at the sediment-water interface. Our results revealed a high relevance of surface methanogenesis on the shelf, where the ratio between surface to deep (below sulfate penetration) methanogenic activity ranged between 0.13 and 105. In addition, methane concentration profiles indicate a partial release of surface methane into the water column as well as a partial consumption of methane by anaerobic methane oxidation (AOM) in the surface sediment. The present study suggests that surface methanogenesis might play a greater role in benthic methane budgeting than previously thought, especially for fueling AOM above the sulfate-methane transition zone.

Historia, literatura y lengua en el epistolario de Ricardo Palma y Miguel De Unamuno

En el presente trabajo partimos de una clara ponderación de la escritura epistolar como espacio gnoseológico que surge de la relación entre Ricardo Palma y Miguel de Unamuno, entre los años 1903 y 1913. Por tanto se inscribe, asimismo, en el campo de estudio de las relaciones culturales entre España y América. Como consecuencia, nuestro propósito principal no supone un abordaje solamente intratextual sino intertextual de la obra de Palma y la de Unamuno, en aquellos textos en los que se cruzan, ya sea bajo la forma de prólogos, comentarios o sencillamente en el intercambio epistolar. En marco esbozado, leemos una serie de problemáticas que se ocupan de la historia, la literatura y la lengua.

Lenguaje y valor en los escritos de Augusto Salazar Bondy (1965 - 1970)

Se examinan los escritos axiológicos de Augusto Salazar Bondy producidos entre 1965 y 1970, en los que predomina el análisis del lenguaje como criterio epistemológico y metodológico. Se señala el aprovechamiento de la metodología analítica por parte del peruano, así como los aspectos en que se separa de la filosofía moral británica y del primer Wittgenstein. Se consideran los aportes en relación a la caracterización de la experiencia del valor, el sentido del lenguaje valorativo y la fundamentación de los valores. Se destaca, para concluir, la concepción de los valores como categorías del obrar y la historicidad de la experiencia valorativa.

Mariátegui, Vallejo y la literatura peruana

Para enriquecer y superar la comprensión eurocéntrica histórica del fenómeno americano es preciso indagar en la reflexión que sobre éste realizan los propios pensadores de América. En este ocasión, nuestra particular elección ha recaído en José Carlos Mariátegui (1895-1930) y su obra Siete ensayos de interpretación de la realidad peruana (1928). Si bien su pensamiento fue poco formal, estuvo enriquecido por intuiciones y observaciones que aún esperan su oportunidad de tener un papel activo en la interpretación de nuestra cultura. Este trabajo se centra en la visión de la literatura peruana a partir de los aportes desde variadas perspectivas que realiza Mariátegui. Si bien parte de un método interpretativo relativamente rígido -materialista, economicista, historicista, lógico-dialéctico-, su obra tiene toda la amplitud crítica y la profundidad existencial que le da su posición privilegiada de observador y partícipe de los procesos políticos y sociales de la vida peruana. En sus comentarios sobre la literatura peruana, Mariátegui destaca el papel de Cesar Vallejo quien, nacido y criado en la sierra peruana, es el primer poeta capaz de representar a la nación con sus dos mundos: el mundo indio y el mundo mestizo. De esta manera, el pensamiento de Mariátegui nos ayuda a entender el carácter de la literatura peruana desde una novedosa y diferente perspectiva.

Plebe y revolución : la participación popular durante las guerras de independencia en el Perú, 1808-1824

Actualmente una de las variantes historiográficas más importantes en el estudio de la independencia en América Latina está circunscrita al análisis de la participación política de los grupos populares. En ese sentido, en aquel contexto de guerra y lucha revolucionaria en el Perú, que va desde la crisis hispana de 1808 hasta la independencia definitiva en 1824, esta investigación, a partir de un conjunto de fuentes de archivo, impresos y periódicos diversos, desarrolla las imágenes y representaciones que las elites peruanas construyeron de estos sectores sociales, algunas de las respuestas que estos últimos les infringieron y las múltiples alternativas políticas, que en aquel escenario beligerante, todos estos actores supieron concebir, negociar y utilizar políticamente.

Hydrocarbon gases in Tertiary and Quaternary sediments offshore Peru

Hydrocarbon gases (methane, ethane, propane, isobutane, n-butane, ethene, and propene) are present in Tertiary and Quaternary shelf, upper-slope, and lower-slope deposits of the Peruvian continental margin. Methane dominates the composition of the hydrocarbon gas at all 10 sites examined during Ocean Drilling Program (ODP) Leg 112. Generation of methane is regulated by the amount of sulfate in pore water. Wherever sulfate concentrations approach or equal zero, methane concentrations increase rapidly, reaching values near 100,000 µL/L of wet sediment at eight of the 10 sites. Methane at all 10 sites results from methanogenesis, which is inhibited where sulfate is present and microbial reduction of sulfate occurs. Hydrocarbon gases heavier than methane also are present, but at much lower concentrations than methane. These hydrocarbons are thought to result from early thermal and microbial diagenesis, based on relative gas compositions and trends of concentrations with depth. With few exceptions, the results obtained in the shipboard and shore-based laboratories are comparable for methane and ethane in sediments of Leg 112. Reanalyses of canned sediments from ODP Leg 104 and from Deep Sea Drilling Project (DSDP) Legs 76 and 84 show that gas samples can be stored for as long as 8 yr, but the amounts of individual hydrocarbon gases retained vary. Nevertheless, the trends of the data sets with depth are similar for fresh and stored samples.

Element contents, sulfur and oxygen isotopes, and molecular biomarkers of phosphatic crust samples from the Chimbote Platform of the shelf off Peru

Authigenic phosphatic laminites enclosed in phosphorite crusts from the shelf off Peru (10°01' S and 10°24' S) consist of carbonate fluorapatite layers, which contain abundant sulfide minerals including pyrite (FeS2) and sphalerite (ZnS). Low d34Spyrite values (average -28.8 per mill) agree with bacterial sulfate reduction and subsequent pyrite formation. Stable sulfur isotopic compositions of sulfate bound in carbonate fluorapatite are lower than that of sulfate from ambient sea water, suggesting bacterial reoxidation of sulfide by sulfide-oxidizing bacteria. The release of phosphorus and subsequent formation of the autochthonous phosphatic laminites are apparently caused by the activity of sulfate-reducing bacteria and associated sulfide-oxidizing bacteria. Following an extraction-phosphorite dissolution-extraction procedure, molecular fossils of sulfate-reducing bacteria (mono-O-alkyl glycerol ethers, di-O-alkyl glycerol ethers, as well as the short-chain branched fatty acids i/ai-C15:0, i/ai-C17:0 and 10MeC16:0) are found to be among the most abundant compounds. The fact that these molecular fossils of sulfate-reducing bacteria are distinctly more abundant after dissolution of the phosphatic laminite reveals that the lipids are tightly bound to the mineral lattice of carbonate fluorapatite. Moreover, compared with the autochthonous laminite, molecular fossils of sulfate-reducing bacteria are: (1) significantly less abundant and (2) not as tightly bound to the mineral lattice in the other, allochthonous facies of the Peruvian crusts consisting of phosphatic coated grains. These observations confirm the importance of sulfate-reducing bacteria in the formation of the phosphatic laminite. Model calculations highlight that organic matter degradation by sulfate-reducing bacteria has the potential to liberate sufficient phosphorus for phosphogenesis.

Geochemistry of phosphatic crusts from the shelf off Peru

Authigenic phosphorite crusts from the shelf off Peru (9°40°S to 13°30°S) consist of a facies with phosphatic coated grains covered by younger phosphatic laminite. The crusts are composed of carbonate fluorapatite, which probably formed via an amorphous precursor close to the sediment water interface as indicated by low F/P2O5 ratios, Sr and Ca isotopes, as well as rare earth element patterns agreeing with seawater-dominated fluids. Small negative Ce anomalies and U enrichment in the laminite suggest suboxic conditions close to the sediment-water interface during its formation. Increased contents of chalcophilic elements and abundant sulfide minerals in the facies with phosphatic coated grains as well as in the laminite denote sulfate reduction and, consequently, point to episodical development of anoxic conditions during phosphogenesis. The Peruvian phosphorites formed episodically over an extended period of time lasting from Middle Miocene to Pleistocene. Individual phosphatic coated grains show a succession of phosphatic layers with varying contents of organic matter and sulfide-rich phosphatic layers. Coated grains supposedly formed as a result of episodic suspension caused by high turbulence and shifting redox conditions. Episodic anoxia in the pore water induced pyritization in the outermost carbonate fluorapatite layer. Phosphatic coated grains were later transported to the place of crust formation, where subsequent laminite formation was favored under lower energy conditions. A similar succession of phosphatic layers with varying contents of organic matter and sulfide-rich layers in the laminite suggests a formation mechanism analogous to that of individual coated grains.

Fauna composition of benthos communities in bottom sediments from the edge and the central part of the shelf in the California upwelling zone

Two shelf communities from the central part off the California Peninsula are described. The community of Amphiodia urtica - Nephtys ferruginea develops in the central part of the shelf within the depth range 95-105 m. The community of Nephtys ferruginea - Amphiura acrystata develops on the shelf edge at depth 110 m. Biomasses of both communities are very low (about 10 g/m**2). Species richness of the shelf community is high; more than 60 species occur in samples (43-51 species per a community). Various echinoderms and some other groups are abundant on the Californian shelf; these groups are absent in shelf areas of Peruvian and Benguela upwellings. Species structures of the communities were analyzed; the communities were shown to consist of coexisting, but not interacting guilds; this indicates that the communities are undersaturated with individuals. At the same time values of ABC-indices indicate that the communities are stable. We suggest that in this case adaptation to unfavorable but stable environment is observed (selection of species-stressolarents). An explanation seems to lie in the penetrating type of the upwelling in the Californian upwelling zone. Low biomass values seem to result from mass development of necto-benthic carnivorous crustaceans-galateids Pleuroncodes planiceps.

"Pues doy Fe de que son tenidos como tales" : Prácticas y discursos legitimantes en el intento de conformación de una posible nobleza rioplatense

A mediados del siglo XVIII los grandes comerciantes de distintos espacios hispanoamericanos, acumulan suficientes caudales que les permiten comprar títulos de nobleza, distinciones o formar mayorazgos que relumbren sus nombres y perpetúen sus bienes adquiridos. Este proceso es mayormente evidente en los espacios mexicanos y peruanos; pero no se conocen casos concretos para el espacio rioplatense. Como planteó José Torre Revello, esto no implica que los comerciantes rioplatenses no intentasen ennoblecerse. El presente estudio de caso detalla como Don Vicente de Azcuénaga intenta fundar un mayorazgo en la ciudad de Buenos Aires a favor de su primogénito Miguel. A través de este estudio basado en las "probanzas" se puede observar como la familia Azcuénaga pretende resaltar su nombre frente al resto de sus contemporáneos, pero las relaciones entre padre e hijo nos conducen a la vez a replantearnos interrogantes referentes a las tradiciones de acumulación y conservación de patrimonios