Carbon pools and fluxes measured during a field campaign conducted in 2010 on the Tibetan Plateau at Kema

The Tibetan highlands host the largest alpine grassland ecosystems worldwide, bearing soils that store substantial stocks of carbon (C) that are very sensitive to land use changes. This study focuses on the cycling of photoassimilated C within a Kobresia pygmaea pasture, the dominating ecosystems on the Tibetan highlands. We investigated short-term effects of grazing cessation and the role of the characteristic Kobresia root turf on C fluxes and belowground C turnover. By combining eddy-covariance measurements with 13CO2 pulse labeling we applied a powerful new approach to measure absolute fluxes of assimilates within and between various pools of the plant-soil-atmosphere system. The roots and soil each store roughly 50% of the overall C in the system (76 Mg C/ha), with only a minor contribution from shoots, which is also expressed in the root:shoot ratio of 90. During June and July the pasture acted as a weak C sink with a strong uptake of approximately 2 g C/m**2/ in the first half of July. The root turf was the main compartment for the turnover of photoassimilates, with a subset of highly dynamic roots (mean residence time 20 days), and plays a key role for the C cycling and C storage in this ecosystem. The short-term grazing cessation only affected aboveground biomass but not ecosystem scale C exchange or assimilate allocation into roots and soil.

Geological investigation of dykes in Shackleton Range, Antarctica

During the Geological Expedition to the Shackleton Range, Antarctica (GEISHA) in 1987/88, samples were taken from twenty-one basaltic dykes for palaeomagnetic investigations. The directions of characteristic remanent magnetization (ChRM) of the dykes were determined by thermal and alternating-field demagnetization of 268 cores drilled from the specimens collected. Moreover, on account of the hydrothermal and sometimes low-grade metamorphism of the dyke rock and the resulting partial modification of the primary magnetization, not only were comprehensive magnetic studies carried out, but also ore-microscopic examination. Only thus was it possible to achieve a reasonable assessment and interpretation of the remanent magnetization. Jurassic and Silurian-Devonian ages were confirmed for the dykes of the northern and northwestern Shackleton Range by comparison of the paleopole positions calculated on the basis of the ChRM of the dykes with the known pole positions for the eastern Antarctic, as well as with polar-wandering curves for Gondwana. Radiometric ages were also determined far some of the dykes. Middle and Late Proterozoic ages are postulated far the dykes in the Read Mountains. Conclusions on the geotectonic relations of the Shackleton Range can also be drawn from the palaeomagnetic data. It has been postulated that the main strike direction, which differs distinctly from that of the Ross orogen, is due to rotation or displacement of the Shackleton Range crustal block; however, this was not corroborated. The pole positions for the Shackleton Range agree with those of rocks of the same age from other areas of East Antarctica and its positions in the Palaeozoic-Mesozoic polar-wandering path for Gondwana are evidence against the idea of rotation and rather suggest that the position of the Shakleton Range crustal block is autochthonous.

Mineral composition, major element oxides and trace element concentration of sediments from ODP Leg 180 sites

Middle Miocene to Holocene fine-grained argillaceous sediments (clays, claystones/muds, and mudstones), which volumetrically dominated the sediment recovery in the Woodlark Basin during Leg 180, were chemically analyzed for major elements, trace elements, and some rare earth elements by X-ray fluorescence. Selected samples also underwent X-ray diffraction (XRD) analysis for mineral determination. The results shed light on sediment provenance when combined with shipboard sediment descriptions, smear slide study, and XRD. The oldest sediments recovered (Site 1108) of middle-late Miocene age include volcanogenic muds with distinctive high MgO and K2O, indicative of a relatively basic calc-alkaline source related to an inferred Miocene forearc succession. The forearc basement, composed of diabase and basalt, was locally exposed (Site 1109) and eroded in the late Miocene (<5.4-9.93 Ma), giving rise to fluvial conglomerates (Sites 1109, 1115, and 1118). Chemically distinctive fine-grained claystones and siltstones (with relatively high Ti, low K) are compatible with derivation from tropically weathered basic igneous rocks, correlated with the Paleogene Papuan ophiolite. Overlying latest Miocene-Pleistocene fine-grained sediments throughout the Woodlark Basin were partly derived from calc-alkaline volcanic sources. However, relatively high abundances of Al2O3 and related element oxides (K2O and Na2O) and trace elements (e.g., Rb and Y) reflect an additional terrigenous input throughout the basin, correlated with pelitic metamorphic rocks exposed on Papua New Guinea and adjacent areas. In addition, sporadic high abundances of Cr and Ni, some other trace metals, and related minerals (talc, crysotile, and chlorite) reflect input from an ophiolitic terrain dominated by ultramafic rocks, correlated with the Paleogene Papuan ophiolite. The source areas possibly included serpentinized ultramafic ophiolitic rocks exposed in the Papua New Guinea interior highlands. Chemical evidence further indicates that fine-grained terrigenous sediment reached the Woodlark Basin throughout its entire late Miocene-Holocene history. Distinctive high-K volcanogenic muds rich in tephra and volcanic ash layers that appear at <2.3 Ma (Sites 1109 and 1115) are indicative of high-K calc-alkaline volcanic centers, possibly located in the Dawson Strait, Moresby Strait, or Dobu Seamount area. Chemical diagenesis of fine-grained sediments within the Woodlark Basin is reflected in clay neomorphism and localized formation of minerals including dolomite, ankerite, and zeolite but has had little effect on the bulk chemical composition of most samples.

Clay mineral assemblages for the last 10 Ma off northeastern Australia

Clay mineral assemblages for the last 10 m.y. are described for Site 823, at 16°S in the Queensland Trough, to the northeast of Australia. Largely unaffected by diagenetic influences, these mostly express the evolution of northeastern Australian continental environments during the late Neogene: (1) beginning during the late Miocene at about 7.0 Ma is an increase of illite derived from rocky substrates at the expense of smectite from deeply weathered soils; this increase was the result of increasing aridity in the Australian interior and globally cooler temperatures, associated with increases in Antarctic glaciation; (2) concomitant and further increases of kaolinite fluxes to the Queensland Trough during the late Miocene-early Pliocene largely reflect an increase in rainfall in northeastern Australia; (3) increases in both soil- and rock-derived minerals probably intensified as a result of late Neogene uplift of the eastern highlands; (4) clay-mineral associations during the Pliocene and Pleistocene display minor variations only and probably resulted in part from differential settling and sea-level changes; (5) similar trends of clay-mineral variations occur at both ODP Site 823 and DSDP Site 588 (Lord Howe Rise). Less abundant kaolinite relative to illite at Site 588 nevertheless suggests a southward decrease of continental humidity and/or of the eastern highlands uplift; (6) influences of global climate and oceanic and atmospheric circulations on clay-mineral associations dominated during the late Miocene and were progressively replaced by influences of more regional environmental variations during the Pliocene and especially the Pleistocene.

(Supplement 3) Radar sounding observations including bedrock and surface elevation and ice thickness in the ASB region, Antarctica

The first Cenozoic ice sheets initiated in Antarctica from the Gamburtsev Subglacial Mountains and other highlands as a result of rapid global cooling ~34 million years ago. In the subsequent 20 million years, at a time of declining atmospheric carbon dioxide concentrations and an evolving Antarctic circumpolar current, sedimentary sequence interpretation and numerical modelling suggest that cyclical periods of ice-sheet expansion to the continental margin, followed by retreat to the subglacial highlands, occurred up to thirty times. These fluctuations were paced by orbital changes and were a major influence on global sea levels. Ice-sheet models show that the nature of such oscillations is critically dependent on the pattern and extent of Antarctic topographic lowlands. Here we show that the basal topography of the Aurora Subglacial Basin of East Antarctica, at present overlain by 2-4.5 km of ice, is characterized by a series of well-defined topographic channels within a mountain block landscape. The identification of this fjord landscape, based on new data from ice-penetrating radar, provides an improved under¬standing of the topography of the Aurora Subglacial Basin and its surroundings, and reveals a complex surface sculpted by a succession of ice-sheet configurations substantially different from today's. At different stages during its fluctuations, the edge of the East Antarctic Ice Sheet lay pinned along the margins of the Aurora Subglacial Basin, the upland boundaries of which are currently above sea level and the deepest parts of which are more than 1 km below sea level. Although the timing of the channel incision remains uncertain, our results suggest that the fjord landscape was carved by at least two ice- flow regimes of different scales and directions, each of which would have over-deepened existing topographic depressions, reversing valley floor slopes.

Modelo de integración del conocimiento-acción a través del Proyecto de Comunicación para el Desarrollo: 25 años de experiencia en comunidades indígenas andinas en Ecuador

El desarrollo como política de las naciones marca el período de la postguerra, que en América Latina se concreta en múltiples programas de Desarrollo Rural. El modelo inicial de crecimiento económico se va enriqueciendo con visiones centradas en el ser humano y sus múltiples concepciones de desarrollo. En este entender el desarrollo desde la diversidad cultural y antropológica de los pueblos de América Latina, surge la comunicación radiofónica como camino común para la persuasión, socialización y apropiación colectiva de conocimientos y ámbito participativo para consensuar objetivos y acordar actividades. El activismo de los años setenta y ochenta produjo un número considerable de experiencias. La mayoría de ellas han llegado hasta nuestros días, pero el giro tomado por las sociedades digitalizadas y las prioridades medioambientales han dado un nuevo rostro a aquellas primeras experiencias centradas en el desarrollo rural endógeno. Este estudio investiga el complejo práctico-teórico que integra comunicación y desarrollo en contextos territoriales interculturales con población marginal y aplicación de políticas de desarrollo rural. En el capítulo I se recogen las modalidades de cómo se ha aplicado la comunicación en programas de desarrollo, para profundizar en el concepto de comunicación para el desarrollo, conocer sus actores y resultados, y concluir que el desarrollo “con rostro humano” se hace con personas no con políticas oficiales. El capítulo II presenta a los Pueblos Indígenas de la Sierra Ecuatoriana como actores de su proceso de desarrollo hacia el Sumak Kawsay. Los temas tratados en este capítulo muestran los valores y capacidades de las comunidades indígenas de la Sierra Ecuatoriana para la autogestión de su desarrollo, y deja constancia y denuncia de la lectura negativa que se ha venido haciendo de su cosmovisión. Se encuentra respuesta conceptual y metodológica en el Workng With People para optimizar aportes culturales de los Pueblos Indígenas al proceso comunicacional y participativo para mejorar las condiciones de vida y lograr mayores espacios de autonomía y libertad El conocimiento que explica la realidad sin cambiarla no tiene sentido para los pobres. La realidad requiere ser comprendida para construir el conocimiento que la explique y la cambie: ese es el aporte del modelo conocimiento/acción que se presenta en el capítulo III. En este capítulo se exponen metodologías abiertas a la creatividad y flexibles que responden a los principios del modelo conocimiento/acción. La comunicación para el desarrollo se abre a todas ellas como ágora pluricultural que requiere un lenguaje común que se construye desde el aprendizaje social. Los conceptos expuestos en el capítulo III se vinculan en una propuesta metodológica que integra el conocimiento y la acción con los principios del Working With People, propuesta que se expone en el capítulo IV. El modelo del Proyecto de Comunicación para el Desarrollo junta en un modelo de comunicación popular y prácticas liberadoras con métodos cognitivos de la realidad para planificar el cambio desde la población y con la población. Finalmente, el capítulo V recoge la experiencia de la Casa Campesina Cayambe ejecutora del Proyecto de Comunicación para el Desarrollo en la adaptación ejecutada con Radio Mensaje. La riqueza de la experiencia tiende a escaparse de los límites conceptuales y los esquemas dejan espacios de vida ignotos; pero los conceptos y esquemas constituyen el camino para que la experiencia pase a ser objeto conocido y conocimiento socializado. El Proyecto de Comunicación para el Desarrollo es resultado de un proceso de desarrollo construido desde la acción de la Casa Campesina Cayambe durante 25 años en Cayambe. En el capítulo V se describe el contexto del territorio de Cayambe, la identidad de la Casa Campesina Cayambe y de Radio Mensaje, y termina describiendo los logros de 25 años trabajando con la gente. El estudio concluye que la comunicación participativa, como ámbito de aprendizaje social aplicado en procesos de desarrollo rural, integra el conocimiento/acción e incorpora nuevos conocimientos en la población con los que se desarrollan competencias locales para planificar el desarrollo endógeno con flexibilidad y de abajo-arriba. La Figura 0-1 grafica los elementos bases sobre los que se construye el proceso de desarrollo. ABSTRACT Development as a policy of nations marks the postwar period which created several Rural Development Programs in Latin America. The initial model of economic growth was enriched with approaches focused on human beings and their multiple conceptions of development. In this regard, the development from cultural and anthropological diversity in Latin America, radio communication emerges as a common means for persuasion, socialization and collective appropriation of knowledge and scope for participation in order to agree on objectives and activities. Activism of the seventies and eighties generated a considerable number of experiences, most of which are present today. However, a turn taken by digitalized societies and environmental priorities has given those first experiences which focused on endogenous rural development a new face. This study researches the theoretical-practical status that integrates communication and development in intercultural contexts with marginal population and the use of rural development policies. Chapter one shows the modalities of how communication in development programs have been applied to deepen the concept of communication for development, to know those who are involved and its findings, and conclude that development “with a human face” is done with people not with official policies. Chapter two presents Indigenous communities in the Ecuadorian highlands, as people involved in their development process towards Sumak Kawsay. The topics in this chapter show the values and capacities indigenous communities in the Ecuadorian highlands have to self-manage their development, and proves, as well as denounces, that their cosmovision has been negatively perceived. A conceptual and methodological response is found in Working With People in order to optimize cultural contributions of Indigenous People to the communicational and participative process to improve life conditions and have greater spaces of autonomy and freedom. Knowledge which explains reality without changing it does not make any sense for the poor. Reality need to be understood in order to build the knowledge that will explain it and change it: that is the contribution of the knowledge/action model presented in chapter three. This chapter presents open methodologies to creativity which are flexible to respond to the principles of the knowledge/action model. Communication for development is open to all of them as pluricultural agora which requires a common language that is built from social learning. The concepts presented in chapter three are linked in a methodological proposal which integrates knowledge and action with principles of Working With People, proposal which is presented chapter four. The model of the Communication for Development Project includes popular communication elements and liberating practices with cognitive methods of reality to plan change from the population and with the population. Finally, chapter five presents the experiences from the Cayambe Country House, which conducted the Communication for Development Project in the adaptation implemented with Radio Mensaje. The wealth of experience tends to scape from the conceptual limits and the schemes leave gaps of unexplored life; but the concepts and schemes constitute the way so that experience becomes a known object and socialized knowledge. The Communication for Development Project is the result of a development process built from the actions of the Cayambe Country House during 25 years in Cayambe. Chapter five describes the context of Cayambe, the identity of the Cayambe Country House and Radio Mensaje, and the achievements after 25 years of working with its people. The study concludes that participatory communication, as an area of social learning applied to rural development processes, integrates knowledge/action and incorporates new knowledge in communities to develop local competencies to plan endogenous development with flexibility and from the bottom – up.

Adults'Education and Agricultural Innovation: A Social Learning Approach

Social learning processes can be the basis of a method of agricultural innovation that involves expert and empirical knowledge. In this sense, the objective of this study was to determine the effectiveness and sustainability of an innovation process, understood as social learning, in a group of small farmers in the southern highlands of Peru. Innovative proposals and its permanence three years after the process finished were evaluated. It was observed that innovation processes generated are maintained over time; however, new innovations are not subsequently generated. We conclude that adult learning processes and innovation based on social learning are more effective and sustainable; however, the farmers internalization in innovation processes is given longer term.