Percent cropland coverage for sub-Saharan Africa

The dataset contains a cropland percent coverage map for Africa created through the combination of five existing land cover products: GLC-2000, MODIS Land Cover, GlobCover, MODIS Crop Likelihood and AfriCover. A synergy map was created in which the products are ranked by experts, which reflects the likelihood or probability that a given pixel is cropland. The cropland map was calibrated with national and sub-national crop statistics using a novel approach. Preliminary validation of the map was undertaken. The resulting cropland map has an accuracy of 83%, which is higher than the accuracy of any of the individual maps. The cropland percent coverage map for Africa is available for overlay on Google Earth or for download at http://agriculture.geo-wiki.org.

Sustentabilidad sub-nacional

La finalidad del presente trabajo es realizar un análisis que complementa y actualiza el estudio realizado en el año 2011 por Molina, Correa y Morabito. En dicho estudio se mostró la situación de la deuda pública de Mendoza (fundamentalmente del nivel y composición de la misma), así como los esfuerzos fiscales que se necesitaban realizar para que la misma sea sustentable en el tiempo. A partir del análisis de la deuda pública consolidada (analizada en su nivel, composición y relación con la tasa de interés) y su vinculación con los resultados financieros de la provincia, se pretende opinar sobre las perspectivas de solvencia a mediano y largo plazo, así como determinar, en su caso, los esfuerzos fiscales necesarios para retomar la senda de la sustentabilidad, sin necesidad de producir cambios bruscos en la cuentas fiscales, que afecten a la población en general y a los contribuyentes en particular. Para tal fin se utilizarán distintos métodos y modelos que acompañen el análisis de las finanzas de las provincias en general.

Estudio preliminar de los efectos letales y sub-letales de extractos etanólicos de cuatro especies xerófitas del altiplano chileno contra Tetranychus cinnabarinus (Acarina: Tetranychidae)

Se evaluaron los efectos letales y subletales de extractos etanólicos de cuatro plantas originarias de la zona alto andina del desierto chileno (Baccharis tola Phil., Fabiana densa J. Remy, Lampayo medicinalis F. Phil. y Azorella compacta Phil.) sobre adultos y huevos de Tetranychus cinnabarinus (Boisduval) (Acari: Tetranychidae), en condiciones de laboratorio (26 ± 2°C, 70 ± 10% HR y fotoperíodo de 16:8 luz: oscuridad). Los mayores niveles de mortalidad por contacto directo sobre adultos fueron obtenidos por A. compacta al 10% (p/v), L. medicinalis 10% (p/v) y A. compacta 7,5% (p/v), los cuales no presentaron diferencias significativas (p<0,05) con respecto al tratamiento control (spirodiclofen). Las CL50 más bajas fueron obtenida por F. densa con 0,71% (p/v) y L. medicinalis con 0,98% (p/v). A. compacta presentó la CL90 más baja con 5,10% (p/v) y la mayor eficacia por obtener un coeficiente de 3,21 (CL90/CL50). Lampayo medicinalis al 10% (p/v) presentó el mayor porcentaje de huevos no eclosionados con un 73,15%. Baccharis tola al 7% (p/v) expuso la mayor toxicidad por efecto residual con una mortalidad de 57,8% sobre adultos de T. cinnabarinus. Fabiana densa mantuvo efecto repelente hasta las 72 horas. Lampayo medicinalis, B. tola y A. compacta perdieron levemente su actividad repelente en el tiempo.

Feldspar Pb-isotope ratios for earliest Pleistocene sediments of the sub-polar North Atlantic Ocean

Relatively little is known in detail about the locations of the early Pleistocene ice-sheets responsible for ice-rafted debris (IRD) inputs to the sub-polar North Atlantic Ocean during intensification of northern hemisphere glaciation (iNHG). To shed new light on this problem, we present the first combined in-depth analysis of IRD flux and geochemical provenance of individual sand-sized IRD deposited in the sub-polar North Atlantic Ocean during the earliest large amplitude Pleistocene glacial, marine isotope stage (MIS) 100 (~2.52 Ma), arguably the key glacial during iNHG. IRD provenance is assessed using laser ablation lead (Pb) isotope analyses of single feldspar grains. We find that the Pb-isotope composition (206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb) of individual ice-rafted (>150 µm) feldspars deposited at DSDP Site 611A, ODP Site 981 and IODP Site U1308 during MIS 100 records a shift from predominantly Archaean-aged circum-North Atlantic Ocean continental sources during early glacial ice-rafting events to dominantly Palaeozoic and Proterozoic-aged sources during full glacial conditions. The distribution of feldspars in Pb-Pb space for full glacial MIS 100 more closely resembles that documented for feldspars deposited at the centre of the last glacial IRD belt (at IODP/DSDP Site U1308/609) during ambient (non-Heinrich-event) ice-rafting episodes of MIS 2 (~23.8 ka) than that documented for MIS 5d (~106 ka). Comparison of our early Pleistocene and last glacial cycle datasets suggests that MIS 100 was characterised by abundant iceberg calving from large ice-sheets on multiple continents in the high northern latitudes (not just on Greenland).

Late Miocene-early Pliocene stable isotope record of benthic foraminifera from ODP Site 177-1088 in the sub-Antarctic South Atlantic

Benthic foraminiferal stable isotope records for the past 11 Myr from a recently drilled site in the sub-Antarctic South Atlantic (Site 1088, Ocean Drilling Program Leg 177, 41°S, 15°E, 2082 m water depth) provide, for the first time, a continuous long-term perspective on deep water distribution patterns and Southern Ocean climate change from the late Miocene through the early Pliocene. I have compiled published late Miocene through Pliocene stable isotope records to place the new South Atlantic record in a global framework. Carbon isotope gradients between the North Atlantic, South Atlantic, and Pacific indicate that a nutrient-depleted watermass, probably of North Atlantic origin, reached the sub-Antarctic South Atlantic after 6.6 Ma. By 6.0 Ma the relative proportion of the northern-provenance watermass was similar to today and by the early Pliocene it had increased to greater than the modern proportion suggesting that thermohaline overturn in the Atlantic was relatively strong prior to the early Pliocene interval of inferred climatic warmth. Site 1088 oxygen isotope values display a two-step increase between ~7.4 Ma and 6.9 Ma, a trend that parallels a published delta18O record of a site on the Atlantic coast of Morocco. This is perhaps best explained by a gradual cooling of watermasses that were sinking in the Southern Ocean. I speculate that relatively strong thermohaline overturn at rates comparable to the present day interglacial interval during the latest Miocene may have provided the initial conditions for early Pliocene climatic warmth. The impact of an emerging Central American Seaway on Atlantic-Pacific Ocean upper water exchange may have been felt in the North Atlantic beginning in the latest Miocene between 6.6 and 6.0 Ma, which would be ~1.5 Myr earlier than previously thought.