This detailed descriptive study used a multi-disciplinary approach bridging anthropology and entomology. A multiple case study design included research in six study areas, defined as blocks. The water supply is irregular in households from both under-privileged and privileged blocks. In under-privileged households where the water supply is irregular, the frequent use of water containers such as water tanks, cisterns, barrels and pots, creates environmental conditions with a greater number of breeding areas of Aedes aegypti. In the more privileged blocks, some households choose to avoid irregularity of water supply by having their own well and pump systems.

New explorations in the desert of northeastern Zacatecas, in central-northern Mexico, revealed dozens of archaeological and geoarchaeological sites. One of them, Ojo de Agua, contains the remains of a Pleistocene spring-fed hydrographic system located at the southeastern end of a large elongated endorheic basin. The locality yielded a particularly dark, highly organic stratigraphic layer commonly known in the Americas as Black Mat (BM), exposed on the natural profiles of a creek, but not associated with cultural materials. Several radiocarbon assessments confirmed the formation of the Ojo de Agua Black Mat during the Younger Dryas chronozone, with ten calibrated results clustering between 12,700–12,100 cal BP. This multi-proxy study confirmed the peculiarity of the deposit and found similarities and differences with other contexts of Younger Dryas age. The Ojo de Agua Black Mat (stratum C2) is far richer in charcoal specks than the related strata, but lacks phytoliths, diatoms or ostracods. No further biological remains were found in it, except for intrusive capillary roots. Clearly water-lain in a shallow pond, the stratum qualifies as a clayey silt with an acidic-to-neutral pH. Rich in heavy metals and with high contents of titanium, the Ojo de Agua Black Mat yielded significant indicators of intense wildfires during the Younger Dryas, but produced no carbon spherules or nanodiamonds supposedly linked to the impact theory.

De acuerdo con el Índice Global del Hambre (GHI, por sus siglas en inglés) de 2012, el hambre a nivel mundial ha disminuido algo desde 1990 pero continúa siendo “serio”. El promedio global enmascara diferencias dramáticas entre regiones y países. A nivel regional, los mayores puntajes del GHI se encuentran en Asia meridional y en el África Subsahariana. Asia meridional redujo sus puntajes de GHI de forma significativa entre 1990 y 1996 —principalmente a través de una reducción en la proporción de niños con bajo peso— pero no pudo mantener este rápido progreso. Y aunque el África Subsahariana progresó menos que Asia meridional en la década de 1990, ha logrado reducir la brecha a partir del nuevo milenio, con un puntaje del GHI en 2012 apenas por debajo del obtenido por Asia meridional. | Non-PR | IFPRI2; GRP24 | COM; MTID; DGO; EPTD; PHND; WCAO

Book | COM; MTID; DGO; EPTD; PHND; WCAO | De acuerdo con el Índice Global del Hambre (GHI, por sus siglas en inglés) de 2012, el hambre a nivel mundial ha disminuido algo desde 1990 pero continúa siendo “serio”. El promedio global enmascara diferencias dramáticas entre regiones y países. A nivel regional, los mayores puntajes del GHI se encuentran en Asia meridional y en el África Subsahariana. Asia meridional redujo sus puntajes de GHI de forma significativa entre 1990 y 1996 —principalmente a través de una reducción en la proporción de niños con bajo peso— pero no pudo mantener este rápido progreso. Y aunque el África Subsahariana progresó menos que Asia meridional en la década de 1990, ha logrado reducir la brecha a partir del nuevo milenio, con un puntaje del GHI en 2012 apenas por debajo del obtenido por Asia meridional. | IFPRI2; GRP24 | Non-PR

[EN] In this PhD thesis, we contribute to a more detailed knowledge of the biogeography of coccolithophores in one of the most productive marine ecosystem on earth: the Peru-Chile Current realm, which extends along the west coast of South America. | [ES] En esta tesis se contribuye a un mayor conocimiento de la biogeografía de los Cocolitóforos en uno de los ecosistemas marinos más productivos de nuestro planeta: el sistema de corrientes de Perú- Chile, que se extiende a lo largo de la costa oeste de Suramérica.

Surveys for freshwater sponges were performed at several water bodies at sandy environments along a north-south direction of particularly the Brazilian coastal line. The results allowed for the distinction of four different species-specific environments along this coastal border. The main fact considered was the dominant or the sole recurrent occurrence of a single sponge species at one particular habitat. The first one is that of the lagoonal mesohaline habitats at the tropical and subtropical realms, indicated by Spongilla alba Carter, 1849. The second one refers to shallow ponds among dunes at the tropical area indicated by Corvoheteromeyenia heterosclera (Ezcurra de Drago, 1974). The third one is that of also shallow ponds close to the dune belt at the temperate region indicated by Racekiela sheilae (Volkmer-Ribeiro, De Rosa-Barbosa & Tavares, 1988). The fourth one is that of organically enriched environments, at the marginal areas of lagoons and mouth of small rivers, evolving towards freshwater muddy ponds and coastal swamps, not far from the ocean border: Ephydatia facunda Weltner, 1895 is the species to occupy this habitat with almost exclusiveness. The above species are thus proposed as indicators of such habitats and have their descriptions improved and that of their environments summarized. A taxonomic key based on the spicules of the four species is proposed. The results presented aim to contribute to the identification of spicules of these sponges in sediment columns recovered at the Brazilian and South American coastal area. Determination of paleo ocean borders are a present issue of upmost importance in what respects projections of timing and fluctuations of ascending/regressing sea levels.<br>Levantamentos para detecção de esponjas dulcícolas foram conduzidos em diversos corpos d'água da faixa arenosa costeira, de norte a sul, particularmente no Brasil. Os resultados permitiram a distinção de quatro ambientes específicos em relação à presença de certas espécies, considerando-se como fator determinante a ocorrência recorrente, exclusiva ou preponderante de uma espécie nos tipos de habitats examinados. O primeiro grupo é o de habitats mesohalinos de lagunas, nas faixas tropical e subtropical, indicado por Spongilla alba Carter, 1849. O segundo é constituído por lagoas rasas, entre dunas, situado na faixa tropical, com a presença de Corvoheteromeyenia heterosclera (Ezcurra de Drago, 1974). O terceiro é o de lagoas/banhados, também rasos, vizinhos ao cordão de dunas, na região temperada, com Racekiela sheilae (Volkmer-Ribeiro, De Rosa-Barbosa & Tavares, 1988). O quarto é constituído por ambientes organicamente enriquecidos, nas áreas marginais de lagunas e proximidades de barras de pequenos rios, evoluindo para lagoas e banhados em processos de colmatação, com fundos lodosos, não distantes da borda oceânica, com a presença quase exclusiva de Ephydatia facunda Weltner, 1895. Essas espécies são por isto propostas como indicadoras de tais habitats, promovendo-se a ampliação de suas descrições e a caracterização sintética desses ambientes. É proposta chave para identificação baseada nas espículas dessas esponjas. Os resultados apresentados visam contribuir para a identificação de suas espículas em colunas de sedimentos recuperados em áreas costeiras do Brasil e da América do Sul. As determinações de paleobordas oceânicas integram estudos com alto grau de interesse no que respeita a projeções temporais e flutuações de níveis ascendentes/regressivos dos oceanos.