Determinants of malnutrition in two states in Sudan

Nearly one in three children in the developing world is malnourished. Poor nutrition contributes to one out of two deaths (53%) associated with infectious diseases among children aged under five in developing countries. Using data from the 2005 World Food Program’s (WFP) Livelihood Vulnerability and Nutritional Assessment of Rural Kassala and Red Sea State this study examines the impact of female headed households and maternal education on malnutrition in children 6-59 months old. The dependent variable investigated in this study is moderate to severe wasting or less than -2 weight for height Z-score, also known as global acute malnutrition (GAM). ^ The study population consisted of 450 households in Kassala State and Red Sea State, Sudan. A total of 900 children 6-59 months of age were part of the households sampled from these states and one child per household (773 children) was randomly chosen for the analysis along with the child’s mother. Results of the study found that 18 percent of children between 6-59 months of age had GAM/wasting. Maternal education, main source of water, and income were strongly related to wasting. Gender of head of household was not found to have a significant relationship with GAM/wasting. Mothers with at least primary education were much less likely to have malnourished children, even after controlling for income and environmental conditions. Children in households with unsafe sources of water were 2.6 more likely to have wasting than those with piped in/tube wells as their main source of water. For every increase of 100 dinar in a household, the children in the household are approximately two-thirds times (.662) less likely to be wasted. ^ The results of this study support the alternate hypothesis that there is an association between maternal education on wasting of children 6-59 months old. The results do not, however, support the alternate hypothesis that there is an association between gender of head of household on wasting of children 6-59 months old. Better understanding of the association of wasting and other measures of malnutrition with maternal education levels can program managers and other health officials to target important nutritional and non-nutritional interventions. ^

Geochemical investigations of elements in sediment core CRP-1 from the Ross Sea, Antarctica

Geochemical data are presented for samples from strata, mainly of Miocene age, in the Cape Roberts-1 core (western McMurdo Sound, Antarctica) to assess the sediment provenance. Bulk (major and trace element) chemistry together with bulk mineralogy of fine-grained sandstones, siltstones, mudstones, and diamictites indicate that chemical alteration of source materials, fractionation due to sedimentary sorting, and diagenetic effects were not significant in the Cape Roberts sediment history. Relevant geochemical parameters are consistent with the Cape Roberts sediments being derived mainly from the crystalline basement and the Beacon Supergroup. On the basis of element distributions, an additional contribution from the Ferrar Dolerite and, mainly above about 60 m, influxes of detritus derived from basanitic to intermediate members of the McMurdo Volcanic Group are recognised.

Geochemistry of minerals in CRP sediment cores from the Ross Sea, Antarctica

Sixty-four volcanic chists, sandstones and tephras between 5.95 and 618.19 meters below sea floor (mbsf) in the Cape Roberts Project cores 2 and 2A cores (CRP-2/2A) were examined for Cenozoic and Mesozoic volcanic components, using optical and Scanning Electron Microscopy. Minerals and glass shards in a selection of samples were analysed by electron microprobe fined with an EDAX detector. Laser-Ablation ICP-Mass-Spectrometry (ICP-MS) was used to determine rare earth elements and 14 additional trace elements in glass shards, pyroxenes and feldspars in order to pin-point the onset of McMurdo Volcanic Group (MVG) activity in the stratigraphic column. Pumices in tephra layers of peralkaline phonolite composition in Unit 7.2 -between 108 and 114 mbsf - were also analysed for trace elements by ICP-MS. This tephra unit is not reworked and its isotopic age (21.44 ± 0.05 Ma) is the age of deposition. The height of the eruptive column responsible for the deposition of the tephra was probably less than 8 km; the source was local, probably within 30 km from the drill site. Phonolite of unit 7.2 of CRP-2/2A has no direct petrogenetic relation with the peralkaline trachyte in the tephra-enriched layer of CRP-1 at 116.55 mbsf. Volcanic clasts and sand grains (glass shards, aegirine-augite, anorthoclase) related to Cenozoic activity of MVG were observed only starting from Unit 9.8, where they are dated at 24.22 ± 0.06 Ma at c. 280 mbsf. In this unit the lowest- occurring basaltic glass shard is found at 297.54 mbsf. Sampled McMurdo volcanics are generally vesicular and vary in composition from alkali basalt to trachyte and peralkaline phonolite. By contrast, below 320 mbsf, aphyric or slightly-porphyritic volcanic clasts become more abundant but they are all non-vesiculated, pigeconite and ilmenite-bearing basalts and dolerite of tholeiitic affinity. These rocks are considered to be related to lava flows and associated intrusions of Jurassic age (Kirkpatrick basalts and Ferrar dolerite). As in CRP-1, McMurdo volcanics appear to derive from a variety of lithologics. Besides glaciers, a dominant role of wind transportation from exposed volcanic rocks may be inferred from the contemporary occurrence of glass shards of different compositions at depths above 297.54 mbsf. These data confirm that the onset of magmatic activity in southern Victoria Land is considerably delayed (by about 24 Ma) with respect to northern Victoria Land.