El Estado y la política de 'Castigo al Campo' durante los gobiernos peronistas : El caso del impuesto al latifundio en la Provincia de Buenos Aires

Fil: Lázzaro, Silvia Beatriz. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

El Estado y la política de 'Castigo al Campo' durante los gobiernos peronistas : El caso del impuesto al latifundio en la Provincia de Buenos Aires

Fil: Lázzaro, Silvia Beatriz. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Amino acid in Deep Sea Drilling Project cores

Several amino acid diagenetic reactions, which take place in the deep-sea sedimentary environment, were investigated, using various Deep Sea Drilling Project (DSDP) cores. Initially it was found that essentially all the amino acids in sediments are bound in peptide linkages; but, with increasing age, the peptide bonds undergo slow hydrolysis that results in an increasingly larger fraction of amino acids in the free state. The hydrolysis half-life in calcareous sediments was estimated to be ~1-2 million years, while in non-carbonate sediment the hydrolysis rate may be considerably slower. The amino acid compositions and the extent of racemization of several amino acids were determined in various fractions isolated from the sediments. These analyses demonstrated that the mechanism, kinetics, and rate of amino acid diagenesis are highly dependent upon the physical state (i.e., free, bound, etc.) in which the amino acids exist in the sedimentary environment. In the free state, serine and threonine were found to decompose primarily by a dehydration reaction, while in the bound state (residue or HCl-insoluble fraction) a reversible aldol-cleavage reaction is the main decomposition pathway of these amino acids. The change in amino acid composition of the residue fraction with time was suggested to be due to the hydrolysis of peptide bonds, while in foraminiferal tests the compositional changes over geological time are the result of various decomposition reactions. Reversible first-order racemization kinetics are not observed for free amino acids in sediments. The explanation for these anomalous kinetics involves a complex reaction series which includes the hydrolysis of peptide bonds and the very rapid racemization of free amino acids. The racemization rates of free amino acids in sediments were found to be many orders of magnitude faster than those predicted from elevated temperature experiments using free amino acids in aqueous solution. The racemization rate enhancement of free amino acids in sediments may be due to the catalysis of the reaction by trace metals. Reversible first-order kinetics are followed for amino acids in the residue fraction isolated from sediments; the rate of racemization in this fraction is slower than that predicted for protein-bound amino acids. Various applications of amino acid diagenetic reactions are discussed. Racemization and the decomposition reaction of serine and threonine can both be used, with certain limitations, to make rough age estimates of deep-sea sediments back to several million years. The extent of racemization in foraminiferal tests which have been dated by some other independent technique can be used to estimate geothermal gradients, and thus heat flows, and to evaluate the bottom water temperature history in certain oceanic areas.

(Table 5) Quaternary paleoproductivity of organic carbon in oceans based on DSDP cores

By analogy with the present-day ocean, primary productivity of paleoceans can be reconstructed using calculations based on content of organic carbon in sediments and their accumulation rates. Results of calculations based on published data show that primary productivity of organic carbon, mass of phosphorus involved in the process, and content of phosphorus in ocean waters were relatively stable during Cenozoic and Late Mesozoic. Prior to precipitation on the seafloor together with biogenic detritus, dissolved phosphorus could repeatedly be involved in the biogeochemical cycle. Therefore, only less than 0.1% of phosphorus is retained in bottom sediments. Bulk phosphorus accumulation rate in ocean sediments is partly consistent with calculated primary productivity. Some epochs of phosphate accumulation also coincide with maxima of primary productivity and minima of the fossilization coefficient of organic carbon. The latter fact can testify to episodes of acceleration of organic matter mineralization and release of phosphorus from sediments leading to increase in the phosphorus reserve in paleoceans and phosphate accumulation in some places.

(Table 1) Average aluminium accumulation rate at 40 DSDP Sites for the time interval 0-10 Ma and relative rates for other time intervals

A six-fold increase in the rate of accumulation of Al in north and central Atlantic and Pacific Ocean sediments indicates vastly increased denudation of the continents during the past 15 Ma. The increase is more apparent in hemipelagic than pelagic sites, demonstrating widely distributed local controls. Similarities in the rate of increase in the Atlantic and Pacific show that tectonic elevation is not responsible for the difference in sedimentation rate. Also, similarities in the difference at sites of low and high latitude suggest that glaciation is not the most significant source. A lack of correspondence between sedimentation rates and Vail's sea-level curve similarly rule out that effect. The conclusion drawn here is that worldwide climatic deterioration during the late Tertiary is the explanation for the striking increase in detrital sedimentation in the World ocean.

Location, intervals and thickness of Cretaceous sections in Indian Ocean DSDP and ODP sites (Table 2)

The Indian Ocean covers approximately 73.5 * 10**6 km**3 from 25°N to 67°S and from 20° to 120°E. Several legs of the Deep Sea Drilling Project (DSDP) and the Ocean Drilling Program (ODP) have operated in its waters, many penetrating the Cretaceous. Most of the scientific drill sites are DSDP related and thus pre-dated modern biostratigraphic conventions. Foraminifers and calcareous nannoplankton were by far the dominant fossil groups studied in the earlier work, supplemented occasionally by studies of other fossil groups, The results of the Ocean Drilling Project phase are yet too young to be fully integrated but have been based on a broader range of techniques and fossil groups. During most of the Cretaceous, the proto-Indian Ocean basin lay in middle to high latitudes. Thus, it is unrealistic to expect successful routine application of low-latitude zonations. No planktonic foraminifer zonal scheme has been developed for the Indian Ocean basin for several reasons. There are no sections with complete or even significant partial sections to allow development of such a zonation. Carbonate compensation depth (CCD) effects have been marked in most sections, and significant intervals are devoid of planktonic foraminifers. The Indian Ocean now covers a great latitudinal range from tropics to polar regions and, at first glance, no scheme can be expected to be applicable over that entire range. In the Cretaceous the area was much smaller, though expanding progressively, and the paleolatitude range was quite small. Calcareous nannoplankton have proved valuable in dating Indian Ocean Cretaceous sediments and have, perhaps in contrast with the foraminifers, been consistently a more reliable means of applying zonal schemes developed elsewhere. For the Albian-Aptian, zonations based on well-known benthic foraminifer lineages (Scheibnerova, 1974) have been useful when nothing else was available or effective. Palynology has been used little, but where used, has proved excellent. It has the added value of providing valuable information on nearby terrestrial vegetation as the fossils were resistant to dissolution. Normally, when different fossil groups have been applied to a section, the results have been compatible or compatible to an acceptable degree. There are a few instances where incompatibility is noteworthy, and Site 263 is a classic example, as even two calcareous nannoplankton studies show irreconcilable differences here. All groups gave different results, but one benthic foraminifer analysis agreed with one calcareous nannoplankton study.

Nanotechnology in the food industry I: applications

Nanotechnology is a multidisciplinary science that is having a boom today, providing new products with attractive physicochemical properties for many applications. In agri/feed/food sector, nanotechnology offers great opportunities for obtaining products and innovative applications for agriculture and livestock, water treatment and the production, processing, storage and packaging of food. To this end, a wide variety of nanomaterials, ranging from metals and inorganic metal oxides to organic nanomaterials carrying bioactive ingredients are applied. This review shows an overview of current and future applications of nanotechnology in the food industry. Food additives and materials in contact with food are now the main applications, while it is expected that in the future are in the field of nano-encapsulated and nanocomposites in applications as novel foods, additives, biocides, pesticides and materials food contact.

A Vertente Cirúrgica de uma Unidade de Cuidados Intensivos Neonatais – 25 Anos de Experiência

Introdução e objectivos: O Hospital de Dona Estefânia é um hospital pediátrico com Área de Cirurgia Pediátrica e uma Maternidade da Apoio Perinatal Diferenciado. O objectivo deste estudo prospectivo histórico é analisar a população de recém-nascidos (RN) admitidos na Unidade de Cuidados Intensivos Neonatais (UCIN) submetidos a intervenção cirúrgicanum período de 25 anos. Métodos e doentes: Os dados foram obtidos de estudos de casuística e do ficheiro electrónico da UCIN. Foi realizada pesquisa individual pelo código de intervenção cirúrgica e pelo código de cada uma das condições cirúrgicas. Todos os RN submetidos a intervenção cirúrgica foram englobados. Cada doente foi contabilizado apenas uma vez mas as anomalias cirúrgicas major foram contabilizadas uma a uma. As taxas de letalidade são brutas, englobando-se no denominador todos os RN com a mesma anomalia, operados. Resultados: Neste período foram admitidos na UCIN 5937 RN dos quais 1140 (19.2%) foram operados. A mediana do tempo de internamento foi 30 dias. O número de RN submetidos a intervenção cirúrgica subiu de 2% dos admitidos em 1983 para 29.4% em 2007. Vinte e seis por cento do total de operados nasceram na maternidade do hospital. A patologia gastrointestinal foi a mais frequente tanto no grupo da patologia congénita como no grupo da adquirida; a patologia torácica/pulmonar ocupou o 2º lugar no grupo da patologia congénita, constituindo a hérnia diafragmática congénita a situação mais frequente. Na alta, 35% dos doentes (n=404) foram enviados para o domicílio, 51% (n=581) foram transferidos para outro serviço e 14% faleceram (n=155). A mortalidade diminuiu de 22% nos primeiros 10 anos para menos de 10% nos últimos 10 anos e 5% nos últimos 5. A mortalidade da atrésia do esófago baixou de 22% nos primeiros 15 anos para 3,8% nos últimos 5 e a da hérnia diafragmática de Bochdalek de 34% nos primeiros 15 anos para 28% nos últimos 10. Conclusões: A concentração de patologia cirúrgica neonatal num centro de referência melhora a experiência das equipas multidisciplinares podendo contribuir para um melhor prognóstico de doentes com patologia grave.

Cephalopoda as prey of juvenile Southern elephant seals at Isla 25 de Mayo/King George, South Shetland Islands

The aim of the present study was to enhance the knowledge of the feeding habits of the juvenile component of the population of Southern elephant seals [Mirounga leonina (Linnaeus, 1758)] from Isla 25 de Mayo, South Shetland Islands, age class whose diet information is scarce. A total of 60 individuals were stomach lavaged in the spring - summer seasons of three consecutive years (2003, 2004 and 2005) of which 53.3 % (n = 32) presented food remnants. The Antarctic glacial squid Psychroteuthis glacialis Thiele, 1921 was the dominant prey taxon in terms of frequency of occurrence (68.7%), numerical abundance (60.1%) and biomass (51.5%), contributing 84.1% to the total relative importance index. Other squid prey species of importance were Slosarczykovia circumantartica Lipinski, 2001 in terms of occurrence (37.5%) and numerical abundance (14%) and Moroteuthis knipovitchi Filippova, 1972 in terms of biomass (16%). All identified cephalopod prey taxa are distributed south of the Antarctic Polar Front, except for the squid Martialia hyadesi Rochebrune & Mabille, 1889 which has a circumpolar distribution associated to the Polar Frontal Zone. No significant differences in the sizes of P. glacialis preyed upon by elephant seals were found between sexes and years. However, significant interannual differences were found in the taxonomical composition of their diet. This would be associated with temporal changes in food availability at the foraging areas of seals, which in turn may have been influenced by changes in oceanographic conditions as a result of the El Niño Southern Oscillation (ENSO) phenomenon that occurred during part of the study period. Furthermore, a differential response of males and females to this temporal variation was observed, with the former being also associated to a predation on octopods. This would suggest a sexual segregation in foraging habits of this species from the early stages of its life cycle.

Abscesso pulmonar de aspiração : dados diagnósticos e resultados terapêuticos em 241 casos

O abscesso de pulmão continua sendo hoje, em plena era dos antibióticos, um importante problema médico. O presente trabalho se propõe mostrar aspectos diagnósticos e terapêuticos da doença em uma série de pacientes coletada nos últimos 34 anos em um hospital universitário especializado em doenças pulmonares. No período de 1968 a 2002 foram reunidos e estudados 241 casos de abscesso pulmonar de aspiração - 199 em homens e 42 em mulheres, com média de idade de 41,3 anos. Em 69,0% dos pacientes esteve presente a ingestão de álcool e em 64,0% o hábito tabágico. Tosse, expectoração, febre e comprometimento do estado geral foram os achados clínicos mais freqüentes, encontrados na quase totalidade dos casos; 62,5% tinham dor torácica e 30,0% hipocratismo digital. Verificaram-se dentes em mau estado de conservação em 81,7 % dos pacientes, episódio de perda de consciência em 78,0% e presença de odor fétido em 66,0%. Em 85,5% das vezes as lesões localizaram-se em segmento posterior de lobo superior ou segmento superior de lobo inferior, 97,1% delas unilaterais, ocorrendo com igual freqüência tanto no pulmão direito como no esquerdo. A maioria das lesões (66,0%) mediram entre 4,0 e 8,0 cm de diâmetro. Em 25 pacientes (10,4%) houve a associação de empiema pleural. Flora mista, indicativa da presença de germes anaeróbios, foi identificada em secreções broncopulmonares ou pleurais em 172 pacientes (71,4 %). Estreptococos e Gram negativos aeróbios foram também algumas vezes encontrados. Todos os pacientes foram inicialmente tratados com antibióticos (penicilina em 78,0% das vezes) e submetidos a sessões de drenagem postural. Em 51 (21,2%) acabou sendo necessário algum procedimento cirúrgico (24 drenagens de empiema, 21 ressecções pulmonares e 6 pneumostomias). Cura foi obtida em 231 pacientes (95,8%) e 10 (4,2%) foram ao óbito, estes em geral com grandes abscessos, três dos quais também com empiema.