983 resultados para FL BoG
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Plates 153-325
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La exposición a la luz, al aire, a elevadas temperaturas y el almacenamiento prolongado produce alteraciones nutricionales y organolépticas en alimentos. Las modificaciones nutricionales pueden ser causadas por especies reactivas de oxígeno (ROS), las cuales producen oxidación de proteínas, lípidos, vitaminas, etc. Mientras que las alteraciones organolépticas involucran pérdidas del flavor por la generación de compuesto volátil off-flavor, debido principalmente al desarrollo de microorganismos y a oxidaciones. Compuestos bioactivos (CB) tales como carotenoides (Car) y flavonoides (Fl) cumplen relevantes funciones biológicas, entre las que se pueden destacar la capacidad antioxidante, antimicrobiana y antitumoral, entre otras. El propósito de este proyecto es el estudio de propiedades biológicas en particular capacidad antioxidante y antimicrobiana de CB como Car y Fl microencapsulados en biopolímeros para determinar el efecto de los mismos sobre las alteraciones nutricionales y organolépticas en alimentos durante el almacenamiento. Los CB serán microencapsulados por secado por aspersión spray drying, atrapamiento en liposomas o múltiple emulsificación evaporación de solvente, utilizando goma arábica, lecitina o quitosano como materiales de pared. Se estudiará la capacidad de los compuestos bioactivos y de los materiales de pared para desactivar ROS por espectroscopia de absorción UV-Vis. Se determinará la actividad antimicrobiana de los mismos frente a microorganismos especialmente psicrotrofos, por difusión en discos sobre placa de agar previamente inoculadas, por curvas de crecimiento y por ensayos de viabilidad. Posteriormente se analizarán las alteraciones nutricionales y organolépticas en muestras de leche en condiciones de iluminación y temperatura que simulen las de almacenamiento. Para tal fin, se evaluará la estabilidad de proteínas y vitaminas, por electroforesis capilar, la formación de compuestos volátiles se determinará por cromatografía de gases y el desarrollo de microorganismos por recuento estándar en placa. Finalmente se evaluará el efecto de la adición de carotenoides y flavonoides microencapsulados sobre la degradación de proteínas y vitaminas, la formación de off-flavor y el desarrollo de microorganismos durante el almacenamiento de leche. Con este proyecto se pretende determinar tanto la capacidad antioxidante como antimicrobiana de carotenoides y flavonoides puros y microencapsulados, así como de los biopolímeros usado para la microencapsulación y su potencial aplicación como conservantes en leche en la formulación de productos nutracéuticos.
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FUNDAMENTO: O diabete melito tipo 2 (DM2) é um fator de risco isolado para coronariopatia, principalmente quando associado à microalbuminúria (MA). Alterações estruturais e funcionais das lipoproteínas não são totalmente esclarecidas nesse contexto. OBJETIVO: Avaliar a transferência de lípides para HDL (T) em pacientes DM2 e a associação com a presença da MA e com o tratamento com estatina ou insulina. MÉTODOS: Estudamos 33 pacientes com DM2 e 34 controles pareados para idade. Uma nanoemulsão lipídica artificial radiomarcada com ³H-Triglicéride (TG) e 14C-colesterol livre (CL) ou ³H-colesterol éster (CE) e 14C-fosfolípide (FL) foi incubada com plasma. A nanoemulsão e as lipoproteínas foram precipitadas, exceto a HDL, que teve sua radioatividade contada. RESULTADOS: A TFL (%) foi maior no grupo com DM2 que no grupo-controle (25,2±3,2 e 19,7±3,2 respectivamente; p < 0,001), assim como a TCL (%): 9,1±2,7 e 6,3±1,5 respectivamente; p < 0,001. O diagnóstico de MA não se associou a mudanças da propriedade de transferência. O uso da insulina associou-se à menor TFL (%): 23,5±2,1 contra 26,1±3,3; p = 0,018. Já o uso da estatina associou-se à queda de todas - TCE (%): 3,5±0,9; TFL (%):23,8±2,0; TTG (%): 3,9±0,8; TCL (%):7,4±1,3 - quando comparado ao grupo que não usava estatina (TCE (%):5,9±2,4; TFL (%):26,9±3,6; TTG (%):6,4±2,2; TCL (%):11,1±2,6). CONCLUSÃO: O DM2 aumentou a transferência de lípides de superfície para HDL, enquanto o uso de estatina diminuiu todas as transferências de lípides. A presença de MA não se associou às alterações das transferências de lípides.
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FUNDAMENTO: A ecocardiografia transesofágica (ETE) é um exame semi-invasivo amplamente utilizado e seu uso associado a sedativos poderá influenciar a segurança do procedimento. OBJETIVO: analisar aspectos da segurança da ETE associada ao uso de midazolam (MZ) e flumazenil (FL) e a influência de variáveis clínicas na taxa de eventos. MÉTODO: estudo prospectivo com 137 pacientes que realizaram ETE com MZ associado à sedação moderada. Analisamos as seguintes ocorrências: complicações com anestesia tópica, ao uso do MZ e complicações relacionadas ao procedimento. Análises uni e multivariada foram usadas para testar a influência das variáveis clínicas: idade, sexo, acidente vascular cerebral (AVC), miocardiopatia (MP), duração do exame, insuficiência mitral (IM) e dose de MZ. RESULTADOS: todos pacientes (65±16 anos; 58% masculino) completaram o exame. As doses médias de MZ e FL foram de 4,3±1,9 mg e 0,28±0,2 mg, respectivamente. A duração do exame e a fração de ejeção (FE) média foram de 16.4±6.1 minutos e 60±9%, respectivamente. O evento mais comum foi a hipóxia leve (SO2<90%), em 11 pacientes; 3 pacientes (2%) apresentaram hipóxia transitória por obstrução da via aérea superior na passagem da sonda, enquanto 8 (5,8%) apresentaram hipóxia devido ao uso do MZ. Hipotensão transitória (PAS<90 mmHg) ocorreu em 1 paciente (0,7%). A análise multivariada mostrou que insuficiência mitral (IM) importante, MP (FE<45%) e altas doses do MZ (>5mg) tiveram associação com tais eventos (p<0,001). A FE no grupo com MP foi de 40%, ao passo que, no grupo com insuficiência mitral (IM), esse percentual foi de 44%, podendo ser este um fator associado a eventos clínicos neste último grupo. CONCLUSÃO: ETE com sedação tem baixas taxas de eventos. Não se observou eventos graves e não houve a necessidade de interrupção dos exames.
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This thesis details the findings of a study relating the transfer of 238U, 228Ra (232Th), 226Ra, and 137Cs from soil to vegetation in an Atlantic blanket bog, upland blanket bog and semi-natural grassland situated along the north-west coast of Ireland. The results of this study provide information on the uptake of these radionuclides by the indigenous vegetation found present in these ecosystems. The ecosystems chosen are internationally recognizable ecosystems and provide a wide variety of vegetation species and contrasting soil physiochemical properties which allow the influence of these parameters on radionuclide uptake to be assessed. The levels of radionuclides in the soil and vegetation were measured using gamma spectrometry, alpha spectrometry and ICP-MS. The nutrient status of the vegetation and soil physiochemical properties were measured using atomic absorption, flame photometry and other analytical techniques. The results of the study indicate that the uptake of 238U and 228Ra (232Th) by vegetation from all three ecosystems was negligible as the levels in all vegetation was below the limits of detection for the methods used in this study. These results appear to indicate that the vegetation studied do not possess the ability to accumulate significant levels of these radionuclides however this assumption cannot be upheld in the case of the Atlantic blanket bog as the levels in the soil of this ecosystem were too low for detection. Similar results were obtained for 226Ra uptake in both the Atlantic blanket bog and grassland for all vegetation with the exception of H. lanatus from the grassland ecosystem. Radium-226 uptake in upland blanket bog was higher and was detectable in the majority of vegetation indigenous to this ecosystem. Transfer factor values ranged from 0.07 to 2.35 and the TF values for E. tetralix were significantly higher than all other vegetation studied. This species of heather demonstrated the ability to accumulate 226Ra to a greater extent than all other vegetation. The uptake of 226Ra by upland blanket bog vegetation appears to be significantly influenced by a range of soil physiochemical properties. The nutrient status of the vegetation, in particular the calcium content in the vegetation appears to have a negative impact on the uptake of this radionuclide. Potassium-40 was detectable in all vegetation present in the three ecosystems and the levels in the grassland soil were significantly higher than the levels in both bogland soils. Transfer factor values for Atlantic blanket bog vegetation ranged from 0.9 to 13 .8 and were significantly higher in E. vaginatum in comparison to C. vulgaris. Potassium-40 TF values for upland blanket bog vegetation on average ranged from 1.4 for C. vulgaris (stems) to 5.2 for E. vaginatum and were statistically similar for all species of vegetation. Transfer factor values for grassland vegetation ranged from 0.7 to 3.8 and were also statistically similar for all species of vegetation indicating that the transfer of 40K to vegetation within the upland bog and grassland ecosystem is not dependent on plant species. Comparisons of 40K TF values for all three ecosystems indicate that the uptake in E. vaginatum from the Atlantic blanket bog was statistically higher than all other vegetation studied. This appears to indicate that E. vaginatum has the ability to accumulate 40K, however, this species of vegetation was also present in the upland blanket and did not demonstrate the same behaviour. The uptake of 40K by vegetation from all three ecosystems was significantly affected by a range of soil physiochemical properties and in some cases the results were contradictory in nature possibly indicating that the affect of these parameters on 40K uptake is species dependent. The most obvious trend in the data was the influence of soil CEC and magnesium levels in vegetation on 40K TF values. A positive correlation was apparent between the CEC of the soil and 40K uptake in vegetation from both the Atlantic blanket bog and grassland ecosystem. A similar trend was apparent between magnesium levels in vegetation and 40K TF values for the upland blanket bog and grassland vegetation. Caesium-13 7 levels were found to be significantly higher in the two bogland soils in comparison to the grassland soil and levels of 137Cs decreased with increasing soil depth. Transfer factor values for Atlantic blanket bog vegetation ranged from 1.9 to 9.6 and TF values were significantly higher in the leaves o f C. vulgaris in comparison to all other vegetation from this ecosystem. Caesium-13 7 TF values for the upland blanket bog vegetation on average ranged from 0.29 for E. tetralix to 1.6 for C. vulgaris. Uptake by the leaves of C. vulgaris was significantly higher than all other vegetation present thereby supporting the trend found within the Atlantic blanket bog vegetation. These results appear to indicate that the leaves of C. vulgaris have the ability to accumulate significant quantities of 137Cs and also that the uptake of 137Cs by this vegetation is dependent on plant compartment as the stems of this vegetation contained significantly lower levels than the leaves in both ecosystems. The uptake of 137Cs by grassland vegetation was very low and was only detectable in a fraction of the vegetation sampled. Caesium-137 TF values for grassland vegetation were in general lower than 0.02. The impact of soil physiochemical properties and nutrient status of vegetation on 137Cs uptake by vegetation appears to be complex and in some cases contradictory. The most apparent trend in the data was the positive influence of vegetation nutrients on 137Cs uptake in particular the magnesium levels present in the vegetation and to a lesser extent the calcium levels present. The results in general indicate that the uptake of 226Ra, 40K and 137Cs by the chosen vegetation is varied and complex and is significantly dependent on the species of vegetation, soil radionuclide concentration, soil physiochemical properties and the nutrient status of the vegetation.
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This thesis details the findings of a study into the spatial distribution and speciation of 238U, 226Ra and 228Ra in the soils of the Cronamuck valley, County Donegal . The region lies on the north-eastern edge of the Barnesmore granite and has been the subject of uranium prospecting efforts in the past. The results of the project provide information on the practicability of geostatistical techniques as a means of estimating the spatial distribution of natural radionuclides and provide insight into the behaviour of these nuclides and their modes of occurrence and enrichment in an upland bog environment. The results of the geostatistical survey conducted on the area indicate that the primary control over the levels of the studied nuclides in the soil of the valley is the underlying geology. Isopleth maps of nuclide levels in the valley indicate a predominance of elevated nuclide levels in the samples drawn from the granite region, statistical analysis of the data indicating that levels of the nuclides in samples drawn from the granite are greater than levels drawn from the non-granite region by up to a factor of 4.6 for 238U and 4.9 for 226Ra. Redistribution of the nuclides occurs via drainage systems within the valley, this process being responsible for transport of nuclides away from the granite region resulting in enrichment of nuclides in soils not underlain by the granite. Distribution of the nuclides within the valley is erratic, the effect of drainage f lows on the nuclides resulting in localized enriched areas within the valley. Speciation of the nuclides within one of the enriched areas encountered in the study indicates that enrichment is as a result of saturation of the soil with drainage water containing trace amounts of radionuclides. 238U is primarily held within the labile fractions (exchangeable cat ions + easily oxidisable organics + amorphous iron oxides ) of the soil , 226Ra being associated with the non- labile fractions, most probably the resistant organic material. 228Ra displays a significant occurrence in both the labile and non- labile fractions. The ability of the soil to retain uranium appears to be affected largely by the redox status of the soil, samples drawn from oxidizing environments tending to have little or no uranium in the easily oxidisable and amorphous iron oxide fractions. This loss of uranium from oxidised soil samples is responsible for the elevated 226Ra /238U disequilibrium encountered in the enriched areas of the valley. Analysis of the data indicates that samples displaying elevated 226Ra/238U ratios also exhibit elevated 228Ra/238U ratios indicating a loss of uranium from the samples as opposed to an enrichment of 226Ra.
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t.4 (1817)
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t.1 (1817)
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t.2 (1817)
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1) It may seem rather strange that, in spite of the efforts of a considerable number of scientists, the problem of the origin of indian corn or maize still has remained an open question. There are no fossil remains or archaeological relics except those which are quite identical with types still existing. (Fig. 1). The main difficulty in finding the wild ancestor- which may still exist - results from the fact that it has been somewhat difficult to decide what it should be like and also where to look for it. 2) There is no need to discuss the literature since an excellent review has recently been published by MANGELSDORF and REEVES (1939). It may be sufficient to state that there are basically two hypotheses, that of ST. HILAIRE (1829) who considered Brazilian pod corn as the nearest relative of wild corn still existing, and that of ASCHERSON (1875) who considered Euchlaena from Central America as the wild ancestor of corn. Later hypotheses represent or variants of these two hypotheses or of other concepts, howewer generally with neither disproving their predecessors nor showing why the new hypotheses were better than the older ones. Since nearly all possible combinations of ideas have thus been put forward, it har- dly seems possible to find something theoretically new, while it is essential first to produce new facts. 3) The studies about the origin of maize received a new impulse from MANGELSDORF and REEVES'S experimental work on both Zea-Tripsacum and Zea-Euchlaena hybrids. Independently I started experiments in 1937 with the hope that new results might be obtained when using South American material. Having lost priority in some respects I decided to withold publication untill now, when I can put forward more concise ideas about the origin of maize, based on a new experimental reconstruction of the "wild type". 4) The two main aspects of MANGELSDORF and REEVES hypothesis are discussed. We agree with the authors that ST. HILAIRE's theory is probably correct in so far as the tunicata gene is a wild type relic gene, but cannot accept the reconstruction of wild corn as a homozygous pod corn with a hermaphroditic tassel. As shown experimentally (Fig. 2-3) these tassels have their central spike transformed into a terminal, many rowed ear with a flexible rachis, while possessing at the same time the lateral ear. Thus no explanation is given of the origin of the corn ear, which is the main feature of cultivated corn (BRIEGER, 1943). The second part of the hypothesis referring to the origin of Euchlaena from corn, inverting thus ASCHERSON's theory, cannot be accepted for several reasons, stated in some detail. The data at hand justify only the conclusion that both genera, Euchlaena and Zea, are related, and there is as little proof for considering the former as ancestor of the latter as there is for the new inverse theory. 5) The analysis of indigenous corn, which will be published in detail by BRIEGER and CUTLER, showed several very primitive characters, but no type was found which was in all characters sufficiently primitive. A genetical analysis of Paulista Pod Corn showed that it contains the same gene as other tunicates, in the IV chromosome, the segregation being complicated by a new gametophyte factor Ga3. The full results of this analysis shall be published elsewhere. (BRIEGER). Selection experiments with Paulista Pod Corn showed that no approximation to a wild ancestor may be obtained when limiting the studies to pure corn. Thus it seemed necessary to substitute "domesticated" by "wild type" modifiers, and the only means for achieving this substitution are hybridizations with Euchlaena. These hybrids have now been analysed init fourth generation, including backcrosses, and, again, the full data will be published elsewhere, by BRIEGER and ADDISON. In one present publication three forms obtained will be described only, which represent an approximation to wild type corn. 6) Before entering howewer into detail, some arguments against ST. HILAIRE's theory must be mentioned. The premendelian argument, referring to the instability of this character, is explained by the fact that all fertile pod corn plants are heterozygous for the dominant Tu factor. But the sterility of the homozygous TuTu, which phenotypically cannot be identified, is still unexplained. The most important argument against the acceptance of the Tunicata faetor as wild type relic gene was removed recently by CUTLER (not yet published) who showed that this type has been preserved for centuries by the Bolivian indians as a mystical "medicine". 7) The main botanical requirements for transforming the corn ear into a wild type structure are stated, and alternative solutions given. One series of these characters are found in Tripsacum and Euchlaena : 2 rows on opposite sides of the rachis, protection of the grains by scales, fragility of the rachis. There remains the other alternative : 4 rows, possibly forming double rows of female and male spikelets, protection of kernels by their glumes, separation of grains at their base from the cob which is thin and flexible. 8) Three successive stages in the reconstruction of wild corn, obtained experimentally, are discussed and illustrated, all characterized by the presence of the Tu gene. a) The structure of the Fl hybrids has already been described in 1943. The main features of the Tunicata hybrids (Fig. -8), when compared with non-tunicate hybrids (Fig. 5-6), consist in the absence of scaly protections, the fragility of the rachis and finally the differentiation of the double rows into one male and one female spikelet. As has been pointed out, these characters represent new phenotypic effects of the tunicate factor which do not appear in the presence of pure maize modifiers. b) The next step was observed among the first backcross to teosinte (Fig. 9). As shown in the photography, Fig. 9D, the features are essencially those of the Fl plants, except that the rachis is more teosinte like, with longer internodes, irregular four-row-arrangement and a complete fragility on the nodes. c) In the next generation a completely new type appeared (Fig. 10) which resembles neither corn nor teosinte, mainly in consequence of one character: the rachis is thin and flexible and not fragile, while the grains have an abscission layer at the base, The medium sized, pointed, brownish and hard granis are protected by their well developed corneous glumes. This last form may not yet be the nearest approach to a wild grass, and I shall try in further experiments to introduce other changes such as an increase of fertile flowers per spikelet, the reduction of difference between terminal and lateral inflorescences, etc.. But the nature of the atavistic reversion is alveadwy such that it alters considerably our expectation when looking for a still existing wild ancestor of corn. 9) The next step in our deductions must now consist in an reversion of our question. We must now explain how we may obtain domesticated corn, starting from a hypothetical wild plant, similar to type c. Of the several changes which must have been necessary to attract the attention of the Indians, the following two seem to me the most important: the disappearance of all abscission layers and the reduction of the glumes. This may have been brought about by an accumulation of mutations. But it seems much more probable to assume that some crossing with a tripsacoid grass or even with Tripsacum australe may have been responsible. In such a cross, the two types of abscission layer would be counterbalanced as shown by the Flhybrids of corn, Tripsacum and Euchlaena. Furthermore in later generations a.tu-allele of Tripsacum may become homozygous and substitute the wild tunicate factor of corn. The hypothesis of a hybrid origin of cultivated corn is not completely new, but has been discussed already by HARSHBERGER and COLLINS. Our hypothesis differs from that of MANGELSDORF and REEVES who assume that crosses with Tripsacum are responsible only for some features of Central and North American corn. 10) The following arguments give indirects evidence in support of our hypothesis: a) Several characters have been observed in indigenous corn from the central region of South America, which may be interpreted as "tripsacoid". b) Equally "zeoid" characters seem to be present in Tripsacum australe of central South-America. c) A system of unbalanced factors, combined by the in-tergeneric cross, may be responsible for the sterility of the wild type tunicata factor when homozygous, a result of the action of modifiers, brought in from Tripsacum together with the tuallele. d) The hybrid theory may explain satisfactorily the presence of so many lethals and semilethals, responsible for the phenomenon of inbreeding in cultivated corn. It must be emphasized that corn does not possess any efficient mechanism to prevent crossing and which could explain the accumulation of these mutants during the evolutionary process. Teosinte which'has about the same mechanism of sexual reproduction has not accumulated such genes, nor self-sterile plants in spite of their pronounced preference for crossing. 11) The second most important step in domestication must have consisted in transforming a four rowed ear into an ear with many rows. The fusion theory, recently revived byLANGHAM is rejected. What happened evidently, just as in succulent pXants (Cactus) or in cones os Gymnosperms, is that there has been a change in phyllotaxy and a symmetry of longitudinal rows superimposed on the original spiral arrangement. 12) The geographical distribution of indigenous corn in South America has been discussed. So far, we may distinguish three zones. The most primitive corn appears in the central lowlands of what I call the Central Triangle of South America: east of the Andies, south of the Amazone-Basin, Northwest of a line formed by the rivers São Prancisco-Paraná and including the Paraguay-Basin. The uniformity of the types found in this extremely large zone is astonishing (BRIEGER and CUTLER). To the west, there is the well known Andian region, characterized by a large number of extremely diverse types from small pop corn to large Cuszco, from soft starch to modified sweet corn, from large cylindrical ears to small round ears, etc.. The third region extends along the atlantic coast in the east, from the Caribean Sea to the Argentine, and is characterized by Cateto, an orange hard flint corn. The Andean types must have been obtained very early, and undoubtedly are the result of the intense Inca agriculture. The Cateto type may be obtained easily by crosses, for instance, of "São Paulo Pointed Pop" to some orange soft corn of the central region. The relation of these three South American zones to Central and North America are not discussed, and it seems essential first to study the intermediate region of Ecuador, Colombia and Venezuela. The geograprical distribution of chromosome knobs is rapidly discussed; but it seems that no conclusions can be drawn before a large number of Tripsacum species has been analysed.
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1) O caráter presença de espinhos nos frutos da mamoneira é determinado por um par de fatores dominantes SS, sendo a forma recessiva ss, inerme. A interação alélica nao é bem intermediária, havendo uma predominância do fator S. Êste resultado foi anteriormente constatado por HARLAND (7), PEAT (8), DOMINGO (2), GURGEL (4) e FERNANDES (3). 2) A constatação da segregação 1 SS : 2 Ss : 1 ss foi feita após extensivas contagens de espinhos, tanto na forma paternal, como também no Fl, F2 e "back-cross". Por essas contagens foi verificado que existem variedades com números diferentes de espinhos, podendo-se distinguir dois tipos: variedades que têm muitos espinhos, com uma média aproximada de 170 espinhos por fruto e variedades que têm um número médio de espinhos, com uma média aproximada de 113 espinhos por fruto. 3) Embora a segregação dos fatores S e s seja monofatorial, todavia foi constadada por uma análise estatística detalhada, a presença de gens modificadores agindo na geração F2, introduzidos pelos tipos paternais. Assim, o segregante SS no F2, tem mais espinhos do que o pai homozigoto da mesma constituição. 4) Foram encontrados dois novos gens cal e ca2, com interação não alélica do tipo de polimeria complementar duplo-recessiva, dando no F2 uma segregação de 15 com espinhos uniformes : 1 com espinho careca, no "back-cross" uma segregação de 3 com espinhos uniformes : 1 com espinho careca. Estes gens determinaram, nos frutos com espinhos, a formação de zonas sem espinhos, ou como denominamos, "carecas". Estes novos fatores foram encontrados numa única variedade, de n.° 51, conhecida por laciniada, em virtude da for- ma especial de suas fôlhas. Esta variedade é de côr verde, apresenta cera na haste e possui numerosos cachos, porém pequenos. Ê tida como planta ornamental e foi originalmente importada de Erfurt, Alemanha. 5) Mesmo nas variedades inermes foi constatada a presença dos gens Cal e Ca2, para distribuição uniforme de espinhos, embora nas ditas variedades não se possa identificar a sua presença, em virtude do gen s ser epistático recessivo sobre Cal e Ca2. 6) Uma vez que os fatores S e CalCa2 sao independentes, isto é, possivelmente situados em cromosômios diferentes, fazendo-se o cruzamento de variedades com espinho careca x variedades sem espinho, obtem-se o PI com número de espinhos intermediário e distribuição uniforme. No F2 obtém-se a segregação de 45 com espinho uniforme : 3 com espinho careca : 16 sem espinho e no "back-cross" a segregação de 3 com espinho uniforme : 1 com espinho careca : 4 sem espinho.
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The present work deals with the study of the effects of selfing and crossing in pures lines of okra inbred for five generations and the methods of breeding in this plant. This work is party of a large program of this Dept. to study heterosis in plants naturally self pollinated. The technic of selfing consists of tying with a string the floral bud before anthesis. To make controlled crosses, it is necessary to emasculate the flowers removing the anthers with small forceps, and to cover the flowers with a bag and wait for 1 or 2 days until the blooming. Also, the male parents are covered with paper bags prior to flowering. Finally, the pollen is brushed lightly over the stigma of the emasculated flowers and the females unit rebagged. The authors have tried without sucess the technic of soda fountain straw used for cotton. The treatments were: I) Fl of the cross pure-line x foreign variety (not improved by breeding). II) Fl of the cross pure-line x parental variety and III) pure-line 5 generations inbred. In order to compare the production of these three treatments, a randomized blocks with 4 replications was designed; since we had 6 families in each treatment, the total number was: 4 replications x 3 treatments x 6 families: = 72. Each familiy was planted in lines of 10 plants. Owing to the design devised, the present experiment corresponds to a split-plot. The analysis of variance of the number and the weight of the pods is given in tables 2 and 4, and shows the following: 1) The production expressed in both numbers and weights of the cross, - pure lines x foreign variety - was statistically smaller than the others treatments, i, e., the cross of pure-lines x parental variety and the pure-lines; 2) The production of the treatments pure-lines x parental variety and selfed purelines was the same. It was proved that the selfing do not produce harmful effects in okra, it was benefical, since after 5 inbred generations the production was the same when compared with Fl of the parental variety. Also, the methods of pure-lines are indicated to improve varieties of okra.
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n.f.:bd.3 (1859-1860)
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n.f.:bd.1 (1855-1856)