990 resultados para Datação 14C
Resumo:
An old erg covers the northern part of the Lake Chad basin. This dune landform allowed the formation of many inter- dune ponds of various sizes. Still present in certain zones where the groundwater level is high (e.g. Kanem, southern Manga), these ponds formed in the past a vast network of lacustrine microsystems, as shown by the nature and the dis- tribution of their deposits. In the Manga, these interdune deposits represent the main sedimentary records of the Holo- cene environmental succession. Their paleobiological (pollens, diatoms, ostracods) and geochemical (δ18O, δ13C, Sr/ Ca) contents are often the basis for paleoenvironmental reconstruction. On the other hand, their sedimentological char- acters are rarely exploited. This study of palustro-lacustrine deposits of the Holocene N'Guigmi lake (northern bank of the Lake Chad; Niger) is based on the relationships between the sedimentological features and the climato-hydrological fluctuations. The mineralogical parameters (e.g. calcium carbonate content, clay mineralogy) and the nature of autoch- thonous mineralization (i.e. amorphous silica, clays, calcium carbonates) can be interpreted using a straightforward hy- dro-sedimentary model. Established to explain the geochemical dynamics of Lake Chad, this model is based on a bio- geochemical cycle of the main elements (i.e. silicium, calcium) directly controlled by the local hydrological balance (i.e. rainfall/evaporation ratio). All these results show that a detailed study of sedimentological features can provide impor- tant paleohydrological informations about the regional aridification since ca 6500 14C BP.
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O objetivo deste trabalho foi avaliar as flutuações sazonais do crescimento vegetativo do cafeeiro (Coffea arabica L.) e suas relações com o fotoperíodo, a remoção dos frutos, a fotossíntese e a resistência estomática. Os tratamentos foram constituídos por dois regimes fotoperiódicos - natural e estendido para 14 horas - em plantas com frutos e sem frutos. O crescimento de ramos e da área foliar decresceu a partir de meados de março, atingindo taxas mínimas nos meses de maio e junho, quando foram registradas as menores temperaturas. Esse modelo de crescimento não foi modificado pela extensão do fotoperíodo para 14 horas, nem pela remoção dos frutos, ainda que os cafeeiros sem frutos exibissem maiores taxas de crescimento dessas variáveis (ramo e área foliar). Não foi observada diferença significativa na fotossíntese potencial decorrente da presença de frutos, nem a extensão do fotoperíodo afetou taxas fotossintéticas. As taxas fotossintéticas potenciais não explicam os declínios do crescimento vegetativo, mas a temperatura mínima do ar correlacionou-se com as quedas do crescimento. A resistência estomática às 14h apresentou valores relativamente elevados, de meados de março a início de maio, coincidindo com elevadas quedas no crescimento de ramos e da área foliar. O declínio inicial no crescimento vegetativo pode estar associado a temperaturas em torno de 14ºC.
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Few studies have aimed to reconstruct landscape change in the area of Eretria (South Central Euboea, Greece) during the last 6000 years. The aim of this paper is to partially fill in this gap by examining the interaction be- tween Mid- to Late Holocene shoreline evolution and human occupation, which is documented in the area from the Late Neolithic to the Late Roman period (with discontinuities). Evidence of shoreline displacements is derived from the study of five boreholes (maximum depth of 5.25 m below the surface) drilled in the lowlands of Eretria. Based on sedimentological analyses and micro/macrofaunal identifications, different facies have been identified in the cores and which reveal typical features of deltaic progradation with marine, lagoonal, fluvio- deltaic and fluvial environments. In addition, a chronostratigraphy has been obtained based on 20 AMS 14C radio- carbon dates performed on samples of plant remains and marine/lagoonal shells found in situ. The main sequences of landscape reconstruction in the plain of Eretria can be summarized as follows: a marine environ- ment predominated from ca. 4000 to 3200 cal. BC and a gradual transition to shallow marine conditions is ob- served ca. 3200-3000 cal. BC due to the general context of deltaic progradation west of the ancient city. Subsequently, from ca. 3000 to 2000 cal. BC, a lagoon occupied the area in the vicinity of the Temple of Apollo and the settlement's development was restricted to several fluvio-deltaic levees, thus severely limiting human activities in the plain. From ca. 2000 to 800 cal. BC, a phase of shallow marine presence prevailed and constrained settlement on higher ground, forcing abandonment of the major part of the plain. Finally, since the eighth century BC, the sea has regressed southward and created the modern landscape.
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The objective of this work was to evaluate basal temperature, thermal sum at different phenological stages, phenological phase duration, yield and seasonality of one nectarine and 14 peach cultivars, between 2006 and 2009. The considered phenological phases were: pruning-sprouting; sprouting-flowering, from swollen bud to open flower; flowering-fruiting, from petal fall to medium-sized fruit; and ripening. Minimum basal temperatures (Tb) obtained were: pruning-sprouting, 8°C, irrespective of the cultivars; sprouting-flowering, 10°C, except for 'Cascata 968', which required 8°C Tb; flowering-fruiting, 12°C, except for 'Oro Azteca', which required 14°C Tb; ripening, 14°C, except for 'Sunblaze', 'Diamante Mejorado' and 'Precocinho' with 12°C Tb. For most cultivars, the maximum basal temperatures were 30, 34, 34 and 28ºC for phases pruning-sprouting, sprouting-flowering, flowering-fruiting and ripening, respectively. 'Turmalina', 'Marli' and 'Tropic Beauty' showed average yields of 3,945.0, 3,969.3 and 3,954.0 kg ha-1, respectively, in 2009, while the nectarine 'Sunblaze' showed around 3,900 kg ha-1 in 2008 and 2009. The cultivars differed for their total cycle and for the accumulated thermal sums which varied, respectively, from 245 days and 1,881.4 degree-days for 'Oro Azteca', to144 days and 1,455.7 degree-days for 'Precocinho'.
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Activation dynamics of hippocampal subregions during spatial learning and their interplay with neocortical regions is an important dimension in the understanding of hippocampal function. Using the (14C)-2-deoxyglucose autoradiographic method, we have characterized the metabolic changes occurring in hippocampal subregions in mice while learning an eight-arm radial maze task. Autoradiogram densitometry revealed a heterogeneous and evolving pattern of enhanced metabolic activity throughout the hippocampus during the training period and on recall. In the early stages of training, activity was enhanced in the CA1 area from the intermediate portion to the posterior end as well as in the CA3 area within the intermediate portion of the hippocampus. At later stages, CA1 and CA3 activations spread over the entire longitudinal axis, while dentate gyrus (DG) activation occurred from the anterior to the intermediate zone. Activation of the retrosplenial cortex but not the amygdala was also observed during the learning process. On recall, only DG activation was observed in the same anterior part of the hippocampus. These results suggest the existence of a functional segmentation of the hippocampus, each subregion being dynamically but also differentially recruited along the acquisition, consolidation, and retrieval process in parallel with some neocortical sites.
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The objective of this work was to verify whether the addition of biochar to the soil affects the degradation of litter and of soil organic matter (SOM). In order to investigate the effect of biochar on the mineralization of barley straw, soil was incubated with 14C-labelled barley straw with or without unlabelled biochar. To investigate the effect of straw on the mineralization of biochar, soil was incubated with 14C-labelled biochar with or without straw. In addition, to investigate the effect of biochar on old SOM, a soil labelled by applying labelled straw 40 years ago was incubated with different levels of biochar. All experiments had a control treatment, without any soil amendment. The effect of biochar on the straw mineralization was small and nonsignificant. Without biochar, 48±0.2% of the straw carbon was mineralized within the 451 days of the experiment. In comparison, 45±1.6% of C was mineralized after biochar addition of 1.5 g kg-1. In the SOM-labelled soil, the organic matter mineralized more slowly with the increasing doses of biochar. Biochar addition at 7.7 g kg-1 reduced SOM mineralization from 6.6 to 6.3%, during the experimental period. The addition of 15.5 g kg-1 of biochar reduced the mineralized SOM to 5.7%. There is no evidence of increased degradation of either litter or SOM due to biochar addition; consequently, there is no evidence of decreased stability of SOM.
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A method for the measurement of carbamoyl-phosphate synthetase I activity in animal tissues has been developed using the livers of rats under normal and hyperproteic diets. The method is based on the incorporation of 14C-ammonium bicarbonate to carbamoyl-phosphate in the presence of ATP-Mg and N-acetyl-glutamate. The reaction is stopped by chilling, lowering the pH and adding ethanol. Excess bicarbonate is flushed out under a gentle stream of cold CO2. The only label remaining in the medium was that incorporated into carbamoyl-phosphate, since all 14C-CO2 from bicarbonate was eliminated. The method is rapid and requires only a low pressure supply of CO2 to remove the excess substrate. The reaction is linear up to 10 min using homogenate dilutions of 1:20 to 1:200 (w/v). Rat liver activity was in the range of 89±8 nkat/g. Hyperproteic diet resulted in a significant 1.4-fold increase. The design of the method allows for the processing of multiple samples at the same time, and incubation medium manipulation is unnecessary, since the plastic incubation vial and its contents are finally counted together.
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Este experimento teve como objetivo avaliar as transformações pós-colheita em pitangas colhidas nos estádios de maturação vermelho-alaranjado (VA) e vermelho predominante (VP) e mantidas sob atmosfera modificada (AM) por filme de cloreto de polivinila (PVC), a 10 ± 0,5 ºC, 14 ± 0,5ºC e (90 ± 1%UR) e a temperatura ambiente (23 ± 2°C e 85 ± 2%UR). O uso de AM associada à refrigeração permitiu manutenção dos sólidos solúveis, acidez titulável, dos açúcares solúveis totais e vitamina C, e também resultou em menor taxa de aumento nos carotenóides totais para frutos do estádio de maturação VA mantido a 10 e 14ºC. Em conjunto, pitangas colhidas no estádio vermelho-alaranjado foram as que apresentaram melhor manutenção das características intrínsecas durante oito dias de armazenamento sob atmosfera modificada a 10ºC.
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Avaliou-se o efeito do tratamento térmico (40ºC por 24 horas) e de diferentes temperaturas de armazenamento (8ºC, 14ºC e 25ºC, a 90%UR), na conservação pós-colheita de abacaxis 'Pérola', colhidos no ponto de maturação "pintado". As avaliações foram realizadas no início (0 dia), visando à caracterização inicial dos frutos, e após 1; 5; 9; 13 e 17 dias, quando os mantidos sob refrigeração foram transferidos para condição ambiente (25ºC, 75-80% UR), e avaliados aos 21; 25 e 29 dias. O delineamento experimental utilizado foi o inteiramente casualizado, em esquema fatorial (2x3x9), tendo-se os frutos tratados termicamente ou não, o armazenamento a 25ºC, 14ºC e 8ºC e nove épocas de avaliação. Os frutos foram avaliados quanto à ocorrência de podridões e de escurecimento interno, aparência e coloração da polpa, teores de sólidos solúveis (SS), acidez titulável (AT), açúcares solúveis totais e redutores e ácido ascórbico, além da relação SS/AT. Os resultados indicam que a coloração da polpa se tornou mais amarela durante o período refrigerado, enquanto os valores da AT aumentaram. Neste período, a relação SS/AT reduziu-se, mas aumentou com a transferência dos frutos para o ambiente, enquanto os teores de açúcares solúveis totais e redutores diminuíram, e estabilizaram-se. Os teores de ácido ascórbico mantiveram-se sem diferenças significativas, mas com tendência de aumento. Os frutos mantidos sob refrigeração apresentaram sintomas de injúria pelo frio, que apareceram em 8 dias, após serem levados ao ambiente, e com maior intensidade nos tratados termicamente.
Resumo:
A method for the measurement of carbamoyl-phosphate synthetase I activity in animal tissues has been developed using the livers of rats under normal and hyperproteic diets. The method is based on the incorporation of 14C-ammonium bicarbonate to carbamoyl-phosphate in the presence of ATP-Mg and N-acetyl-glutamate. The reaction is stopped by chilling, lowering the pH and adding ethanol. Excess bicarbonate is flushed out under a gentle stream of cold CO2. The only label remaining in the medium was that incorporated into carbamoyl-phosphate, since all 14C-CO2 from bicarbonate was eliminated. The method is rapid and requires only a low pressure supply of CO2 to remove the excess substrate. The reaction is linear up to 10 min using homogenate dilutions of 1:20 to 1:200 (w/v). Rat liver activity was in the range of 89±8 nkat/g. Hyperproteic diet resulted in a significant 1.4-fold increase. The design of the method allows for the processing of multiple samples at the same time, and incubation medium manipulation is unnecessary, since the plastic incubation vial and its contents are finally counted together.
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Des programmes de recherche pluridisciplinaires sur l’occupation du sol et le pastoralisme de la Préhistoire au Moyen Âge dans le sud du massif alpin sont menés, depuis 1998, sur les massifs du Haut Champsaur, de Freissinières et de l’Argentièrois (Hautes-Alpes). Des dix phases d’occupation et d'activité agropastorale mises en évidence (prospections pédestres et fouilles), entre 1600 et 2700 m d’altitude, trois se distinguent: la fin du Néolithique, l’âge du Bronze et la période médiévale. Au travers des premières données archéologiques et environnementales, cet article présente, depuis le milieu du IIIe millénaire au début du Ier millénaire, les grandes caractéristiques de l’occupation du sol mais aussi l’originalité et l’importance de l’activité humaine dans cette zone alpine. La fin du Néolithique et l’âge du Bronze correspondent à une multiplication des gisements archéologiques marquant de façon évidente une rupture dans la gestion de l'espace montagnard. Les paysages sont largement façonnés par les activités humaines et l’entretien des terres cultivées, des prairies et des alpages, paraît continu. À la lumière des données de terrain, l’une des évolutions qui apparaît sur les sites d’altitude durant cette période concerne l’apparition de structures pastorales bâties entre 2 067 et 2 303 m d’altitude (datation 14C).
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Painovuosi nimekkeestä.
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The deterioration of surface waters is one of the most important issues in the environmental management of the European Union. Thus, the EU Water Framework Directive 2000/60/EC (WFD) requires “good ecological and chemical status” of surface waters by 2015 allowing only a slight departure from ecological reference conditions characterized by the biological communities typical for the conditions of minimal anthropogenic impact. The WFD requires the determination of ecological reference conditions and the present ecological status of surface waters. To meet this legislative demand, sedimentary diatom assemblages were used in these studies with various methods 1) to assess natural and human activity induced environmental changes, 2) to characterize background conditions 3) to evaluate the present ecological status and 4) to predict the future of the water bodies in the light of palaeolimnological data. As the WFD refers to all surface waters, both coastal and inland sites were included. Two long and two short sediment cores from the Archipelago Sea in the northern Baltic Sea were examined for their siliceous microfossils in order to assess (1) the Holocene palaeoenvironmental history and (2) the recent eutrophication of the area. The diatom record was divided into local diatom assemblage zones (LDAZ, long cores) and diatom assemblage zones (DAZ, short cores). Locally weighted weighted averaging regression and calibration (LWWA) was applied for the quantitative reconstruction of past TN concentrations (short cores). An age model for the long cores was constructed by using independent palaeomagnetic and AMS-14C methods. The short cores were dated using radiometric (210Pb, 226Ra and 137Cs) methods. The long cores date back to the early history of the Archipelago Sea, which was freshwater – no salinity increase referable to the brackish phase of the Yoldia Sea is recognized. The nutrient status of the lacustrine phase was slightly higher in the Archipelago Sea than in the Baltic Proper. Initial brackish-water influence is observed at 8 150 ±80 cal. BP (LDAZ4), but fully brackish conditions were established at 7 700 ±80 cal. BP (LDAZ5). The diatom assemblages indicate increasing salinity, warming climate and possible eutrophic conditions during the lacustrine to brackish-water transition. The decreasing abundance of Pseudosolenia calcar-avis (Schultze) Sundström and the increasing abundance of the ice-cover indicator species Pauliella taeniata (Grunow) Round and Basson indicate decreasing salinity and climatic cooling after ca. 5 000 cal. BP. Signs of eutrophication are visible in the most recent diatom assemblage zones of both short cores. Diatom-inferred total nitrogen (DI-TN) reconstructions partially fail to trace the actual measured total nitrogen concentrations especially from the late 1980s to the mid 1990s. This is most likely due to the dominating diatom species Pauliella taeniata, Thalassiosira levanderi Van Goor and Fragilariopsis cylindrus (Grunow) W. Krieger being more influenced by factors such as the length of the ice-season rather than nutrient concentrations. It is concluded that the diatom assemblages of the study sites are principally governed by climate fluctuations, with a slight influence of eutrophication visible in the most recent sediments. There are indications that global warming, with reduced ice cover, could impact the spring blooming diatom species composition in the Archipelago Sea. In addition, increased sediment accumulation in the early 90s coincides with the short ice-seasons suggesting that warming climate with decreasing ice-cover may increase sedimentation in the study area. The diverse diatom assemblages dominated by benthic species (54 %) in DAZ1 in the Käldö Fjärd core can be taken as background diatom assemblages for the Archipelago Sea. Since then turbidity has increased and the diatom assemblages have been dominated by planktonic diatoms from around the mid 1800s onwards. The reconstructed reference conditions for the total nitrogen concentrations fluctuate around 400 μg l-1. Altogether two short sediment cores and eight short cores for top-bottom analysis were retrieved from Lake Orijärvi and Lake Määrjärvi to assess the impact of the acid mine drainage (AMD) derived metals from the Orijärvi mine tailings on the diatom communities of the lakes. The Cu (Pb, Zn) mine of Orijärvi (1757 – 1956) was the first one in Finland where flotation techniques (1911 – 1955) were used to enrich ore and large quantities of tailings were produced. The AMD derived metal impact to the lakes was found to be among the heaviest thus far recorded in Finland. Concentrations of Cu, Pb and Zn in Lake Orijärvi sediments are two to three orders of magnitude higher than background values. The metal inputs have affected Lake Orijärvi and Lake Määrjärvi diatom communities at the community levels through shifts in dominant taxa (both lakes) and at the individual level through alteration in frustule morphology (Lake Orijärvi). At present, lake water still has elevated heavy metal levels, indicating that the impact from the tailings area continues to affect both lakes. Lake Orijärvi diatom assemblages are completely dominated by benthic species and are lacking planktonic diatoms. In Lake Määrjärvi the proportion of benthic and tychoplanktonic diatoms has increased and the planktonic taxa have decreased in abundance. Achnanthidium minutissimum Kützing and Brachysira vitrea (Grun.) R. Ross in Hartley were the most tolerant species to increased metal concentrations. Planktonic diatoms are more sensitive to metal contamination than benthic taxa, especially species in the genus Cyclotella (Kützing) Brébisson. The ecological reference conditions assessed in this study for Lake Orijärvi and Lake Määrjärvi comprise diverse planktonic and benthic communitites typical of circumneutral oligotrophic lakes, where the planktonic diatoms belonging to genera Cyclotella , Aulacoseira Thwaites, Tabellaria Ehrenberg and Asterionella Hassall dominate in relative abundances up to ca. 70%. The benthic communities are more diverse than the planktonic consisting of diatoms belonging to the genera Achnanthes Bory, Fragilaria Lyngbye and Navicula St. Vincent. This study clearly demonstrates that palaeolimnological methods, especially diatom analysis, provide a powerful tool for the EU Water Frame Work Directive for defining reference conditions, natural variability and current status of surface waters. The top/bottom approach is a very useful tool in larger-scale studies needed for management purposes. This “before and after” type of sediment sampling method can provide a very time and cost effective assessment of ecological reference conditions of surface waters.
Resumo:
O controle químico, térmico e a refrigeração são os processos mais utilizados no tratamento pós-colheita das bananas. O objetivo deste trabalho foi avaliar o efeito do tratamento térmico, químico e da combinação dos dois métodos e estes associados à baixa temperatura de conservação no controle da antracnose na pós-colheita da banana. Para tanto os experimentos foram realizados em três épocas quando, bananas (Musa sp) da variedade 'Prata Anã' (AAB) no estádio pré-climatérico eram coletadas e suas pencas individualizadas. As pencas foram submetidas a quatro tratamentos com cinco repetições cada: 1. Tratamento térmico (imersão em água a 56ºC por seis minutos, seguido de resfriamento em água à temperatura ambiente); 2. Tratamento químico por seis minutos (imersão em calda fungicida (prochloraz 2,5 mL.L-1)); 3. Tratamento térmico seguido do químico; 4. Testemunha, imersão em água por seis minutos. Após os tratamentos, as pencas eram divididas em duas partes iguais, sendo que uma parte ficou em câmara fria (14ºC com variação de 2ºC) e a outra permaneceu à temperatura ambiente. O tratamento térmico não foi eficiente no controle da doença. O fungicida prochloraz a 2,5 mL.L-1 foi eficiente no controle da podridão pós-colheita. A refrigeração retardou o surgimento da doença em até 12 dias. Os resultados indicam que a baixa temperatura, associada ou não ao controle químico, é capaz de controlar a podridão pós-colheita dos frutos por 12 dias.
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OBJETIVO: examinar a função lútea em adolescentes com ciclos menstruais regulares. MÉTODOS: foram incluídas neste estudo, de coorte prospectivo, 55 adolescentes eumenorrêicas, com idade entre 14 e 19 anos e menarca aos 12,2 anos. Examinaram-se o dia da ocorrência de ovulação, o grau de vascularização do corpo lúteo e o índice de resistência dos vasos ovarianos, as concentrações de progesterona e a resposta do endométrio. A ovulação foi identificada por ultra-sonografia transvaginal a partir do 2º ou 5º dia do ciclo, repetindo-a a cada dois dias. A vascularização e o índice de resistência lútea foram aferidos por dopplervelocimetria no 10º dia pós-ovulação. Os níveis de progesterona sérica foram estimados por quimioluminescência nos dias 6, 9 e 12 da fase lútea. A histologia endometrial foi analisada após biópsia feita entre o 8º e o 10º dia pós-ovulação. Usou-se software SPSS para análise estatística, assumindo-se significância quando p<0,05. RESULTADOS: A ovulação foi observada em média no 17º dia. Os níveis séricos de progesterona foram de 11,4, 10,9 e 3,9 ng/mL respectivamente nos dias 6, 9 e 12 pós-ovulação; a média dos níveis de progesterona nos três dias foi de 10,3 ng/ml. A vascularização do corpo lúteo foi escassa em 34,6%, moderada em 23,6% e exuberante em 41,8%. O índice de resistência foi de 0,441 dez dias após a ovulação. O endométrio mostrou-se sincrônico em 85,5% das biópsias e fora de fase em 14,5%. As correlações entre o dia da ovulação e o tipo de endométrio (p=0,29), níveis de progesterona e o tipo endométrio (p=0,454), grau de vascularização (p=0,99) e índice de resistência do corpo lúteo (p=0,23) não foram estatisticamente significantes. A histologia endometrial e o grau de vascularização também não mostraram associação (p=0,61). CONCLUSÃO: a função lútea em adolescentes eumenorrêicas, avaliada pela datação do endométrio em ciclo único, mostrou-se anormal em 14,5%. As variáveis grau e intensidade da vascularização, concentração sérica de progesterona ou dia da ocorrência de ovulação não mostraram associação com a histologia endometrial.