999 resultados para 18-181
Resumo:
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.
Resumo:
The Global River Discharge (RivDIS) data set contains monthly discharge measurements for 1018 stations located throughout the world. The period of record varies widely from station to station, with a mean of 21.5 years. These data were digitized from published UNESCO archives by Charles Voromarty, Balaze Fekete, and B.A. Tucker of the Complex Systems Research Center (CSRC) at the University of New Hampshire. River discharge is typically measured through the use of a rating curve that relates local water level height to discharge. This rating curve is used to estimate discharge from the observed water level. The rating curves are periodically rechecked and recalibrated through on-site measurement of discharge and river stage.
Resumo:
A espécie endêmica G. elliptica R. E. Fries não apresentava estudos fitoquímicos e biológicos detalhados na literatura. Assim, o objetivo desse trabalho foi avaliar a composição química e as propriedades biológicas dos óleos essenciais, extratos brutos, alcaloides totais, tortas, frações das tortas, amostras isoladas dessa espécie. O material vegetal foi coletado em Paranapiacaba (Santo André, SP, Brasil). O óleo essencial extraído das folhas por destilação à vapor apresentou um rendimento de 0,2%. A análise histológica das folhas encontrou óleo em células oleíferas localizadas no parênquima esponjoso. A composição do óleo (CG-EM) indicou espatulenol e óxido de cariofileno como compostos majoritários. Os alcaloides totais foram obtidos dos extratos brutos das folhas e dos galhos e analisados por CG-EM, identificando quatro aporfinas (nornuciferina, estefarina, corituberina e asimilobina) e duas protoberberinas (discretamina e caseadina). Os alcaloides totais foram fracionados em coluna cromatográfica ou por Extração em Fase Sólida e purificados por cromatografia em camada preparativa, originando duas amostras (Amostra 9 e 10). Na Amostra 9, foram identificados dois alcaloides aporfinicos nornuciferina e asimilobina (CG-EM e RMN-1H). Na Amostra 10, foram identificados (LC-EM/EM) cinco alcaloides aporfínicos (desidronantenina, glaunidina, liriodenina, N-óxido de oliverina e telikovina) e um alcaloide protoberberínico (caseadina). Caseadina, glaunidina, N-óxido de oliverina e telikovina não foram previamente identificados em Guatteria. Os resíduos dos extratos brutos livres de alcaloides foram fracionados pelo método de partição com solventes de polaridade crescente. Os extratos brutos e as frações acetato de etila e butanólicas de folhas e galhos apresentaram flavonoides (NP-PEG). Nos ensaios biológicos, a melhor atividade antioxidante (sequestro do radical DPPH) foi encontrada para a fração clorofórmica dos galhos (EC50=24,25±1,14 µg/mL) e a torta dos galhos (EC50=26,23±4,20 µg/mL). No ensaio antimicrobiano pelo método turbidimétrico a atividade mais importante foi obtida contra Staphylococcus aureus (ATCC 6538) para os alcaloides totais dos galhos (CIM/CBM=0,12±0,01/0,26 mg/mL) e das folhas (CIM/CBM=0,21±0,01/0,28 mg/mL), e fração hexânica das folhas (CIM/CBM=0,24±0,02/>1 mg/mL). Uma alta atividade antitumoral foi observada frente a células humanas de mama (MCF-7) para Amostra 10 (IC50=2,28±0,18 µg/mL), fração de acetato de etila das folhas (IC50=4,47±0,40 µg/mL), óleo essencial (IC50=7,01±0,23 µg/mL) e os alcaloides totais das folhas (IC50=9,32±0,36 µg/mL). Para as células de próstata (PC-3), foi encontrada atividade para a Amostra 10 (IC50=1,37±0,36 µg/mL) e o óleo essencial (IC50=5,32±0,35 µg/mL). A futura aplicação dos extratos e frações de G. elliptica como um agente antitumoral parece ser segura, pois mantiveram uma viabilidade celular maior do que 90% no ensaio de citotoxicidade com culturas de fibroblasto murino (BALB/c 3T3, ATCC CCL-163) nas concentrações onde a atividade antitumoral foi promissora (<30 µg/mL) contra MCF-7 e/ou PC-3.
Resumo:
The ultimate composition of any sandstone is affected by a host of primary and secondary factors, including the lithologies present in source terranes, climate, depositional environment and diagenesis. In the case of a subduction complex, however, unequivocal identification of detrital provenance may be impossible because of the cumulative effects of tectonic and sedimentary transport. Long-distance sedimentary transport (> 1000 km) is common within trenches, and abyssal-plain turbidites can be tectonically transported for long distances as the underlying oceanic basement drifts towards a subduction front. Post-accretionary displacement can occur as a consequence of strike-slip faulting, and the total distance of tectonic dislocation may reach several thousand kilometers. The present-day Aleutian forearc region (North Pacific Ocean) illustrates many of the "problems" which typify subduction zones. Several petrologic suites can be identified, and there are significant variations in detrital modes in both time and space. The Aleutian region serves as a sobering modern analog for accreted rock units such as the Franciscan Complex of California, where intercalations of discrete sandstone suites have been noted. In the absence of paleomagnetic control, interpretations of sediment provenance within ancient subduction complexes probably should be restricted to the generic level.
Resumo:
Sand and sandstone compositions from different types of basins reflect provenance terranes governed by plate tectonics. One hundred and one thin sections of Upper Miocene to Holocene sand-sized material were examined from DSDP/IPOD Sites in the North Pacific Ocean and the Bering Sea. The Gazzi-Dickinson point-counting method was used to establish compositional characteristics of sands from different tectonic settings. Continental margin forearc sands from the western North America continental margin arc system are clearly different from backarc/marginal-sea sands from the Aleutian intraoceanic arc system. The forearc sands have average QFL percentages of 29-42-29, LmLvLst percentages of 32-34-34, 3 Fmwk%M and 0.82 P/F. Aleutian backarc sands have average QFL percentages of 8-22-69. LmLvLst percentages of 9-85-6, 0.5 Fmwk%M and 0.96 P/F. A trend of increasing QFL%Q and decreasing LmLvLst%Lv westward in the backarc region of the Aleutian Ridge reflects the influence of the Asiatic continental margin. Aleutian backarc sands without continental influence have average QFL percentages of 1-20-79, LmLvLst percentages of 1-98-1, 0 Fmwk%M and 0.99 P/F. Of the continental margin forearc samples, sands on the Astoria Fan (west of the Oregon-Washington trench) contain the highest LmLvLst%Lv and lowest P/F; sands from mixed transform-fault and trench settings (Delgada Fan and Gulf of Alaska samples) have slightly higher Qp/Q (0.03); and sands from the Pacific-Juan de Fuca-North America triple junction have the highest Fmwk%M. Delgada Fan and Gulf of Alaska sands have average QFL percentages of 27-38-35, LmLvLst percentages of 37-26-37, 2 Fmwk%M and 0.86 P/F. Astoria Fan sands have average QFL percentages of 35-41-24, LmLvLst percentages of 30-47-23, 3 Fmwk%M and 0.74 P/F. The triple-junction sands have average QFL percentages of 28-59-13, LmLvLst percentages of 25-26-49, 9 Fmwk%M and 0.87 P/F. The petrologic data from the modern ocean basins examined in this study can provide useful analogs for interpretation of ancient oceanic sequences. Our data suggest some refinements of, but generally substantiate, existing petrologic models relating sandstone composition to tectonic setting.
Resumo:
Die Europäische Binnenfischerei-Beratungskommission (EIFAC) wurde als Regionalorganisation der FAO im Jahre 1957 gegründet. Es ist ihre Aufgabe, die Binnenfischerei zu fördern und fortzuentwickeln und die Regierungen der Mitgliedsstaaten sowie die FAO in diesem Zusammenhang zu beraten. In der Zeit vom 24.5.-26.5.1994 fand unter der Leitung des Berichterstatters am Sitz der FAO in Rom die 18. Tagung der EIFAC mit über 70 Delegierten und Beobachtern aus 26 Mitgliedsländern statt.
Resumo:
Treatment of the labile cluster [Os3(CO)11(MeCN)] with PH3 affords the substituted product [Os3(CO)11(PH3)](1) in high yield. Subsequent reaction of (1) with Na2CO3 in MeOH, followed by acidification, gives the hydrido phosphido cluster [Os3(µ-H)(CO)10(µ-PH2)](2). When (2) is heated to 45–60 °C in the presence of [Os3(CO)11(MeCN)] a hexanuclear complex with the formulation [Os6(µ-H)2(CO)21(µ3-PH)](3) is obtained. If this reaction is repeated using [Os3(CO)10(MeCN)2] instead of [Os3(CO)11(MeCN)], an acetonitrile-containing product, [Os6(µ-H)2(CO)20(MeCN)(µ3-PH)](4), is obtained. An X-ray analysis of (4) shows that two Os3 triangular units are linked by a µ3-phosphinidene ligand, which symmetrically bridges an Os–Os edge of one triangle and is terminally co-ordinated to one Os atom of the second triangle. When (3) is treated with a weak base, such as [N(PPh3)2]Cl or [PPh3Me] Br, deprotonation to the corresponding cluster monoanion [Os6(µ-H)(CO)21(µ3-PH)]–(5) occurs. Treatment of (5) with a weak acid regenerates (3) in quantitative yield. Thermolysis of (3) leads to a closing up of the metal framework, affording the cluster [Os6(µ-H)(CO)18(µ6-P)], which readily deprotonates to give the anion [Os6(CO)18(µ6-P)]–(7) in the presence of [N(PPh3)2] Cl or [PPh3Me]Br. The same anion (7) may also be obtained by direct thermolysis of (5). An X-ray analysis of the [PPh3Me]+ salt of (7) confirms that the phosphorus occupies an interstitial site in a trigonal-prismatic hexaosmium framework, and co-ordinates to all six metal atoms with an average Os–P distance of 2.31 (1)Å. Proton and 31P n.m.r. data on all the new clusters are presented, and the position of the phosphorus resonance in the 31P n.m.r. spectrum is related to the changes in the environment of the phosphorus atom.
Resumo:
Background Flavonoids are a group of phenolic secondary plant metabolites that are ubiquitous in plant-based diets. Data from anthropological, observational and intervention studies have shown that many flavonoids are bioactive. For this reason, there is an increasing interest in investigating the potential health effects of these compounds. The translation of these findings into the context of the health of the general public requires detailed information on habitual dietary intake. However, only limited data are currently available for European populations. Objective The objective of this study is to determine the habitual intake and main sources of anthocyanidins, flavanols, flavanones, flavones, flavonols, proanthocyanidins, theaflavins and thearubigins in the European Union. Design We use food consumption data from the European Food Safety Authority (EFSA) and the FLAVIOLA Food Composition Database to estimate intake of flavonoids. Results Mean (±SEM) intake of total flavonoids in Europe was 428±49 mg/d, of which 136±14 mg/d were monomeric compounds. Gallated flavan-3-ols (53±12 mg/d) were the main contributor. The lowest flavonoid intake was observed in Mediterranean countries (monomeric compounds: 95±11 mg/d). The distribution of intake was skewed in many countries, especially in Germany (monomeric flavonoids; mean intake: 181 mg/d; median intake: 3 mg/d). Conclusions The habitual intake of flavonoids in Europe is below the amounts found to have a significant health effect.
Resumo:
O objetivo foi de avaliar os efeitos da intensidade do ganho de peso no período de recria, dos 13 aos 18 meses de idade, sobre a taxa de prenhez (TP) de novilhas de corte mantidas em pastagem nativa e acasaladas no sobreano durante o outono. O período experimental foi compreendido entre 15/11/2002 à 20/09/2003, sendo a recria, de 15/11/2002 à 23/04/2003 e o acasalamento, de 24/04/2003 à 07/06/2003. Os tratamentos foram constituídos em: 20 novilhas com peso médio de 208 kg submetidas a um ganho diário médio (GDM) de 0,595 kg/dia (G600); 23 novilhas com peso médio de 197 kg submetidas a um GDM de 0,656 kg/dia (G700) e 24 novilhas com peso médio de 181 kg submetidas a um GDM de 0,723 kg/dia (G800). Os GDM foram estabelecidos para que todos os animais atingissem, aproximadamente, 300 kg ao início da estação de monta. Foram avaliados os efeitos dos tratamentos sobre o peso, a altura da garupa (AG), o perímetro torácico (PT), a relação peso:altura (PA), o escore de trato reprodutivo (ETR) e sobre a TP. Não foram observadas diferenças (P>0,05) no incremento da AG (GAG) e do PT (GPT) e na PA, ao início do acasalamento, em relação aos grupos experimentais. O peso vivo foi altamente correlacionado (P<0,05) com a AG, PT e PA ao longo de todo o período de recria. As taxas de prenhez foram 30,0, 47,8 e 50,0% para os grupos G600, G700 e G800, respectivamente, não existindo diferença significativa entre os grupos (P>0,05). Os grupos G700 e G800, submetidos a maior taxa de ganho de peso, apresentaram maiores valores (P<0,05) de ETR em relação ao G600 ao início da estação de monta. Novilhas com ETR mais elevados apresentaram uma tendência (P>0,05) de maior TP. A TP de novilhas de corte ao sobreano esteve associada com a intensidade de ganho de peso na recria independente das variações de peso no acasalamento.