Turbiditic trench deposits at the South-Chilean active margin

The active plate margin of South America is characterized by a frequent occurrence of large and devastating subduction earthquakes. Here we focus on marine sedimentary records off Southern Chile that are archiving the regional paleoseismic history over the Holocene and Late Pleistocene. The investigated records - Ocean Drilling Program (ODP) Site 1232 and SONNE core 50SL - are located at ~40°S and ~38°S, within the Perú-Chile trench, and are characterized by frequent interbedded strata of turbiditic and hemipelagic origin. On the basis of the sedimentological characteristics and the association with the active margin of Southern Chile, we assume that the turbidites are mainly seismically triggered, and may be considered as paleo-megaearthquake indicators. However, the long-term changes in turbidite recurrence times appear to be strongly influenced by climate and sea level changes as well. During sea level highstands in the Holocene and Marine Isotope Stage (MIS) 5, recurrence times of turbiditic layers are substantially higher, primarily reflecting a climate-induced reduction of sediment availability and enhanced slope stability. In addition, segmented tectonic uplift changes and related drainage inversions likely influenced the postglacial decrease in turbidite frequencies. Glacial turbidite recurrence times (including MIS 2, MIS 3, cold substages of MIS 5, and MIS 6), on the other hand, are within the same order of magnitude as earthquake recurrence times derived from the historical record and other terrestrial paleoseismic archives of the region. Only during these cold stages sediment availability and slope instability were high enough to enable recording of the complete sequence of large earthquakes in Southern Chile. Our data thus suggest that earthquake recurrence times on the order of 100 to 200 years are a persistent feature at least during the last glacial period.

Stable oxygen isotope record of Globigerinoides ruber of ODP Site 133-820 off the Great Barriere Reef

Oxygen-isotope ratio measurements are presented for the planktonic species Globigerinoides ruber collected from shallow-water, upper-slope sediments from Holes 820A and 820B in 280 m of water, on the seaward edge of the Great Barrier Reef. Correlation of the Site 820 isotope curve with deep-sea reference curves of the Pacific Ocean (Core V28-238, Hole 677A, Hole 607A) permits the definition of isotope stages 1 to 19 in the top 145 m of Holes 820A and 820B. However, paleontological data indicate that stages 4 and 7 might be missing and that two hiatuses occur at a depth of 8.05 to 12.1 and 34.55 to 35.8 mbsf. Using deep-sea Hole 677A as a reference for ice-volume variations, we determine the difference in isotopic signature between it and Site 820. We propose that this difference is a regional signal representing a progressive 4°C increase in surface-water temperature at Site 820. The proposed temperature change was initiated at about 400 k.y. and corresponds to a change from high-to-low frequency variations in Pleistocene isotope signals. We postulate that these changes may have catalyzed the growth of the Great Barrier Reef. The shift also coincides with changes in seismic character and some physical and chemical sediment characteristics.

Na 1 Nachlass Max Horkheimer, 19 - Korrespondenzen u.a. mit Alfred Haas (p. I 10, 1-250)

20 Briefe zwischen Alfred Haas und Max Horkheimer, 1935-1941; 2 Briefe von Willy Haas an Max Horkheimer, 1938; 3 Briefe zwischen Virginia Haber und Max Horkheimer, 12.09.1945, August 1945; 7 Briefe zwischen Hugo Hahn und Max Horkheimer, 1942-1946; 1 Brief von Max Horkheimer an Charles G. Haines, 23.10.1940; 1 Brief von Max Horkheimer an Hall, 02.07.1939; 2 Briefe zwischen H. Duncan Hall und Max Horkheimer, 04.08.1939, 24.07.1939; 2 Briefe zwsichen Herbert Berkerath und Max Horkheimer, 10.10.1939, 09.10.1939; 23 Briefe zwischen Wolfgang Hallgarten und Max Horkheimer, 1937-1941; 1 Brief von Max Horkheimer an die American Philosophic Society Philadelphia, 15.04.1940; 2 Briefe zwischen Betty Drury und Max Horkheimer, 29.02.1940, 20.02.1940; 6 Briefe zwischen Nina Almond und Max Horkheimer, 1939; 1 Brief von Ruth E. Hollander an Max Horkheimer, 08.09.1938; 1 Brief von dem Brooklyn College an Wolfgang Hallgarten, 29.04.1938; 4 briefe zwischen dem Brooklyn College und Max Horkheimer, 18.05.1938, 17.05.1938; 2 Briefe zwischen Robert Maynard Hutchins und Max Horkheimer, 02.11.1937, 28.10.1937; 2 Briefe zwsichen Hardt und Max Horkheimer, 01.10.1943; 4 Briefe zwischen Gertrude Hardt und Max Horkheimer, 1947-1948; 4 Briefe zwischen den Harper & Brothers New York und Max Horkheimer, 24.10.1950, 1950; 1 Brief von Friedrich Pollock an Margot von Mendelssohn, 13.09.1950; 1 Brief von Hartoch an Max Horkheimer, 09.06.1937; 4 Briefe zwischen dem Harvard College Cambridge Massachusetts und Max Horkheimer, 1939-1940; 3 Briefe zwischen Felix Hase und Max Horkheimer, 1936, 13.03.1936; 1 Brief von Freda E. Hecht an Max Horkheimer, 01.03.1947; 1 Brief von Ernest S. Hediger an Max Horkheimer, 02.09.1940; 2 Briefe zwischen Agnes Heilbut und Max Horkheimer, 18.07.1938,; 7 Briefe zwischen Eduard Heimann und Max Horkheimer, 1936-1939; 1 Brief von Fritz Hein an Max Horkheimer, 14.06.1949; 2 Briefe zwischen Walter Heinemann und Max Horkheimer, 15.02.1945, 12.03.1945; 2 Briefe zwischen Philipp Heller und Max Horkheimer, 16.09.1944, 09.10.1944; 1 Brief von Max Horkheimer an Hellmann, 23.03.1939; 4 Briefe zwischen L. E. Hellmann und Max Horkheimer, 1939; 4 Briefe zwischen P. A. Hemerijk und Max Horkheimer, 1936-1937, 03.02.1936; 5 Briefe zwischen Carl G. Hempel und Max Horkheimer, 1939-1941; 1 Lebenslauf von Hans Henning; 1 Brief von Else Henschke an Max Horkheimer, 24.07.1940; 1 Briefe von Isi Hepner an Max Horkheimer, 23.01.1941; 1 Brief von Leo Löwenthal an Isi Hepner, 03.02.1941; 1 Brief von Gertrude E. Herman anMax Horkheimer, 10.12.1949; 1 Brief von Wilhelm G. Hertz an Max Horkheimer, 29.09.1938; 2 Briefe zwischen Wieland Herzfelde und der National City Bank of New York, 28.11.1939, 30.11.1939; 2 Briefe zwischen Karl Hess und Max Horkheimer, 14.08.1935, 25.10.1934; 4 Briefe zwischen Karl Heymann und Max Horkheimer, 1947, 1949; 19 Briefe zwischen Robert Hilb und Max Horkheimer, 1937-1941; 2 Briefe zwischen Joseph Rosenthal und Max Horkheimer, 12.11.1940, 25.10.1940; 2 Briefe zwischen Henry Church und Max Horkheimer, 14.12.1940, 18.12.1940; 1 Brief von Ellen Hilb an Max Horkheimer, 11.03.1938; 1 Brief von Emil Hilb an Max Horkheimer, 15.04.1939; 2 Briefe zwischen Yoshitaro Hirano und Max Horkheimer, 1936, 23.01.1936; 2 Briefe von Max Horkheimer an Hirsch, 1938; 1 Brief von Arnold Hirsch an Max Horkheimer, 14.07.1949; 4 Briefe zwischen Charles Hirsch und Max Horkheimer, 1937, 1938; 2 Briefe von Max Horkheimer an Ernst Hirsch, Oktober 1938; 1 Brief von Max Horkheimer an Julius Hirsch, 24.02.1942;

Pliocene-Pleistocene oxygen isotope record DSDP Site 586, Ontong Java Plateau, Pacific Ocean i

Oceanographic changes in the western equatorial Pacific during the past 6 Ma are inferred from oxygen isotopic analyses of planktic and benthic foraminifera from Ontong Java Plateau (DSDP Site 586). The taxa are Globigerinoides sacculifer, Pulleniatina, Cibicidoides wuellerstorfi, and Oridorsalis umbonatus. Cooling and ice buildup are indicated by an 18O enrichment of 0.3 per mil in the planktic species near 3.4 Ma. This shift apparently is compensated in the benthic data by a warming of the deep waters by between 1° and 2° C. We suggest that the dominant source of upper deep water supply to the Pacific changed from Antarctic to North Atlantic at that time, the North Atlantic-derived water being warmer. Near 2.8 Ma (approximately) the planktic foraminifera again record an enrichment in 18O (Delta delta18O=0.25 per mil). We suggest ice buildup in the northern hemisphere as the cause, because of subsequent sharp increase in fluctuations of the delta18O signal, that is, instability. The enrichment is magnified in the benthic foraminifera (Delta delta18O = 0.5 per mil) by a cooling of the deep water by 1.5° at the time, presumably signalling a glacial-type reduction of North Atlantic Deep Water (NADW) production. Episodic divergence between the signals of G. sacculifer and Pulleniatina in the Pleistocene apparently reflects periods of increased upwelling in the western equatorial Pacific. The amplitude of ice volume fluctuations cannot be reconstructed from delta18O data alone, unless there are constraints on temperature variations. The increase in amplitude of fluctuation of the benthic and planktic signals during the Pleistocene may be attributed either to an increase in maximum ice volume, or to an increase in the fractionation of continental ice, or a combination of both causes.

Pliocene-Pleistocene carbon isotope record of foraminifera from DSDP Site 89-586

Oceanographic changes in the western equatorial Pacific during the past 6 m.y. are inferred from carbon isotopic analyses of planktonic and benthic foraminifers from Ontong Java Plateau (DSDP Site 586). Sample spacing is 1.5 m (ca. 35,000-75,000 yr). An overall trend of d13C toward lighter values is evident for the last 5 m.y. in all four foraminiferal taxa analyzed (G. sacculifer, Pulleniatina, P. wuellerstorfi, and O. umbonatus). This trend is interpreted as an enrichment of the global ocean with 12C, because of the addition of carbon from organic carbon reservoirs (or lack of removal of carbon to such reservoirs), as a consequence of an overall drop in sea level. Differences between shallow- and deep-water d13C decrease slightly during this time interval, suggesting a moderate drop in productivity. This drop is not sufficient to explain the drop in sedimentation rate, however, much of which apparently must be ascribed to winnowing effects. A marked convergence in the d13C values of planktonic taxa exists within the last 2 m.y. We propose that this convergence indicates nutrient depletion in thermocline waters, caused by the vigorous removal of phosphate in marginal upwelling regions, or by the stripping of intermediate waters in their source regions. No large shifts are seen in the carbon isotope record of the last 6 m.y., in contrast to the oxygen isotope record. Some indication of cyclicity is present, with a period between 0.5 and 1.0 m.y. (especially in the earlier portion of the record).

Response of nannoplankton to major changes in sea-surface temperature at the South Chatham Rise, southeastern New Zealand

A high-resolution history of paleoceanographic changes in the subpolar waters of the southern margin of the Subtropical Convergence Zone during the last 130 kyr, is present in foraminiferal assemblages of DSDP Site 594. The foraminifera indicate that sea-surface temperatures during the Last Interglacial Climax were warmer than today, and that between substage 5d through to the end of isotope stage 2, temperatures were mostly cooler than Holocene temperatures. The paleotemperatures suggest that (1) the Subtropical Convergence was located over the site during substage 5e, later moving further north, then moving southwards to near the site during the Holocene, and (2) the Polar Front was positioned over the Site during glacial stages 6, 4, 2 and possibly parts of stage 3. Several major events are indicated by the nannofloral assemblages during these large changes in sea-surface temperature and associated reorganization of ocean circulation. First, the time-progressive trends between E. huxleyi and medium to large Gephyrocupsa are unique to this site, with E. huxleyi dominating over medium Gephyrocupsa during stages 5c-a, middle part of stage 4 and after the middle point of stage 3. This unusual trend may (at least partly) be caused by the shift of the Polar Front across the site. Second, upwelling flora (E. huxleyi and small placoliths) increase in abundance during stages 1, 3 and 5, suggesting that upwelling or disturbance of water stratification took place during the interglacials. Thirdly, there are no significant differences between the distribution patterns of the various morphotypes of medium to large Gephyrocupsu, and the combined value of all medium Gephyrocupsu increases in abundance during glacials (stages 2 and 4 and the end of stage 6), similar to the abundance trends in benthic foraminifera. Finally, subordinate nannofossil taxa also show distinctive climatic trends during the last glacial cycle: (1) Syrucosphaera spp. are present in increased abundance during warmer extremes in climate (substages 5e, 5a, and stage 1); (2) Coccolithus pelagicus and Culcidiscus leptoporus dominate the subordinate nannofossil taxa, and their relative proportions seem to provide a useful paleoceanographic index, with C. pelagicus dominating when the Polar Front Zone is over the site (stages 6, 4 and 2), whilst C. leptoporus is relatively more abundant when the STC is positioned over the site (stages 1 and 5e). Increased abundance of C. pelagicus also can indicate intensified coastal upwelling.

The influence of number of counts in the myocardium in the determination of reproducible functional parameters in gated-SPECT studies simulated with GATE

Myocardial perfusion gated-single photon emission computed tomography (gated-SPECT) imaging is used for the combined evaluation of myocardial perfusion and left ventricular (LV) function. The aim of this study is to analyze the influence of counts/pixel and concomitantly the total counts in the myocardium for the calculation of myocardial functional parameters. Material and methods: Gated-SPECT studies were performed using a Monte Carlo GATE simulation package and the NCAT phantom. The simulations of these studies use the radiopharmaceutical 99mTc-labeled tracers (250, 350, 450 and 680MBq) for standard patient types, effectively corresponding to the following activities of myocardium: 3, 4.2, 5.4-8.2MBq. All studies were simulated using 15 and 30s/projection. The simulated data were reconstructed and processed by quantitative-gated-SPECT software, and the analysis of functional parameters in gated-SPECT images was done by using Bland-Altman test and Mann-Whitney-Wilcoxon test. Results: In studies simulated using different times (15 and 30s/projection), it was noted that for the activities for full body: 250 and 350MBq, there were statistically significant differences in parameters Motility and Thickness. For the left ventricular ejection fraction (LVEF), end-systolic volume (ESV) it was only for 250MBq, and 350MBq in the end-diastolic volume (EDV), while the simulated studies with 450 and 680MBq showed no statistically significant differences for global functional parameters: LVEF, EDV and ESV. Conclusion: The number of counts/pixel and, concomitantly, the total counts per simulation do not significantly interfere with the determination of gated-SPECT functional parameters, when using the administered average activity of 450MBq, corresponding to the 5.4MBq of the myocardium, for standard patient types.

Rosuvastatin prevents myocardial necrosis in an experimental model of acute myocardial infarction

Dyslipidemia is related to the progression of atherosclerosis and is an important risk factor for acute coronary syndromes. Our objective was to determine the effect of rosuvastatin on myocardial necrosis in an experimental model of acute myocardial infarction (AMI). Male Wistar rats (8-10 weeks old, 250-350 g) were subjected to definitive occlusion of the left anterior descending coronary artery to cause AMI. Animals were divided into 6 groups of 8 to 11 rats per group: G1, normocholesterolemic diet; G2, normocholesterolemic diet and rosuvastatin (1 mg·kg-1·day-1) 30 days after AMI; G3, normocholesterolemic diet and rosuvastatin (1 mg·kg-1·day-1) 30 days before and after AMI; G4, hypercholesterolemic diet; G5, hypercholesterolemic diet and rosuvastatin (1 mg·kg-1·day-1) 30 days after AMI; G6, hypercholesterolemic diet and rosuvastatin (1 mg·kg-1·day-1) 30 days before and after AMI. Left ventricular function was determined by echocardiography and percent infarct area by histology. Fractional shortening of the left ventricle was normal at baseline and decreased significantly after AMI (P < 0.05 in all groups), being lower in G4 and G5 than in the other groups. No significant difference in fractional shortening was observed between G6 and the groups on the normocholesterolemic diet. Percent infarct area was significantly higher in G4 than in G3. No significant differences were observed in infarct area among the other groups. We conclude that a hypercholesterolemic diet resulted in reduced cardiac function after AMI, which was reversed with rosuvastatin when started 30 days before AMI. A normocholesterolemic diet associated with rosuvastatin before and after AMI prevented myocardial necrosis when compared with the hypercholesterolemic condition.

La participació en l'esport escolar i l'autoconcepte en escolars de 10 a 11 anys de la província de Guipúscoa. 'La participación en el deporte escolar y el autoconcepto en escolares de 10 a 11 años de la provincia de Guipúzcoa'.

El resumen es traducción del publicado con el artículo

Fighting by sleep-deprived rats as a possible manifestation of panic: effects of sodium lactate

Increased fighting is an effect of desynchronized sleep deprivation (DSD) in rats, and recently this behavior has been suggested to be spontaneous panic and equivalent to panic disorder. In the present study we tested this hypothesis by evaluating the effect of sodium lactate on this aggressiveness, because this substance is recognized to induce spontaneous panic attacks in patients. A total of 186 male albino Wistar rats, 250-350 g, 90-120 days of age, were submitted to DSD (multiple platform method) for 0, 4, or 5 days. At the end of the deprivation period the rats were divided into subgroups respectively injected intraperitoneally with 1.86, 2.98 and 3.72 g/kg of 1 M sodium lactate, or 1.86 and 3.72 g/kg of 2 M sodium lactate. The control animals were submitted to the same procedures but received equivalent injections of sodium chloride. Regardless of DSD time, sleep-deprived animals that received sodium lactate presented a significantly higher mean number of fights (0.13 ± 0.02 fights/min) and a longer mean time spent in confrontation (2.43 ± 0.66 s/min) than the controls (0.01 ± 0.006 fights/min and 0.12 ± 0.07 s/min, respectively; P<0.01, Student t-test). For the sodium lactate group, concentration of the solution and time of deprivation increased the number of fights, with the mean number of fights and mean duration of fighting episodes being greater with the 2.98 g/kg dose using 1 M lactate concentration. These results support the hypothesis that fighting induced by DSD is probably a spontaneous panic manifestation. However, additional investigations are necessary in order to accept this as a promising animal model for studies on panic disorder.

Características da pulverização produzida por pontas Yamaho da série 'D'

This study evaluated the characteristics of spray produced by Yamaho nozzle tip'D'series. The droplet size of nozzle tips D3, D4, D5, D6 and D8 were evaluated at 703, 1.050, 1.406, 1.758, 2.110, 2.461 e 2.813 kPa pressures (100, 200, 250; 350, e 400 psi) by means of laser equipment, as well as the flow rate of nozzle tip at the pressures of 702, 1.125, 1.406, 1.828, 2.110, 2.532 e 2.813 kPa (100, 160, 200, 260,300; 360 e 400 psi) which were compared with values indicated by manufacturer. The droplet produced at all pressures presented a very fine spray, which in agriculture may promote losses by evaporation and drift. For all nozzle tips, except D8 in pressures 1.828, 2.532 e 2.813 kPa, the difference between the observed flow rate indicated by the manufacturer was higher than 5%. The paper demonstrates that the nozzle tip tested, in spite of not having uniform flow rate, may promote the contamination of spray operator and environment due to the droplet spectrum produced.

Desempenho hidráulico de microaspersor autocompensante, novo e usado

Pós-graduação em Agronomia (Ciência do Solo) - FCAV

Efeito de tratamento de superfície do titânio comercialmente puro na resistência de união com cimentos ionomérico e resinosos

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Aspectos metalúrgicos de revestimentos em dutos depositados com a superliga de níquel ERNiCrMo-4 pelos processos MIG convencional e MIG com adição de arame frio

Este trabalho estuda o perfil metalúrgico de revestimentos em dutos depositados pelos processos MIG C e MIG AF. A indústria petroquímica, e outras que utilizam dutos como meio de transporte de seus insumos, depara-se com um grande desafio: como aumentar a vida útil desses dutos em um ambiente severo de trabalho. No caso específico da petroquímica, os dutos servem como meio de transporte para petróleo e gás, que são produtos extremamente agressivos às paredes internas desses tubos que sofrem degradação por corrosão causada, principalmente, pela composição química, pressão e temperatura desses produtos. Nesse contexto a soldagem de revestimentos realizada com ligas à base de Níquel, torna-se uma excelente opção para a construção, reparo e manutenção de equipamentos cuja aplicação seja voltada a ambientes severos de trabalho, tornando possível aperfeiçoar as características requeridas, como por exemplo, a resistência à corrosão. É nesse cenário que surge o mote para a realização desta pesquisa, baseada em trabalhos que indicam que o processo de soldagem MIG/MAG com o da adição de arame frio possui a finalidade de avaliar as características metalúrgicas do revestimento em dutos depositados pelo processo derivativo MIG convencional – MIG-C e MIG com adição de arame frio – MIG AF – utilizando a liga de Níquel ERNiCrMo-4 em dutos de aço carbono. As soldas foram depositadas em dutos de diâmetro de 228,6 mm, formando uma camada de revestimento interno de quatro passes, divididos em três segmentos da circunferência do duto, em três diferentes energias de soldagem: 1,1; 0,9 e 0,7 kJ/mm. Desses segmentos retiraram-se corpos de prova dos dutos para a produção das amostras. Após a metalografia, realizada nas amostras, seguiu-se com a análise e caracterização ao microscópio óptico, microscópio eletrônico de varredura e ensaio de microdureza. Os revestimentos apresentaram excelente qualidade superficial para todos os pacotes operacionais aplicados na obtenção das soldas. As análises das regiões estudadas: metal de base; zona parcialmente misturada e zona termicamente afetada, mostraram-se compatíveis com os da literatura estudada, tanto para o MIG com adição de arame frio, quanto para o convencional. Na ZTA, foram observados valores de Tungstênio em torno de 1,0%, o aumento dos níveis de dureza foi creditado a esse fato. Os resultados de microdureza indicaram que para ambos os casos, MIG C e MIG AF, nas 4 regiões analisadas ocorreram de maneira semelhante, sendo a região da ZTA a que apresentou maiores valores na faixa de 400 a 500 HV, enquanto que nas demais regiões a faixa ficou entre 250 a 350 HV. Os resultados indicam que o processo com arame frio, MIG AF, mostrou-se tão eficiente quanto o convencional, MIG C. A energia de soldagem aumentou a diluição de Fe no metal de solda. Precipitados ricos em Mo e Cr foram encontrados no metal de solda.

Obtenção de um ataque químico padrão, zona de annealing parcial e temperatura de fechamento para o epídoto através do método dos traços de fissão

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)