Habermas e o debate em torno do secularismo: implicações para o lugar da religião na esfera pública

A presente dissertação tem como objetivo principal investigar o conceito de pós-secularismo na filosofia de Jürgen Habermas. Para tanto, buscamos compreender como a religião aparece ao longo da construção do pensamento habermasiano, pontuando as diversas revisões feitas pelo filósofo e suas escolhas metodológicas, que resultaram numa mudança de perspectiva sobre o papel da religião na esfera pública das sociedades contemporâneas. A discussão de Jürgen Habermas se insere num debate mais amplo sobre o reexame do conceito de secularismo, envolvendo não apenas a filosofia, mas a ampla gama das ciências humanas e sociais. Assim, procuramos apresentar o contexto geral desse debate e os principais interlocutores com quem ou contra quem Habermas constrói sua argumentação. Por fim, tentamos mostrar de que maneira as revisões feitas por Habermas nos seus últimos escritos a respeito da religião, bem como a apropriação do conceito de sociedades pós-seculares, se enquadram na moldura geral da teoria habermasiana, principalmente dentro da estrutura do agir comunicativo e da política deliberativa.

Sobre o conceito de desenvolvimento: da imagem de ocidente ao imaginário ocidental

Esta dissertação trata da construção sociológica do conceito de desenvolvimento, caracterizando-o como imaginário social, temporalidade explícita e auto-atribuída do socialhistórico (nos termos de Cornelius Castoriadis). Este imaginário é um conjunto entrelaçado de significações articuladas cosmologicamente e tributárias de uma teologia, mesmo em suas simbologias e concepções secularizadas. Essa cosmologia se sobrepõe a uma concepção de natureza humana distinta e a uma ontologia ocidental dualista. Neste quadro, o desenvolvimento aparece como conceito central da cosmologia ocidental e da ciência social, que orquestra essas significações no imaginário imprimindo a necessidade de uma ordenação de elementos com vistas a uma finalidade paramétrica ou valorativa, uma versão de teodicéia complementada por uma governamentalidade elementos formados pelo encontro da tradição bíblica com o pensamento grego. O desenvolvimento é a expressão paradigmática do imaginário social ocidental. Ao traçar suas características principais, explorando um pouco de suas origens, o conceito de desenvolvimento é reconstruído como um instrumento analítico para permitir a comparação entre as diversas concepções particulares e específicas de desenvolvimento encontradas no pensamento social e na política contemporânea.

Religião, ensino religioso e cotidianos da escola: discutindo a laicidade na rede pública estadual do Rio de Janeiro

As diferentes religiões circulam no espaço escolar como mais um elemento das diferenças que caracterizam e desafiam a escola. Por esse motivo, devem ser respeitadas. Entretanto, nem sempre a escola se mantém laica e, muitas vezes, as religiões aparecem de forma desigual e segregadora. Enquanto algumas, em especial, as cristãs, são exaltadas, outras são reprimidas ou invisibilizadas, o que demonstra um desrespeito às diferenças religiosas e à laicidade da escola. Nesse sentido, faz-se necessário abordar a questão complexa e conflituosa das diferenças culturais e religiosas no espaço escolar e as suas consequências no processo de ensino-aprendizagem e sensação de pertencimento dos estudantes, em especial dos adeptos das minorias religiosas. Para a investigação e análise da presença da religião no espaço escolar e os impactos causados por ela, a cultura material escolar tem grande relevância. Através dos objetos encontrados na escola, ou até mesmo, através da ausência deles, podemos aferir como a escola trata a diferença e como ela pode se tornar um agente fomentador de intolerância religiosa. Livros didáticos, murais, avaliações, entre outros materiais, são fontes importantes. Além disso, a forma como os educadores tratam a questão também é uma importante fonte para a análise da presença das religiões e seus embates no cotidiano escolar. Dentro dessa discussão, entra a religião legitimada, dentro da escola, através da disciplina de Ensino Religioso, sua contextualização histórica, interesses políticos e religiosos e suas consequências.

Autonomia legislativa e participação igualitária: o Direito Político de Jean-Jacques Rousseau no desenvolvimento do problema teológico-político da modernidade

O presente trabalho tem por objetivo apresentar os conceitos de lei e soberania no Contrato Social de Rousseau sob uma perspectiva histórico-filosófica, retratando o surgimento do modelo filosófico-jurídico da legitimação do poder a o nascimento (ou renascimento, a depender de como se considere o período imperial romano) do conceito de soberania como completa liberdade em relação às leis existentes, ou sujeição apenas à própria razão. A partir desse fato histórico, como de outros relativos à filosofia tardoescolástica de Escoto, com sua distinctio formalis ex natura rei que permitiu a emergência de uma antropologia como a de Rousseau, que divide os seres humanos em camadas sobrepostas e o voluntarismo nominalista de Ockham, que permitiu a elaboração de um conceito como vontade geral. Procura-se demonstrar também como a concepção nominalista de um Deus absconditus tornou a justificação de um poder que é pura vontade separada daqueles que ordena ininteligível. Neste sentido, a crise de heteronomia em relação à transcendência que não é pura heteronomia, mas participação na ordem criada acaba gerando uma crise da heteronomia em razão ao poder secular, dando origem à autonomia soberana do povo pela vontade geral.

Análise morfométrica das estruturas maxilo-mandibulares de indivíduos pré-colombianos e contemporâneos da Costa Central do Peru

O objetivo deste trabalho foi avaliar morfometricamente as modificações ocorridas ao longo de 500 anos nas estruturas maxilo-mandibulares de indivíduos da Costa Central do Peru. Foram utilizadas telerradiografias laterais de 30 crânios secos, sem deformidades esqueléticas e em normoclusão, do período Pré-colombiano (grupo Pré-colombiano) e de 30 peruanos nativos contemporâneos, com características esqueléticas e oclusais semelhantes, provenientes da mesma região geográfica (grupo Contemporâneo). Estas telerradiografias foram digitalizadas e 14 pontos cefalométricos foram marcados e utilizados como marcos anatômicos homólogos para a análise morfométrica. O tamanho do centróide, a forma e a alometria foram comparados entre os grupos para a amostra total, para homens e para mulheres, pelos testes de one-way ANOVA, função discriminante e regressão multivariada, respectivamente. As mesmas avaliações foram realizadas para homens e mulheres do mesmo grupo. O tamanho do centróide foi significativamente maior para o grupo Contemporâneo tanto para a amostra total, quanto para homens e mulheres, demonstrando que as estruturas maxilo-mandibulares dos indivíduos contemporâneos é maior do que de seus ancestrais. Quando homens e mulheres foram comparados intra-grupos o tamanho do centróide foi significativamente maior para os homens do grupo Contemporâneo, com a mesma tendência para os homens pré-colombianos, porém sem significância estatística. Observou-se diferenças significativas entre os grupos para a forma das estruturas maxilo-mandibulares indicando que ao longo do tempo houve um deslocamento posterior da região da pré-maxila e um deslocamento considerável para cima e para trás da apófise coronóide, uma abertura do ângulo na região goníaca e um alongamento no sentido vertical da região da sínfise mandibular. Essas mudanças morfológicas foram mais evidentes nas mulheres do que nos homens, parecendo haver maior efeito das tendências seculares nas mulheres. Não houve diferenças morfológicas entre homens e mulheres quando comparados intra-grupos, demonstrando que os resultados observados não foram influenciados pelo dimorfismo sexual. As diferenças de tamanho existentes intra-grupos foram responsáveis por apenas 6% das diferenças de forma, e portanto não há efeito causal do tamanho sobre as diferenças de forma observadas entre os grupos. Pode-se concluir que as diferenças morfológicas das estruturas maxilo-mandibulares encontradas neste estudo sugerem mudanças nas condições ambientais da população da Costa Central do Peru ao longo de 500 anos e podem contribuir para o melhor esclarecimento dos fatores etiológicos das más oclusões.

Dos quintais às prateleiras: as imagens quilombolas e a produção da louça em Itamatatiua - Alcântara - Maranhão

Esta pesquisa aborda os diversos sentidos atribuídos à produção de louça por mulheres que moram em Itamatatiua, uma comunidade remanescente de quilombo localizada em Alcântara, Maranhão. Em uma etnografia, a sua secular produção de louça é analisada à luz da categoria zona de contato, enquanto âmbito privilegiado para a observação dos discursos pelos quais as fazedoras de louça de Itamatatiua constituem-se não apenas como quilombolas, mas também como mulheres, pretas, e artesãs. Habitando um território considerado terras de Santa Tereza, as mulheres de Itamatatiua constroem suas narrativas em relação às suas percepções sobre os atores externos ao povoado, como os turistas, pesquisadores, consultores de design que buscam nas suas territorialidades uma forma de acessar o passado. O resultado compartilhado e percebido é o que denomino imagens quilombolas. Estas imagens, constituídas de narrativas, formas de agir e pensar e aqui assumidas também como imagens gráficas (fotografias, peças gráficas e material audiovisual) revelam camadas históricas e discursos hegemônicos que são ressemantizados nos constantes encontros com turistas e pesquisadores, incluindo a mim mesma como pesquisadora e designer. As narrativas das mulheres sobre o saber-fazer da louça, sobre o seu imaginário sobre os turistas, sobre o que os consultores buscam no quilombo são alguns entre outros componentes das imagens quilombolas.

Conspirando música: uma etnografia macrossociologicamente informada do conceito goffmaniano de equipe

Este trabalho é um estudo sociológico sobre o dia a dia de um grupo de indivíduos envolvidos na e pela realização conjunta e simultânea de um processo coletivo de produção, isto é, pela coordenação de ações a um só tempo com vistas a um objetivo coletivo comum. Quando se entende o coral da Escola JXa como uma equipe goffmaniana, este objetivo coletivo comum passa a ser a manutenção de uma impressão diante de um público através da produção musical. Assim, busca-se descrever aqui como os integrantes daquele coral conjugavam seus esforços para parecerem músicos apresentando músicas para uma audiência. Necessariamente, isso implica na mobilização proficiente de parâmetros culturais já estabelecidos como musicais em determinada sociedade. Deste modo, para que aquela equipe pudesse almejar a manutenção de uma impressão, seus integrantes precisariam ter aprendido a entender e a reproduzir convenções musicais. Daí a importância para a análise de se considerar a longa duração de um campo bourdieusiano. No caso do coral da Escola JXa, as convenções de produção musical eram sintetizadas pela formação SATBar, através da qual se dividia funcionalmente o coral em quatro tipos de cantores − soprano, contralto, tenor e barítono. Além desta categorização, de origem europeia e renascentista, a presença de uma regente e de um conjunto de instrumentistas também se apresentava como condicionamento histórico da produção musical daquela equipe. Assim, tenta-se entender como se construíam identidades individuais − de músicos - e coletiva − de um coral − através da atualização situacional de um cânone secular. Além disso, busca-se caracterizar as dinâmicas entre o dia a dia daquele coral e instituições macrossociais mais amplas - como a classificação heteronormativa dos gêneros −, mediadas pelas convenções musicais. Finalmente, descreve-se como se manifestava o imperativo categórico situacional dos integrantes do coral − manter-se leal à manutenção da identidade da equipe − imediatamente antes, durante e imediatamente depois das apresentações em público.

U.S. west coast relative sea levels from tide gauges [abstract]

EXTRACT (SEE PDF FOR FULL ABSTRACT): Examining secular changes in relative sea level along the U.S. west coast, we have identified strong tectonic signals. Tectonism exists not only on a coherent plate-wide scale (assuming a rigid plate approximation), but also on a sub-plate scale. In fact, differential tectonism between exotic or suspect geological terrain explains much of the spatial patterns of west coast tide-gauge data. Peltier's isostatic model appears not to explain the spatial pattern, implying glacio-isostatic adjustment is not the dominant contribution to the low-frequency signals. Eustatic effects cannot be identified unambiguously. These studies suggest several major questions/observations with regard to relative sea-level studies ...

Stratigraphy and chronology of Holocene marine sedment core from the California continental borderland and their paleoceanographic/paleoclimatic significance [abstract]

EXTRACT (SEE PDF FOR FULL ABSTRACT): Paleomagnetic secular variation (PSV) records have been recovered from three marine sediment cores from Santa Catalina basin, California continental borderland, in order to more accurately date these late Quaternary sediments. ... The sedimentation rates derived from the time/depth curves suggest a constant rate of 20-25 cm/ky for the last 6700 years throughout Santa Catalina basin, and more variable rates (but constant within each core) of 13-86 cm/ky prior to 6700 ybp. The sedimentation rates prior to 6700 ybp are lowest in the southcentral portion of the basin and systematically increase toward the north end of the basin. These results suggest that 6700±300 ybp marks a major change in paleoceanographic processes within Santa Catalina basin.

Calibration of an audio-frequency ion trap mass spectrometer

A method for calibration of an audio-frequency (AF) ion trap mass spectrometer is described. The method is proposed to surmount the obstacle that there is a lack of a proper calibrant for mass spectrometers in the mass-to-charge ratio (m/z) range of 10(6) to 10(10). To calibrate such mass spectra, we determine the point of ejection, q(eject), on the stability diagram of the ion trap operated in a mass-selective axial instability mode. This is accomplished by measuring the radial secular frequencies (and therefore, the m/z value) of a single trapped particle using a light scattering method, followed by monitoring the action of particle ejection in real time to obtain the q(eject). A delayed ejection with q(eject) = 0.949 +/- 0.004 is found at a trap driving frequency of Ohm/2pi = 200-600Hz. Theoretical analysis for the origin of the delayed ejection indicates that the delay is predominantly resulted from the existence of multipole components in the fields due to trap imperfections. Inclusion of -3% of the octopole with respect to the basic quadrupole field can satisfactorily account for our observations. An m/z accuracy approaching 0.1% is attainable after proper calibration of the AF ion trap mass spectrometer. (Int J Mass Spectrom 214 (2002) 63-73) (C) 2002 Elsevier Science B.V. All rights reserved.

地磁场的长期变化

In this paper, we studied the secular variations of the main geomagnetic field during 1900-2000 in details. Emphasis is put on three aspects of the secular variations, i.e. westward drifts and intensity variations of non-dipole part, the decay of the dipole field. Firstly, we introduced the method of correlation analysis of moving random pattern into Geomagnetism in order to overcome the weakness of available methods on westward drift studies. We had committed testing and modifying the method, and analyzed the westward drifts and intensity variations of the non-dipole parts of geomagnetic field and 6 planetary-scale geomagnetic anomalies by this way. The globe and area characters of the westward drifts and intensity variations were discussed in detail. Second, the lat-dependence and dispersion of drift velocities were examined carefully. The results showed the velocities of the different wavelengths (from m = 1 to m = 10) geomagnetic potential were changing with the latitude. The lat-dependence of drift velocities is related to the latitude distributing of the geomagnetic potential. There was a negative dispersion in the westward drift, namely, the components of long wavelength drift faster than that of short wavelengths. Finally, we calculated the moments of the geomagnetic dipole, and found that the intensity of the dipole fields has been decreasing. Linking to the results in paleomagnetism, we draw a conclusion that the geomagnetic polarities may be reversed in 700 years.

华南震旦纪-寒武纪两期成磷事件及其地球动力学意义

Phosphorus is an important biological and ecological element that to a certain degree constrains ecological environment and nutrient (including carbon) cycling. Marine sedimentary phosphorites are the principal phosphorus supply of the mankind. In the eastern to southern margins of the Yangtze Craton, South China, there are two phosphogenetic events at the Doushantuo stage of the Late Sinian and the Meishucun stage of the Early Cambrian respectively, corresponding two explosion events of life across the Precambrian\Cambrian boundary. Phosphorus ores from the Sinian and Cambrian phosphate in South China can be classified roughly into two categories, namely, grained and non-grained phosphorites. Grained phosphorites, hosted in dolostone type of phosphogenetic sequences and with larger industrial values, occur mainly in margins of the Upper Yangtze Platform, formed in shallow-water environments with high hydraulic energy and influenced by frequent sea-level change. Non-grained phosphorites, hosted principally in black-shale type of phosphogenetic sequences and with smaller industrial values, are distributed mainly in the Jiangnan region where deeper-water sub-basins with low hydraulic energy were prevailing at the time of phosphogenesis. Secular change ofδ~(13)C, δ~(18) O, ~(86)Sr/~(87)Sr values of carbonates from Sinian and Cambrian sequences were determined. A negative abnormal ofδ~(13)C, δ~(18)O values and positive abnormal of 86Sr/87Sr values from the fossiliferous section of the Lowest Cambrian Meishucun Formation implies life depopulation and following explosion of life across the PrecambriamCambrian boundary. Based on a lot of observations, this paper put forward a six-stage genetic model describing the whole formational process of industrial phosphorites: 1) Phosphorus was transported from continental weathering products and stored in the ocean; 2) dissolved phosphates in the seawater were enriched in specific deep seawater layer; 3) coastal upwelling currents took this phosphorus-rich seawater to a specific coastal area where phosphorus was captured by oceanic microbes; 4) clastic sediments in this upwelling area were enriched in phosphorus because of abundant phosphorus-rich organic matters and because of phosphorus absorption on grain surfaces; 5) during early diagenesis, the phosphorus enriched in the clastic sediments was released into interstitial water by decomposition and desorption, and then transported to the oxidation-reduction interface where authigenic phosphates were deposited and enriched; 6) such authigenic phosphate-rich layers were scoured, broken up, and winnowed in shallow-water environments resulting in phosphate enrichment. The Sinian-Cambrian phosphorites in South China are in many aspects comparable with coastal-upwelling phosphorites of younger geological ages, especially with phosphorites from modern coastal upwelling areas. That implies the similarities between the Sinian-Cambrian ocean and the modern ocean. Although Sinian-Cambrian oceanic life was much simpler than modern one, but similar oceanic planktons prevail, because oceanic planktons (particularly phytoplanktons) are crucial for phosphate enrichment related to coastal upwelling. It implies also a similar seawater-layering pattern between the Sinian-Cambrian ocean and the modern ocean. The two global phosphate-forming events and corresponding life-explosion events at the Sinian and Cambrian time probably resulted from dissolved-phosphate accumulation in seawater over a critical concentration during the Earth's evolution. Such an oceanic system with seawater phosphorus supersaturation is evidently unstable, and trends to return to normal state through phosphate deposition. Accordingly, this paper put forward a new conception of "normal state <=> phosphorus-supersaturation state" cycling of oceanic system. Such "normal state <=> phosphorus-supersaturation state" cycling was not only important for the three well-known global phosphate-forming events, also related to the critical moments of life evolution on the Earth. It might be of special significance. The favorable paleo-oceanic orientation in regard to coastal-upwelling phosphorite formation suggests a different orientation of the Yangtze Craton between the Sinian time and the present time (with a 135° clockwise difference), and a 25° anti-clockwise rotation of the Yangtze Craton from late Sinian to early Cambrian. During the Sinian-Cambrian time, the Yangtze Craton might be separated from the Cathaysia Block, but might be still associated with the North China Craton.

地磁场的西向漂移和差动旋转

The westward drift is one of the most important characteristics of the secular variations in the main geomagnetic field. The drift exists not only in the main field itself, but also in the secular variation field of the main field. Based on the International Geomagnetic Reference Field (IGRF) models for 1900-2000 and the secular variation model for the period 2000-2005, the characteristics of the westward drift are studied in this paper on several aspects, such as, the bulk rotation and differential rotation of the main field, the dipersion of the drift rates, as well as the westward drift in the secular variation field. The bulk drift and its temporal changes in the main field are analyzed. The results show that the average drift rate during 20th century is 0.183°/α, and the transitions of the drift rate are closely related with the occurrence of geomagnetic jerks. The calculation of the westward drift at various latitudes reveals a latitudinal dependence of the westward drift rate, implying that the geomagnetic field rotates in a differential fashion, instead of rigid rotation. The maximum westward drift is found near the 15°secular variation field of the main field is also discussed in this paper. The results show that the westward drift rate in the secular variation field is much larger than that in the main field. The drift rate of the geomagnetic potential is proposed to represente the westward drift of the whole geomagnetic field, after comparing the spatial patterns, temporal changes, behavior of the westward drift and rationality between the geomagnetic potential and geomagnetic components X, Y and Z.

中-新元古代海洋的硫和碳同位素的演化

Data on seawater carbon isotope in the Mesoproterozoic and Neoproterozoic is abundant. However, the sulfur isotopic age curve of seawater sulfates determined through the analysis of sulfur isotopic composition of marine evaporite is uncertain in the Mesoproterozoic and Neoproterozoic since evaporites are generally rare in Precambrian. The Mesoproterozoic and Neoproterozoic Carbonate Formations preserve not only the carbon isotopic records, but also the sulfur isotopic records of coeval seawater in the Huabei Platform and the Yangtze Platform, China. Sulfur isotopic composition can be determined by the extraction of trace sulfate from carbonate samples. Successive measurements of sulfur and carbon isotopic compositions of carbonate samples from the Mesoproterozoic and Neoproterozoic strata in the Huabei Platform and the Yangtze Platform was accomplished through the extracting of trace sulfate from carbonates. Sulfur and carbon isotopic compositions of coeval seawater were obtained from analytical results of sulfur and carbon isotopes of the same sample without diagenetic alteration. The high-resolution age curve of sulfur isotope given in this paper may reflect the trend of variations in sulfur isotope composition of seawater sulfates during the Mesoproterozoic and Neoproterozoic. It can be correlated with the characteristics of variation in age curve of carbon isotope of coeval seawater carbonates. The δ34S values of seawater varied from +10.3-37.0‰ during the Mesoproterozoic, which took on oscillated variation on the whole. The δ34S values took on high values in the Mesoproterozoic Chuanlinggou stage, Tuanshanzi stage Tieling stage and in Neoproterozoic Jing'eryu stage. The average of those was about +30‰. The sulfates have low δ34S values in the Mesoproterozoic Yangzhuang stage and Hongshuizhuang stage, The average of those was all lower than +20‰. There occured large-amplitude changs in δ34S values of seawater during the Mesoproterozoic. Large-amplitude oscillate of 534S values occured in the intervals of 1600~1400Ma and 1300~1200Ma. The δ13C values of seawater are mostly negative in Changcheng stage of late Paleoproterozoic, -0 ± 1‰ range in Jixian stage of Mesoproterozoic , and the positive 2±2‰ commonly in early Neoproterozoic Jing'eryu stage. From 1000 Ma to 900 Ma, about 108 years interval of oceanic 513C record is shortage. At the end of Paleoproterozoic (1700 - 1600 Ma), the oceanic 813C values change from -3‰ to 0‰, but strongly oscillate near 1600 Ma. Two larger variations of seawater 513C values occur in the Mesoproterozoic: one is a cycle of about 4%o happens at ca. 1400 Ma; another is rise from >2‰ to>5‰ at ca. 1250 Ma and then become stable at the near 1000 Ma. There appears a large positive excursion over +20‰ in 534S value of ancient seawater sulfates in the early Doushantuo stage. Simultaneously, 8 C values of ancient seawater occur a positive excursion reaching 10‰. These allow δ4S values and 513C values to reach high values of+51.7‰ and +6.9‰, respectively. The range of variation in 834S values of seawater is relatively narrow and 513C values are quite high in the middle Doushantuo stage. Then, δ34S values of seawater become oscillating, the same happens in δ13C values. Negative excursions in 834S values and 813C values occur simultaneously at the end of the Doushantuo stage, and the minimum of δ34S values and δ13C values dropped to -11.3‰ and -5.7‰, respectively. The ancient seawater in the Dengying stage has high δS values and δ13C values. Most of the δ34S values of the trace sulfate samples varied between +23.6‰ and +37.9‰ except two boundaries of the Dengying Formation, and the S13C values of the carbonate samples of the Dengying Formation varied between +0.5‰ and +5.0‰. There appeared large negative excursion in 834S values and δ13C values of ancient seawater at the bounder of Precambrian-Cambrian. The isotopic characteristics of sulfur and carbon implicated that the organic productivity and isotopic fractionation caused by biology were low and the palaeoceanic environment was quite unstable during the Mesoproterozoic. The increase and subsequent oscillation of seawater δ13C value occurred from 1700 to 1600 Ma and near 1300 Ma may be responsible to the two global tectonic events happened at coeval time. The characteristics of variation in sulfur and carbon isotopes of ancient seawater imply strong changes in oceanic environment, which became beneficial to inhabitation and propagation of organism. The organic production and the burial rate of organic carbon once reached a quite high level during the Doushantuo stage. However, the state of environment became unstable that means the global climate and the environment possibly were fluctuating and reiterating after the global glaciation. The negative excursions of S34S values and δ13C values occurring at the end of the Doushantuo stage represent a global event, which might be relative to the oxidation of deep seawater. The isotopic characteristics of sulfur and carbon implicated that there were a high organic productivity and a high burial rate of organic carbon in the Dengying stage. It is obvious that the palaeoceanic environment in Dengying stage was stable corresponding and beneficial for biology to inhabit and propagate except for the two boundaries. The tendency of sulfur and carbon isotopic variations maybe resulted from the gradual oxygenation of ocean environment during the Dengying stage. It has been reported that the secular variations of the sulfur isotopic compositions in seawater was negative correlated with that of carbon isotopic compositions. However, our results show that it is not the case. They were negatively correlated in some intervals and positively in some other intervals of the Mesoproterozoic and Neoproterozoic. The difference in correlation may be associated with the changes in conditions of redox in oceanic environment, e.g. sharp change of the oxidation-reduction interface. The strong changes in global environment may induce the abnormality to occur in the biogeo chemical S and C cycles in the ocean and accordingly sharp Variations in isotopic composition of seawater sulfur and carbon during the Mesoproterozoic and Neoproterozoic. Simultaneously, the global tectonism caused large changes of 87Sr/86Sr ratios. The leading factor that causes the variation in isotopic composition is different in the different intervals of the Mesoproterozoic and Neoproterozoic. Thus, there may exist different models of the biogeochemical S and C cycles in the ocean during the Mesoproterozoic and Neoproterozoic.

西南天山托云盆地白垩-新生代古地磁结果及其构造意义

Western China is regarded as an assemblage of blocks or microplates. The India/Asia postcollisional kinematics of these blocks has attracted many geologists to pay attentions, especially on the geodynamics and intracontinental deformation of Tibetan and adjoining parts of central Asia. So far there are still many debates on the amount of continental shortening and extrusion within Western China blocks. Paleomagnetism plays a very important role in the paleogeographic reconstruction and depiction of kinematics of the blocks, however the unequilibrium of paleomagentic data obtained from Western China prevents paleomagnetists from studying the kinematics and intracontinental deformation on the Tibetan plateau and the central Asia. Moreover, shallower inclinations observed in the Cretaceous and Cenozoic terrestrial red sediments in central Asia makes it difficult to precisely estimate the northward convergence of Tibetan plateau and its adjacent areas since the onset of the Indian/Asian collision. In this thesis, detailed rock magnetic, chronological and paleomagnetic studies have been carried out on the Tuoyun Basin in the southwestern Tianshan to discuss the possible continental shortening and tectonic movements since the Cretaceous-Tertiary. Ar-Ar geochronological study has been conducted on the upper and lower basalt series from the Tuoyun Basin, yielding that the lower and upper basalt series were extruded during 115-113 Ma and 61.8-56.9 Ma, respectively. Both the age spectrum and inverse isochron show that the samples from the upper and lower basalt series have experienced no significant thermal events since extrusion of the baslts. Rock magnetic studies including temperature dependence of magnetization and susceptibility during a heating-cooling cycle from temperature up to 600 ℃ suggest that the baslt samples from the lower and upper basalt series are ferromagnetically predominant of magnetite and a subordinate hematite with a few sites of titanomagnetite. The predominant magnetic mineral of the intercalated red beds is magnetite and hematite. Anisotropy of magnetic susceptibility shows that both the baslts and the intercalated red beds are unlikely to have undergone significant strain due to compaction or tectonic stress since formation of the rocks. The stable characteristic remanent magnetization (ChRM) isolated from the most samples of the upper and lower basalt series and intercalated red beds, passes fold test at the 99% confidence level. Together with the geochronological results, we interpret the characteristic component as a primary magnetization acquired in the formation of rocks. Some sites from both the upper and lower basalts yielded shallower inclinations than the reference field computed from the Eurasia APW, we prefer to argue that these shallow inclinations might be related to geomagnetic secular variation, whereas the shallow inclination in the intercalated red beds is likely to be related to detrital remanent magnetization. Paleomagnetic results from the early Cretaceous-Paleogene basalts indicate that no significant N-S convergence has taken place between the Tuoyun Basin and the south margin of Siberia. Furthermore, the Cretaceous and Tertiary paleomagnetic results suggest that the Tuoyun Basin was subjected to a local clockwise rotation of 20°-30° with respect to Eurasia since the Paleocene time, which is probably subsequent to the Cenozoic northward compression of the Pamir arc.