O refúgio no direito internacional contemporâneo: entre a segurança nacional e a proteção do indivíduo

O direito internacional dos refugiados constitui um dos mais importantes mecanismos de proteção internacional do indivíduo, sendo objeto de Convenção com alto número de ratificações e de legislação nacional ainda mais protetiva. Não obstante o amplo acervo normativo disponível, desenvolvido para lidar com os desafios impostos pelos frequentes fluxos migracionais que marcaram a primeira metade do século XX, fenômenos recentes tornaram evidente a necessidade de revisão, ainda que parcial, de sua estrutura. Políticas de controle de fronteiras adotadas na Europa levaram ao incremento do fluxo de refugiados entre Estados do Sul. Paralelamente, a transferência de parte do controle para fora das águas territoriais europeias fenômeno observado também no sudeste asiático põe o direito internacional dos refugiados em confronto com a regulamentação do direito do mar. Enquanto isto, o Brasil, por não possuir histórico recente relevante de recebimento de migrantes, enfrenta grande dificuldade para garantir até mesmo o reconhecimento da condição de refugiado. Neste contexto, é imprescindível o enfrentamento de tais problemas, compatibilizando o instituto do refúgio com as necessidades das primeiras décadas do século XXI.

Desenvolvimento regional e mercado de trabalho em perspectiva compara-da: Vale do Paraíba Fluminense e Camaçari (BA)

Este trabalho analisa os diferentes rumos do desenvolvimento em duas regiões brasileiras: a me-sorregião do Vale do Paraíba Fluminense e o município de Camaçari, na Bahia. Ao longo dos anos 1990, o Brasil recebeu uma onda de investimentos estrangeiros, com foco especial para as indústrias automobilísticas. Estados e municípios deflagraram disputas pela atração das mesmas, entre eles, o estado do Rio de Janeiro e o estado da Bahia. Em duas regiões de tradição industrial em outras matrizes, observou-se o aporte de indústrias multinacionais automotivas. No entanto, os resultados em termos de desenvolvimento regional foram diferentes. Este estudo buscou estu-dar o desenvolvimento em cada região, cujo ponto de contato se dá na conjuntura da luta pela atração industrial na segunda metade da década de 1990. Entende-se que o contexto inicial de cada região foi fundamental para os diferenciais de desenvolvimento observados. Ao mesmo tempo, destacamos os resultados gerados pela vinda das montadoras automotivas em termos do mercado de trabalho e seus transbordamentos.

3.0～2.0Ma B. P.南海南部深海沉积物孢粉记录及其对全球变化的响应

为了重建东亚季风区域2.5MaB.P.前后植被和气候变化的历史，更好地了解低纬度地区植被变化及其对全球变化的响应，本研究选择了南海南部ODP1143站深海沉积物中的孢粉样品进行研究。通过高分辨率（7ka）的孢粉样品的分析研究，建立起3.0～2.0MaB.P.时段南海深海沉积孢粉组合序列，系统建立了这一时段植被演替序列。在此基础上，重点研究了2.5MaB.P.前后气候变化在南海周边地区植被演替中的响应，为探索和揭示东亚古季风及古环境演变提供了孢粉学依据。 ODP 1143站位于南沙海区，北纬9º22´，东经113º17´，深海柱状样采于水深2772m的大陆坡。本研究以生物地层学和氧同位素年代学为依据建立了年龄框架，对1143站135～95m（3.0～2.6 Ma B. P.）深海沉积中的孢粉样品进行了分析，建立了3.0～2.0MaB.P.时段南海深海沉积孢粉组合序列。孢粉样品处理方法主要是用盐酸去掉钙质和氢氟酸浸泡溶解硅质后，再用筛子将样品在超声波发生器中震荡过滤。孢粉的鉴定和统计在光学透视显微镜下完成。研究结果表明： 1、孢粉谱的主要特征是沉积率变化显著。与3.0～2.6 Ma B. P. 相比，2.6～2.0 Ma B. P.各类型花粉及孢子沉积率均有显著提高。该结果表明2.6 Ma B. P.南海海平面有显著下降，可与北半球冰盖形成、东亚季风增强相对应。 2、2.6 Ma B. P.以来，各类型孢粉沉积率变化与深海氧同位素分期相对应，代表了多次冰期-间冰期旋回。该结果表明南海海平面曾有多次上升和下降。 3、频谱分析结果表明，3.0～2.0 Ma B. P.存在0.1 Ma（偏心率）和46.9ka（斜率）的周期。

A modern pollen record from the central Gulf of California

As one facet of an effort to tie the pollen record of central Gulf of California deep cores to modern analogs, pollen was analyzed in the uppermost 150-200 years of varved core 7807-1410 taken nearby. Sampling at 2- to 8-year resolution yielded a noncomplacent record, suggesting pollen in these sediments may be a potential high resolution proxy record of short-term climatic events. The pollen spectrum as a whole matches that of upper-most DSDP Site 480 (means of all samples). Lack of a ratio or influx shift following damming of local rivers and a surplus of low-spine Compositae pollen relative to mainland sites support Baumgartner's theory that terrigenous influx to the site is largely aeolian and also suggest that a significant fraction of the pollen influx may come from Baja California.

一氧化氮(NO)调节白皮松花粉管生长和细胞壁构建的研究

花粉管是种子植物受精过程中的雄性生殖单位载体，具有典型的顶端极性生长特点，因此成为近年来研究植物细胞间相互识别、胞内外信号传递的模式系统。裸子植物花粉管与被子植物花粉管相比具有萌发时间长、生长缓慢等特点。一氧化氮（NO）作为一个重要的胞内信号分子，参与调节植物生长发育和多种生理过程，但是，有关NO对花粉管生长的作用机制目前尚不清楚。本研究以裸子植物白皮松(Pinus bungeana)花粉为材料，应用不同浓度的NO释放剂SNAP和SNP, NO清除剂cPTIO和哺乳动物一氧化氮合酶抑制剂L-NNA处理，对白皮松花粉萌发和花粉管伸长进行了细胞学研究，从而为进一步揭示NO调控裸子植物花粉管生长机理提供参考。 本论文首先研究了NO释放剂、清除剂及NOS抑制剂对白皮松花粉萌发和花粉管生长的影响。结果显示，SNAP和SNP能够促进白皮松花粉萌发和花粉管伸长，并具有浓度效用，但对其花粉管的形态特征无明显影响；cPTIO和L-NNA能够抑制白皮松花粉萌发和花粉管生长，并且具有浓度效应，同时还可使花粉管顶端膨大呈球形，并丧失花粉管的极性生长。运用NO特异探针DAF-2DA标记显示，SNAP和SNP处理可促进花粉管胞内NO产生；经cPTIO和L-NNA处理后，花粉管内荧光强度比对照花粉管明显减弱。上述结果表明，NO参与裸子植物花粉管极性生长，并且适量NO可以促进花粉管的生长。 用显微注射技术将Ca2+特异探针注射入白皮松花粉管，以检测白皮松花粉管胞内Ca2+浓度梯度。结果显示，SNAP和SNP处理后，NO荧光增加的同时，花粉管顶端Ca2+浓度梯度增加。与此相反，cPTIO和L-NNA处理后，NO荧光降低的同时，花粉管顶端Ca2+浓度梯度也相应降低。应用非损伤微测技术测定花粉管胞外Ca2+内流，结果显示，SNAP和SNP促进胞外Ca2+内流，而cPTIO和L-NNA则抑制胞外Ca2+内流。据此，我们推测，在白皮松花粉管中，NO可能通过调节胞外Ca2+内流来调节胞内Ca2+浓度梯度，然而，我们不能排除在NO信号传递过程中，胞内Ca2+库可能影响胞内Ca2+浓度梯度。 通过微丝特异探针标记的白皮松花粉管显示，SNAP和SNP可使花粉管顶端细微丝束解聚，而cPTIO和L-NNA处理后，花粉管中微丝聚合，尤其在花粉管顶端形成粗的微丝束，并一直延伸到花粉管的最顶端。结合上述Ca2+结果，我们认为，经NO处理后，白皮松花粉管微丝骨架的动态变化，可能是通过Ca2+浓度来进行调控的。通过FM4-64探针标记显示，正常生长白皮松花粉管胞吞作用主要集中在顶端和亚顶端，并且形成倒“V”形的分布模式，SNAP与SNP处理后荧光分布模式与对照花粉管类似，但达到饱和所用时间相对较短；而L-NNA处理后顶端膨大丧失极性的花粉管，荧光分布在膨大花粉管靠近质膜的区域，未见倒“V”形分布模式；经L-NNA处理后，顶端没有膨大的花粉管，荧光几乎均匀分布于整个花粉管，并且L-NNA处理后达到饱和的时间较对照长。上述结果表明，适量NO能够促进白皮松花粉管胞吞。 免疫抗体标记技术分析发现，对照花粉管的酯化果胶质和AGPs都集中在顶端，酸性果胶质分布在侧壁，胼胝质均匀分布在整个花粉管壁上。L-NNA处理后的花粉管，在其顶端出现酸性果胶和酯化果胶，以及有胼胝质积累，而AGPs则分布在花粉管的基部。运用傅里叶红外光谱技术（Fourier Transform Infared Spectroscopy, FTIR）技术分析白皮松花粉管顶端细胞壁成分，结果显示，SNAP处理后花粉管顶端酯化果胶增加而酸性果胶降低；与之相反，经L-NNA处理后的花粉管，其顶端酯化果胶降低而酸性果胶增加。 综上所述，在白皮松花粉管中，NO促进胞外Ca2+内流，从而维持胞内Ca2+浓度梯度，进而影响花粉管顶端微丝骨架的组装，促进囊泡运输，使花粉管顶端酯化果胶累积，最终促进花粉管的正常生长。

Hydrological studies of Matatilla Reservoir, Uttar Pradesh

Matatilla Reservoir, located in semi arid region, (Lat. 25 degree 15'N and Long. 78 degree 23'E) has an area (at FRL) of 13,893 ha, volume and shore development 0.663 and 1.65, shoreline 73.6 km. Volume and shore development indicate that greater part of the reservoir is shallow, which is a favourable point for fish productivity. Temperature and dissolved oxygen gradually decreased with the increase in depth. Carbon dioxide was absent from the surface but invariably present in the bottom (3.6 ppm) pH remained alkaline (7.2-8.4 ppm) throughout the year. Alkalinity, chloride, calcium, magnesium, hardness and priductivity was maximum in pre-monsoon and minimum in monsoon except for calcium and manganesium in post-monsoon. Phosphate, nitrogen and ammonical nitrogen were found in traces. These variations may be due to influx and outflow of water and use of reservoir water for multipurpose activities.

Studies on the seasonal cycle of sea surface temperatures, salinities and phytoplankton in Puttalam Lagoon, Dutch Bay and Portugal Bay along the west coast of Ceylon.

The monthly average temperatures at Puttalam Lagoon, Dutch Bay, Portugal Bay towards Kovilmunai and Portugal Bay towards Pallugaturai showed a distinct annual cycle. The peak was in April and values gradually fell till September. There was a further gradual fall in temperature from October to January. The highest temperatures in all four stations were in April. The highest salinities in all the stations were from May to October i.e., during the south-west monsoon. The salinities at Dutch Bay and Portugal Bay were high in March and April corresponding to the highest temperatures reached during these months. Two maxima have been observed in phytoplankton production. A primary maximum in May-June and a secondary maximum in October. The primary and secondary maxima are due to the influx of nutrient laden waters from the rivers Kal Aru and Pomparippu Aru. The phytoplankton producing blooms were Rhizosolenia alata. Rhizosolenia imbricata, Chaetoceros lascinosus, Chaetoceros pervianus, Ch,aetoceros diversus, Coscinodiscus gigas, Thallasionema nitzschioides, Thalassiosira subtilis, Thallassiothrix frauenfeldii, Asterionella japonica, Sceletonema costatum, Bacteriastrum varians and Biddulphia sinensis. Sudden outbursts of a single species were common. These diatoms were species of Chaetoceros and Rhizosolenia, and Thallassiothrix frauenfeldii. Wide fluctuations have been observed in the distribution of phytoplankton but no definite conclusions can be drawn as the period of observation was only one year.

The fisheries resources of Lake Nakivali

Lake Nakivali is one of the four small lakes that form what is known as the koki lake sysyem. It is 14km long,6km wide.26km sqaured in area and has maximum depth of 3.5m at high water level. The lake is located in lake-swamp complex with river Rwizi as the principle inflow, and a number of peripheral lakes among which are four major ones,i.e Lake Nakivali, Mburo, Kachira and Kijanebalola. Lake Nakivali is a controlled lake with four official landing sites, namely: Kikusi, Kahirimbi, Kashojwa and Rukinga. The latter three are located within a Refugee settlement whereas Kikusi is outside. The Nakivali Refugee settlement initially established for Rwandese of Tutsi origin in 1963, now has at least seven nationalities which include people from Rwanda, Democratic Republic of Congo, Somalia, Sudan, Ethiopia, Kenya and Eritrea. By the end of 2006, the lake’s hinterland of about 378 km squared contained 43,448 people of whom 22,448 were refugees. This large population has had stressful impacts on both land and lake resources to the extent that now there is an apparent overfishing on the lake.

A comparative ecological study on internationally important wetlands of Khoor-e-Kolahy and Tiab

Ecological study on Kolahy and 'flab estuaries were carried out during 1996-1997. Water and sediment sampling was done seasonally. In order to study the physical and chemical characteristic of the water, various animal fauna from different material niches including planktons and fish from water, benthousi from the sediment , and surface living animal such as Arthropod (Crabs) and Waterbirds were identified. I he result shoved, that water salinity of both estuaries was the same as the general salinity existing its the Persian Gulf water, and its variation is same IN those waters Minimum water salinity in both estuaries are seen during Bahairdan or early winter mooth(Jaa.), which is about 31ppt and Maximum is during .rirldlun.) or summer mouth at about 19 ppt. Dissolved otygen and pH are slime as the general Persian Gulf waters., Dissolve Oxygen being directly associated to temperature and its fluctuation is between 7- Sing/I and pH between 7.5-LS. The animals of both estuaries are almost similar having a sal factory species diversity . The birds of the region are often seasonal migrants , the maximum population of which occurs in winter season and the minimum during summer month. Nam coverage is richer in Tiab than Kolahy estuary, where in Kolahy a signal Mangrove tree is in exigence. 'Ile total coverage of Mangrove forest in Tiab is estimated about -29 hec.Both estuaries are included with in the international Ramsar Convention sites in 1971. Due to national importance of these estuaries inproviding refugee for various birds species and also hinting grounds and access traffic for local fishing vehicles, Actiog as an important access for various inhabitancy living with these area of the Persian Gulf. Due to importance or prawn aquacultur for the economical well being of local inhabitance, these areas provide a suitable grandees for prawn production. I-test statistics show, there are no significant difference among various invertebrate and vertebrate animals. In over all out look 21) phytoplankton genera, 21) zeoplankton genera 17 miafauna and 32 roaerofauna genera , 11 different species Carcineacearions and 119 species of walerbirds were identified with in the Tiab and Kolahy estuariesregioos. The X statistic show that the animal density is directly associated to season. Where density of miofauna and maerofauna in both estuaries are in maiticrourn during summer and the minimums existing during the winter season. In addition the bentic invertebrate population density in closlly association to birds population density since , the later, feeds on the former animals. Where the increasing in bird population density during the winter season, the bentic invertebrate animal population density decreases. The over all trend of animal population density in winter tend to increased towards the summer seasons, which this is due to climatic conditions of the region. The bird population on the contrary to other animals of both estuaries tend to increase from summer towards the winter seasons and which this bird population density is in maximum in winter with in the region.

The Nile perch fishery: traditional and emerging fisheries, overfishing and the use of illegal gears on Lake Albert

The fisheries of Lake Albert have come under increasing focus due to several driving forces that have synergistically evolved resulting into concerns from diverse stakeholders. The driving forces include: the commercialization of the fisheries with entry into the value chain of industrial fish processing, a decline in fish stocks especially of the large-size fishes and the emergency of the light - fishing targeting small pelagic fishes. In addition, the assumption by some opinion leaders that light-fishing (use of light) has destroyed the Nile perch fishery of Lake Albert, other factors such as cross-border fishing conflicts, the emergence of oil, an influx of traders in fish-related activities, and the limited regulatory and enforcement regimes for the diverse commercially exploited fish fauna of Lake Albert all require continuous information and action.

Increased gas production from hydrates by combining depressurization with heating of the wellbore

To extract gas from hydrate reservoirs, it has to be dissociated in situ. This endothermic dissociation process absorbs heat energy from the formation and pore fluid. The heat transfer governs the dissociation rate, which is proportional to the difference between the actual temperature and the equilibrium temperature. This study compares three potential gas production schemes from hydrate-bearing soil, where the radial heat transfer is governing. Cylindrical samples with 40% pore-filling hydrate saturation were tested. The production tests were carried out over 90 min by dissociating the hydrate from a centered miniature wellbore, by either lowering the pressure to 6, 4, or 6 MPa with simultaneous heating of the wellbore to 288 K. All tests were replicated by a numerical simulation. With additional heating at the same wellbore pressure, the gas production from hydrates could, on average, be increased by 1.8 and 3.6 times in the simulation and experiments, respectively. If the heat influx from the outer boundary is limited, a simulation showed that the specific heat of the formation is rapidly used up when the wellbore is only depressurized and not heated. © 2012 American Chemical Society.

Effects of ammonium on growth, nitrogen and carbohydrate metabolism of Potamogeton maackianus A. Benn

Growth, nitrogen and carbohydrate metabolism in relation to eutrophication were studied for a submerged plant Potamogeton maackianus, a species common in East Asian shallow lakes. The plants were grown in six NH4+-N concentrations (0.05, 0.50, 1.00, 3.50, 5.00 and 10.00 mg/L) for six days. NH4+-N levels in excess of 0.50 mg/L inhibited the plant growth. The relationships between external NH4+-N availability and total nitrogen (TN), protein-N, free amino acid-N (FAA-N) and NH4+-N in plant tissues, respectively, conformed to a logarithmic model suggesting that a feedback inhibition mechanism may exist for ammonium uptake. The response of starch to NH4+-N was fitted with a negative, logarithmic curve. Detailed analysis revealed that the influx NH4+-N had been efficiently incorporated into organic-N and eventually stored as protein at the expense of starch accumulation. These data suggest that this species may be able to tolerate high levels of ammonium when dissolved oxygen is sufficient.

Distribution of phytoplankton in the Three-Gorge Reservoir during rainy and dry seasons

After damming of the Yangtze River, in order to explore the impacts of the Three-Gorge Dam (TGD) on the aquatic ecosystem, phytoplankton composition, abundance and biomass spatial distribution were studied in the Three-Gorge Reservoir (TGR), and the closest upstream anabranch Xiangxi River, which is 38 kin away from the Three-Gorge Dam (TGD) during August (rainy season) 2004 and April (dry season) 2005. In surveys, 6 transects (2 downstream and 4 cross-stream) and 25 stations have been investigated and 314 samples were collected from the surface to the river bed with water samplers. In TGR, 63 taxa and 60 taxa were identified in the rainy and dry seasons, respectively. In the Xiangxi River, 39 taxa were observed in the rainy and dry seasons. Algal blooms occurred in the Xiangxi River and at the influx region of the Yangtze and Xiangxi in both seasons, but had not occurred prior to damming. In the rainy season, the dominant species was Chroomonas acuta with 1.84 x 10(7) cells l(-1), and in the dry season the dominant species were Asterionella formosa and Cryptomonas ovata with 1.34 x 10(7) cells l(-1) and 1.79 x 10(6) cells(.)l(-1), respectively. In the main channel of TGR, there were no significant correlations between phytoplankton abundance and the concentrations of the main soluble nutrients. In the Xiangxi River, significant negative correlations were observed between phytoplankton abundance and nitrate (Spearman, p < 0.01, n=21), phosphate (Spearman, p < 0.05, n=21) and silicate (Spearman, p < 0.01, n=21) in the rainy season, and similar correlations were also observed with nitrate (Spearman, p < 0.05, n=28) and silicate (Speannan, p < 0.01, n=28), but not with phosphate in the dry season. Since the damming of the Yangtze River, eutrophication in the anabranch within the backwater has occurred and become severe, and the frequency of algal bloom within TGR and anabranches is expected to increase. (c) 2006 Elsevier B.V. All rights reserved.

Intercellular calcium wave propagation in linear and circuit-like bone cell networks

In the present study, the mechanism of intercellular calcium wave propagation in bone cell networks was identified. By using micro-contact printing and self-assembled monolayer technologies, two types of in vitro bone cell networks were constructed: open-ended linear chains and looped hexagonal networks with precisely controlled intercellular distances. Intracellular calcium responses of the cells were recorded and analysed when a single cell in the network was mechanically stimulated by nano-indentation. The looped cell network was shown to be more efficient than the linear pattern in transferring calcium signals from cell to cell. This phenomenon was further examined by pathway-inhibition studies. Intercellular calcium wave propagation was significantly impeded when extracellular adenosine triphosphate (ATP) in the medium was hydrolysed. Chemical uncoupling of gap junctions, however, did not significantly decrease the transferred distance of the calcium wave in the cell networks. Thus, it is extracellular ATP diffusion, rather than molecular transport through gap junctions, that dominantly mediates the transmission of mechanically elicited intercellular calcium waves in bone cells. The inhibition studies also demonstrated that the mechanical stimulation-induced calcium responses required extracellular calcium influx, whereas the ATP-elicited calcium wave relied on calcium release from the calcium store of the endoplasmic reticulum.

Palaeoenvironmental changes from pollen record in deep sea core PC-1 from northern Okinawa Trough, East China Sea during the past 24 ka

A pollen record of core PC-1 from the northern Okinawa Trough, East China Sea (ECS), provides information on vegetation and climate changes since 24 cal. kaBP. A total of 103 samples were palynologically analyzed at 8 cm intervals with a time resolution of 230 a. Four pollen zones are recognized: zone I (812-715 cm, 24.2-21.1 cal. kaBP), zone II (715-451 cm, 21.1-15.2 cal. kaBP), zone III (451-251 cm, 15.2-10.8 cal. kaBP), zone IV (251-0 cm, 10.8-0.3 cal. kaBP), corresponding to Late MIS 3, Last Glacial Maximum (LGM), deglaciation and Holocene, respectively. The LGM is characterized by the dominance of herbs, mainly Artemisia, and high pollen influx, implying an open vegetation on the exposed continental shelf and a cool and dry climate. The deglaciation is a climate warming stage with Pinus percentage increased and Artemisia percentage decreased and a rapid sea-level rise. The Holocene is characterized by predominance of tree pollen with rapid increase in Castanea-Castanopsis indicating the development of mixed evergreen and deciduous broad-leaved forest and a warm, humid climate. Low pollen influx during the Holocene probably implies submergence of the continental shelf and retreat of the pollen source area. The vegetation indicated by pollen assemblage found in this upper zone is consistent with the present vegetation found in Kyushu, Japan. Originating from the humid mountain area of North Luzon of the Philippines, Tasmania and New Zealand, Phyllocladus with sporadic occurrence throughout PC-1 core probably suggests the influence of Palaeo-Kuroshio Current or intense summer monsoon. The observed changes in Pinus and Herbs percentage indicate fluctuations of the sea level, and high Pinus percentage corresponds to high sea level. Spectrum analysis of the pollen percentage record reveals many millennial-scale periodicities, such as periodicities of 6.8, 3.85 2.2, 1.6 ka.