Development of Border Economic Zones in Thailand: Expansion of Border Trade and Formation of Border Economic Zones

In the wake of economic globalization and development in Thailand, movement of people and commodities at the Thai borders is also becoming pronounced. Economic interdependence between Thailand and neighboring countries is growing through border customhouses. As a policy, Thailand is trying to stimulate trade and investment with neighboring countries following the ACMECS (Ayeyawady-Chao Phraya-Mekong Economic Cooperation Strategy) scheme. In this report, first, movement of people and goods at the borders will be examined. Second, clarification of where and how development is proceeding will be presented. Last, this study will attempt to review the perspectives of policies on neighboring countries after Thaksin.

THE CONQUEST OF CENTRAL BRAZIL: FRONTIERS AND FRONTS PIONEERING IN THE NINETEENTH CENTURY

The process of territorial formation in Brazil is examined in this paper in order to establish, through a study that favors more interior region of Portuguese America, a suitable analytical arsenal geohistorica an interpretation of the built legacy of colonial Lusitanian action on American soil. Thus, it is expected to recover some aspects not yet addressed conclusively by the specialized literature, the importance of colonial territorial nexus in the construction and maintenance of the substrate material on which the new politically independent state would claim jurisdiction after 1822. Through the examination of so-called western border, articulated through the contacts held between the cities network of Goias and the strong, prisons, villages and towns planned in Mato Grosso, outline an interpretation of regional dynamics in the moments preceding the running of the Brazilian political emancipation.

Military crisis management in the next decade (2020-2030) : inducing consent or relying on compliance?

The most outstanding conceptual challenge of modern crisis management is the principle of consent. It is not a problem only at the operational level - it challenges the entire decision-making structures of crisis management operations. In post-cold war times and especially in the 21st century, there has been a transition from peacekeeping with limited size and scope towards large and complex peace operations. This shift has presented peace operations with a dilemma. How to balance between maintaining consent for peace operations, whilst being able to use military force to coerce those attempting to wreck peace processes? To address such a dilemma, this research aims to promote understanding, on what can be achieved by military crisis management operations (peace support operations) in the next decade. The research concentrates on the focal research question: Should military components induce consent or rely on the compliance of conflicting parties in crisis management operations of the next decade (2020 – 2030)? The focus is on military – political strategic level considerations, and especially on the time before political decisions to commit to a crisis management operation. This study does not focus on which actor or organisation should intervene. The framework of this thesis derives from the so called ‘peacebuilding space’, the scope of peace operations and spoiler theory. Feasibility of both peace enforcement and peacekeeping in countering future risk conditions are analysed in this framework. This future-orientated qualitative research uses the Delphi-method with a panel of national and international experts. Citation analysis supports identification of relevant reference material, which consists of contemporary literature, the Delphi-questionnaires and interviews. The research process followed three main stages. In the first stage, plausible future scenarios and risk conditions were identified with the Delphi-panel. In the second stage, operating environments for peace support operations were described and consequent hypotheses formulated. In the third stage, these hypotheses were tested on the Delphi-panel. The Delphi-panel is sufficiently wide and diverse to produce plausible yet different insights. The research design utilised specifically military crisis management and peace operations theories. This produced various and relevant normative considerations. Therefore, one may argue that this research; which is based on accepted contemporary theory, hypotheses derived thereof and utilising an expert panel, contributes to the realm of peace support operations. This research finds that some degree of peace enforcement will be feasible and necessary in at least the following risk conditions: failed governance; potential spillover of ethnic, religious, ideological conflict; vulnerability of strategic chokepoints and infrastructures in ungoverned spaces; as well as in territorial and extra-territorial border disputes. In addition, some form of peace enforcement is probably necessary in risk conditions pertaining to: extremism of marginalised groups; potential disputes over previously uninhabited and resource-rich territories; and interstate rivalry. Furthermore, this research finds that peacekeeping measures will be feasible and necessary in at least risk conditions pertaining to: potential spillover of ethnic, religious, ideological conflict; uncontrolled migration; consequences from environmental catastrophes or changes; territorial and extra-territorial border disputes; and potential disputes over previously uninhabited and resource-rich territories. These findings are all subject to both generic and case specific preconditions that must exist for a peace support operation. Some deductions could be derived from the research findings. Although some risk conditions may appear illogical, understanding the underlying logic of a conflict is fundamental to understanding transition in crisis management. Practitioners of crisis management should possess cognizance of such transition. They must understand how transition should occur from threat to safety, from conflict to stability – and so forth. Understanding transition is imperative for managing the dynamic evolution of preconditions, which begins at the outset of a peace support operation. Furthermore, it is pertinent that spoilers are defined from a peace process point of view. If spoilers are defined otherwise, it changes the nature of an operation towards war, where the logic is breaking the will of an enemy - and surrender. In peace support operations, the logic is different: actions towards spoilers are intended to cause transition towards consent - not defeat. Notwithstanding future developments, history continues to provide strategic education. However, the distinction is that the risk conditions occur in novel futures. Hence, lessons learned from the past should be fitted to the case at hand. This research shows compelling evidence that swaying between intervention optimism and pessimism is not substantiated. Both peace enforcement and peacekeeping are sine qua non for successful military crisis management in the next decade.

Evolução de um sistema lacustre árido Permiano, parte superior da Formação Pedra de Fogo, borda oeste da Bacia do Parnaíba

Análise faciológica e estratigráfica realizada na região de Filadélfia, TO, borda oeste da Bacia do Parnaíba, permitiu redefinir o paleoambiente da parte superior da Formação Pedra de Fogo, de idade permiana. Os depósitos estudados constituem uma sucessão de aproximadamente 100 m de espessura, predominantemente siliciclástica, com carbonatos e evaporitos subordinados, onde foram definidas 21 fácies sedimentares agrupadas em seis associações de fácies (AF): AF1) Lacustre com rios efêmeros; AF2) Lago influenciado por ondas de tempestade; AF3) Sabkha continental; AF4) Lago central; AF5) Dunas eólicas; e AF6) Lago/oásis com inundito. Estas associações indicam que durante o Permiano, um extenso sistema lacustre de clima árido, desenvolveu-se adjacente a campos de dunas eólicas e sabkha continental, com contribuições de rios efêmeros. Incursões fluviais nos lagos propiciavam a formação de lobos de suspensão e fluxos em lençol (AF1). Planícies de sabkha (AF3) formaram-se nas porções marginais do lago que, eventualmente eram influenciados por ondas de tempestades (AF2), enquanto zonas centrais eram sítios de intensa deposição pelítica (AF4). O baixo suprimento de areia eólica neste sistema propiciou a formação de um campo de dunas restrito (AF5), com desenvolvimento de lagos de interdunas (oásis), onde proliferavam núcleos de samambaias gigantes, inundados esporadicamente por rios efêmeros (AF6). Os dados faciológicos, corroborados pela paleogeografia da região durante o Permiano Superior, indicam que a sedimentação da parte superior da Formação Pedra de Fogo ocorreu sob condições climáticas quentes e áridas.

Estudo petrográfico e geoquímico dos ironstones da base da Formação Pimenteiras, Borda Oeste da Bacia do Parnaíba, Tocantins

Ironstones, que ocorrem na base da Formação Pimenteiras (Devoniano), na borda noroeste da Bacia do Parnaíba, foram investigados ao longo dos perfis Xambioá-Vanderlândia e Colinas do Tocantins-Couto Magalhães. Esses ironstones formam camadas de espessura decimétrica, descontínuas e intercaladas em arenitos e siltitos, que jazem sobre rochas do cinturão Araguaia. Além da textura oolítica, os ironstones de Xambioá-Vanderlândia diferem dos de Colinas do Tocantins-Couto Magalhães por conterem menores quantidades de material terrígeno, notadamente quartzo, e maiores proporções de oxi-hidróxidos de Fe. São ainda mais enriquecidos em V, Sr, Zr e Σ_ETR e mais empobrecidos em Al₂O>sub>3 e Rb. Diferem também no padrão de distribuição dos ETR normalizados ao North American Shale Composite (NASC), especialmente com relação aos valores de (ETRI)_N, os quais, mais altos nos ironstones oolíticos e mais baixos nos não oolíticos, geram curvas convexas e côncavas, respectivamente. No campo, não foram estabelecidas as relações espaciais entre as duas variedades de ironstones, porém sugere-se que elas representem diferentes fácies da mesma formação ferrífera. Possivelmente, a deposição da fácies não oolítica ocorreu mais afastadamente da borda continental, em ambiente de águas mais profundas e calmas, onde foram descarregadas maiores quantidades de sedimentos detríticos; a deposição da fácies oolítica transcorreu em águas mais rasas e agitadas, com menor suprimento de material terrígeno. O transporte do Fe poderia ter resultado, em grande parte, da erosão fluvial de áreas continentais marcadas por ambientes redutores, o que teria favorecido a solubilidade daquele metal na forma de complexos orgânicos.

Extremo-oeste paranaense: história territorial, região, identidade e (re)ocupação

Pós-graduação em História - FCHS

Heteroduplex formation and S1 digestion for mapping alternative splicing sites

The identification of alternatively spliced transcripts has contributed to a better comprehension of developmental mechanisms, tissue-specific physiological processes and human diseases. Polymerase chain reaction amplification of alternatively spliced variants commonly leads to the formation of heteroduplexes as a result of base pairing involving exons common between the two variants. S1 nuclease cleaves single-stranded loops of heteroduplexes and also nicks the opposite DNA strand. In order to establish a strategy for mapping alternative splice-prone sites in the whole transcriptome, we developed a method combining the formation of heteroduplexes between 2 distinct splicing variants and S1 nuclease digestion. For 20 consensuses identified here using this methodology, 5 revealed a conserved splice site after inspection of the cDNA alignment against the human genome (exact splice sites). For 8 other consensuses, conserved splice sites were mapped at 2 to 30 bp from the border, called proximal splice sites; for the other 7 consensuses, conserved splice sites were mapped at 40 to 800 bp, called distal splice sites. These latter cases showed a nonspecific activity of S1 nuclease in digesting double-strand DNA. From the 20 consensuses identified here, 5 were selected for reverse transcription-polymerase chain reaction validation, confirming the splice sites. These data showed the potential of the strategy in mapping splice sites. However, the lack of specificity of the S1 nuclease enzyme is a significant obstacle that impedes the use of this strategy in large-scale studies.

Territorial Strategic Planning as a support instrument for Regional and Local Development: a comparative analysis between Lisbon and Barcelona Metropolitan Areas

MARQUES, B.P. (2011) "Territorial Strategic Planning as a support instrument for Regional and Local Development: a comparative analysis between Lisbon and Barcelona Metropolitan Areas", in Atas do 17.º Congresso da APDR, do 5.º Congresso de Gestão e Conservação da Natureza e do Congresso Internacional da APDR/AECR, Bragança e Zamora, pp. 1265-1272, ISBN 978-989-96353-2-6.

Cohesion, competition and contradiction: INTERREG and Franco-British Cross border co-operation

Aquest article resumeix el desenvolupament del programa INTERREG i la cooperació a la frontera franc-britànica en els últims vint anys. Això és seguit per una anàlisi de la forma transfronterera cooperació pot entendre recorrent a les discussions conceptuals de canviar la governança europea i les relacions de poder entre els diferents nivells de govern. Aquestes idees conceptuals proporcionen un context per a un examen en profunditat de la iniciativa INTERREG IIIA, a la frontera franc-britànica que es destaquen alguns dels principals problemes i les contradiccions de la cooperació transfronterera.

Cross-Border Cooperation Between Spain and Portugal: A case Study of the Southern Regions

After centuries of lack of contacts between Spain and Portugal, the democratization of both countries allowed for a rapprochement which today is becoming more intensive. The crucial factor of the growing integration of Spanish and Portuguese border regions into a cross-border region is naturally the INTERREG programme. Both regions are disadvantaged within the European Union and their respective countries as poor regions. They have the status of a ‘double periphery’. In the 1980s and particularly 1990s actors on both sides of the border intensified their contacts in order to overcome their double peripherality. The growing number of projects, the improvement of infrastructures and the revival of associationism will certainly change the quality of life of these regions, which are still among the lowest in both countries. The continuation of the INTERREG programme after 2007-2013 will be an important consolidating tool for the further development of cross-border cooperation.

The Emergence and Governance of Euroregions: The Case of the Euregio on the Dutch-German Border

Amb una història que data de la dècada de 1950, la EUREGIO és un de les més antigues euroregions a Europa. Es pot considerar com un cas exitós d'una regió transfronterera (CBR) en el sentit que s'ha establert fermament com una agència de fronteres dins del seu tram de la frontera holandesa-alemanya. L'EUREGIO també ha estat una de les protagonistes principals darrere de l'Associació de Regions Frontereres Europees (ARFE), que en les últimes dècades va actuar per difondre el model d'euroregió a tot el territori europeu. Aquest capítol té diversos objectius. En primer lloc, es presenta el cas de la EUREGIO i presenta evidència sobre la seva història, estructura orgànica i polítiques. En segon lloc, s'analitzen les condicions del context en què la EUREGIO ha sorgit i les estructures de govern que es van crear com a resultat. Es fa especial èmfasi en la posició i el paper de l'Euroregió en el context més ampli del marc de governança europea multinivell generat per la política de cohesió de la UE. El capítol conclou amb un intent d'avaluar l'èxit i l'impacte de la EUREGIO i una discussió dels reptes relacionats amb la doble funció de l'EUREGIO com a representant dels interessos de les autoritats locals i les agències de cohesió de la UE posada en pràctica de les polítiques.

Gain-of-function haplotype in the epithelial calcium channel TRPV6 is a risk factor for renal calcium stone formation.

The rate-limiting step of dietary calcium absorption in the intestine requires the brush border calcium entry channel TRPV6. The TRPV6 gene was completely sequenced in 170 renal calcium stone patients. The frequency of an ancestral TRPV6 haplotype consisting of three non-synonymous polymorphisms (C157R, M378V, M681T) was significantly higher (P = 0.039) in calcium stone formers (8.4%; derived = 502, ancestral = 46) compared to non-stone-forming individuals (5.4%; derived = 645, ancestral = 37). Mineral metabolism was investigated on four different calcium regimens: (i) free-choice diet, (ii) low calcium diet, (iii) fasting and (iv) after a 1 g oral calcium load. When patients homozygous for the derived haplotype were compared with heterozygous patients, no differences were found with respect to the plasma concentrations of 1,25-vitamin D, PTH and calcium, and the urinary excretion of calcium. In one stone-forming patient, the ancestral haplotype was found to be homozygous. This patient had absorptive hypercalciuria. We therefore expressed the ancestral protein (157R+378V+681T) in Xenopus oocytes and found a significantly enhanced calcium permeability when tested by a (45)Ca(2+) uptake assay (7.11 +/- 1.93 versus 3.61 +/- 1.01 pmol/min/oocyte for ancestral versus derived haplotype, P < 0.01). These results suggest that the ancestral gain-of-function haplotype in TRPV6 plays a role in calcium stone formation in certain forms of absorptive hypercalciuria.

Formation of aluminosilicate-bearing quartz veins in the Simano nappe (Central Alps): structural, thermobarometric and oxygen isotope constraints

We combined structural analysis, thermobarometry and oxygen isotope geochemistry to constrain the evolution of kyanite and/or andalusite-bearing quartz veins from the amphibolite facies metapelites of the Simano nappe, in the Central Alps of Switzerland. The Simano nappe records a complex polyphase tectonic evolution associated with nappe stacking during Tertiary Alpine collision (D1). The second regional deformation phase (132) is responsible for the main penetrative schistosity and mineral lineation, and formed during top-to-the-north thrusting. During the next stage of deformation (D3) the aluminosilicate-bearing veins formed by crystallization in tension gashes, in tectonic shadows of boudins, as well as along shear bands associated with top-to-the-north shearing. D2 and D3 are coeval with the Early Miocene metamorphic peak, characterised by kyanite + staurolite + garnet + biotite assemblages in metapelites. The peak pressure (P) and temperature (T) conditions recorded are constrained by multiple-equilibrium thermobarometry at 630 +/- 20 degrees C and 8.5 +/- 1 kbar (similar to 27 km depth), which is in agreement with oxygen isotope thermometry indicating isotopic equilibration of quartz-kyanite pairs at 670 +/- 50 degrees C. Quartz-kyanite pairs from the aluminosilicate-bearing quartz veins yield equilibration temperatures of 645 +/- 20 degrees C, confirming that the veins formed under conditions near metamorphic peak. Quartz and kyanite from veins and the surrounding metapelites have comparable isotopic compositions. Local intergranular diffusion in the border of the veins controls the mass-transfer and the growth of the product assemblage, inducing local mobilization of SiO2 and Al2O3. Andalusite is absent from the host rocks, but it is common in quartz veins, where it often pseudomorphs kyanite. For andalusite to be stable at T-max, the pressure in the veins must have been substantially lower than lithostatic. An alternative explanation consistent with structural observations would be inheritance by andalusite of the kyanite isotopic signature during polymorphic transformation after the metamorphic peak.

Le modèle antarctique

Il existe actuellement des différends frontaliers entre les États circumpolaires-Nord qui entravent la bonne gouvernance de la région. Afin d'identifier des pistes de solution pour améliorer la gouvernance en Arctique et faciliter la coopération, nous analysons le processus qui a mené, à l'autre pôle, à la création du Traité sur l’Antarctique de 1959. Nous utilisons une approche néolibérale institutionnelle comme cadre théorique ainsi qu’une méthodologie basée sur le traçage de processus. Nous avons identifié quatre variables (les intérêts des États, le contexte politique, le leadership, et l’Année géophysique internationale [AGI]) que nous avons étudiés au cours de trois périodes historiques et dont l’évolution a contribué à la formation du régime antarctique. Les étapes menant à l'élaboration d'un régime identifié dans la théorie institutionnaliste dynamique de Frischmann s'appliquent aux différentes périodes que nous avons déterminées. La première période historique correspond à l'identification du problème d'interdépendance. Les États ont d’abord tenté d’assouvir leurs intérêts particuliers envers le continent antarctique par l’intermédiaire de stratégies individuelles. Le statut imprécis du continent antarctique caractérisé par des revendications territoriales conflictuelles, la volonté des superpuissances d’effectuer d’éventuelles revendications territoriales et le leadership exercé par les États-Unis ont toutefois permis de faire évoluer les États vers des stratégies coopératives. La deuxième période historique correspond à l'étape de la négociation de l’entente. Le leadership d’un groupe de scientifiques et des États-Unis ainsi que le contexte politique de la Guerre froide ont favorisé la cohésion des États intéressés par les affaires antarctiques et leur investissement dans une coopération multilatérale souple dans le cadre d’un événement ponctuel, l’AGI. La troisième période correspond à la mise en oeuvre de l’entente, soit l’AGI. Lors de cet événement, une entente tacite, un engagement d’honneur, qui suspendait les considérations territoriales en Antarctique, a été respectée par les parties. La coopération dans le cadre de l’AGI s’est avérée un succès. Les États se sont montrés satisfaits des gains que comportait la coopération scientifique dans un environnement pacifique. L’AGI a permis aux États d’expérimenter la coopération multilatérale et d’observer le comportement des autres participants au sein de l’institution. En raison de la satisfaction des États vis-à-vis la coopération dans le cadre de l'entente souple, l'élaboration du traité de 1959 a été facilitée. Notre étude nous a permis d’identifier des éléments clefs qui ont favorisé la formation du régime antarctique et qui pourraient servir d’inspiration pour l'élaboration de futurs régimes. La présence d’un leadership tout au long du processus a permis de promouvoir les avantages de la coopération sous différentes formes et de renforcer les relations entre les États présents dans les affaires antarctiques. La réalisation d'une entente souple dans le cadre de l'AGI, centrée autour des intérêts communs aux parties, comprenant un engagement d’honneur, permettant de mettre de côté les points de discorde, ont aussi été des points centraux dans la réussite et la poursuite de la coopération au-delà de l’AGI. Cette approche graduelle allant du droit souple vers le droit contraignant est sans aucun doute l’élément le plus important ayant facilité le rapprochement des différentes parties et éventuellement la création du Traité sur l’Antarctique.