Incidencia de la política "desarrollo pacífico" en las relaciones de china y la ASEAN. Una aproximación desde la soberanía de las islas Spratly, 2004 – 2012

El interés de este trabajo es el de analizar la Política Exterior de la Republica Popular China, más específicamente la conocida como Desarrollo Pacífico, y su incidencia en las disputas territoriales del Sudeste Asiático. El trabajo se dividirá en 3 partes, donde cada una tratara distintos aspectos del Desarrollo Pacífico, y través del mismo se explicará como por medio de distintos conceptos se pueden entender las múltiples posiciones chinas, así como las preocupaciones de los países que conforman el bloque ASEAN. El propósito de este documento será demostrar que a pesar de que dicha política ha ayudado de forma sustancial a mejorar las relaciones entre ambos bandos y ha traído bastantes beneficios políticos, no ha sido suficiente para eliminar la tensión en la zona y dar una solución a las disputas que se viven.

La política exterior de China hacia América Latina : un análisis de la relación de China y Colombia (periodo 2010-2015)

Esta monografía tiene como objetivo analizar la política exterior de China hacia América Latina en materia económica, política y cultural, con énfasis en las relaciones con Colombia, durante el periodo de 2010 a 2015. Los conceptos de Soft Power y desarrollo pacífico son centrales en el estudio porque sirven para entender la proyección de la política exterior china y cómo mediante ello pretende posicionar una mayor influencia en la región. El trabajo es de tipo analítico, porque identifica la política exterior china y su alcance.

Development and evaluation of a species diagnostic polymerase chain reaction-restriction fragment-length polymorphism procedure for cryptic members of the Culex sitiens (Diptera : Culicidae) subgroup in Australia and the southwest Pacific

Members of the Culex sitiens subgroup are important vectors of arboviruses, including Japanese encephalitis virus, Murray Valley encephalitis virus and Ross River virus. Of the eight described species, Cx. annulirostris Skuse, Cx. sitiens Wiedemann, and Cx. palpalis Taylor appear to be the most abundant and widespread throughout northern Australia and Papua New Guinea (PNG). Recent investigations using allozymes have shown this subgroup to contain cryptic species that possess overlapping adult morphology. We report the development of a polymerase chain reaction-restriction fragment-length polymorphism (PCR-RFLP) procedure that reliably separates these three species. This procedure utilizes the sequence variation in the ribosomal DNA ITS1 and demonstrates species-specific PCR-RFLP profiles from both colony and field collected material. Assessment of the consistency of this procedure was undertaken on mosquitoes sampled from a wide geographic area including Australia, PNG, and the Solomon Islands. Overlapping adult morphology was observed for Cx. annulirostris and Cx. palpalis in both northern Queensland and PNG and for all three species at one site in northwest Queensland.

Late Miocene development of the western Pacific warm pool: Planktonic foraminifer and oxygen isotopic evidence

The disappearance at ~10 Ma of the deep dwelling planktonic foraminifer Globoquadrina dehiscens from the western Pacific including the South China Sea was about 3 Myr earlier than its final extinction elsewhere. Accompanying this event at ~10 Ma was a series of faunal turnover characterized by increase in mixed layer, warm-water species and decrease to a minimum in deepwater species. Paleobiological and isotopic evidence indicates sea surface warming and a deepened local thermocline that we interpret as related to the development of an early western Pacific warm pool. The stepwise decline of G. dehiscens and other deep dwelling species from the NW and SW Pacific suggests more intensive warm water pileup than equatorial localities where surface bypass flow through the narrowing Indonesia seaway appears to remain efficient during the late Miocene. Planktonic delta18O values from the South China Sea consistently lighter than the tropical western Pacific during the Miocene also suggest, similar to today, more variable hydrologic conditions along the periphery than in the core of the warm pool. Stronger hydrologic variability affected mainly by monsoons and increased thermal gradient along the western margin of the late Miocene warm pool may have contributed to the decline of deep dwelling planktonic species including the early extinction of G. dehiscens from the South China Sea region. The late Miocene warm pool became influential and paleobiologically detectable from ~10 Ma, but the modern warm pool did not appear until about 4 Ma, in the middle Pliocene.