Análisis del impacto del fenómeno de la piratería marítima en el comercio marítimo internacional de la región del mar de China (2006-2008)

El fenómeno trasnacional de la piratería marítima se ha convertido en una de las principales amenazas para el desarrollo y el crecimiento del comercio marítimo internacional, especialmente en aquellas zonas que presentan altos flujos comerciales,las cuales de igual forma, se convierten en puntos geográficos favorables para las practicas ilegales de los piratas.

Análisis de la importancia geopolítica del mar del sur para la Asean y China. Periodo 2002-2011

El conflicto territorial presente en el Mar del Sur hace que sea uno de los conflictos de mayor atención en los últimos tiempos. Su riqueza energética impide que alguno de los países litigantes piense en ceder sus intereses sobre esta porción marítima. China y los países miembros de la ASEAN son las partes del conflicto, que entre momentos de cooperación y disensión buscan una solución a este problema. Sin embargo, los intentos diplomáticos y normativos para poner fin a este conflicto, no han sido suficientes, puesto que las agresiones y violaciones en este mar se convierten en una constante que pone en riesgo una de las regiones con mayor influencia en la economía mundial.

Las implicaciones de la expansión china en el sudeste asiático

El artículo presenta la génesis, proceso e implicaciones de la expansión estratégica de la República Popular China hacia el Sudeste asiático. En ese sentido, la hipótesis que se presenta es que Beijing aspira a un renacer pacífico en el Sur con objetivos en el campo económico, estratégico y político. En el plano de la economía lo que se pretende es la estabilidad en el vecindario, condición fundamental para el éxito de su modelo económico, financiero y comercial. En el ámbito estratégico se busca un acceso a fuentes de energía alternativas al carbón, y en lo político, China ha buscado reducir la influencia americana y disminuir el margen de maniobra de Taiwán. En una primera parte se presenta un análisis histórico para introducir al lector en las variables históricas más relevantes para la comprensión del tema en cuestión. En la segunda se estudia el litigio del Mar del Sur de China y la importancia que éste posee política y geoestratégicamente. Finalmente, se examina la influencia china en el Sudeste asiático en tres campos: el cultural, el económico del cual hace parte el financiero y comercial y por último en el geoestratégico.-----L’article illustre la genèse, le processus et les implications de l’expansion stratégique de la République Populaire Chine dans le Sud-est Asiatique. De ce fait, l’hypothèse qui nous présenterons demeure Sur l’idée que Pékin cherche une renaissance pacifique vers le Sud en vue des objectifs économiques, stratégiques et politiques. En ce qui concerne l’économie, la Chine veux la stabilité dans la région, car ceci est une condition essentielle pour la réussite du modèle économique, financer et commercial. Quant à la question stratégique, elle cherche l’accès aux sources alternatives d’énergie. Dans le domaine politique, Pékin aspire à réduire l’influence américaine et à isoler le Taiwan. Dans une première partie, nous introduirons les variables historiques les plus essentielles afin d’expliquer les racines de la problématique en question. Dans la deuxième, le contentieux pour la Mer du Sud de Chine sera analysé ainsi que son importance politique et geoestratégique. Finalement, nous étudierons le processus de l’influence chinoise dans le Sud-est Asiatique. Cela sera divisé en trois domaines, le culturel, l’économique dont le commercial et financière, et le geostratégique.-----This article illustrates the genesis, the process and the implications of the strategic expansion of the People’s Republic of China towards South East Asia. Therefore, the hypothesis that we present is that Beijing is pursuing a Pacific rise in the South aiming for economic, strategic and political goals. Regarding the subject of economy, China seeks stability in the region, due to the fact that it has become essential in the success of its economic, financial and commercial model. Regarding the strategic field China is looking for a way to access alternative energy sources. Politically speaking, Beijing has sought to reduce American influence in the region as well as the isolation of Taiwan. In the first part of the article the reader will find a historical introduction for a better understanding of the subject here treated. In the second part, the litigation of the South China Sea is analyzed due to its political and geostrategical importance. Finally, Chinese influence on South East Asia is examined in three fields: cultural, economic, including financial and commercial aspects as well as the geostrategic field.

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.

Nodal variations and long-term changes in the main tides on the coasts of China

The long-term changes in the main tidal constituents (O1, K1, M2, N2, and S2) along the coasts of China and in adjacent seas are investigated based on 17 tide-gauge records covering the period 1954–2012. The observed 18.61 year nodal modulations of the diurnal constituents O1 and K1 are in agreement with the equilibrium tidal theory, except in the South China Sea. The observed modulations of the M2 and N2 amplitudes are smaller than theoretically predicted at the northern stations and larger at the southern stations. The discrepancies between the theoretically predicted nodal variations and the observations are discussed. The 8.85 year perigean cycle is identifiable in the N2 parameters at most stations, except those in the South China Sea. The radiational component of S2 contributes on average 16% of the observed S2 except in the Gulf of Tonkin, on the south coast, where it accounts for up to 65%. We confirmed the existence of nodal modulation in S2, which is stronger on the north coast. The semidiurnal tidal parameters show significant secular trends in the Bohai and Yellow Seas, on the north coast, and in the Taiwan Strait. The largest increase is found for M2 for which the amplitude increases by 4–7 mm/yr in the Yellow Sea. The potential causes for the linear trends in tidal constants are discussed.

Spatial and temporal variations of the seasonal sea level cycle in the northwest Pacific

The seasonal sea level variations observed from tide gauges over 1900-2013 and gridded satellite altimeter product AVISO over 1993-2013 in the northwest Pacific have been explored. The seasonal cycle is able to explain 60-90% of monthly sea level variance in the marginal seas, while it explains less than 20% of variance in the eddy-rich regions. The maximum annual and semi-annual sea level cycles (30cm and 6cm) are observed in the north of the East China Sea and the west of the South China Sea respectively. AVISO was found to underestimate the annual amplitude by 25% compared to tide gauge estimates along the coasts of China and Russia. The forcing for the seasonal sea level cycle was identified. The atmospheric pressure and the steric height produce 8-12cm of the annual cycle in the middle continental shelf and in the Kuroshio Current regions separately. The removal of the two attributors from total sea level permits to identify the sea level residuals that still show significant seasonality in the marginal seas. Both nearby wind stress and surface currents can explain well the long-term variability of the seasonal sea level cycle in the marginal seas and the tropics because of their influence on the sea level residuals. Interestingly, the surface currents are a better descriptor in the areas where the ocean currents are known to be strong. Here, they explain 50-90% of inter-annual variability due to the strong links between the steric height and the large-scale ocean currents.

BIOLOGICAL ASPECTS OF THE SAILFIN DORY Zenopsis conchifer (LOWE, 1852) CAUGHT BY DEEP-SEA TRAWLING FISHERY OFF SOUTHERN BRAZIL

Biological aspects of sailfin dory, Zenopsis conchifer, were studied from 839 individuals obtained from deep-sea commercial bottom trawling off southern Brazil at depths up to 526 m in 2002 and 2003. Samples included fish from 101 mm Lt and 15 g up to 640 mm Lt and 2,9 g. The sex-ratio was 50% at 150 mm Lt and between 300-350 mm Lt, with females outnumbering males in the remaining size classes. Reproductive activity seems to peak between July and August ( austral winter). Size at attainment of 50% maturity (Lt(50)) was 311 mm Lt in females. The mean length and maturity of the specimens increased with depth, suggesting that larger fish concentrate in deeper waters.

Intrusiones de la corriente de Kuroshio en el mar de China oriental

[EN]The Kuroshio is known to intrude onto the continental shelf in the southern East China Sea northeast of Taiwan. Two types of intrusions are observed: large and small, depending on how far the Kuroshio penetrates onto the ECS continental shelf, and on the location where it crosses the shelf break. This study demonstrates that cyclonic eddies from the western Pacific induce some of these large Kuroshio intrusions. The large intrusions are identified from more than 20 years of drifter tracks archived in the Global Drifter Program historical database and from weekly and biweekly drifter deployments carried out between April 2008 and September 2009 west of the Green Island (Taiwan). Kuroshio intrusions are observed in all seasons. Cyclonic mesoscale eddies, generated in the Subtropical Countercurrent and North Equatorial Current regions of the northwest Pacific Ocean, propagate westward into the Kuroshio and are well correlated with the observed intrusions. During the intrusions, the mean sea level anomaly computed from AVISO gridded maps shows a well defined cyclonic circulation southeast of the I-Lan ridge. The mean sea level anomaly also shows the meandering pattern of the Kuroshio when it intrudes onto the continental shelf of the southern East China Sea. The high correlation between the Kuroshio volume transport in the East Taiwan Channel (observed with moorings) and the satellite sea level anomaly permits us to use sea level anomaly as a proxy for the Kuroshio volume transport. When direct transport measurements are not available, this proxy is used to verify that intrusions due to the westward propagating eddies occur when the Kuroshio transport is low. An analytical reduced gravity model of an incident baroclinic current upon a step shelf is used to explain the difference between the large and small intrusions.

Plio-Pleistocene Mg/Ca and TEX86 sea surface temperature records of ODP Sites 184-1143 and 165-999,

The western warm pools of the Atlantic and Pacific oceans are a critical source of heat and moisture for the tropical climate system. Over the past five million years, global mean temperatures have cooled by 3-4 °C. Yet, current reconstructions of sea surface temperatures indicate that temperature in the warm pools has remained stable during this time. This stability has been used to suggest that tropical sea-surface temperatures are controlled by some sort of thermostat-like regulation. Here we reconstruct sea surface temperatures in the South China Sea, Caribbean Sea and western equatorial Pacific Ocean for the past five million years, using a combination of the Mg/Ca, TEXH86-and Uk'37 surface temperature proxies. Our data indicate that during the period of Pliocene warmth from about 5 to 2.6 million years ago, the western Pacific and western Atlantic warm pools were about 2 °C warmer than today. We suggest that the apparent lack of warming seen in the previous reconstructions was an artefact of low seawater Mg/Ca ratios in the Pliocene oceans. Taking this bias into account, our data indicate that tropical sea surface temperatures did change in conjunction with global mean temperatures. We therefore conclude that the temperature of the warm pools of the equatorial oceans during the Pliocene was not limited by a thermostat-like mechanism.

Reconstruction of sea surface temperature and salinity of the Arabian Sea

High-frequency suborbital variations (Dansgaard-Oeschger cycles) characterize the climatic history of the Northern Hemisphere as observed in Greenland ice cores, deep-sea sediments of the North Atlantic, the Californian borderland, the Arabian Sea, the South China Sea, and the Chinese loess area. Paleoceanographic data from core KL126 from the Bay of Bengal in combination with data from the other Asian monsoonal areas indicate that the feedback processes involving snow and dust of the Tibetan Plateau vary the summer monsoon capacity to transport moisture into central South Asia and into the atmosphere. We postulate that the summer monsoon initiates, amplifies, and terminates these cycles in the Northern Hemisphere.

Rare earth elements of modern seeps from the Gulf of Mexico, the Black Sea, and the Congo Fan

At marine seeps, methane is microbially oxidized resulting in the precipitation of carbonates close to the seafloor. Methane oxidation leads to sulfate depletion in sediment pore water, which induces a change in redox conditions. Rare earth element (REE) patterns of authigenic carbonate phases collected from modern seeps of the Gulf of Mexico, the Black Sea, and the Congo Fan were analyzed. Different carbonate minerals including aragonite and calcite with different crystal habits have been selected for analysis. Total REE content (SumREE) of seep carbonates varies widely, from 0.1 ppm to 42.5 ppm, but a common trend is that the SumREE in microcrystalline phases is higher than that of the associated later phases including micospar, sparite and blocky cement, suggesting that SumREE may be a function of diagenesis. The shale-normalized REE patterns of the seep carbonates often show different Ce anomalies even in samples from a specific site, suggesting that the formation conditions of seep carbonates are variable and complex. Overall, our results show that apart from anoxic, oxic conditions are at least temporarily common in seep environments.

Early - Late Miocene palaeoclimate data and palaefloras of 48 samples from Southern China

Southern China, especially Yunnan, has undergone high tectonic activity caused by the uplift of Himalayan Mountains during the Neogene, which led to a fast changing palaeogeography. Previous study shows that Southern China has been influenced by the Asian Monsoon since at least the Early Miocene. However, it is yet not well understood how intense the Miocene monsoon system was. In the present study, 63 fossil floras of 16 localities from Southern China are compiled and evaluated for obtaining available information concerning floristic composition, stratigraphic age, sedimentology, etc. Based on such reliable information, selected mega- and micro-floras have been analysed with the coexistence approach to obtain quantitative palaeoclimate data. Visualization of climate results in maps shows a distinct spatial differentiation in Southern China during the Miocene. Higher seasonalities of temperature and precipitation occur in the north and south parts of Southern China, respectively. During the Miocene, most regions of Southern China and Europe were both warm and humid. Central Eurasia was likely to be an arid center, which gradually spread westward and eastward. Our data provide information about Miocene climate patterns in Southern China and about the evolution of these patterns throughout the Miocene, and is also crucial to unravel and understand the climatic signals of global cooling and tectonic uplift.