917 resultados para Islam - Indonesia


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The post-Soviet area, along with the countries of the Middle East, North Africa and Western Europe, have become one of the main global exporters of Islamic militants. Currently on the territory of Syria, and to a lesser extent of Iraq, there are several thousands of foreign fighters from the post-Soviet states. The causes of the war migration from the former USSR states to the Middle East have their roots in the dynamic changes taking place inside Islam in the post-Soviet area: primarily the growth of Salafism and militant Islam, as well as the internationalisation and globalisation of the local Islam. The deep political, economic, social and ideological changes which Muslims underwent after the collapse of the USSR, led to the creation of a specific group within them, for which Islam in its radical form became the main element of their identity. Homo sovieticus, without fully eradicating his Soviet part, became Homo jihadicus who not only identifies himself with the global Ummah, but is also ready to leave his country and join jihad beyond its borders in the name of the professed ideas.

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Indonesia is the world’s largest Muslim-majority country. It is of immense importance for the security situation and economic integration in Pacific Asia. Political events in Indonesia have a profound impact on the whole region of Southeast Asia. Nevertheless, the 2014 parliamentary and presidential elections were hardly reported in the foreign media. The presidential elections in particular turned out to be a hard test for the young democracy.

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While part of a single country, the Indonesian archipelago covers several biogeographic regions, and the high levels of national shipping likely facilitate transfer of non-native organisms between the different regions. Two vessels of a domestic shipping line appear to have served as a transport vector for the Asian green mussel Perna viridis (Linnaeus, 1758) between regions. This species is indigenous in the western but not in the eastern part of the archipelago, separated historically by the Sunda Shelf. The green mussels collected from the hulls of the ferries when in eastern Indonesia showed a significantly lower body condition index than similar-sized individuals from three different western-Indonesian mussel populations. This was presumably due to reduced food supply during the ships' voyages. Although this transportinduced food shortage may initially limit the invasive potential (through reduced reproductive rates) of the translocated individuals, the risk that the species will extend its distributional range further into eastern Indonesia is high. If the species becomes widely established in eastern Indonesia, there will then be an increased risk of incursions to Australia, where the mussel is listed as a high-priority pest species.

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The Australian-Indonesian monsoon has a governing influence on the agricultural practices and livelihood in the highly populated islands of Indonesia. However, little is known about the factors that have influenced past monsoon activity in southern Indonesia. Here, we present a ~6000 years high-resolution record of Australian-Indonesian summer monsoon (AISM) rainfall variations based on bulk sediment element analysis in a sediment archive retrieved offshore northwest Sumba Island (Indonesia). The record suggests lower riverine detrital supply and hence weaker AISM rainfall between 6000 yr BP and ~3000 yr BP compared to the Late Holocene. We find a distinct shift in terrigenous sediment supply at around 2800 yr BP indicating a reorganization of the AISM from a drier Mid Holocene to a wetter Late Holocene in southern Indonesia. The abrupt increase in rainfall at around 2800 yr BP coincides with a grand solar minimum. An increase in southern Indonesian rainfall in response to a solar minimum is consistent with climate model simulations that provide a possible explanation of the underlying mechanism responsible for the monsoonal shift. We conclude that variations in solar activity play a significant role in monsoonal rainfall variability at multi-decadal and longer timescales. The combined effect of orbital and solar forcing explains important details in the temporal evolution of AISM rainfall during the last 6000 years. By contrast, we find neither evidence for volcanic forcing of AISM variability nor for a control by long-term variations in the El Niño-Southern Oscillation (ENSO).

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Mode of access: Internet.