Derisory Results or Reasons to be Cheerful? Evaluating the Implantation of the European Neighbourhood Policy in Ukraine, Moldova and Belarus. Natolin Research Paper 01/January 2011

This paper considers the implementation of the European Neighbourhood Policy (ENP) in Ukraine, Moldova and Belarus. The paper presents a portrait of the three neighbours in terms of their current political and socio-economic profiles, as well as the status of their relations with the European Union. Subsequently, it provides an overview of the development of ENP. A general set of conclusions are offered in relation to the key issue of good governance, where, the paper argues, ENP has delivered derisory results, with patchy effects across the region. Moreover, the paper identifies the democratic back-sliding in Ukraine and entenched authoritarianism in Belarus, which ENP has done very little to address. The EU’s willingness to provide better mobility options for ENP citizens to visit and work in the EU is a key test for the Eastern Partnership (EaP) in the coming year. This paper sees that whilst there are reasons to be cheerful here, with the EU’s recent offer of greater Visa Liberalisation for Ukraine and Moldova, there remains much to be done and in the meantime the EU remains a ‘Fortress Europe’. The paper concludes with a set of recommendations for ENP, which include the need to finally tackle corruption in the region, bring more differentiation into ENP, soften the EU’s borders through more generous Visa regimes, develop a more robust Belarus strategy and to think more creatively about the use of ENP funds for regional and cross- border activities.

The Sahel Crisis: Where do European and African Perspectives Meet? IES Policy Brief Issue 2013/02/March 2013

Summary. The crisis in Mali has brought the Sahel to the centre of international attention. This fragile region not only suffers from longstanding development challenges, but also from an acute security vacuum that has triggered military intervention. Many questions have arisen as a consequence of the crisis. Has the European Union the ability to cope with such a complex and dynamically evolving security environment? How have divergent views on the political roadmap to be adopted, and the lack of resources at the African level, impacted the crisis response? Can the different players involved agree on what are the most pertinent needs and challenges to be addressed? Are they ready for long-term engagement? Can regional organisations effectively collaborate and are they able to successfully integrate different agendas? Following a conference organised by the Institute for European Studies, the Egmont Institute and the Observatoire de l’Afrique on these questions this Policy Brief builds on the findings of the conference and provides an analytical overview of the regional crisis by focusing on the main challenges facing the Sahel, the local and regional dynamics at play and the military and security response.

Mineral and chemical composition of hydrothermally altered rocks and sediments from the Middle Valley, ODP Leg 139 data

The Middle Valley segment at the northern end of the Juan de Fuca Ridge is a deep extensional rift blanketed with 200-500 m of Pleistocene turbiditic sediment. Sites 857 and 858 were drilled during Ocean Drilling Program Leg 139 to determine whether these two sites were hydrologically linked end members of an active hydrothermal circulation system. Site 858 was placed in an area of active hydrothermal discharge with fluids up to 270°C venting through anhydrite-bearing mounds on top of altered sediment. The shallow basement of fine-grained basalt that underlies the vents at Site 858 is interpreted as a seamount that was subsequently buried by turbidites. Site 857 was placed 1.6 km south of the Site 858 vents in a zone of high heat flow and numerous seismically imaged ridge-parallel faults. Drilling at Site 857 encountered sediments that are increasingly altered with depth and that overlie a series of mafic sills at depths of 460-940 m below sea floor. Sill margins and adjacent baked sediment are highly altered to magnesian chlorite and crosscut with veins filled with quartz, chlorite, sulfides, epidote, and wairakite. The sill interiors vary from slightly altered, with unaltered plagioclase and clinopyroxene in a mesostasis replaced by chlorite, to local zones of intense alteration and brecciation. In these latter zones, the sill interiors are pervasively replaced by chlorite, epidote, quartz, pyrite, titanite, and rare actinolite. The most complete replacement is associated with brecciated horizons with low recovery and slickensides on fracture surfaces, which we interpret as intersections between faults and the sills. Geochemically, the alteration of the sill complex is reflected in significant whole-rock depletions in Ca, Sr, and Na with corresponding enrichments in Mg, Al, and most metals. The latter results from the formation of conspicuous sulfide poikiloblasts. In contrast, metamorphism of the Site 858 seamount includes incomplete albitization of plagioclase phenocrysts and replacement of sparse mafic phenocrysts. Much of the basement alteration at Site 858 is confined to crosscutting veins except for a highly altered and veined horizon at the contact between basaltic basement and the overlying sediment. The sill complex at Site 857 is more highly depleted in 18O (d18O = 2.4 per mil - 4.7 per mil) and more pervasively replaced by secondary minerals relative to the extrusives at Site 858 (d18O = 4.5 per mil - 5.5 per mil). There is no evidence of significant albitization of the plagioclase at Site 857, suggesting high Ca/Na in the pore fluids. Fluid-inclusion data from hydrothermal minerals in altered mafic rocks and veins at Sites 857 and 858 show a consistency of homogenization temperatures, varying from 245 to 270°C, which is within the range of temperatures observed for the fluids venting at Site 858. The consistency of the fluid inclusion temperatures, the lack of albitization within the Site 857 sills, and the apparently low water/rock ratio collectively suggest that the sill complex at Site 857 is in thermal equilibrium and being altered by a highly evolved Ca-rich fluid similar to the fluids now venting at Site 858. The alteration evident in these two deep crustal drillsites is a result of the ongoing hydrothermal circulation and is consistent with downhole logging results, instrumented borehole results, and hydrothermal fluid chemistry. The pervasive alteration of the laterally extensive sill-sediment complex at Site 857 determines the chemistry of the fluids that are venting at Site 858. The limited alteration of the Site 858 lavas suggests that this basement edifice acts as a penetrator or ventilator for the regional hydrothermal reservoir with much of the flow focussed at the highly altered and veined sediment-basalt contact.

(Table 2) Facies and grain-size description for Mississippi Fan sediments of DSDP Leg 96

Eight lithologic facies recognized in the Mississippi Fan sediments drilled during DSDP Leg 96 are defined on the basis of lithology, sedimentary structures, composition, and texture. Of these, the calcareous biogenic sediments are of minor importance, volumetrically, as compared with the dominant resedimented terrigenous facies. Clay, mud, and silt are the most abundant sediments at all the sites drilled, with some sand and gravel in the midfan channel fill and an abundance of sand on the lower fan. Facies distribution and vertical sequences reflect the importance of sediment type and supply in controlling fan development. Sea-level changes and diapiric activity have also played an important role. Clay and sand fraction mineralogy closely mirror the dominant sediment source, namely, the Mississippi River system and adjacent continental shelf. Local and regional variation in composition on the fan mostly reflects facies differences.