The European Council’s Guidelines for the Area of Freedom, Security and Justice 2020: Subverting the ‘Lisbonisation’ of Justice and Home Affairs? CEPS Essay No. 13, 14 July 2014

In its Conclusions of 26-27 June 2014, the European Council has adopted the new “Strategic Guidelines for Legislative and Operational Planning for the coming years within the EU’s Area of Freedom, Security and Justice (AFSJ)”. These Guidelines reveal a pre-Lisbon Treaty mindset among the EU member states and the Justice and Home Affairs Council. This essay argues that the Guidelines are mainly driven by the interests and agendas of national Ministries of Interior and Justice and are only “strategic” to the extent that they aim at first, re-injecting ‘intergovernmentalism’ or bringing back the old EU Third Pillar ways of working to the new EU institutional setting of the AFSJ and second, at sidelining the EU Charter of Fundamental Rights and rule of law in the AFSJ. The paper argues that the European Council Guidelines seek to prevent the advances in Justice and Home Affairs cooperation as envisaged in the Treaty of Lisbon, particularly its emphasis on supranational democratic, legal and judicial accountability. As a consequence of this move to ‘de-Lisbonise’ JHA cooperation, fundamental rights and rule of law-related initiatives will be neglected and the interest of the individual will be displaced from the centre of gravity in the coming AFSJ 2020 policy agenda.

(Table 1) Chemical composition of interstitial waters from the area of gas hydrate generation, Sea of Okhotsk

Distributions of halogens (Cl, Br and I) in interstitial waters from sediments containing methane hydrate and in water of the hydrate itself are presented. High concentrations of halogens do not occur in interstitial waters from sediments that contain gas hydrates. The main reason for their low concentrations is the poverty of organic matter in sediments.

(Table T2) Integrated intensity (peak area) of matrix minerals of ODP Hole 173-1068A

Mass-wasting deposits characterize the Upper Jurassic(?) to Lower Cretaceous sedimentary record of the Iberia Abyssal Plain. These deposits include olistostromes at Site 897, olistostromes and/or possible rock-fall deposits at Site 899, a breccia succession at Site 1068, slumped and fractured deposits at Site 1069, and a breccia succession at Site 1070. Whereas the exact origin of these deposits is uncertain, the regional common occurrence of middle to upper Mesozoic mass-wasting deposits suggests that they record the early rifting evolution of the west Iberia margin. This data report presents both qualitative and semiquantitative results from XRD analyses of the breccia matrix at Site 1068. In this study the matrix is defined as the fine-grained particles (as viewed through a binocular microscope) plus cement. Results are based on analytical methods that aimed to isolate the desired matrix from larger clast contamination prior to XRD analyses. In addition, the breccia was sampled at a higher resolution than was conducted aboard ship, producing a more complete description of downcore matrix mineralogical changes. The data presented here may be used to (1) further justify the subunit designation of Unit IV made aboard ship, (2) help determine to what degree the matrix and the larger clasts (studied in thin section aboard ship; Shipboard Scientific Party, 1998, doi:10.2973/odp.proc.ir.173.106.1998) are compositionally distinct, (3) help identify the extent of hydrothermal fluid migration in the breccia, and (4) support the proposed shipboard hypothesis that the Site 1068 breccia succession resulted from multiple mass-wasting.