Germany’s engagement in the resolution of the Syrian conflict. OSW COMMENTARY NUMBER 194/25.01.2016

German Tornado Recce aircraft have been engaged in reconnaissance operations over Syria since January 2016. In December 2015 the German government and parliament decided that up to 1,200 Bundeswehr soldiers would take part in the international coalition fighting Islamic State in Syria. This decision marks a new chapter in Germany’s activity in the Middle East. The increasing destabilisation of the southern neighbourhood and the consequences this has for the EU and Germany have forced the German government to increase its level of engagement in the region. Even though Germany is a third-rate player in the Middle Eastern game, it is nonetheless ever more engaged politically and wants to be viewed as a neutral mediator between the competing actors in the region. It has also allocated more funds on regional development co-operation and humanitarian aid. Germany, whose attention has been directed towards Europe’s eastern neighbourhood, is currently turning its attention to the South. The Middle East (and Africa) is taking on increasing significance in German foreign and security policy. This may affect NATO’s eastern flank and the EU’s eastern neighbourhood since part of Germany’s instruments and funds may be redirected to the South.

(Table T1) Bulk calcium carbonate content of ODP Hole 194-1198A sediments

Weight percent calcium carbonate (wt% CaCO3) content was determined on 328 samples from Ocean Drilling Program Hole 1198A. Two intervals were analyzed, one within lithologic Subunit IA between 14.52 and 41.13 meters below seafloor (mbsf) (25 cm sampling interval) and one within Subunit IB between 67.42 and 100.12 mbsf (15-30 cm interval), allowing the comparison of the nature of cyclic siliciclastic-carbonate variations during the late and early Pleistocene. Overlap with a previously analyzed interval in Hole 1198A illustrates the good agreement in data generated by differing methodologies and extends the continuous record of bulk wt% CaCO3 from 0 to 41.13 mbsf. Although Subunits 1A and 1B exhibit nearly the same variability, from 93% to 63% and 94% to 68%, respectively, Subunit 1A is characterized by a longer cycle length.