EU Policies on Mixed Migration Flows in the Mediterranean Sea. EU Centre Singapore Background Brief No. 13, February 2015

The tragic deaths of over 300 people off the coast of Lampedusa in 2013 and many other incidents involving migrants from Middle East and North Africa (MENA) crossing the Mediterranean in order to seek refuge in Europe has led to a European Union (EU) level debate on asylum policies and how to deal with irregular migration. However, no concrete policy has been agreed since the tragic events at Lampedusa in 2013 and continuous crossings that have resulted in many more deaths. This background brief provides an overview of the existing EU policies on asylum seekers and in addressing irregular migration and some of the actions which the relevant Member States take when confronted with continuous flows of irregular migrants. This brief concludes that the EU should delink the rescue of irregular migrants from security concerns, provide a legal basis which offers protection to irregular migrants, and create a transparent working environment in which member states are better able to support each other when dealing with such events.

Distribution of planktonic foraminifera in surface sediments of the Mediterranean Sea

The Mediterranean Sea is a partillay isolated ocean where excess evaporation over precipitation results in large east to west gradients in temperature and salinity. Recent planktonic foraminiferal distributions have been examined in 66 surface sediment samples from the Mediterranean Sea. In addition to mapping the frequency distribution of 16 species, the faunal data has been subjected to cluster analysis, factor analysis and species diversity analysis. The clustering of species yields assemblages that are clearly temperature related. A warm assemblage contains both tropical and subtropical elements, while the cool assemblage can be subdivided into cool-subtropical, transitional and polar-subpolar groupings. Factor analysis is used to delineate the geographic distribution of four faunal assemblages. Factor 1 is a tropical-subtropical assemblage dominated by Globigerinoiden ruber. It has its highest values in the warmer eastern basin. Transitional species (Globorotalia inflata and Globigerina bulloides) dominate factor 2 with highest values occurring in the cooler western basin. Factor 3 reflects the distribution of Neogloboquadrina dutertrei and is considered to be salinity dependent. Subpolar species dominate factor 4 (Neoglobuquadrina pachyderma and G. bulloides), with highest values occurring in the northern part of the western basin where cold bottom water is presently being formed. The Shannon-Weiner index of species diversity shows that high diversity exists over much of the western basin and immediately east of the Strait of Sicily. This region is marked by equitable environmental conditions and relatively even distribution of individuals among the species. Conversely, in areas where temperature and salinity values are more extreme, diversity values are lower and the assemblages are dominated by one or two species.