The Southern Gas Corridor. The Azerbaijani-Turkish project becomes part of the game between Russia and the EU. OSW POINT OF VIEW 53, 2015-08-20

The Southern Gas Corridor is a system of three complementary gas pipeline projects controlled by Azerbaijan and Turkey, each at a different stage of implementation. The crisis in EU-Russia relations over Ukraine has made the two players interested in the Southern Gas Corridor once again. Brussels views it as an opportunity for a genuine diversification of gas supplies and a way to reinforce its position against Russia. In turn, Moscow’s proposal for Turkey and Greece to join the Turkish Stream gas pipeline project changes the energy map of the regional projects, which indirectly affects the Southern Gas Corridor. This has raised concern in Azerbaijan, which has been making efforts to manoeuvre between the interests of Moscow and Brussels.

Benthic foraminiferal abundances at the Cretaceous/Paleogene boundary of ODP Hole 117-1049C at Blake Nose, Northwest Atlantic (Appendix A)

Sediments recovered at lower bathyal ODP Site 1049 on Blake Nose (Northwestern Atlantic) offer an opportunity to study environmental changes at the Cretaceous/Paleogene (K/P) boundary relatively close to the Chicxulub impact structure on the Yucatan peninsula, Mexico. In Hole 1049C, the boundary is located at the base of a 9-cm-thick layer with abundant spherules, considered to be impact ejecta. Uppermost Maastrichtian oozes below, and lowermost Danian pelagic oozes above the spherulebed contain well-preserved bathyal benthic foraminifera. The spherule-bed itself, in contrast, contains a mixture of shallow (neritic) and deeper (bathyal) species, and specimens vary strongly in preservation. This assemblage was probably formed by reworking and down-slope transport triggered by the K/P impact. Across the spherule-bed (i.e., the K/P boundary) only ~7% of benthic foraminiferal species became extinct, similar to the low extinction rates of benthic foraminifera worldwide. Quantitative analysis of benthic foraminiferal assemblages and morphogroups in the >63-µm size fraction indicates a relatively eutrophic, stable environment during the latest Maastrichtian, interrupted by a sudden decrease in the food supply to the benthos at the K/P boundary and a decrease in diversity of the faunas, followed by a stepped recovery during the earliest Danian. The recovery was probably linked to the gradual recovery of surface-dwelling primary producers.