Tajikistan: a chronic stagnation. OSW COMMENTARY NUMBER 200/15.03.2016

Since gaining its independence Tajikistan has faced severe political, economic and social problems. The last several months has seen a clear increase in their intensity. This is in part caused by the deteriorating economic situation in Russia and the significant fall of remittances from the Tajik labour migrants in Russia, as well as by President Emomali Rahmon’s rising authoritarianism. Despite this intensification, qualitatively speaking Tajikistan’s problems have been unchanged for years. Besides the state’s structural weakness, the main cause is the ongoing neo-colonial dependence on Russia, which effectively limits Dushanbe’s room for political manoeuvre and keep Tajikistan in Russia’s sphere of control. This dependence on the one hand protects the country from collapsing, but on the other it precludes the development of the state, resulting in Tajikistan’s enduring stagnation. Similar processes also take place in other countries of post-Soviet Central Asia. However, in the case of Tajikistan the dependence and stagnation it causes are the strongest and their mechanisms most easily observed.

Dissolved organic carbon in sediments of the central Arctic Ocean collected during POLARSTERN cruise ARK-XXVII/3 from August-September 2012

Marine organic matter (OM) sinks from surface waters to the seafloor via the biological pump. Benthic communities, which use this sedimented OM as energy and carbon source, produce dissolved organic matter (DOM) in the process of remineralization, enriching the sediment porewater with fresh DOM compounds. We hypothesized that in the oligotrophic deep Arctic basin the molecular signal of freshly deposited primary produced OM is restricted to the surface sediment pore waters which should differ from bottom water and deeper sediment pore water in DOM composition. This study focused on: 1) the molecular composition of the DOM in sediment pore waters of the deep Eurasian Arctic basins, 2) whether the signal of marine vs. terrigenous DOM is represented by different compounds preserved in the sediment pore waters and 3) whether there is any relation between Arctic Ocean ice cover and DOM composition. Molecular data, obtained via 15 Tesla Fourier transform ion cyclotron resonance mass spectrometer, were correlated with environmental parameters by partial least square analysis. The fresher marine detrital OM signal from surface waters was limited to pore waters from < 5 cm sediment depth. The productive ice margin stations showed higher abundances of peptides, unsaturated aliphatics and saturated fatty acids formulae, indicative of fresh OM/pigments deposition, compared to northernmost stations which had stronger aromatic signals. This study contributes to the understanding of the coupling between the Arctic Ocean productivity and its depositional regime, and how it will be altered in response to sea ice retreat and increasing river runoff.