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.

Visual description and Radiolarian abundance estimates of ODP Hole 200-1223A sediments

Among the groups of oceanic microfossils, only Radiolaria occur in abundances and preservation states sufficient to provide biostratigraphic control for restricted intervals within sediments recovered in Hole 1223A. The distribution of these microfossils has been divided into four major intervals, A-D. Radiolaria distribution Interval A occupies the depth range 0-3.0 meters below seafloor (mbsf), where the abundance of specimens is very low and preservation is poor. Radiolaria distribution Interval B occupies the depth range 3.02-7.1 mbsf. Radiolaria in Interval B are locally rare to abundant and well preserved, and assemblages range in age from pure early Eocene to early Eocene admixed with late Neogene taxa. Radiolaria distribution Interval C occupies the depth range 7.1-36.99 mbsf and is characterized by sediments either barren of microfossils or containing extremely rare early Eocene specimens. Radiolaria distribution Interval D occupies the depth range 36.99-38.7 mbsf (base of the recovered sedimentary section), where early Eocene Radiolaria are present in rare to common frequencies, but opal-A to opal-CT recrystallization has degraded the preservation state. The late Neogene assemblage of Radiolaria distribution Interval B is dated at 1.55-2.0 Ma, based on occurrences of Eucyrtidium matuyamai, Lamprocyclas heteroporos, and Theocorythium trachelium trachelium. The early Eocene assemblage of Radiolaria distribution Intervals B and D is somewhat problematically assigned to the Buryella clinata Zone.

UM Men's Swimming, 1971 200 Medley Relay Team

[L-R Bob Zann, Tim Norlen, Larry Day, Ray McCullough]