Selbstbestimmung und Parteien in Südtirol: Territoriale und europäische Parteistrategien zwischen Autonomie und Sezession = Self-determination and parties in South Tyrol: Territorial and European party strategies between autonomy and secession. EDAP Paper 03/2016 03/2016

Since the final conflict settlement between Italy and Austria in 1992, ethnic politics in South Tyrol experienced insightful transformations. The consociational political system, which was implemented to tame centrifugal tendencies, has been losing its balance over the last decade, with proautonomy stances ceding ground to secessionist pressure in the Germanspeaking intra-ethnic arena. Adopting a contextual and strategic perspective on self-determination, this article traces the evolution of ethno-regionalist party strategies on the territorial and European dimension of party competition through a quantitative and qualitative content analysis of their electoral manifestos in the period between 1993 and 2013. In line with newest research on party strategies, the article empirically shows the strategic capacity of ethnic minority parties to challenge each other not only by shifting their positions on the different issue dimensions but also by the reframing of issues. While the increasing competition on the center-periphery axis leads to a new territorial frame, the rise of secessionism is accompagned by an end to the pro-European elite consensus.

Planktonic foraminiferal stratigraphy, datum levels and ages of ODP Sites 184-1146 and 184-1148, South China Sea

Over 30 first and last occurrence (FO and LO, respectively) planktonic foraminifer datums were recognized from the Oligocene-Miocene section of Ocean Drilling Program (ODP) Site 1148. Most datum levels occur in similar order as, and are by correlation as probably synchronous with, their open-ocean records. Several datum levels represent local bioevents resulting from dissolution and Site 1148's unique paleoceanographic setting in the northern South China Sea. An age of 9.5-9.8 Ma is estimated for the local LO of Globoquadrina dehiscens (257 meters composite depth [mcd]), whereas the local LO of Globorotalia fohsi s.l. (301 mcd) is projected to be at ~13.0 Ma and the local FO of Globigerinatella insueta (367 mcd) is projected to be at ~18.0 Ma. The combined planktonic foraminifer and nannofossil results indicate that the Oligocene-Miocene section at Site 1148 is not complete. Unconformities up to 2-3 m.y. in duration, occurring at and before the Oligocene/Miocene boundary (OHS1, OHS2, OHS3, and OHS4 = MHS1), are associated with slump deposits between 457 and 495 mcd that signal tectonic instability during the transition from rifting to spreading in the South China Sea. Shorter unconformities of <0.5 m.y. duration that truncate the Miocene section were more likely to have been caused by sea-bottom erosion as well as dissolution. A total of 12 Miocene unconformities, MHS1 through MHS12, are mainly affected by dissolution and an elevated carbonate compensation depth (CCD) during Miocene third-order glaciations recorded in deep-sea positive oxygen isotope Mi glaciation events. Respectively, they fall at ~457 mcd (MHS1 = Mi-1), 407 mcd (MHS2 = Mi-1a), 385 mcd (MHS3 = Mi-1aa), 366 mcd (MHS4 = Mi-1b), 358 mcd (MHS5 = MLi-1), 333 mcd (MHS6 = Mi-2), 318 mcd (MHS7 = MSi-1), 308 mcd (MHS8 = Mi-3), 295 mcd (MHS9 = Mi-4), 288 mcd (MHS10 = Mi-5), 256 mcd (MHS11 = Mi-6), and 250 mcd (MHS12 = Mi-7). The correlation of these unconformities with Mi events indicates that some related driving mechanisms have been operating, causing deepwater circulation changes concomitantly in world oceans and in the marginal South China Sea.

Economic policies and programs in South America

Mode of access: Internet.

Laboratory investigation of residual liquid organics from spills, leaks, and the disposal of hazardous wastes in groundwater /

Mode of access: Internet.

Wanderings and excursions in South Wales, with the scenery of the River Wye /

Includes index.