The stakes of politics and electoral administration : a comparative study of Southeast Asian democracies

Elections play a crucial role in political stability in post-democratization, and electoral administrations are the key to the electoral process. However, not all newly democratized countries have established reliable electoral administration. New democracies in Southeast Asia, such as the Philippines, Indonesia and Thailand, have independent election commissions which have different characteristics, especially in terms of neutrality. Based on three cases, this paper claims that the stakes of politics are the major determinant of the variations in neutrality. The high stakes of politics in Thailand brought about the partisan election commission, while the low stakes in Indonesia made the electoral system relatively neutral. Like Thailand, the high stakes of politics in the Philippines also cause political intervention in the electoral administration.

Annual report of the Commissioners of Fisheries, Game and Forests of the State of New York.

2nd (1896)

Annual report of the Commissioners of Fisheries, Game and Forests of the State of New York.

7th (1901)

(Table T1) Pore-water strontium content, and Sr isotope composition and ages of pore waters and sedimentary carbonates of ODP Leg 171B sites

Strontium concentrations and 87Sr/86Sr values were measured on pore-water and sedimentary carbonate samples from sediments recovered at Sites 1049-1053 on the Blake Spur during Ocean Drilling Program Leg 171B. These sites form a 40-km-long depth transect extending along the crest of the Blake Spur from near the upper edge of the Blake Escarpment (a steep cliff composed of Mesozoic carbonates) westward toward the interior of the Blake-Bahama Platform. Although these sites were selected for paleoceanographic purposes, they also form a hydrologic transect across the upper eastern flank of the Blake-Bahama Platform. Here, we use pore-water strontium concentrations and isotopes as a proxy to define patterns of fluid movement through the flanks of this platform. Pore-water strontium concentration increases with depth at all sites implying that strontium has been added during sediment burial and diagenesis. The isotopic values decrease from seawater-like values in the shallow samples (~0.70913) to values as low as 0.707342 in one of the deepest samples (~625 meters below seafloor). The change in pore-water strontium isotopic values is independent of the strontium isotopic compositions predicted from the host sediment age and measured on bulk carbonate in some samples. In most cases the difference between predicted sediment strontium isotopic composition and measured value is less than ±2 about the mean of the measured strontium value. Both the increase in concentration and the decrease in the strontium isotope values with increasing depth indicate that strontium was expelled from older carbonates. The strontium concentration and isotope profiles vary between sites according to their proximity to the Blake-Bahama Platform edge. Profiles from Site 1049 (nearest the platform edge) show the greatest amount of mixing with modern seawater, whereas the site most distal to the platform edge (Site 1052) shows the most significant influence of older, deeper carbonates on the pore-water strontium isotopic composition.

(Table 2B) Geochemistry of Ariadne II sediments corrected for dilution by salt from pore waters and are carbonate free in the eastern South Pacific

Sediment depth is given in mbsf.

Fountain. In the center of the circular driveway between the Michigan Union and the Administration Bldg.

Gift of Clas of 1956

Mexican Americans and the administration of justice in the Southwest /

"March 1970."