The Role of the Court of Justice in the Implementation of the Single European Act

This paper will begin by evoking the judicial achievements obtained on the eve of the enactment of the Single European Act. Next, it will explain the innovations introduced by the Single European Act, and emphasize the divergent interpretations that they are likely to receive. Then, the author will modestly strive to express several personal suggestions for a solution, as an external observer

Competition, Integration and Economic Efficiency in the EEC from the Point of View of the Private Firm

As early as 1956, experts appointed by the six original Member State governments to investigate measures to pursue integration after the failure of the European Defence Community clearly established this link between the abolition of barriers to trade and an increase in the intensity of competition. In what has come to be known as the Spaak Report, the experts noted the technology gap then separating Europe from the United States and proposed, as a remedial measure, the creation of a \u27\u27vast zone of common economic policy, constituting a powerful production unit, and allowing a continued expansion, and increased stability, an accelerated raising of the standard of living and the development of harmonious relations between the States belonging to it. The authors of the Spaak Report envisioned an enlarged market in which firms would be able to grow to optimum size without acquiring a de facto monopoly: \u27\u27The strength of a vast market is to allow the combination of mass production with the absence of monopoly. Moreover, it was felt that this wider market would compel firms to do away with obsolete production methods and to increase the quantity and quality of their goods. Thus, free movement of goods was seen as a means of increasing competition, which itself was seen as a means of enhancing economic efficiency

Impact of oceanic processes on the carbon cycle during the last termination

During the last termination (from ~18 000 years ago to ~9000 years ago), the climate significantly warmed and the ice sheets melted. Simultaneously, atmospheric CO2 increased from ~190 ppm to ~260 ppm. Although this CO2 rise plays an important role in the deglacial warming, the reasons for its evolution are difficult to explain. Only box models have been used to run transient simulations of this carbon cycle transition, but by forcing the model with data constrained scenarios of the evolution of temperature, sea level, sea ice, NADW formation, Southern Ocean vertical mixing and biological carbon pump. More complex models (including GCMs) have investigated some of these mechanisms but they have only been used to try and explain LGM versus present day steady-state climates. In this study we use a coupled climate-carbon model of intermediate complexity to explore the role of three oceanic processes in transient simulations: the sinking of brines, stratification-dependent diffusion and iron fertilization. Carbonate compensation is accounted for in these simulations. We show that neither iron fertilization nor the sinking of brines alone can account for the evolution of CO2, and that only the combination of the sinking of brines and interactive diffusion can simultaneously simulate the increase in deep Southern Ocean δ13C. The scenario that agrees best with the data takes into account all mechanisms and favours a rapid cessation of the sinking of brines around 18 000 years ago, when the Antarctic ice sheet extent was at its maximum. In this scenario, we make the hypothesis that sea ice formation was then shifted to the open ocean where the salty water is quickly mixed with fresher water, which prevents deep sinking of salty water and therefore breaks down the deep stratification and releases carbon from the abyss. Based on this scenario, it is possible to simulate both the amplitude and timing of the long-term CO2 increase during the last termination in agreement with ice core data. The atmospheric δ13C appears to be highly sensitive to changes in the terrestrial biosphere, underlining the need to better constrain the vegetation evolution during the termination

Carbon isotope offsets between benthic foraminifer species of the genus Cibicides (Cibicidoides) in the glacial sub-Antarctic Atlantic

©2016. American Geophysical Union. All Rights Reserved. Epibenthic foraminifer δ 13 C measurements are valuable for reconstructing past bottom water dissolved inorganic carbon δ 13 C (δ 13 C DIC ), which are used to infer global ocean circulation patterns. Epibenthic δ 13 C, however, may also reflect the influence of 13 C-depleted phytodetritus, microhabitat changes, and/or variations in carbonate ion concentrations. Here we compare the δ 13 C of two benthic foraminifer species, Cibicides kullenbergi and Cibicides wuellerstorfi, and their morphotypes, in three sub-Antarctic Atlantic sediment cores over several glacial-interglacial transitions. These species are commonly assumed to be epibenthic, living above or directly below the sediment-water interface. While this might be consistent with the small δ 13 C offset that we observe between these species during late Pleistocene interglacial periods (Δδ 13 C = −0.19 ± 0.31‰, N = 63), it is more difficult to reconcile with the significant δ 13 C offset that is found between these species during glacial periods (Δδ 13 C = −0.76 ± 0.44‰, N = 44). We test possible scenarios by analyzing Uvigerina spp. δ 13 C and benthic foraminifer abundances: (1) C. kullenbergi δ 13 C is biased to light values either due to microhabitat shifts or phytodetritus effects and (2) C. wuellerstorfi δ 13 C is biased to heavy values, relative to long-term average conditions, for instance by recording the sporadic occurrence of less depleted deepwater δ 13 C DIC . Neither of these scenarios can be ruled out unequivocally. However, our findings emphasize that supposedly epibenthic foraminifer δ 13 C in the sub-Antarctic Atlantic may reflect several factors rather than being solely a function of bottom water δ 13 C DIC . This could have a direct bearing on the interpretation of extremely light South Atlantic δ 13 C values at the Last Glacial Maximum

Reflections

The American Society of International Law Committee recommended that the Manley 0. Hudson Medal be awarded to Professor Eric Stein for his lifetime of significant contributions to international and comparative law. Stein, the Hessel E. Yntema Professor of Law, Emeritus, at the University of Michigan Law School, had been an active supporter of ASIL as Honorary Vice President, Counsellor, and Honorary Editor of, and frequent contributor to, the American Journal of International Law. His many books and articles established him as a leading thinker and writer on European Community law and on what he described in a famous article as the Uses, Misuses, and Nonuses of Comparative Law

Effets internes des obligations imposées à l'état

info:eu-repo/semantics/publishe

L'acquiescement en droit des gens

info:eu-repo/semantics/publishe