European Integration and Europeanisation: Benefits and Disadvantages for Business. Bruges European Economic Policy (BEEP) Briefing 29/2013

European integration is a project of great economic importance for the 500 million consumers and 21 million companies in Europe. With the economic borders between Member States removed, Europeanisation becomes inevitable for companies. The paper proposes a framework to analyse the benefits and disadvantages for business that come with the process of European integration, structured according to the logic of the four fundamental freedoms of movement within the Internal Market (freedom of movement of goods, services, capital and people) complemented by the section on technology and innovation, and the general EU regulatory environment. Whereas the business decisions need to be taken on a case-by-case basis, taking into consideration firm’s own capabilities and resources as well as industry specificities, several recommendations for companies willing to Europeanise are made, based on an analysis of the regulatory macro-environment of the EU. Above all, any company willing to be successful in the EU has to become a learning organisation, responsive to the advancements of the macro-environment. The ability to anticipate the regulatory developments and to adjust one’s own business and corporate strategy accordingly is the key to achieving sustainable competitive advantage in the European Union.

Social Content of the International Sphere: Symbols and Meaning in Franco-German Relations, CES Germany & Europe Working Papers, No. 02.2, 2002

“The Franco-German friendship is rich in memories and gestures that are at once important and symbolic, and that characterize the exceptional nature of the relationship between our two countries,” reflects former French economics minister and European Commission President Jacques Delors. Such symbolic acts and joint memories are not primarily about cooperation in specific instances. Rather, more generally, they denote what it means to act together. They lend significance to a relationship; they signify what is “at stake,” or what it is “all about.” They are about a deeper and more general social purpose underlying specific instances of cooperation. They are about the value and intrinsic importance that social relations incorporate. Symbols contribute to the institutionalization of social meaning and social purpose in dealing with one another. In this paper I clarify the concept of “predominantly symbolic acts and practices among states,” systematically explore such acts for the bilateral Franco-German relationship between the late 1950s and the mid-1990s, and scrutinize the specific meaning and effects that these practices have helped to generate and perpetuate.

Consensus, contradiction, and conciliation of interests: the geo-economics of the Energy Union. EPC Policy Brief, 8 July 2015

European Union energy policy calls for nothing less than a profound transformation of the EU's energy system: by 2050 decarbonised electricity generation with 80-95% fewer greenhouse gas emissions, increased use of renewables, more energy efficiency, a functioning energy market and increased security of supply are to be achieved. Different EU policies (e.g., EU climate and energy package for 2020) are intended to create the political and regulatory framework for this transformation. The sectorial dynamics resulting from these EU policies already affect the systems of electricity generation, transportation and storage in Europe, and the more effective the implementation of new measures the more the structure of Europe's power system will change in the years to come. Recent initiatives such as the 2030 climate/energy package and the Energy Union are supposed to keep this dynamic up. Setting new EU targets, however, is not necessarily the same as meeting them. The impact of EU energy policy is likely to have considerable geo-economic implications for individual member states: with increasing market integration come new competitors; coal and gas power plants face new renewable challengers domestically and abroad; and diversification towards new suppliers will result in new trade routes, entry points and infrastructure. Where these implications are at odds with powerful national interests, any member state may point to Article 194, 2 of the Lisbon Treaty and argue that the EU's energy policy agenda interferes with its given right to determine the conditions for exploiting its energy resources, the choice between different energy sources and the general structure of its energy supply. The implementation of new policy initiatives therefore involves intense negotiations to conciliate contradicting interests, something that traditionally has been far from easy to achieve. In areas where this process runs into difficulties, the transfer of sovereignty to the European level is usually to be found amongst the suggested solutions. Pooling sovereignty on a new level, however, does not automatically result in a consensus, i.e., conciliate contradicting interests. Rather than focussing on the right level of decision making, European policy makers need to face the (inconvenient truth of) geo-economical frictions within the Union that make it difficult to come to an arrangement. The reminder of this text explains these latter, more structural and sector-related challenges for European energy policy in more detail, and develops some concrete steps towards a political and regulatory framework necessary to overcome them.

Tidal and spatial variations of DI13C and aquatic chemistry in a temperate tidal basin during winter time

Here, the pelagic carbonate system and the ?13C signature of dissolved inorganic carbonate (DIC) were investigated in a tidal basin of the southern North Sea, the Jade Bay, with respect to tidal cycles and a transect towards the North Sea in winter time (January and November, 2010). Physical parameters, major and trace elements, and nutrient concentrations were considered, too. Primary production and pelagic organic matter respiration were negligible during winter time. Both, the compositional variations on the transects as well as during the tidal cycles indicate the mixing of North Sea with fresh water. The combined spatial co-variations of different parameters indicate an introduction of fresh water that was enriched in DI12C, metabolites (e.g., ammonia), protons, and dissolved redox-sensitive elements (e.g., Mn2+). During the January campaign, the discharge via the flood gates was limited due to ice cover of the hinterland drainage ditches, allowing for an observation of tidal variations without significant mixing contributions from surface water discharges. Considering a binary mixing model with North Sea and fresh water as end-members, the extrapolated fresh water end-member composition for this campaign is estimated to contain about 3.8 mmol/kg DIC , and enhanced concentrations of NH4+, Mn2+, and protons compared to North Sea water. The fast temporal response of dissolved geochemical tracers on tidal variations in the Jade Bay indicates a continuous supply of a fresh water component. The measured composition of fresh waters entering the Jade Bay via flood gates (end of October, 2010) did not match the values estimated by the binary mixing model. Therefore, the overall fresh water component likely is a mixture between sources originating from flood gates and (in January) dominating submarine groundwater discharge entering the Jade Bay. This model is consistent with the results obtained during the November campaign, when a more important contribution from flood gates is expected and a more variable fresh water end-member is estimated. The co-variations of the concentrations and the stable carbon isotope composition of DIC are applied to evaluate possible superimposed sink-source-transformation processes in the coastal waters and a general co-variation scheme is suggested.

Stable carbon and oxygen isotope composition of benthic foraminifera

Seventeen surface sediment samples from the North Atlantic Ocean off NE-Greenland between 76° and 81°N, and nine samples from the South Atlantic Ocean close to Bouvet Island between 48° and 55°S were taken with the aid of a Multiple Corer and investigated for their live (Rose Bengal stained) benthic foraminiferal content within the upper 15 cm of sediment. Preferentially endobenthic Melonis barleeanum, Melonis zaandami, and Bulimina aculeata as well as preferentially epibenthic Lobatula lobatula were counted from 1-cm-thick sediment slices each and analyzed for stable carbon and oxygen isotopic compositions of their calcareous tests. Live and dead specimens were counted and measured separately. The carbon isotopic composition of the foraminifera was compared to that of the dissolved inorganic carbon (DIC) of simultaneously sampled bottom water. During a period of one month, one station off NE-Greenland was replicately sampled once every week and samples were processed as above. Live specimens of Lobatula lobatula are confined to the uppermost two centimeters of sediment. Live specimens of Melonis spp. are found down to 8 cm within the sediment but with a distinct sub-surface maximum between 2 and 5 cm. The down-core distribution of live Bulimina aculeata shows a distinct surface maximum in the top centimeter and constant but low numbers down to 11-cm subbottom depth. The average stable carbon isotopic composition (d13C versus per mil PDB) of live Lobatula lobatula off NE-Greenland is by 0.4±0.1 per mil higher than the d13CDIC of the ambient bottom water at the time of sampling. There is evidence that this species calcify before the ice-free season, when bottom water d13CDIC is supposed to be higher. This would reconfirm the one-to-one relationship between d13C of ambient water DIC and cibicids, widely used by paleoceanographers. Live Melonis barleeanum show a negative offset from bottom water DIC of -1.7±0.6 per mil in the uppermost sediment and of -2.2±0.5 per mil in 3-4-cm subbottom depth. All d13C values of live Melonis spp. decrease within the upper four centimeters, regardless of the time of sampling and site investigated. The offset of live Bulimina aculeata from bottom water d13CDIC values of 8 stations rather constantly amounts to -0.6±0.1 per mil, no matter what subbottom depth the specimens are from. At one station however, where is strong indication of elevated organic carbon flux, the negative offset averaged over all sub-bottom depths increases to -1.5±0.2 per mil. Buliminids actively move within the sediment and by this either record an average isotope signal of the pore water or the signal of one specific calcification depth. The recorded signal, however, depends on the organic carbon flux and reflects general but site-specific pore water d13CDIC values. If compared with epibenthic d13C values from the same site, not influenced by pore water and related phytodetritus layer effects, Buliminad13C values bear some potential as a paleoproductivity proxy. Specimens of Melonis spp. seem to prefer a more static way of life and calcify at different but individually fix depths within the sediment. Although live specimens thus record a stratified pore water d13C signal, there is no means yet to correct for bioturbational and early diagenetic effects in fossil faunas.

The works of Plato. A new and literal version chiefly from the text of Stallbaum ...

Vol. I translated by Henry Cary, vol. II, by Henry Davis, vols. III-VI, by George Burges.

Biographical directory of the American Congress, 1774-1961 : the Continental Congress, September 5, 1774, to October 21, 1788 and the Congress of the United States, from the First to the Eighty-sixth Congress, March 4, 1789, to January 3, 1961, inclusive.

"This volume, compiled by Clifford P. Reynolds, publications technician of the [Joint] Committee [on Printing], is a revision of the Dictionary of the United States Congress and the general government, published in 1859 and again revised in 1869, by Charles Lanman; the Biographical annals of the civil government of the United States in 1876, by Joseph Lanman and James Anglin, and the Lanman edition of 1876 as corrected by Joseph M. Morrison in 1887; the Political register and congressional directory of 1878; by Ben: Perley Poore; the Biographical congressional directory of 1903, by O. M. Enyart; the Biographical congressional directory in 1911, the Biographical directory of the American Congress of 1927, by Ansel Wold, and the 1949 edition by James L. Harrison."

General school laws.

Vol. for 1864 bound with Report of the Superintendent of Public Instruction, 1863.

Canada, past, present and future : being a historical, geographical, geological and statistical account of Canada West /

"Business directory of Canada West": v.1, 184 p. at end.

Agriculture, Rural Development, Food and Drug Administration, and related agencies appropriations for 2006 : hearings before a Subcommittee of the Committee on Appropriations, House of Representatives, One Hundred Ninth Congress, first session /

Shipping list no. : 2005-0156-P (pt. 1A), 2005-0131-P (pt. 1B), 2005-0136-P (pt. 2), 2005-0172-P (pt. 3-5, 7), 2005-0185-P (pt. 6), 2005-0168-P (pt. 8), 2006-0066-P (pt. 9).

The Chorle and the Birde.

The Hors the Shepe & the Ghoos, "intended to accompany this, and a general title to both" (cf. note at end) were issued in 1822, as no 36.

Connaissance des temps /

Some issues accompanied by supplemental CD-ROMs.

General public school laws of Alabama, 1915.

Mode of access: Internet.

Annual report of the Adjutant General of the State of Wisconsin.

1864-65 have subtitle: with reports from the Quartermaster General and Surgeon General.

The Percy anecdotes : original and select /

Includes indexes for each v. and a general index, v. 20.