Gibt es eine politische Philosophie der Europäischen Union? = Is there a political philosophy of the European Union?. ZEI Discussion Paper C223, 2014

In a theoretical context, the European Union is generally interpreted through the prism of integration theories, which in turn reflect the ever changing empirical reality of the integration process. ZEI Director Ludger Kühnhardt asks if and to what extent the process of European integration has begun to generate a specific political philosophy which uses the EU - and not the classical notion of the state – as the starting and reference point for its reasoning. Kühnhardt examines examples – such as the European notion of civil rights and the notion of the Union itself, but also critical categories such as euroskepticism – which indicate that the EU itself is beginning to be the starting point and frame of reference for a reflection on the common good. For now, a political philosophy in the context of the European Union exists only in an embryonic stage, but the topic may generate intellectual insights through further and deeper research.

What drives the European Parliament? The Case of the General Data Protection Regulation. Bruges Political Research Papers 47/2015.

This paper evaluates which factors influence the European Parliament’s decision-making, based on a case study: the 2012 proposal for a General Data Protection Regulation. Following a ‘competitive testing’ approach, six different hypotheses are successively challenged in order to explain why the EP adopted a fundamental rights- oriented position. The first three factors relate to the internal organization of the EP’s work, i.e. the role played by the lead committee, by the rapporteur and by secretariat officials. The last three factors are external-related, i.e. lobbying activities, outside events and institutional considerations. Based on the empirical findings, it is argued that even though the EP’s position is due to a range of various factors, some of them prove to be more relevant than others, in particular the rapporteur and lead committee’s roles. New institutionalism theories also provide a comprehensive explanation for the EP’s willingness to achieve a fundamental rights oriented outcome.

Lithology and approximate sub-bottom depths and ages of the transition of soft to firm ooze and of firm ooze to chalk at DSDP Leg 89 and 90 Sites

Leg 90 recovered approximately 3705 m of core at eight sites lying at middle bathyal depths (1000-2200 m) (Sites 587 to 594) in a traverse from subtropical to subantarctic latitudes in the southwest Pacific region, chiefly on Lord Howe Rise in the Tasman Sea. This chapter summarizes some preliminary lithostratigraphic results of the leg and includes data from Site 586, drilled during DSDP Leg 89 on the Ontong-Java Plateau that forms the northern equatorial point of the latitudinal traverse. The lithofacies consist almost exclusively of continuous sections of very pure (>95% CaCO3) pelagic calcareous sediment, typically foraminifer-bearing nannofossil ooze (or chalk) and nannofossil ooze (or chalk), which is mainly of Neogene age but extends back into the Eocene at Sites 588, 592, and 593. Only at Site 594 off southeastern New Zealand is there local development of hemipelagic sediments and several late Neogene unconformities. Increased contents of foraminifers in Leg 90 sediments, notably in the Quaternary interval, correspond to periods of enhanced winnowing by bottom currents. Significant changes in the rates of sediment accumulation and in the character and intensity of sediment bioturbation within and between sites probably reflect changes in calcareous biogenic productivity as a result of fundamental paleoceanographic events in the region during the Neogene. Burial lithification is expressed by a decrease in sediment porosity from about 70 to 45% with depth. Concomitantly, microfossil preservation slowly deteriorates as a result of selective dissolution or recrystallization of some skeletons and the progressive appearance of secondary calcite overgrowths, first about discoasters and sphenoliths, and ultimately on portions of coccoliths. The ooze/chalk transition occurs at about 270 m sub-bottom depth at each of the northern sites (Sites 586 to 592) but is delayed until about twice this depth at the two southern sites (Sites 593 and 594). A possible explanation for this difference between geographic areas is the paucity of discoasters and sphenoliths at the southern sites; these nannofossil elements provide ideal nucleation sites for calcite overgrowths. Toward the bottom of some holes, dissolution seams and flasers appear in recrystallized chalks. The very minor terrigenous fraction of the sediment consists of silt- through clay-sized quartz, feldspar, mica, and clay minerals (smectite, illite, kaolinite, and chlorite), supplied as eolian dust from the Australian continent and by wind and ocean currents from erosion on South Island, New Zealand. Changes in the mass accumulation rates of terrigenous sediment and in clay mineral assemblages through time are related to various external controls, such as the continued northward drift of the Indo-Australian Plate, the development of Antarctic ice sheets, the increased desertification of the Australian continent after 14 m.y. ago, and the progressive increase in tectonic relief of New Zealand through the late Cenozoic. Disseminated glass shards and (altered) tephra layers occur in Leg 90 cores. They were derived from major silicic eruptions in North Island, New Zealand, and from basic to intermediate explosive volcanism along the Melanesian island chains. The tephrostratigraphic record suggests episodes of increased volcanicity in the southwest Pacific centered near 17, 13, 10, 5 and 1 m.y. ago, especially in the middle and early late Miocene. In addition, submarine basaltic volcanism was widespread in the southeast Tasman Sea around the Eocene/Oligocene boundary, possibly related to the propagation of the Southeast Indian Ridge through western New Zealand as a continental rift system.

Table 1: Main characteristics of the BIOTA observatories included in this study & Table 3: Occurrence of termite taxa at the observatories

Termites are the most important soil ecosystem engineers of semi-arid and arid habitats. They enhance decomposition processes as well as the subsequent mineralisation of nutrients by bacteria and fungi. Through their construction of galleries, nests and mounds, they promote soil turnover and influence the distribution of nutrients and also alter texture and hydrological properties of soils, thereby affecting the heterogeneity of their ecosystem. The main aim of the present thesis was to define the impact of termites on ecosys-tem functioning in a semi-arid ecosystem. In a baseline study, I assessed the diversity of termite taxa in relation to the amount of precipitation, the vegetation patterns and the land use systems at several sites in Namibia. Subsequently, I focussed on a species that is highly abundant in many African savannas, the fungus growing and mound building species Macro-termes michaelseni (Sjöstedt, 1914). I asked how this species influences the spatial hetero-geneity of soil and vegetation patterns. From repeated samplings at 13 sites in Namibia, I obtained 17 termite taxa of 15 genera. While the type of land use seems to have a minor effect on the termite fauna, the mean annual precipitation explained 96% and the Simpson index of vascular plant diversity 81% of the variation in taxa diversity. The number of termite taxa increased with both of these explanation variables. In contrast to former studies on Macrotermes mounds in several regions of Africa that I reviewed, soil analyses from M. michaelseni mounds in the central Namibian savanna revealed that they contain much higher nitrogen contents when compared to their parent material. Further analyses revealed that nitrate forms a major component of the nitrogen content in termite mounds. As nitrate solves easily in water, evaporation processes are most probably responsible for the transport of solved nitrates to the mound surface and their accumulation there. The analysed mounds in central Namibia contained higher sand propor-tions compared to the mounds of the former studies. Through the higher percentage of coarse and middle sized pores, water moves more easily in sandy soils compared to more clayey soils. In consequence, evaporation-driven nitrate accumulation can occur in the studied mounds at high rates. ff...

Sedimentation rates calculated on surface sediment samples from different site of the Atlantic and Pacific Oceans (Table 1)

Radiocarbon ages on CaCO3 from deep-sea cores offer constraints on the nature of the CaCO3 dissolution process. The idea is that the toll taken by dissolution on grains within the core top bioturbation zone should be in proportion to their time of residence in this zone. If so, dissolution would shift the mass distribution in favor of younger grains, thereby reducing the mean radiocarbon age for the grain ensemble. We have searched in vain for evidence supporting the existence of such an age reduction. Instead, we find that for water depths of more than 4 km in the tropical Pacific the radiocarbon age increases with the extent of dissolution. We can find no satisfactory steady state explanation and are forced to conclude that this increase must be the result of chemical erosion. The idea is that during the Holocene the rate of dissolution of CaCO3 has exceeded the rain rate of CaCO3. In this circumstance, bioturbation exhumes CaCO3 from the underlying glacial sediment and mixes it with CaCO3 raining from the sea surface.

Institutes of natural philosophy, theoretical and practical. With some corrections; change in the order of the branches; and the addition of an appendix to the astronomical part, selected from Mr. Ewing's Practical astronomy.

"Appendix to the astronomy. Containing solar and lunar tables, with their explanation and use, and the projection of eclipses, selected from 'Ewing's Practical astronomy'": [233]-297.

The San Jose scale, Aspidiotus perniciosus and some other destructive scale-insects of the State of New York /

Brief explanation printed on the verso of plates.

An analysis of the distinction between deep and shallow expert systems /

This paper analyzes the relationship between the techniques used to build expert systems and the behaviors they exhibit to show that there is not sufficient evidence to link the behavioral shortcomings of first-generation expert systems to the shallow methods of representation and inference they employ. There is only evidence that the shortcomings are a consequence of a general lack of knowledge. Moreover, the paper shows that the first-generation of expert systems employ both shallow methods and most of the so-called deep methods. Lastly, we show that deeper methods augment but do not replace shallow reasoning methods; most expert systems should possess both."

Northwest books, report of the Committee on Books of the Inland Empire Council of Teachers of English, 1942;

First edition issued as a mimeographed booklet in 1933. cf. "In explanation," signed: Rufus A. Coleman.

American church silver of the seventeenth and eighteenth centuries, with a few pieces of domestic plate, exhibited at the Museum of Fine Arts, July to December, 1911.

"American silversmiths": p. [127]-161.

A brief report on the study of governmental organization for the water resources of the Delaware River Basin

A brief abstract of the study on water resources administration made by the Syracuse University Research Group, giving the basic recommendations of the study and the reasoning behind them.

Some thoughts on the conduct of the understanding in the search of truth ...

First published in the author's Posthumous works, 1706. Written about 1697 for a new chapter in the Essay concerning human understanding.

A grammar of botany : illustrative of artificial, as well as natural classification: with an explanation of Jussieu's system /

"Abbé Correa published for the use of his class in Philadelphia [in 1815] a reduction of the genera of Muhlenberg's Catalogue according to the system of Jussieu." cf. J. W. Harshberger's The botanists of Philadelphia, Philadelphia, 1899, p. 8.

A full description of the daguerreotype process /

Includes Chilton's explanation of apparatus; French improvements reprinted from The Athenaeum, London, of 30 November 1839; observations by Chilton; and the first exposure-table by D. W. Seager.

Travels in the interior of Africa, from the Cape of Good Hope to Morocco from the years 1781 to 1797; through Caffraria, the kingdoms of Mataman, Angola, Massi, Monœnugi, Muschato [!] &c.

Translation of Landreise in das Innere von Afrika.