The role of Central Europe in the German economy. The political consequences. OSW Report June 2016

Recent publications allow us to conclude that the economic relations between Germany and Central Europe have come to the ‘end of history’, and nothing new will happen. However, a deeper analysis of these relationships reveals interesting new trends. Since joining the European Union the states of Central Europe have not settled for maintaining the average level of economic development, but have continued to narrow the distance between them and Western Europe, something which the global financial crisis did not prevent. Their improved economic situation also affected their relations with Germany. The latest results from the Visegrád Group states show them to be Germany’s most important trading partner, and their balance of trade in goods is in a state of equilibrium, while many euro area countries have recorded high trade deficits with Germany. The aim of this report is to display the trends in trade and investment between Germany and Central Europe, based on the example of the Visegrád Group. The author will also attempt to answer the question of whether the advancing economic cooperation between Germany and the V4 countries will lead to the further modernisation of those countries’ economies, or whether it will run the risk of leaving them in the ‘middle income trap’.

Neurogénese no cérebro adulto

Dissertação para obtenção do grau de Mestre no Instituto Superior de Ciências da Saúde Egas Moniz

Formación corporal motora. Una noción que se construye con los sujetos de enseñanza en Educación Física

Según el Plan de estudios 435/03 del Profesorado en Educación Física que se dicta en el Centro Regional Universitario Bariloche dependiente de la Universidad Nacional del Comahue existe, en los trayectos formativos de primer, segundo y tercer año, una asignatura cuya denominación es Formación Corporal Motora en adelante (FCM). En la misma se ha intentado, durante estos años, articular disciplinas deportivas como el Atletismo, la Gimnasia y la Natación. En esta comunicación se trata el encuadrede conocimiento que se desarrolla en la asignatura FCM3 del tercer nivel de la formación, planteando un espacio diferente respecto a la construcción de corporeidad y motricidad del sujeto. Se plantea como alternativa a las perspectivas gimnástica- higienista y físico-deportiva en la formación de profesionales de la Educación Física.Entonces ¿cómo se visibiliza la formación corporal motora del sujeto desde la enseñanza de las destrezas en las diversas propuestas pedagógicas? En este sentido, nada de lo que se lleve adelante en la enseñanza es ni neutral ni inocente,está teñido de sentido, de significado, de poder y de utopía. Siguiendo a Zerbino el reto es preguntarse ¿"qué estamos sosteniendo con aquello que hacemos"?

Formación corporal motora. Una noción que se construye con los sujetos de enseñanza en Educación Física

Según el Plan de estudios 435/03 del Profesorado en Educación Física que se dicta en el Centro Regional Universitario Bariloche dependiente de la Universidad Nacional del Comahue existe, en los trayectos formativos de primer, segundo y tercer año, una asignatura cuya denominación es Formación Corporal Motora en adelante (FCM). En la misma se ha intentado, durante estos años, articular disciplinas deportivas como el Atletismo, la Gimnasia y la Natación. En esta comunicación se trata el encuadrede conocimiento que se desarrolla en la asignatura FCM3 del tercer nivel de la formación, planteando un espacio diferente respecto a la construcción de corporeidad y motricidad del sujeto. Se plantea como alternativa a las perspectivas gimnástica- higienista y físico-deportiva en la formación de profesionales de la Educación Física.Entonces ¿cómo se visibiliza la formación corporal motora del sujeto desde la enseñanza de las destrezas en las diversas propuestas pedagógicas? En este sentido, nada de lo que se lleve adelante en la enseñanza es ni neutral ni inocente,está teñido de sentido, de significado, de poder y de utopía. Siguiendo a Zerbino el reto es preguntarse ¿"qué estamos sosteniendo con aquello que hacemos"?

Location, intervals and thickness of Cretaceous sections in Indian Ocean DSDP and ODP sites (Table 2)

The Indian Ocean covers approximately 73.5 * 10**6 km**3 from 25°N to 67°S and from 20° to 120°E. Several legs of the Deep Sea Drilling Project (DSDP) and the Ocean Drilling Program (ODP) have operated in its waters, many penetrating the Cretaceous. Most of the scientific drill sites are DSDP related and thus pre-dated modern biostratigraphic conventions. Foraminifers and calcareous nannoplankton were by far the dominant fossil groups studied in the earlier work, supplemented occasionally by studies of other fossil groups, The results of the Ocean Drilling Project phase are yet too young to be fully integrated but have been based on a broader range of techniques and fossil groups. During most of the Cretaceous, the proto-Indian Ocean basin lay in middle to high latitudes. Thus, it is unrealistic to expect successful routine application of low-latitude zonations. No planktonic foraminifer zonal scheme has been developed for the Indian Ocean basin for several reasons. There are no sections with complete or even significant partial sections to allow development of such a zonation. Carbonate compensation depth (CCD) effects have been marked in most sections, and significant intervals are devoid of planktonic foraminifers. The Indian Ocean now covers a great latitudinal range from tropics to polar regions and, at first glance, no scheme can be expected to be applicable over that entire range. In the Cretaceous the area was much smaller, though expanding progressively, and the paleolatitude range was quite small. Calcareous nannoplankton have proved valuable in dating Indian Ocean Cretaceous sediments and have, perhaps in contrast with the foraminifers, been consistently a more reliable means of applying zonal schemes developed elsewhere. For the Albian-Aptian, zonations based on well-known benthic foraminifer lineages (Scheibnerova, 1974) have been useful when nothing else was available or effective. Palynology has been used little, but where used, has proved excellent. It has the added value of providing valuable information on nearby terrestrial vegetation as the fossils were resistant to dissolution. Normally, when different fossil groups have been applied to a section, the results have been compatible or compatible to an acceptable degree. There are a few instances where incompatibility is noteworthy, and Site 263 is a classic example, as even two calcareous nannoplankton studies show irreconcilable differences here. All groups gave different results, but one benthic foraminifer analysis agreed with one calcareous nannoplankton study.

Carbon dioxide assimilation rate, gas and ion composition in samples, and bacterial production of organic matter within and above the Broken Spur and TAG hydrothermal fields, Mid-Atlantic Ridge

Rate of CO2 assimilation was determined above the Broken Spur and TAG active hydrothermal fields for three main ecosystems: (1) hydrothermal vents; (2) 300 m near-bottom layer of plume water; and (3) bottom sediments. In water samples from warm (40-45°C) vents assimilation rates were maximal and reached 2.82-3.76 µg C/l/day. In plume waters CO2 assimilation rates ranged from 0.38 to 0.65 µg C/l/day. In bottom sediments CO2 assimilation rates varied from 0.8 to 28.0 µg C/l/day, rising up to 56 mg C/kg/day near shrimp swarms. In the most active plume zone of the long-living TAG field bacterial production of organic matter (OM) from carbonic is up to 170 mg C/m**2/day); production of autotrophic process of bacterial chemosynthesis reaches about 90% (156 mg C/m**2/day). Thus, chemosynthetic production of OM in September-October is almost equal to that of photosynthetic production in the oceanic region. Bacterial production of OM above the Broken Spur hydrothermal field is one order lower and reaches only 20 mg C/m**2/day.

The complete works of Samuel Rowlands, 1598-1628, now first collected ...

v.3. Heavens glory, seeke it, &c., 1628. The famous history of Gvy erle of Warwicke, 1682. Miscellaneous poems. Notes, by Sidney J.H. Herrtage. Glossary, by Sidney J.H. Herrtage.

Coniston tales /

First published in: Nothing much: a monthly magazine.

Rolfe's Shakespeare /

Another ed. issued simultaneously, with flexible cloth binding (12mo), in series: English classics.

Tit-bits, or, How to prepare a nice dish at a moderate expense /

Includes index.

Shakspere quarto facsimiles /

--v. 25 Romeo and Juliet; the 1st quarto, 1597.--v. 26 Romeo and Juliet; the 2nd quarto, 1599.--v. 27 King Henry V; the 1st quarto, 1600.--v. 28 King Henry V; the 3rd quarto, 1608.--v. 29 Titus Andronicus; the 1st quarto, 1600.--v. 30 Sonnets; the 1st quarto, 1609.--v. 31 Othello; the 1st quarto, 1622.--v. 32 Othello, the 2nd quarto, 1630.--v. 33 King Lear; the 1st quarto, 1608.--v. 34 King Lear; the 2nd quarto, 1608.--v. 35 Lucrece; the 1st quarto, 1594.--v. 36 Romeo and Juliet; the undated quarto.--v. 37 First part of the Contention; the 1st quarto, 1594.--v. 38 True tragedy; the 1st quarto, 1595.--v. 39 Famous victories of Henry the fifth; the earliest known quarto, 1598.--v. 40-41 The troublesome raigne of John, king of England; the 1st quarto, 1591.--v. 42 Richard the third; the 3rd quarto 1602.--v. 43 Richard the third; the 6th quarto, 1622.

The century Shakespeare.

T.p. in green and black; illustrated lining papers.

Slovenské pohl'ady.

Redaktori: Svetozár Hurban (Vajanský), Jozef Škultéty.

If the Germans conquered England, and other essays,

"Practically all the essays in this book have appeared in the New statesman ... The sketch of T. M. Kettle appeared in the Daily news, and that of the Sheehy-Skeffington in the Ploughshare. The essay, "On nationalism and nationality," was written as a preface to a report of the Nationalities and subject races conference as long ago as 1910."--Pref. note.

Plays.

Each play has also special t.p.