Voyages dans l'intérieur de l'Afrique,

Translation of Tagebuch seiner reise von Cairo nach Murzuck der haupstadt des konigreichs Fessan in Afrika in 1797 und 1798.

Weltgeschichte.

Includes indexes.

Kolonial- und Kleinbahnen

von F. Baltzer, Geh. Oberbaurat und vortragendem Rat im Reichskolonialministerium, ordentl. Honorarprofessor an der techn. Hochschule zu Berlin

Continuous retinal vessel diameter m easurements: the future in retinal vessel assessment?

PURPOSE. To establish an alternative method, sequential and diameter response analysis (SDRA), to determine dynamic retinal vessel responses and their time course in serial stimulation compared with the established method of averaged diameter responses and standard static assessment. METHODS. SDRA focuses on individual time and diameter responses, taking into account the fluctuation in baseline diameter, providing improved insight into reaction patterns when compared with established methods as delivered by retinal vessel analyzer (RVA) software. SDRA patterns were developed with measurements from 78 healthy nonsmokers and subsequently validated in a group of 21 otherwise healthy smokers. Fundus photography and retinal vessel responses were assessed by RVA, intraocular pressure by contact tonometry, and blood pressure by sphygmomanometry. RESULTS. Compared with the RVA software method, SDRA demonstrated a marked difference in retinal vessel responses to flickering light (P 0.05). As a validation of that finding, SDRA showed a strong relation between baseline retinal vessel diameter and subsequent dilatory response in both healthy subjects and smokers (P 0.001). The RVA software was unable to detect this difference or to find a difference in retinal vessel arteriovenous ratio between smokers and nonsmokers (P 0.243). However, SDRA revealed that smokers’ vessels showed both an increased level of arterial baseline diameter fluctuation before flicker stimulation (P 0.005) and an increased stiffness of retinal arterioles (P 0.035) compared with those in nonsmokers. These differences were unrelated to intraocular pressure or systemic blood pressure. CONCLUSIONS. SDRA shows promise as a tool for the assessment of vessel physiology. Further studies are needed to explore its application in patients with vascular diseases.

Világpolitikai tendenciák 2011-ben = Global political trends in 2011

Az Amerikai Egyesült Államok – mint a világ gazdaságilag és katonailag legerősebb hatalma – hamarosan leküzdi a jelenlegi válságot és továbbra is vezető hatalom marad. Európában a főbb tennivalókat továbbra is a demográfiai helyzet, a migráció kezelése és az összeurópai intézmények kialakítása jelenti. A szovjet utódállamok etnikai feszültségekkel és demográfiai hanyatlással, továbbá az orosz befolyás erősödésével számolhatnak. A háborús térségekben a feszültség nem fog csökkenni – Irak, Afganisztán Irán, Észak-Afrika és a Közel-Kelet továbbra is a figyelem középpontjában lesz. Kína gazdasági növekedése következtében a világ második legnagyobb hatalmává léphet elő. Összességében megállapítható, hogy a világ az elmúlt években nem lett biztonságosabb és ez a tendencia folytatódik 2011-ben is. / === / The economic and political processes experienced in the world are followed by great attention not only by experts, but also by public opinion. The most important conclusions of the study are as follows: the United States – as the economically and politically strongest power in the world – will soon overcome the present crisis and preserve its leading power status. The main task in Europe will remain handling the demographic decline and migration, as well as to establish appropriate pan-European institutions. The post-Soviet successor states are facing ethnical tensions and demographic decline. In addition , they cannot resist the strengthening Russian influence. The tension in the war-zones is not expected to significantly ease, Iraq, Afghanistan, North Africa and the Middle East will remain high on the world's agenda. China – thanks to its economic growth – is going to become the second greatest power of the world. In the study we can read in detail about the development tendencies of the regions and states. To sum up, the world has not become safer at all in the past years and this tendency will continue also in 2011.

Földfelvásárlások Afrikában

Egy brit hátterű multinacionális cég, a ProCana igen komoly beruházást jelentett be 2007-ben: Mozambik Massingir nevű régiójában egy nagykapacitású bioetanol üzemet kívántak felépíteni. Ennek érdekében összesen 30 000 hektár földet kívántak bérelni a mozambiki kormánytól, amin cukornádat termeltek volna. A terv szerint a termésből helyben készült bioetanolt a maputói kikötőben tankhajókba töltve Európába exportáltak volna. A beruházás értékét több mint félmilliárd dollárra tették, amely nagyjából 2 000 munkahelyet teremtett volna, nem is beszélve arról, hogy jelentősen hozzájárult volna Mozambik infrastruktúrájának fejlődéséhez és az exportjának növekedéséhez.

Database of the GLAMAP project

A uniform chronology for foraminifera-based sea surface temperature records has been established in more than 120 sediment cores obtained from the equatorial and eastern Atlantic up to the Arctic Ocean. The chronostratigraphy of the last 30,000 years is mainly based on published d18O records and 14C ages from accelerator mass spectrometry, converted into calendar-year ages. The high-precision age control provides the database necessary for the uniform reconstruction of the climate interval of the Last Glacial Maximum within the GLAMAP-2000 project.

Compilation of 220 sediment core d13C data from the glacial Atlantic Ocean

We compare a compilation of 220 sediment core d13C data from the glacial Atlantic Ocean with three-dimensional ocean circulation simulations including a marine carbon cycle model. The carbon cycle model employs circulation fields which were derived from previous climate simulations. All sediment data have been thoroughly quality controlled, focusing on epibenthic foraminiferal species (such as Cibicidoides wuellerstorfi or Planulina ariminensis) to improve the comparability of model and sediment core carbon isotopes. The model captures the general d13C pattern indicated by present-day water column data and Late Holocene sediment cores but underestimates intermediate and deep water values in the South Atlantic. The best agreement with glacial reconstructions is obtained for a model scenario with an altered freshwater balance in the Southern Ocean that mimics enhanced northward sea ice export and melting away from the zone of sea ice production. This results in a shoaled and weakened North Atlantic Deep Water flow and intensified Antarctic Bottom Water export, hence confirming previous reconstructions from paleoproxy records. Moreover, the modeled abyssal ocean is very cold and very saline, which is in line with other proxy data evidence.

Sedimentology of sites 14-141, 41-366, 47-397 and 79-544B

Along the N-S-transect of DSDP-Sites 5446, 397, 141, and 366, oxygen and carbon isotopes, flux rates of calcium carbonate, terrigenous matter, and biogenic opal, clay minerals and the size distribution of terrigenous partictes were determined in order to assess the ties between atmospheric and oceanic surface and deep-water circulation off northwest Africa during the late Neogene. During the last 9 m.y., both the paleoceanography in the eastern Atlantic and west African paleodimates were intimately correlated with the evolution of the polar ice sheets as reflected in the benthos d18O curves of the 4 DSDP-Sites. These records make it possible to distinguish six major time intervals which were charaterized by long-term persistent regimes of climatic stability or climatic change. Short-term, "Milankovitch"-type cycles superimpose the long-term climatic evolution and may reflect the chronostratigraphic control fluctuations of the solar insolation persisting back to pre-Pleistocene times. Relatively stable, warm climates prevailed during the late Tortonian/early Messinean, 9 to 6 m.y., and the early Pliocene, 4.5 to 3.5 m.y. ago. Based on d18O curves, the amplitudes of short-term climatic variation were generally low, and the ice sheets were smaller than during peak Holocene time. Oceanic circulation and resulting paleoproductivity in upwelling zones were insignificant. The strength of dust supplying meridional trade winds was low (3 to 5 m/s), interglacial-style zonal winds near the ITCZ were dominant, as indicated by the high abundance of kaolinite. Phases of fluvial sediment supply were common. Humidity was characteristic of the climate in northwest Africa for the major part of this time. Major episodes of climatic deterioration in the subtropics occurred in the latest Miocene/early Pliocene, between some 5.6 and 5.2 and between 4.9 and 4.6 m.y. ago, in the late Pliocene, between 3.2 and 2.4 m.y. ago, and again in the Quaternary, near 1 m.y. ago. The episodes were correlated with marked increases of the global ice volume, as revealed by drastic increases of d18O values. They suggest sea-level falls of up to 70 m below the present sea level in the latest Miocene and earliest Pliocene and of 145 m in the latest Pliocene and Quaternary. The climatic changes resulted in strongly enhanced meridional trade winds as suggested by coarser terrigenous grain-sizes, increased mass accumulation rates of eolian dust, and changes in clay-mineral composition from dominantly kaolinite to illite and chlorite. The meridional trade winds reached speeds of 8 to 10 m/s with a maximum near 15 m/s. The enhanced winds probably led t o intensified coastal upwelling as shown by the contemporaneous local increase i n the deposition of biogenic silica and the local depletion of 13C at Site 397. The most drastic environmental changes near 2.4 and 1 m.y. ago coincide with hiatuses which may indicate phases of general erosion due to strongly enhanced deep-water circulation in the northeast At1antic along the northwest African continental margin. The occasional occurrence of quartz grains coarser than 250 µm may suggest ice-rafted debris in sediments off Morocco. During these time intervals the climate in NW-Africa was dominantly arid. Nevertheless, fluvial runoff (and humidity) continued to be important during intermittent warm phases of the short-term climatic cycles. During the end and the beginning of (inter-) glacial times, fluvial supply of nutrients seems to be the dominant factor, controling phases of enhanced paleoproductivity observed off northwest Africa, whereas during phases of glacial maximum strenger fertility of (increased) coastal upwelling becomes more important. A long-term evolution of paleoenvironments during the last 40 m.y. is depicted in the sediments of Site 366 and is clearly controlled by the plate tectonic route of this Site. During Oligocene times, Site 366 lay in the center of the equatorial upwelling, as shown by the high content of biogenic silica contributing up to 100 % of the carbonate-free sediment fraction >6 µm. The influence of equatorial upwelling abruptly terminated near 15 m.y. ago, a change in the record exaggerated by a hiatus of about 2 m.y. Prior to 25 m.y., the terrigenous input at the paleolatitude of Site 366 was restricted t o eolian sediment supply from South Africa by southeasterly trade winds, as shown by dominantly illite and chlorite in the clay fraction and extremely fine-grained terrigenous matter. Near the Oligocene/Miocene boundary, Site 366 drifted across the equator into the belt of the northeasterly trade winds, which is inferred from the increased content of kaolinite and coarser grain sizes of the terrigenous sediment fraction. The clay-mineral and grain-size compositions of Site 366 do not reflect a noteworthy northward shift of the ITCZ during late Miocene and early Pliocene times, i.e. no marked global circulation asymmetry due to the possible absence of a major Northern Hemisphere glaciation (Flohn 1981). This lack of a more northerly position of the ITCZ may result from a bipolar glaciation already existing during late Miocene times, such as also suggested by the evidence of tillites on Iceland and in southern Alaska during those intervals (e.g., Denton & Amstrong 1969, Mudie & Helgason 1983).

Tillsammans för god vattenstatus : Förvaltningsplan för Kumo älvs-Skärgårdshavets-Bottenhavets vattenförvaltningsområde 2016-2021

Förvaltningsplanen är ett allmänt planeringsdokument med den mest aktuella informationen om yt- och grundvattnen i Kumo älvs-Skärgårdshavets-Bottenvikens vattenförvaltningsområde, vattnens tillstånd och behovet av att förbättra tillståndet. Förvaltningsplanen innehåller bland annat resultaten från bedömningen av vattnens status och övervakningsprogrammen för yt- och grundvattnen. En central del av förvaltningsplanen är sammanfattningen av de vårdåtgärder som planeras för att förbättra vattnens tillstånd samt bedömningen av åtgärdernas genomslagskraft vattenförvaltningsperioden 2016-2021. Sammanfattningen baseras på vattenförvaltningsområdets åtgärdsprogram, som innehåller information om enskilda vattendrag och vattenförekomster samt enskilda grundvattenområden. Åtgärdsprogrammen är mer användbara dokument än förvaltningsplanen om man behöver information om vattnen i ett begränsat område, till exempel om deras status samt behov av åtgärder och åtgärdernas effekter. Miljörapporten om effekterna av åtgärdsprogrammen utgörs av kapitel 14 i förvaltningsplanen. Kumo älvs-Skärgårdshavets-Bottenvikens vattenförvaltningsområde omfattar de vattendrag som rinner ut i Skärgårdshavet, Bottenviken, Kvarken och södra Bottenhavet från Kisko å till Pöntiönjoki inklusive vattendragens avrinningsområden.

Lebensrealitäten im Zentrum der Wissensvermittlung. Afrikaspezifische Veranstaltungen der entwicklungspolitischen Bildungsarbeit

Der vorliegende Beitrag beschäftigt sich mit afrikaspezifischen Veranstaltungen der entwicklungspolitischen Bildungsarbeit und den durch Referent/inn/en vermittelten Inhalten über den Lebensalltag in afrikanischen Ländern. Es wird aufgezeigt, dass der Prozess der Herausbildung des vermittelten Wissens in den Veranstaltungen durch das Zusammenspiel verschiedener Aspekte charakterisiert ist. Dazu gehören die institutionelle und diskursive Einordnung entwicklungspolitischer Bildungsarbeit in die Gesellschaft, die biographischen Hintergründe der Referent/inn/en und ihre Wahrnehmung gesellschaftlicher Wirklichkeit. (DIPF/Orig.)

Afrikabilder aus ethnopsychoanalytischer Perspektive

In diesem Beitrag wird diskutiert, welches Potenzial die ethnopsychoanalytische Theorieperspektive für eine Reflexion Globalen Lernens im Kontext oder in Bezug auf Afrika haben kann. Dabei wird zunächst der Ansatz der Ethnopsychoanalyse näher erläutert. Anschließend werden Konsequenzen für afrikabezogenes Globales Lernen gezogen. (DIPF/Orig.)

"Repräsentationen" Afrikas in deutschen Schulbüchern am Beispiel des Schulfachs Geschichte (Sek I und II). Eine Stichprobenanalyse

Dieser Artikel befasst sich mit der Repräsentation Afrikas in schulischen Geschichtsbüchern. Am Beispiel von drei aktuellen Lehrwerken zeigen die Autorinnen sowohl negative Darstellungsweisen als auch positive Entwicklungen in Bezug auf den Umgang mit dem Kontinent, seiner Geschichte und Bevölkerung auf. In einem abschließenden Teil stellen sie einen Zusammenhang zwischen den Analyseergebnissen und dem Bewusstsein über bis in die heutige Zeit reproduzierte Diskurse und über Alltagsrassismen dar. (DIPF/Orig.)

Arm aber gemütlich. Afrikabilder deutscher Jugendlicher

Internationale Jugendbegegnungen in Ländern der Entwicklungszusammenarbeit ermöglichen Teilnehmenden ein erfahrungsbasiertes statt theoretisch vermitteltes Bild des jeweiligen Landes/Kontinents. Basierend auf Daten einer qualitativen Forschungsarbeit zu internationalen Jugendbegegnungen im Nord-Süd-Kontext wird das Afrikabild einer deutschen Jugendgruppe nach einem dreiwöchigen Aufenthalt in Ruanda beschrieben: Afrikaner sind (finanziell) von den Industriestaaten abhängig. Trotz ihrer Armut sind sie zufrieden und es herrscht Gemütlichkeit. Sie singen und tanzen und der Glaube spielt eine wichtige Rolle. Abschließend wird diskutiert, wie Begegnungen konzipiert werden sollten, damit solche defizitorientierten und Armut romantisierenden Bilder vermieden werden können. (DIPF/Orig.)