Documente privitoare la istoria românilor.

Includes indexes.

Imbunătățirea agriculturei ca bază a îmbunătățirei soartei țăranilor. [microform]

Microfilm (negative).

Buletinul

Mode of access: Internet.

Discursuri de Receptiune

Mode of access: Internet.

Radiocarbon ages and pollen record of a sediment core from Lake Lyadhej-To

An 1180-cm long core recovered from Lake Lyadhej-To (68°15'N, 65°45'E, 150 m a.s.l.) at the NW rim of the Polar Urals Mountains reflects the Holocene environmental history from ca. 11,000 cal. yr BP. Pollen assemblages from the diamicton (ca. 11,000-10,700 cal. yr BP) are dominated by Pre-Quaternary spores and redeposited Pinaceae pollen, pointing to a high terrestrial input. Turbid and nutrient-poor conditions existed in the lake ca. 10,700-10,550 cal. yr BP. The chironomid-inferred reconstructions suggest that mean July temperature increased rapidly from 10.0 to 11.8 °C during this period. Sparse, treeless vegetation dominated on the disturbed and denuded soils in the catchment area. A distinct dominance of planktonic diatoms ca. 10,500-8800 cal. yr BP points to the lowest lake-ice coverage, the longest growing season and the highest bioproductivity during the lake history. Birch forest with some shrub alder grew around the lake reflecting the warmest climate conditions during the Holocene. Mean July temperature was likely 11-13 °C and annual precipitation-400-500 mm. The period ca. 8800-5500 cal. yr BP is characterized by a gradual deterioration of environmental conditions in the lake and lake catchment. The pollen- and chironomid-inferred temperatures reflect a warm period (ca. 6500-6000 cal. BP) with a mean July temperature at least 1-2 °C higher than today. Birch forests disappeared from the lake vicinity after 6000 cal. yr BP. The vegetation in the Lyadhej-To region became similar to the modern one. Shrub (Betula nana, Salix) and herb tundra have dominated the lake catchment since ca. 5500 cal. yr BP. All proxies suggest rather harsh environmental conditions. Diatom assemblages reflect relatively short growing seasons and a longer persistence of lake-ice ca. 5500-2500 cal. yr BP. Pollen-based climate reconstructions suggest significant cooling between ca. 5500 and 3500 cal. yr BP with a mean July temperature 8-10 °C and annual precipitation-300-400 mm. The bioproductivity in the lake remained low after 2500 cal. yr BP, but biogeochemical proxies reflect a higher terrestrial influx. Changes in the diatom content may indicate warmer water temperatures and a reduced ice cover on the lake. However, chironomid-based reconstructions reflect a period with minimal temperatures during the lake history.

Pollen profile and age determination for sediment core M72/5_619-1 (22-GC3)

Sediments from the Black Sea, a region historically dominated by forests and steppe landscapes, are a valuable source of detailed information on the changes in regional terrestrial and aquatic environments at decadal to millennial scales. Here we present multi-proxy environmental records (pollen, dinoflagellate cysts, Ca, Ti and oxygen isotope data) from the uppermost 305 cm of the core 22-GC3 (42°13.53' N, 36°29.55' E) collected from a water depth of 838 m in the southern part of the Black Sea in 2007. The records span the last ~ 18 kyr (all ages are given in cal kyr BP). The pollen data reveal the dominance of the Artemisia-steppe in the region, suggesting rather dry/cold environments ~ 18-14.5 kyr BP. Warming/humidity increase during melt-water pulses (~ 16.1-14.5 kyr BP), indicated by d18O records from the 22-GC3 core sediment and from the Sofular Cave stalagmite, is expressed in more negative d13C values from the Sofular Cave, usually interpreted as the spreading of C3 plants. The records representing the interstadial complex (~ 14.5-12.9 kyr BP) show an increase in temperature and moisture, indicated by forest development, increased primary productivity and reduced surface run-off, whereas the switch from primary terrigenous to primary authigenic Ca origin occurs ~ 500 yr later. The Younger Dryas cooling is clearly demonstrated by more negative d13C values from the Sofular Cave and a reduction of pines. The early Holocene (11.7-8.5 kyr BP) interval reveals relatively dry conditions compared to the mostly moist and warm middle Holocene (8.5-5 kyr BP), which is characterized by the establishment of the species-rich warm mixed and temperate deciduous forests in the low elevation belt, temperate deciduous beech-hornbeam forests in the middle and cool conifer forest in upper mountain belt. The border between the early and middle Holocene in the vegetation records coincides with the opening of the Mediterranean corridor at ~ 8.3 kyr BP, as indicated by a marked change in the dinocyst assemblages and in the sediment lithology. Changes in the pollen assemblages indicate a reduction in forest cover after ~ 5 kyr BP, which was likely caused by increased anthropogenic pressure on the regional vegetation.

Pollen record and age determination of profile CS98-10 at Cape Shpindler, Yugorski Peninsula, northwest Russia

New pollen and radiocarbon data from an 8.6-m coastal section, Cape Shpindler (69°43' N; 62°48' E), Yugorski Peninsula, document the latest Pleistocene and Holocene environmental history of this low Arctic region. Twelve AMS 14C dates indicate that the deposits accumulated since about 13,000 until 2000 radiocarbon years BP. A thermokarst lake formed ca. 13,000-12,800 years BP, when scarce arctic tundra vegetation dominated the area. By 12,500 years BP, a shallow lake existed at the site, and Arctic tundra with Poaceae, Cyperaceae, Salix, Saxifraga, and Artemisia dominated nearby vegetation. Climate was colder than today. Betula nana became dominant during the Early Preboreal period about 9500 years BP, responding to a warm event, which was one of the warmest during the Holocene. Decline in B. nana and Salix after 9500 years BP reflects a brief event of Preboreal cooling. A subsequent increase in Betula and Alnus fruticosa pollen percentages reflects amelioration of environmental conditions at the end of Preboreal period (ca. 9300 years BP). A decline in arboreal taxa later, with a dramatic increase in herb taxa, reflects a short cold event at about 9200 years BP. The pollen data reflect a northward movement of tree birch, peaking at the middle Boreal period, around 8500 years BP. Open Betula forest existed on the Kara Sea coast of the Yugorski Peninsula during the Atlantic period (8000-4500 years BP), indicating that climate was significantly warmer than today. Deteriorating climate around the Atlantic-Subboreal boundary (ca. 4500 years BP) is recorded by a decline in Betula percentages. Sedimentation slowed at the site, and processes of denudation and/or soil formation started at the beginning of the Subatlantic period, when vegetation cover on Yugorski Peninsula shifted to near-modern assemblages.

Pollen and macrofossil profiles from six cores in Illinois, U.S.A

Pollen analysis of Wisconsinan sediments from eleven localities in northern and central Illinois, combined with the results of older studies, allows a first general survey of the vegetational changes in Illinois during the last glaciation. In the late Altonian (after 40,000 B.P.), pine was already the most prevalent tree type in northern Illinois. Probably because of the influence of the last Altonian ice advance to northern Illinois, pine migrated to the south and reached south-central Illinois, which was at that time a region of prairie, with oak and hickory trees in favorable sites. Likewise in the late Altonian, spruce appeared in northern Illinois. Spruce also expanded its area to the south during the Wisconsinan, reaching south-central Illinois only after 21,000 B.P., in the early Woodfordian. Deciduous trees (predominantly oak) were present in south-central Illinois throughout the Wisconsinan. Their prevalence decreased to the north. The vegetation during the different subdivisions of the last glacial period in Illinois was approximately as follows: Late Altonian: Pine/spruce forest with some deciduous trees in northern and central Illinois; prairie and oak/hickory stands in south-central Illinois; immigration of pine. Farmdalian: Pine/spruce forest in central Illinois; deciduous trees and pine in south-central Illinois, with areas of open vegetation, perhaps similar to the present-day transition of prairie to forest in the northern Great Plains. Woodfordian: Northern and central Illinois ice covered; in south central Illinois, spruce and oak as dominant tree types, but also pine and grassland. During the Woodfordian, pine and spruce disappeared again from south-central Illinois, and oak/hickory forest and prairie again prevailed. The ice-free areas of northern Illinois become populated temporarily with spruce, but later there is proof of deciduous forest in this region. Pollen investigations in south-central Illinois have shown convincingly that deciduous trees could survive relatively close (less than 60 km) to the ice margin. Therefore the frequently presented view that arctic climatic conditions prevailed in North America during the last glaciation far south of the ice margin can be refuted for the Illinois area, confirming the opinion of other authors resulting from investigations of fossil mollusks and frost-soil features. The small number of localities investigated still permits no complete reconstruction of the vegetation zones and their possible movements in Illinois. During the Altonian and Farmdalian in Illinois, a vegetational zonation probably existed similar to that of today in North America. As the ice pushed southward as far as 39° 20' N. lat in the early Woodfordian, this zonation was apparently broken up under the influence of a relatively moderate climate. In any case, the Vandalia area, which was only about 60 km south of the ice, was at that time neither in a tundra zone nor in a zone of boreal coniferous forest.

Pollen flux off Cape Blanc

Fluxes of airborne freshwater diatoms (FD), phytoliths (PH), and pollen grains (PO) collected with sediment traps off Cape Blanc, northwest Africa, from 1988 till 1991 are presented. Both continental rainfall variations and wind mean strength and direction play a key role in the temporal fluctuations of the fluxes of eolian traces in the pelagic realm. Drier conditions in Northern Africa in 1987 could have preceded the high lithogenic input and moderate FD flux in 1988. The PH peak in summer 1988 was probably caused by increased wind velocity. Wetter rainy seasons of 1988/89 might have promoted a significant pollen production in summer 1989, and FD in late 1989 and early 1990, as well as contributed to the reduction of the lithogenic flux in 1989/90. Decreased fluxes of FD, PH and PO, and higher contribution of the 6-11 µm lithogenic fraction in 1991 would mainly reflect minor intensity and decreased amount of continental trade winds. Air-mass backward trajectories confirm that the Saharan Air Layer is predominantly involved in the spring/summer transport. Trade winds play a decisive role in the fall/winter months, but also contribute to the transport during late spring/summer. Origin of wind trajectories does not support a direct relationship between transporting wind-layers and material source areas in Northern Africa. High winter fluxes of eolian tracers and high amount of trade winds with continental origin in summer warn against a simplistic interpretation of the seasonal eolian signal preserved in the sediments off Cape Blanc, and the wind layer involved in its transport.

Pollen records from Bol'shoy Lyakhovsky Island, Siberia

Cryolithological, ground ice and fossil bioindicator (pollen, diatoms, plant macrofossils, rhizopods, insects, mammal bones) records from Bol'shoy Lyakhovsky Island permafrost sequences (73°20'N, 141°30'E) document the environmental history in the region for the past c. 115 kyr. Vegetation similar to modern subarctic tundra communities prevailed during the Eemian/Early Weichselian transition with a climate warmer than the present. Sparse tundra-like vegetation and harsher climate conditions were predominant during the Early Weichselian. The Middle Weichselian deposits contain peat and peaty soil horizons with bioindicators documenting climate amelioration. Although dwarf willows grew in more protected places, tundra and steppe vegetation prevailed. Climate conditions became colder and drier c. 30 kyr BP. No sediments dated between c. 28.5 and 12.05 14C kyr BP were found, which may reflect active erosion during that time. Herb and shrubby vegetation were predominant 11.6-11.3 14C kyr BP. Summer temperatures were c. 4 °C higher than today. Typical arctic environments prevailed around 10.5 14C kyr BP. Shrub alder and dwarf birch tundra were predominant between c. 9 and 7.6 kyr BP. Reconstructed summer temperatures were at least 4 °C higher than present. However, insect remains reflect that steppe-like habitats existed until c. 8 kyr BP. After 7.6 kyr BP, shrubs gradually disappeared and the vegetation cover became similar to that of modern tundra. Pollen and beetles indicate a severe arctic environment c. 3.7 kyr BP. However, Betula nana, absent on the island today, was still present. Together with our previous study on Bol'shoy Lyakhovsky Island covering the period between about 200 and 115 kyr, a comprehensive terrestrial palaeoenvironmental data set from this area in western Beringia is now available for the past two glacial-interglacial cycles.

Pollen records of five sediment cores from northern Germany

Within a larger program research work is being done on the history of settlement and landscape of the 'Siedlungskammer' Flögeln and the adjacent area. The 'Siedlungskammer' consists of an isolated pleistocene sand ground (Geest-island) surroundet by bogs. Starting from the edge of the Geest, near which large-scale archaeological excavations are carried out, three raised bog profiles were taken at 300, 500 and 4000 m off the prehistoric settlement. They were investigated by means of pollen analysis, and reflect in a decreasing way the activities of man on the Geestisland. Another pollen diagram from the nearby fen peat was worked out for comparison. At the same time it helped to date back a prehistoric sand path to the Roman period. The pollen diagrams cover the vegetational history without gaps from the early Atlantic period to modern times. The vegetation was decisively determined by the poor soils of this area. T'he pollen diagrams give evidence of the activity of settlers since the Neolithic age, with some gaps in the beginning, but later continuously from the middle of the Bronze age until the early migration period. The influence of the nearby settlement, which existed from the Birth of Christ to the 4/5th century, comes out distinctly. Among the cereals which were then cultivated here, there also was rye, at least in the 4/5th century, but most probably already during the Roman period. Besides that people cultivated barley, oats, and flax. The settlement break during the so-called dark ages between the 4/5th century and the time about 800 A.D. was confirmed by pollen analysis. During this time the area was once more covered by forests. The fluctuations of man's activities during the late Middle Ages and modern times, as they are made visible by pollen analysis, correspond to historically wellknown developments.

Vänskap är magisk : En reparativ läsning av samtida svensk seriekonst

In this thesis, I do a reparative reading of contemporary Swedish comics, that uses feminine signifiers, both in their imagery and writing. A crucial point of departure, in this thesis, is how literature can ”do” theory and be seen as a way of creating knowledge. I explore what the comics does to me, as a reader, and how. I experiment with the form and style of academic writing in order to clearly define my position and situate the production of knowledge. By focusing on the affects and nourishment, that the comics contain, I try to imagine a feminist other, with the help of my figuration: Nietzsche Minaj, and my imaginary utopian place: ”mitt flick(tionella) rum”. I conclude, that the comics both reproduce and transform feminine signifiers, while challenging the idea of dichotomies, in the spirit of gurlesque theory.

"En personalstyrka som går på knäna" : - En kvalitativ studie om betydande faktorer i sjuksköterskeyrket

I sjukhuskorridorerna står flera rum tomma och operationssalar används inte fullt ut. Anledningen är inte att medborgarna blivit friskare, inte heller är det ekonomin som är huvudorsaken, skälet är bristen på sjuksköterskor1. År 2015 publicerades en artikel om att allt fler sjuksköterskor lämnar Falu Lasarett på grund av dess tunga tre skift2. Vid denna studies början ville vi gå till botten med vad som är attraktivt i sjuksköterskeyrket, varför man väljer att bli sjuksköterska när yrket tycks vara kantat av negativa faktorer. Det vi tidigt märkte var att yrket inte endast kunde beskrivas som antingen attraktivt eller oattraktivt. Syftet med studien blev därför att identifiera attraktiva och oattraktiva faktorer i sjuksköterskeyrket. För att nå syftet eftersöktes respondenter via sociala medier där spridningen blev stor och stoppades när nio sjuksköterskor valt att delta. Respondenterna hade anställning på Falu Lasarett och intervjuas med hjälp av processmetoden "attraktivt arbete". Denna metod har varit ett verktyg i insamlandet av teori och empiri, faktorerna har gett oss handfasta sökord och varit användbara för respondenterna att resonera kring. Resultatet visade att respondenterna upplevde att relationer och social kontakt bidrog till yrkets attraktivitet. De ansåg sig även bli stimulerade av det varierande arbetet i form av tankearbete, praktiskt arbete och det resultat de presterade. De förbättringsområden som studien identifierat är föga förvånande; lön, arbetstid, arbetstakt, status, erkänsla, företaget, ledarskap men även faktorn eftertraktad bedömdes som mindre attraktiv då respondenterna ansåg att de endast var eftertraktade på grund av sin yrkestitel. Störst fokus har lagts på ledarskap, en faktor som tidigt identifierades som ett förbättringsområde. Problematiken kring ledarskapet tycks bottna i det faktum att chefsrekryteringar sker internt på arbetsplatsen och att de chefsutbildningar som erbjuds inte räcker till. Studien har för avsikt att identifiera förbättringsområden, ingen intention har funnits om att studien skulle resultera i en handlingsplan. Vi ser ämnet för komplext för att en C-uppsats skulle kunna landa i en lösning på de problem som sjuksköterskeyrket dras med.

Från nationsbyggare till global marknadsnomad : Om medborgarskap i svensk utbildningspolitik under 1990-talet

I den här avhandlingen är intresset riktat mot svensk utbildningspolitik och medborgarskap. I tider av globalisering, och med ett etablerat svenskt medlemskap i Europeiska unionen, har det nationella policyskapandet kring utbildningens medborgardanande funktion hamnat under ökat tryck. I studien undersöks hur detta hanteras i svensk utbildningspolitik under 1990-talet, en tid som utmärker sig genom betydande förändringar på utbildningsområdet i Sverige. Frågan är, mera precist, vilken riktning för skolans, enligt lag befästa, uppdrag att fostra demokratiska medborgare som utstakas i svensk utbildningspolitik vid denna tid. Genom att fästa vikt vid mål, visioner och motiv som formuleras i utbildningspolitiska 1990-talstexter klarläggs förståelser av medborgarskap som karaktäriserar svensk utbildningspolitik under denna tid. Även en bredare historisk analys görs, ur vilken historiska målsättningar med skolans medborgarfostran som föregår 1990-talets framträder. Studiens syfte är kritiskt. Förståelserna granskas utifrån vad de innesluter och vad de utesluter, vilka möjliga konsekvenser de kan tänkas få för olika individer och grupper i samhället, och om det finns öppningar för tänkbara alternativ. Studien visar på två historiska skiften vad gäller medborgarskapets innehåll och mening i det inhemska policyskapandet. Det första skiftet äger rum under 1990-talets tidiga del. Då bryts en etablerad samhällsbyggande medborgarroll upp, till förmån för andra mera marknadsorienterade medborgarroller. Under 1990-talets senare del, då marknadsorienteringen förstärks i neoliberal riktning, sker ett andra skifte; en historiskt vedertagen gemenskapstanke – nationen – bryts upp som grund för medborgerlig gemenskap. Denna tanke ersätts av en annan som är globaliseringsinriktad, vilken visar sig ha andra inne- och uteslutande mekanismer för olika individer och samhällsgrupper. Utifrån dessa forskningsrön tecknas avslutningsvis några konturer till ett alternativt sätt att tänka kring medborgarskap och gemenskap. Detta alternativ tar form i ambitionen att, i högre grad än vad som blir synligt i svensk utbildningspolitik, resonera kring möjligheter för ett medborgarskap bortom förhandstecknade indelningsgrunder för ett “vi”. Språk som politisk och samhällelig förändringskraft ges en central betydelse i avhandlingen. I analysen av texternas tal om skolans medborgarfostrande roll undersöks pågående politiska motsättningar när det gäller att vinna tal- och tolkningsföreträde till skolans fostransmål. Utgångarna av dessa motsättningar belyses genom tre områden för medborgarfostran som urskilts som centrala; ett politiskt, ett kulturellt samt ett ekonomi- och arbetslivsriktat. Genom dessa har rådande medborgarskapsdiskurser tagit form, ur vilka de utbildningspolitiska förståelserna av medborgarskap gestaltas och diskuteras.

Recension av Andkjær, Søren, Bentsen, Peter & Ejbye-Ernst, Niels (2009) ”Friluftsliv: Natur, samfund og pædagogik” : Ambitiöst om friluftsliv i Danmark – kanske alltför ambitiöst...

Friluftsliv uppvisar ett uppsving som för många säkert är oväntat men som nog till stor del är i samklang med den skandinaviska tidsandan. Visserligen är det ett i huvudsak urbant fenomen, de senaste årens fokus på fysisk aktivitet, konditionsträning och fitness, aktiviteter som dessutom ofta äger rum inomhus i speciella kommersiellt drivna träningshallar – där är luften inte fri! – men trenden tar sig också uttryck i löpning eller joggning i urbana parkområden eller i lagom tuktad natur i anslutning till städer. Man kan tänka att steget inte skulle vara långt till verkliga naturupplevelser, och, som sagt, det finns ett uppsving. Det nymornade intresset för autentiska naturupplevelser kan säkert också bottna i en civilisationskritisk trend i det tidiga tredje millenniet, vars beståndsdelar spretar på ett sätt som gör det omöjligt att närmare skärskåda företeelsen i detta sammanhang. Istället konstaterar vi att forskningen varit kvick att fånga upp friluftsintresset, vilket inte minst märks i recensionsfloran på den här webbplatsen, som denna gång utvidgas med en recension av Friluftsliv: Natur, samfund og pædagogik av Peter Bentsen, Søren Andkjær och Niels Ejbye-Ernst (Munksgaard Danmark). Erik Backman, som disputerat i ämnet, har läst och recenserar, och han bjuder redaktörerna på många tips till förbättringar inför nästa upplaga av boken.