Human and climatic impact on mires: a case study of Les Amburnex mire, Swiss Jura Mountains

Modern period long-term human and climatic impacts on a small mire in the Jura Mountains were assessed using testate amoebae, macrofossils and pollen. This multiproxy data analysis permitted detailed interpretations of local and regional environmental change and thus a partial disentanglement of the different variables that influence long-term mire development. From the Middle Ages until a.d. 1700 the mire vegetation was characterised by ferns, Caltha and Vaccinium, but then abruptly changed into the modern vegetation characterised by Cyperaceae, Potentilla and Sphagnum. The cause for this change was most probably deforestation, possibly enhanced by climatic cooling. A decrease in trampling intensity by domestic animals from a.d. 1950 onwards allowed Sphagnum growth and climatic warming in the a.d. 1980s and 1990s may have been responsible for considerable changes in the species composition. The mire investigated is an example of the rapid changes in mire vegetation and peat development that occurred throughout the central European mountain region during the past centuries as a result of changing climate and land-use practice. These processes are still active today and will determine the future development of high-altitude mires.

Writing theatre history – The mainstream approach and alternatives

Main questions: 1. How to deal with the beginnings of theatre? 2. Do we have to consider a “second birth of theatre” in the Middle Ages? 3. What influences do media have on writing theatre histories?

A Late-glacial and Holocene record of climatic change from a Swiss peat humification profile

Colorimetric measurements of alkaline extracts from two Swiss peat cores have provided a complete 14500-year-long record of peat humification, a proxy of effective precipitation. Peat from the cold Younger Dryas (11050–9550 cal. bc) was well preserved despite low levels of precipitation. A particularly dry period, peaking at c. 7100 cal. bc, is indicated by well-decomposed peat. Peat from c. 6750–4250 cal. bc shows a low degree of decomposition, indicating a wet bog surface despite relatively warm temperatures and therefore indicating high levels of precipitation. A sharp transition to higher levels of decomposition c. 4450–3750 cal. bc indicates a major transition to a drier bog surface. Subsequently, peat humification generally decreases towards the end of the deeper profile (c. cal. ad 1050), indicating a gradual return to wetter conditions. This gradual decrease is punctuated by periods of particularly low humification which appear to be due to shifts to higher levels of effective precipitation from c. 2500 to 1350 cal. bc, c. 1050 to 550 cal. bc, centered around 150 cal. bc, and from c. cal. ad 550 onwards. Anthropogenic influences appear to have affected peat humification at the site at least since the Middle Ages. This study indicates that humification in colder regions/time periods could be more affected by temperature than precipitation and vice versa.

Una bella roba. ‘Novellare’ als Erzählkonzept in Boccaccios ›Decameron‹

Der narrative Entwurf von Boccaccios ›Decameron‹ und Boccaccios theoretische Reflexionen über das Erzählen stehen klar im Fluchtpunkt der horazischen Lehre des prodesse et delectare. Vor diesem Horizont entwickelt Boccaccio sein Konzept des novellare, das einerseits ein ‚Wiedererzählen’ (analog zu mhd. erniuwen) beinhaltet und andererseits zu einer neuen Autonomie des Erzählens vorstößt. Beobachten lässt sich dieser Vorgang des Erneuerns weniger in Boccaccios theoretischen Ausführungen (etwa im Schlusswort des ›Decameron‹ oder in den ›Genealogie deorum gentilium‹) als in seiner dichterischen Praxis. Als Schlüsseltext wird im Vortrag die Novelle von der duldsamen Griselda herangezogen, die das ›Decameron‹ beschließt und die mit den Worten una bella roba endet. Das ‚schöne Kleid’ ist einerseits traditionelle Dichtungsmetapher (im Horizont des investire bzw. integumentum), andererseits intradiegetischer Bestandteil des Erzähl-‚Stoffs’ der Novelle. Bei Boccaccio dürfte das Gewand der Griselda, zusammen mit deren wiederholt thematisierter Nacktheit, dazu dienen, eine in die Novelle verpackte stoische Lehre zu vergegenwärtigen, diese in eine Erzählung ‚einzukleiden’. Das Kleid der Griselda wird so zur ‚Pathosformel’ (in der Begrifflichkeit A. Warburgs) bzw. zum ‚Faltenwurf’ (in der Begrifflichkeit G. Didi-Hubermans), mithin zur Verkörperung eines ‚neuen Erzählens’, das sich (im Gegensatz etwa zu Dante) von metaphysischen Entwürfen emanzipiert und in der Autonomie sprachlicher Kunstfertigkeit, bis an die Grenzen des Erzählbaren gehend und didaktische Ansprüche überwindend, die Möglichkeiten literarischer Darstellung ausreizt. Von den Zeitgenossen wurde dieses Experiment zwar wahrgenommen, in seinen Dimensionen aber nur ansatzweise erkannt. Symptomatisch für diese Form der Rezeption ist Petrarcas lateinische Übersetzung der ›Griselda‹-Novelle (›Seniles‹, XVII,3), wobei der Verfasser – seinerseits die Kleidermetaphorik bemühend – das Übersetzen als ein stilo alio retexere auffasst und seine Version den (wohl vorwiegend männlich intendierten Lesern) als auf Gott hin orientierte Lehre anempfiehlt: ut legentes ad imitandam saltem femine constantiam excitarem, ut [...] hoc prestare Deo nostro audeant. Diese Rückführung von Boccaccios erzählerischem Wagnis ins Didaktische zeigt sich auch in der Rezeption von Petrarcas Übersetzung, durch welche die Novelle im Europa des 14. und 15. Jahrhunderts weite Verbreitung fand: In einer der Haupthandschriften von Chaucers ›Canterbury Tales‹, dem Hengwrt Manuscript (Aberystwyth, National Library of Wales), wird die auf der ›Griselda‹-Novelle aufbauende Erzählung des Scholaren (›The Clerk’s Tale‹) mit Bestandteilen aus Petrarcas Übersetzung glossiert; in einer Handschrift aus dem Besitz des Nürnberger Humanisten Hartmann Schedel (München, Bayerische Staatsbibliothek, Clm 504) wird Petrarcas Konzept des stilo alio retexere erläutert als: claram facere, nudare [...], aperire, wobei hier die in Boccaccios Novelle intradiegetisch enthaltene Spannung von ‚Einkleidung’ und ‚Nacktheit’ auf einer lehrhaften Ebene fortwirkt.

“Crye Fredome”? Medievalism and Twenty-First-Century Scottish National Identity

It is a well-documented fact that the Middle Ages have had a long history of instrumentalisation by nationalisms. 19th-century Eu¬rope in particular witnessed an origins craze during the process of nation-building. In the post-Shoah, post-modern West, on the other hand, we might expect this kind of medievalist master nar¬rative to have been consigned to the dustbin of history. And yet, as nationalism surges again in Europe, negotiations of national identi¬ties in medieval dress seem to have become fashionable once more. In order to come to terms with the fragmented and often contradictory presence of the Middle Ages in these discourses of national identity, I propose we consider medievalism a utilitarian product of the cultural memory. Rather than representing any ‘real’ Middle Ages, then, medievalism tailors available knowledge of the medieval past to the diverse social needs and ideologies of the present. This paper looks at a selection of Scottish examples of present-day medievalism in an attempt to investigate, in particular, the place of the medieval Wars of Scottish Independence in contemporary negotiations of ‘Scottishness’. Both the relationships envisioned between self and other and the role played by ‘the land’ in these cultural, social and political instances of national introspection offer starting points for critical inquiry. Moreover, the analysis of a scholarly intervention in the run-up to the 2014 Scottish independence referendum indicates an intriguing dialogue of academic and non-academic voices in the context of Scottish medievalist cultural memory. We thus find a wide array of uses of the Scottish Middle Ages, some of which feed into the burgeoning nationalism of recent years, while others offer more pensive and ambivalent answers to the question of what it means to be Scottish in the 21st century.

Salinity of the Eocene Arctic Ocean from oxygen isotope analysis of fish bone carbonate

Stable isotope analysis was performed on the structural carbonate of fish bone apatite from early and early middle Eocene samples (~55 to ~45 Ma) recently recovered from the Lomonosov Ridge by Integrated Ocean Drilling Program Expedition 302 (the Arctic Coring Expedition). The d18O values of the Eocene samples ranged from -6.84 per mil to -2.96 per mil Vienna Peedee belemnite, with a mean value of -4.89 per mil, compared to 2.77 per mil for a Miocene sample in the overlying section. An average salinity of 21 to 25 per mil was calculated for the Eocene Arctic, compared to 35 per mil for the Miocene, with lower salinities during the Paleocene Eocene thermal maximum, the Azolla event at ~48.7 Ma, and a third previously unidentified event at ~47.6 Ma. At the Azolla event, where the organic carbon content of the sediment reaches a maximum, a positive d13C excursion was observed, indicating unusually high productivity in the surface waters.

Reconstructed glaciation limits in Eurasia (digitized from map Fig.1)

Based on field investigations in northern Russia and interpretation of offshore seismic data, we have made a preliminary reconstruction of the maximum ice-sheet extent in the Barents and Kara Sea region during the Early/Middle Weichselian and the Late Weichselian. Our investigations indicate that the Barents and Kara ice sheets attained their maximum Weichselian positions in northern Russia prior to 50 000 yr BP, whereas the northeastern flank of the Scandinavian Ice Sheet advanced to a maximum position shortly after 17000 calendar years ago. During the Late Weichselian (25 000-10000 yr BP), much of the Russian Arctic remained ice-free. According to our reconstruction, the extent of the ice sheets in the Barents and Kara Sea region during the Late Weichselian glacial maximum was less than half that of the maximum model which, up to now, has been widely used as a boundary condition for testing and refining General Circulation Models (GCMs). Preliminary numerical-modelling experiments predict Late Weichselian ice sheets which are larger than the ice extent implied for the Kara Sea region from dated geological evidence, suggesting very low precipitation.

Varved sediments of the Arabian Sea

The upper Holocene marine section from a kasten core taken from the oxygen minimum zone off Karachi (Pakistan) at water depth 700 m contains continuously laminated sediments with a sedimentation rate of 1.2 mm/yr and a unique record of monsoonal climatic variability covering the past 5000 years. Our chronostratigraphy is based on varve counts verified by conventional and AMS14C dating. Individual hemipelagic varve couplets are about 0.8-1.5 mm thick, with light-colored terrigenous laminae (A) deposited mainly during the winter monsoon alternating with dark-colored laminae (B) rich in marine organic matter, coccoliths, and fish debris that reflect deposition during the high-productivity season of the late summer monsoon (August-October). Precipitation and river runoff appear to control varve thickness and turbidite frequency. We infer that precipitation decreased in the river watershed (indicated by thinning varves) after 3500-4000 yr B.P. This is about the time of increasing aridification in the Near East and Middle East, as documented by decreasing Nile River runoff data and lake-level lowstands between Turkey and northwestern India. This precipitation pattern continued until today with precipitation minima about 2200-1900 yr B.P., 1000 yr B.P., and in the late Middle Ages (700-400 yr B.P.), and precipitation maxima in the intervening periods. As documented by spectral analysis, the thickness of varve couplets responds to the average length of a 250-yr cycle, a 125-yr cycle, the Gleissberg cycle of solar activity (95 yr), and a 56-yr cycle of unknown origin. Higher frequency cycles are also present at 45, 39, 29-31, and 14 yr. The sedimentary gray-value also shows strong variability in the 55-yr band plus a 31-yr cycle. Because high-frequency cyclicity in the ENSO band (ca. 3.5 and 5 yr) is only weakly expressed, our data do not support a straightforward interaction of the Pacific ENSO with the monsoon-driven climate system of the Arabian Sea.

Analyses of lake La Thuile sediment core

Lake La Thuile, in the Northern French Prealps (874 m a.s.l.), provides an 18 m long sedimentary sequence spanning the entire Lateglacial/Holocene period. The high resolution multi-proxy (sedimentological, palynological, geochemical) analysis of the uppermost 6.2 meters reveals the Holocene dynamics of erosion in the catchment in response to landscape modifications. The mountain belt is at relevant altitude to study past human activities and the watershed is sufficiently disconnected from large valleys to capture a local sedimentary signal. From 12,000 to 10,000 cal. BP (10 to 8 ka cal. BC), the onset of hardwood species triggered a drop in erosion following the Lateglacial/Holocene transition. From 10,000 to 4500 cal. BP (8 to 2.5 ka cal. BC), the forest became denser and favored slope stabilization while erosion processes were very weak. A first erosive phase was initiated at ca . 4500 cal. BP without evidence of human presence in the catchment. Then, the forest declined at approximately 3000 cal. BP, suggesting the first human influence on the landscape. Two other erosive phases are related to anthropic activities: approximately 2500 cal. BP (550 cal. BC) during the Roman period and after 1600 cal. BP (350 cal. AD) with a substantial accentuation in the Middle Ages. In contrast, the lower erosion produced during the Little Ice Age, when climate deteriorations are generally considered to result in an increased erosion signal in this region, suggests that anthropic activities dominated the erosive processes and completely masked the natural effects of climate on erosion in the late Holocene.

Persona y naturaleza : de Pedro Lombardo a Martin Heidegger

Pese a los indicios que podrían encontrarse en la filosofía griega, la noción de persona es de origen netamente cristiano y no pudo haber sido formulada sino dentro de ese horizonte de pensamiento. El hombre ha sido creado a imagen de Dios y es persona porque, en primer término, Dios lo es. Aquí se enlazan, durante el medioevo, las cuestiones antropológicas y teológicas (trinitarias y cristológicas). Un ejemplo paradigmático se encuentra en las Sentencias de Pedro Lombardo y sus comentadores, entre los que hemos reparado especialmente en Tomás de Aquino. En este contexto, “naturaleza" (divina o humana) y “persona" son nociones íntimamente vinculadas, pues es propio de tales naturalezas el existir y manifestarse como seres personales. Esa relación, sin embargo, se pierde durante la modernidad, época en que persona y naturaleza se vuelven términos antagónicos. Martin Heidegger, agudo crítico de esa transformación en la historia del pensar, propone una concepción de lo humano que, no obstante su “ateísmo metodológico", finalmente parece aproximarse a la noción cristiana de persona.

Sentidos y belleza en Tomás de Aquino

La percepción de lo bello, algo que alcanza al hombre como totalidad, se inicia en los sentidos, entre los cuales Tomás de Aquino ha privilegiado a la vista y al oído. Este hecho pone a la luz dos aspectos que el presente trabajo quiere destacar: por una parte, el respeto que el Aquinate ha mostrado a una tradición que, originada en Platón y comunicada por Agustín al medioevo, hace de la vista y el oído los únicos sentido capaces de percibir la belleza. Por otra parte, destaca que los análisis elaborados por Tomás sobre el tema constituyen un aporte a la especulación tradicional. Así, esta ponencia se ocupará de la vinculación entre lo bello, la vista y el oído, tanto en sus fuentes cuanto en las contribuciones efectuadas por el Aquinate.

Variantes en el uso del concepto de natura en la teoría política medieval a partir de la segunda mitad del siglo XIII : natura multipliciter dicitur

La circulación hacia mediados del siglo XIII de los libri morales de Aristóteles transformó ampliamente la ética y el pensamiento político de la edad media. El conocimiento medieval de la filosofía moral aristotélica produjo un cambio cualitativo en diferentes temas de la filosofía práctica; como consecuencia de ello, a partir del siglo XIII, una parte importante de la teoría política tomó de Aristóteles el concepto de natura y muchos tratados se apoyaron en él y lo utilizaron para fundamentar el nacimiento del orden político que Aristóteles llamó polis, Tomás de Aquino civitas vel provincia y Juan de París communitas civitatis vel regni. Con todo, aunque el concepto aristotélico de natura fue relevante y aunque el modelo aristotélico logró inspirar a los autores de textos políticos medievales, la natura aristotélica no fue la única natura a la que recurrieron los textos políticos al momento de fundamentar teóricamente el surgimiento del orden político. El artículo analiza los diferentes conceptos de natura y reconstruye su lugar dentro de las explicaciones del nacimiento y constitución de las distintas variantes del orden político en la filosofía política medieval.

La noción medieval de cogitativa y sus posibles proyecciones en psicología y psicoterapia

La doctrina de los sentidos internos -y, en particular, la de la cogitativa-, esbozada en la antigüedad, desarrollada en el Medioevo, y redescubierta parcialmente por la psicología contemporánea, constituye una elaboración conceptual originalísima con importantes consecuencias prácticas para la psicología. El presente estudio procura una primera aproximación en este sentido a la noción de cogitativa, examinando sus posibles proyecciones en los campos de la psicoterapia y de la comprensión etiológica de las enfermedades psíquicas, e indagando en las semejanzas que dicho concepto podría guardar con desarrollos psicológicos contemporáneos.

(Table 2) Similarity Indexes (Pearson's correlation coefficient) of the silicoflagellate assemblages of IODP Exp302

The silicoflagellate and ebridian assemblages in early middle Eocene Arctic cores obtained by IODP Expedition 302 (ACEX) were studied in order to decipher the paleoceanography of the upper water column. The assemblages in Lithologic Unit 2 (49.7-45.1 Ma), one of the biosiliceous intervals, were usually endemic as compared to the assemblages that occurred outside of the Arctic Ocean. The presence of these endemic assemblages is probably due to a unique environmental setting, controlled by the degree of mixing between the low-salinity Arctic waters and relatively high salinity waters supplied from outside the Arctic Ocean, such as the Atlantic and possibly the Western Siberian Sea. Using the basin-to-basin fractionation model, the early middle Eocene Arctic Ocean corresponds to an estuarine circulation type, which includes the modern-day Black Sea. The abundant down-core occurrence of ebridians strongly suggests the past presence of low-salinity waters, and may indicate that low oxygen concentrations prevailed in the euphotic layer, on the basis of the ecology of the modern ebridian Hermesinum adriaticum.

Pollen records of the Bykovsky Peninsula

New pollen and radiocarbon data from the Bykovsky Peninsula document the Late Pleistocene and Holocene environmental history of the Laptev Sea coast. More than 60 AMS-14C and conventional 14C dates indicate that the deposits accumulated during the last 60,000 radiocarbon yr BP. High concentration of green alga colonies (Pediustrum and Botryococcus) in the investigated sediment show that sedimentation was mostly in shallow water environments. Scarce grass and sedge communities dominated the vegetation 53-60 kyr BP. Climate was cold and dry. Open Poaceae and Cypcraccae associations with Asteraceae, Ranunculaceae, and Cichoriaceac, dominated in the area about 48-42.5 kyr BP. Steppic communities with Artemisia and shrubby tundra communities with Salix and Betula sect. Nanae were also present. Climate was dry, but relatively warm. Vegetation cover became denser about 42.5-33.5 kyr BP, reflecting more favorable climate conditions. Scarce Poaceae communities with some Caryophyllaceae, Asteraceae, Cichoriaceae, and Selaginella rupestris covered the Bykovsky Peninsula area during the Sartan (Late Weichselian) stage about 26-16 kyr BP. Disturbed, uncovered soils were very common in the area. Climate was extremely cold and dry. Poaceae and Cyperaceae associations with Caryophyllaceae, Asteraceae, Cichoriaceae dominated the vegetation in the late Sartan, ca 16-12.2 kyr BP. Climate was significantly warmer than in the early Sartan time. The lee Complex sedimentation was interrupted about 12 kyr BP; most likely it was connected with the beginning of the Allerod warnring. Shrubby (Betula sect. Nanae, Alnusfnuicosa, Salix, Ericales) tundra was widely distributed on the Bykovsky Peninsula during the early-middle Holacene. Climate was most favorable between 8200 and 4500 yr BP. Vegetation became similar to modern after 4500 yr BP, suggesting a deterioration of climate.