999 resultados para Early medieval kingdoms
Resumo:
The excavation site Reigoldswil is located at 550 m above sea level on the Jura chain hillside in north-western Switzerland. The mountains divide the Rhine valley from an agriculturally rich region. The origin of the village lies in the early medieval time. Until now the skeletons of one cemetery have been morphologically studied. Around 216 individuals were excavated from under the foundation walls of a church and in the open field. They date to the 7/8th up to the 10th century. The striking part is the high amount of subadult (0-18 years) individuals with 58% (n=126). One of these children, an approximately 1.5 year old toddler from the 7th century, was buried in a stone cist. Its bones show morphological traces like porotic lesions of the greater wings of the sphenoidale, the squama, the mandibule and the scapula as new bone formation on both femora and tibiae. These signs could be an indicator for Möller-Barlow disease (Ortner 2003, Brickley and Ives 2008, Stark in press). As scurvy is associated with an insufficient intake of vitamin C, malnutrition must be assumed. A reason might be the geographic location or/and a harsh climat with crop failure and famine the first settler had to face. Besides the morphological diagnose amino acids of the bone collagen have been analyzed (Kramis et. al.). Further examinations, such as radiocarbon dating and stable isotope ratios (C, N, O, S) to specify nutrition, are planned.
Resumo:
Human bone is the most direct source for reconstructing health and living conditions of ancient populations. However, many diseases remain undetected in palaeopathology. Möller-Barlow disease (scurvy) is a historically well-documented metabolic disease and must have been common in clinical and sub-clinical severity. Due to long incubation periods and the subtle nature of bone changes osteological evidence is relatively rare (Brickley & Ives 2008). Möller-Barlow disease is caused by deficiency of dietary vitamin C (ascorbic acid) and evokes symptoms like fatigue, haemorrhage, inflammations, delayed wound healing and pain. Vitamin C is a cofactor for the hydroxylation of the amino acids proline and lysine which are essential for the production of intact connective tissue by cross-linking the propeptides in collagen. In a preliminary study we tested the detectability of Möller-Barlow disease by analysis of relative quantitative variability of hydroxylated amino acids in collagen (Pendery & Koon 2013). Samples (N=9) were taken from children with (n=3, cranium, femur, tibia) and without (n=4, cranium, femur, tibia) apparent bone reactions indicative of Möller-Barlow disease, as well as from adults with lethal traumata (n=2; negative controls). The skeletal remains originated from two early medieval cemeteries from Switzerland. Gas chromatographic (GC) analysis revealed minor differences between the samples. So far children with no pathologic alterations had fairly same values as negative controls while children with bone reactions paradoxically exhibited even slightly higher values of hydroxyproline and hydroxylysine. Future research demands for larger sample size and has to discuss sampling strategies. Beside possible misdiagnosis of Möller-Barlow disease it is arguable if only the newly built bone should be analysed even though this could lead to problems related to small sample quantity. It also remains to be seen to which extent varying turnover rates of different skeletal elements, especially in children, must be taken into account.
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Lake Butrint (39°47 N, 20°1 E) is a ca. 21 m deep, coastal lagoon located in SW Albania where finely-laminated sediments have been continuously deposited during the last millennia. The multi-proxy analysis (sedimentology, high-resolution elemental geochemistry and pollen) of a 12 m long sediment core, supported by seven AMS radiocarbon dates and 137Cs dating, enable a precise reconstruction of the environmental change that occurred in the central Mediterranean region during the last ∼4.5 cal kyrs BP. Sediments consist of triplets of authigenic carbonates, organic matter and clayey laminae. Fluctuations in the thickness and/or presence of these different types of seasonal laminae indicate variations in water salinity, organic productivity and runoff in the lake's catchment, as a result of the complex interplay of tectonics, anthropogenic forcing and climate variability. The progradation of the Pavllo river delta, favoured by variable human activity from the nearby ancient city of Butrint, led to the progressive isolation of this hydrological system from the Ionian Sea. The system evolved from an open bay to a restricted lagoon, which is consistent with archaeological data. An abrupt increase in mass-wasting activity between 1515 and 1450 BC, likely caused by nearby seismic activity, led to the accumulation of 24 homogenites, up to 17 cm thick. They have been deposited during the onset of finely laminated sedimentation, which indicates restricted, anoxic bottom water conditions and higher salinity. Periods of maximum water salinity, biological productivity, and carbonate precipitation coincide with warmer intervals, such as the early Roman Warm Period (RWP) (500 BC–0 AD), the Medieval Climate Anomaly (MCA) (800–1400 AD) and recent times (after 1800 AD). Conversely, lower salinity and more oxic conditions, with higher clastic input were recorded during 1400–500 BC, the Late Roman and the Early Medieval periods (0–800 AD) and during the Little Ice Age (1400–1800 AD). Hydrological fluctuations recorded in Butrint are in phase with most central and western Mediterranean records and correlate with NAO variability. In contrast, opposite hydrological patterns have been recorded in the Eastern Balkans and the Levant during the last millennium, emphasizing a complex spatial variability in the region. Phases of maximum settlement intensity in Butrint (Roman-Late Antique) coincide with warmer and/or stable climate periods (0–800 AD and MCA, respectively), indicating a long-term influence of climatic conditions on human activities. The Late Holocene sedimentary record of Lake Butrint demonstrates the complex interplay of climate variability, tectonics and human impact in the recent evolution of coastal Mediterranean regions.
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A Holocene pollen diagram from Kleiner Mochowsee (northern Niederlausitz, East Germany) shows pine as an important constituent of the woodland south of the Schwielochsee. Oak woodland was widespread since the Atlantic. Betula lost its importance at the end of the Preboreal. Fagus is represented continuously in the pollen record since the Atlantic, Carpinus since the Subboreal. However, the two latter tree species remain without great importance throughout the whole pollen record. The poor sandy soils are furthermore reflected by the low values of Corylus during the Boreal, comparable to other records from Berlin and its surrounding area. The 'classical' elm decline could be shown for the Niederlausitz, radiocarbon dates assume a contemporaneous age for this event with other records from northern Germany. Only small-scaled human impact is indicated in prehistoric times, during the migration period it seems to have ceased completely. Later, in the Medieval, deforestation and tillage can be shown. Secale was cultivated since the early Medieval; an accompanying weed flora appeared at the same time. Cultivation of Fagopyrum and Linum usitatissimum could be shown for the late Medieval times.
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El presente artículo es un estudio sobre las actividades competitivas desarrolladas en el seno de las bandas armadas del norte de Europa en la Alta Edad Media: el juego, el reto y el combate, incluyendo los enfrentamientos violentos. Estas actividades no sólo eran una forma de pasatiempos, sino también aspectos muy importantes que revelan parte del funcionamiento de estas bandas. De hecho, podían representar desafíos para la cohesión de la comitiva, pero eran parte de su propia organización. Las comitivas eran dinámicas y sus estructuras siempre cambiaban, y las actividades competitivas, tanto las pacíficas y como las menos, definían y redefinían los rangos dentro del grupo
Resumo:
El presente artículo es un estudio sobre las actividades competitivas desarrolladas en el seno de las bandas armadas del norte de Europa en la Alta Edad Media: el juego, el reto y el combate, incluyendo los enfrentamientos violentos. Estas actividades no sólo eran una forma de pasatiempos, sino también aspectos muy importantes que revelan parte del funcionamiento de estas bandas. De hecho, podían representar desafíos para la cohesión de la comitiva, pero eran parte de su propia organización. Las comitivas eran dinámicas y sus estructuras siempre cambiaban, y las actividades competitivas, tanto las pacíficas y como las menos, definían y redefinían los rangos dentro del grupo
Resumo:
El presente artículo es un estudio sobre las actividades competitivas desarrolladas en el seno de las bandas armadas del norte de Europa en la Alta Edad Media: el juego, el reto y el combate, incluyendo los enfrentamientos violentos. Estas actividades no sólo eran una forma de pasatiempos, sino también aspectos muy importantes que revelan parte del funcionamiento de estas bandas. De hecho, podían representar desafíos para la cohesión de la comitiva, pero eran parte de su propia organización. Las comitivas eran dinámicas y sus estructuras siempre cambiaban, y las actividades competitivas, tanto las pacíficas y como las menos, definían y redefinían los rangos dentro del grupo
Resumo:
Acknowledgements We would like to thank Charles and Helen Gray for permitting access to the land and for support in the excavation of the hoard. Thanks also to Bruce Mann and the Aberdeenshire Council Archaeology Service for advice and supporting the radiocarbon dating. Fraser Hunter and Tanja Romankiewicz assisted during a very cold excavation. Fraser and Alice Blackwell kindly read and commented on drafts of this paper. The fieldwork was funded through a donation to the University of Aberdeen’s Development Trust and undertaken as part of the Northern Picts project, in association with the Tarbat Discovery Centre.
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El Tolmo de Minateda (Hellín, Albacete) ofrece una secuencia estratigráfica sin solución de continuidad entre los siglos VII y IX d. D. En este trabajo se discute la potencialidad explicativa de dicha secuencia aplicada a la cerámica y a la arquitectura altomedievales, como instrumentos de reconocimiento del cambio social y cultural. El análisis de ambos casos de estudio permite la caracterización material del siglo VIII y plantea interesantes cuestiones arqueológicas en torno al significado histórico del 711.
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Estudiamos las evidencias de la ocupación tardoantigua y altomedieval en el entorno de la ciudad de Eio-Iyyu (El Tolmo de Minateda, Hellín, Albacete). Mediante el reconocimiento superficial del terreno y la revisión de los materiales arqueológicos se propone la caracterización del poblamiento entre los ss. VII d.C. y IX d.C. El análisis ofrece una ocupación densa en la que empiezan a reconocerse espacios campesinos agregados que podría corresponder a aldeas campesinas.
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La Huerta de Alicante, prototipo de los denominados regadíos deficitarios o secanos mejorados, ofrece uno de los mejores ejemplos de cómo la escasez hídrica activó la búsqueda de soluciones técnicas, propició la inversión en infraestructuras hidráulicas y desarrolló unas peculiares relaciones entre los labradores regantes y los propietarios del agua. La gestión de los recursos hídricos y su distribución por estricto cómputo horario por parte del municipio alicantino hasta 1739 permitió, pese a los condicionantes físicos y climáticos, el desarrollo de una actividad agrícola significativa durante los siglos modernos. La temprana separación del agua de la tierra a la que estaba adscrita en los primeros repartos medievales provocó numerosos conflictos a lo largo de la historia e intentos de unificar ambas propiedades, algo que nunca se consiguió.
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The purpose of this study is to analyze the distribution, forms, and function(s) of iron amulets deposited in the late Iron Age gravefields of Lovö, with the goal of ascertaining how (and so far as possible why) these objects were utilized in rituals carried out during and after burials. Particular emphasis is given to re-interpreting the largest group of iron amulets, the iron amulet rings, in a more relational and practice-focused way than has heretofore been attempted. By framing burial analyses, questions of typology, and evidence of ritualized actions in comparison with what is known of other cult sites in Mälardalen specifically– and theorized about the cognitive landscape(s) of late Iron Age Scandinavia generally– a picture of iron amulets as inscribed objects made to act as catalytic, protective, and mediating agents is brought to light.