65 resultados para hyrax middens


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Ce mémoire porte sur la variabilité stylistique présente dans l’assemblage céramique du site McDonald, dans la région de Saint-Anicet, et a pour principal objectif de déterminer comment s’exprime cette variabilité à travers les différents niveaux identitaires auxquels appartiennent les Iroquoiens du Saint-Laurent, soit la famille linguistique iroquoienne, la sphère d’interaction des Iroquoiens du Saint-Laurent, les provinces culturelles, les villages, les clans et les maisonnées. Cette étude abordera également la distribution spatiale des vases retrouvés sur le site à l’aide d’un travail de remontage effectué à l’échelle du site. Cette méthode permettra également d’aborder le mode d’occupation du site McDonald, notamment par l’étude de la relation existant entre le contenu des habitations et celui présent dans chacun des dépotoirs. Une fois ce travail effectué, l’étude de la variabilité stylistique sera abordée par une étude comparative des unités décoratives observées sur les différents registres de décoration des vases à l’intérieur d’un site, c’est-à-dire entre les différentes maisons-longues qui le composent, mais également avec d’autres sites iroquoiens de la vallée du Saint-Laurent. Une étude simultanée des résultats de ces comparaisons intra et intersites aura pour objectif d’identifier la variabilité présente dans les différents niveaux identitaires auxquels appartiennent les habitants du site McDonald et plus précisément la maisonnée, le clan, le village et la province iroquoienne.

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This paper summarizes some of the geoarchaeological evidence for early arable agriculture in Britain and Europe, and introduces new evidence for small-scale but very intensive cultivation in the Neolithic, Bronze Age and Iron Age in Scotland. The Scottish examples demonstrate that, from the Neolithic to the Iron Age, midden heaps were sometimes ploughed in situ; this means that, rather than spreading midden material onto the fields, the early farmers simply ran an ard over their compost heaps and sowed the resulting plots. The practice appears to have been common in Scotland, and may also have occurred in England. Neolithic cultivation of a Mesolithic midden is suggested, based on thin-section analysis of the middens at Northton, Harris. The fertility of the Mesolithic middens may partly explain why Neolithic farmers re-settled Mesolithic sites in the Northern and Western Isles.

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Excavations on the multi-period settlement at Old Scatness, Shetland have uncovered a number of Iron Age structures with compacted, floor-like layers. Thin section analysis was undertaken in order to investigate and compare the characteristics of these layers. The investigation also draws on earlier analyses of the Iron Age agricultural soil around the settlement and the midden deposits that accumulated within the settlement, to create a 'joined-up' analysis which considers the way material from the settlement was used and then recycled as fertiliser for the fields. Peat was collected from the nearby uplands and was used for fuel and possibly also for flooring. It is suggested that organic-rich floors from the structures were periodically removed and the material was spread onto the fields as fertilisers. More organic-rich material may have been used selectively for fertiliser, while the less organic peat ash was allowed to accumulate in middens. Several of the structures may have functioned as byres, which suggests a prehistoric plaggen system.

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Samples taken from middens at the Neolithic site of Catalhoyuk in Turkey have been analysed using IR spectroscopy backed up by powder XRD and SEM-EDX. Microcomponents studied include fossil hack-berries (providing evidence of ancient diet and seasonality), mineral nodules (providing evidence of post-depositional change) and phytoliths (mineralised plant cells, providing evidence of usage of plant species). Finely laminated ashy deposits have also been investigated allowing chemical and mineralogical variations to be explored. It is found that many layers which appear visually to be quite distinctive have, in fact, very similar mineralogy. (C) 2009 Elsevier B.V. All rights reserved.

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Samples taken from middens at the Neolithic site of Catalhoyuk in Turkey have been analysed using IR spectroscopy backed up by powder XRD and SEM-EDX. Microcomponents studied include fossil hack-berries (providing evidence of ancient diet and seasonality), mineral nodules (providing evidence of post-depositional change) and phytoliths (mineralised plant cells, providing evidence of usage of plant species). Finely laminated ashy deposits have also been investigated allowing chemical and mineralogical variations to be explored. It is found that many layers which appear visually to be quite distinctive have, in fact, very similar mineralogy. (C) 2009 Elsevier B.V. All rights reserved.

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Land snail middens occur widely throughout the circum-Mediterranean, particularly in the Maghreb and Libya, but are relatively understudied when compared with the better known coastal marine middens. The site of Taforalt (Grotte des Pigeons) in north east Morocco contains thick ashy deposits with considerable numbers of land snails, dating between 13,000 and 11,000 BP. The site has been excavated periodically since its discovery in 1908, but little attention has been paid to the land snail component. Recent excavations at the site as part of the Cemeteries and Sedentism Project has facilitated reinvestigation of the Iberomaurusian layers, including the upper ashy midden unit. This investigation addresses questions surrounding chronological variation in the lithic assemblage, subsistence strategies, population health and mortuary practices. Preliminary work on the land snails has identified a low species diversity in the grey series midden layers, characterised by the large edible species Alabastrina alabastrites, Helix cf aspersa, Dupotetia dupotetiana, Otala punctata and Cernuella sp, which appear to represent an abrupt intensification in the use of land snails as a food source. Significant quantities of associated plant material and animal bone suggest that land snails are part of a broader based diet which is adopted from around 13,000 BP.

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Melting of the Greenland Ice Sheet (GrIS) is accelerating and will contribute significantly to global sea level rise during the 21st century. Instrumental data on GrIS melting only cover the last few decades, and proxy data extending our knowledge into the past are vital for validating models predicting the influence of ongoing climate change. We investigated a potential meltwater proxy in Godthåbsfjord (West Greenland), where glacier meltwater causes seasonal excursions with lower oxygen isotope water (δ18Ow) values and salinity. The blue mussel (Mytilus edulis) potentially records these variations, because it precipitates its shell calcite in oxygen isotopic equilibrium with ambient seawater. As M. edulis shells are known to occur in raised shorelines and archaeological shell middens from previous Holocene warm periods, this species may be ideal in reconstructing past meltwater dynamics. We investigate its potential as a palaeo-meltwater proxy. First, we confirmed that M. edulis shell calcite oxygen isotope (δ18Oc) values are in equilibrium with ambient water and generally reflect meltwater conditions. Subsequently we investigated if this species recorded the full range of δ18Ow values occurring during the years 2007 to 2010. Results show that δ18Ow values were not recorded at very low salinities (< ~ 19), because the mussels appear to cease growing. This implies that Mytilus edulis δ18Oc values are suitable in reconstructing past meltwater amounts in most cases, but care has to be taken that shells are collected not too close to a glacier, but rather in the mid-region or mouth of the fjord. The focus of future research will expand on the geographical and temporal range of the shell measurements by sampling mussels in other fjords in Greenland along a south–north gradient, and by sampling shells from raised shorelines and archaeological shell middens from prehistoric settlements in Greenland.

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The character of settlement patterns within the late Mesolithic communities of north-west Europe is a topic of substantial debate. An important case study concerns the five shell middens on the island of Oronsay, Inner Hebrides, western Scotland. Two conflicting interpretations have been proposed: the evidence from seasonality indicators and stable isotope analysis of human bones has been used to support a model of year-round settlement on this small island; alternatively, the middens have been interpreted as resulting from short-term intermittent visits to Oronsay within a regionally mobile settlement pattern. We contribute to this debate by describing Storakaig, a newly discovered site on the nearby island of Islay, undertaking a Bayesian chronological analysis and providing evidence for technological continuity between Oronsay and sites elsewhere in the region. While this new evidence remains open to alternative interpretation, we suggest that it makes regional mobility rather than year-round settlement on Oronsay a more viable interpretation for the Oronsay middens. Our analysis also confirms the likely overlap of the late Mesolithic with the earliest Neolithic within western Scotland.

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This paper discusses the ongoing ethnoarchaeological research carried out in Yamana shell middens of Tierra del Fuego. Ethnoarchaeology is used in this research as a tool to improve the archaeological methodology by testing it against anthropological, ethnographical and ethnological sources for achieving more accurate reconstructions of past societies. The ethnographical/ethnological information also is coupled with an experimental approach devised to understand physical and social processes, such as site formation processes and resource use and management. Specifically, this experimental approach was applied to the archaeological sites Tunel VII and Lanashuaia I (Tierra del Fuego, Argentina). (C) 2011 Elsevier Ltd and INQUA. All rights reserved.

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OBJETIVO: avaliar as diferenças produzidas nas dimensões e forma de arco pelos tratamentos com aparelho expansor fixo tipo Hyrax e aparelho expansor removível tipo Placa de Hawley com parafuso expansor palatino centralizado. MATERIAL E MÉTODOS: foram selecionados modelos de estudo iniciais e finais de 31 crianças portadoras de mordida cruzada posterior, de ambos os gêneros, de origem étnica diversa e na fase da dentadura mista, tratadas nos cursos de Graduação e Pós-Graduação em Ortodontia do Departamento de Clínica Infantil da Faculdade de Odontologia de Araraquara - UNESP. Destas crianças, 15 foram tratadas com uso do aparelho expansor fixo tipo Hyrax e as demais 16 crianças foram tratados com expansão rápida da maxila efetuada com o aparelho expansor fixo. Foram realizadas medidas das distâncias intercaninos e intermolares, da inclinação do processo alveolar e inclinação dentária nas imagens escaneadas do arco superior e do contorno do palato, obtido com auxílio de um template ajustável e do programa de análises Radiocef Studio. RESULTADOS E CONCLUSÕES: os resultados indicam uma mudança significante nas distâncias intercaninos e intermolares em ambos os grupos e uma inclinação dentária e do processo alveolar para vestibular significante no grupo tratado com o aparelho expansor fixo. A expansão conseguida pelo aparelho expansor fixo foi aproximadamente o dobro da promovida pelo aparelho expansor removível.

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OBJETIVO: na presente pesquisa utilizou-se o aparelho Hyrax tendo como objetivo avaliar as alterações transversais e verticais da maxila. Foram selecionados 20 pacientes de ambos os gêneros, entre 7 e 11 anos de idade, que apresentavam mordida cruzada posterior uni ou bilateral. METODOLOGIA: foram realizadas telerradiografias em norma frontal (PA) antes e após a expansão. A fim de evitar que a falta de padronização dessas radiografias pudesse influenciar nos resultados, idealizou-se um método de padronização para tais radiografias. RESULTADOS E CONCLUSÕES: os resultados mostraram que a correção da mordida cruzada posterior com o aparelho Hyrax, que ocorreu em todos os casos, foi em função tanto da abertura da sutura palatina mediana como também da inclinação dos molares. A medida JgE-JgD relacionada com a expansão maxilar aumentou significantemente em todos os casos tratados. Nas avaliações dentárias, as medidas verticais não apresentaram diferenças significantes, ao contrário das medidas transversais (FTE-FTD; FBE-FBD; LO.BTE; LO.BTD; BTE.BTD). A largura da cavidade nasal também aumentou significantemente (CNE-CND). O método de padronização proposto permite, portanto, utilizar as medidas que avaliam a expansão rápida da maxila, através das radiografias póstero-anteriores, com segurança, também no sentido vertical.

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INTRODUÇÃO: o problema transversal em Ortodontia pode ser de origem dentária, esquelética ou uma combinação de ambas e pode ser tratado de várias maneiras de acordo com o tipo de tecido envolvido e o arco dentário acometido. em se tratando de um problema esquelético e maxilar, o ortodontista poderá lançar mão da disjunção ortopédica, dependendo da idade óssea, obtendo uma correção da atresia, um alinhamento dentário espontâneo resultante do aumento no perímetro do arco e um sorriso mais amplo, beneficiando esteticamente o paciente. Porém, este tratamento de disjunção mandibular se torna inviável, já que este osso tem sua sutura fusionada precocemente. A expansão neste caso é alveolar e sua estabilidade é questionada. OBJETIVO: relatar um caso clínico, apresentando uma nova alternativa de tratamento para o apinhamento inferior: a Distração Osteogênica da Sínfise Mandibular (DOSM). Neste procedimento, é feita uma osteotomia sagital na sínfise, criando-se uma sutura artificial para que uma separação óssea seja conseguida, utilizando uma mecânica com aparelho disjuntor de Hyrax modificado. RESULTADOS: os resultados do tratamento apresentado mostram uma melhora na forma do arco, diminuição do corredor bucal, correção do apinhamento dentário e também uma estabilidade do tratamento, sem dano aos tecidos adjacentes. Neste caso clínico, a DOSM se mostrou uma excelente opção de tratamento.

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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In many situations, it is difficult to evaluate the location of nests of ants, especially in tropical systems, or to determine which trail system corresponds with which nest, as in the case of high-density populations of leaf-cutting ants, Atta spp. Fragments of colored drinking straws coated with an attractant, generally vegetable oil and/or a starchy carbohydrate, are carried by ants and following removal of the attractant are deposited in middens, allowing determination of the origin of foraging workers.

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Introduction: The force delivered during rapid maxillary expansion (RME) produces areas of compression on the periodontal ligament of the supporting teeth. The resulting alveolar bone resorption can lead to unwanted tooth movement in the same direction. The purpose of this study was to evaluate periodontal changes by means of computed tomography after RME with tooth-tissue-borne and tooth-borne expanders. Methods: The sample comprised 8 girls, 11 to 14 years old, with Class I or II malocclusions with unilateral or bilateral posterior crossbites Four girls were treated with tooth-tissue-borne Haas-type expanders, and 4 were treated with tooth-borne Hyrax expanders. The appliances were activated up to the full 7-mm capacity of the expansion screw. Spiral CT scans were taken before expansion and after the 3-month retention period when the expander was removed. One-millimeter thick axial sections were exposed parallel to the palatal plane, comprising the dentoalveolar area and the base of the maxilla up to the inferior third of the nasal cavity. Multiplanar reconstruction was used to measure buccal and lingual bone plate thickness and buccal alveolar bone crest level by means of the computerized method. Results and Conclusions: RME reduced the buccal bone plate thickness of supporting teeth 0.6 to 0.9 mm and increased the lingual bone plate thickness 0.8 to 1.3 mm. The increase in lingual bone plate thickness of the maxillary posterior teeth was greater in the tooth-borne expansion group than in the tooth-tissue-borne group. RME induced bone dehiscences on the anchorage teeth's buccal aspect (7.1 ± 4.6 mm at the first premolars and 3.8 ± 4.4 mm at the mesiobuccal area of the first molars), especially in subjects with thinner buccal bone plates. The tooth-borne expander produced greater reduction of first premolar buccal alveolar bone crest level than did the tooth-tissue-borne expander. © 2006 American Association of Orthodontists.