Rozprawy doktorskie na temat „Norse in Greenland”

From approximately 985CE, two Norse settlements were founded on the South and South-Western coasts of Greenland. Roughly 500 years later, the final recorded Norse voyage to Greenland marked the end of their contact with the outside world and by around 1500CE, both settlements were devoid of any living Norsemen. Numerous theories regarding the ultimate fate of the settlers have been put forward, with most modern prevailing theories describing issues driven by worsening climate, failing economic and farming prospects and dwindling populations. While resource shortages resulting from diminishing trade with other Nordic areas have been identified as possible contributing factors, little research has been done specifically on their impact on the Norse Greenlanders. This thesis seeks to begin reframing the story of the Norse settlements in Greenland through the lens of iron resource shortages. This issue was investigated through comparative studies of Greenlandic, Norwegian and Icelandic Norse iron tools. The iron items were analysed using two forms of shape analysis (SHAPE v.1.3 and MorphoJ) and comparative dimension and weight analysis. In addition, information on other Norse uses of iron was gathered from archaeological and historical sources. The findings provided evidence for wide-ranging adaptive practices undertaken by the Norse Greenlanders. This implies that the Norse understood the severity of their worsening situation and implemented measures to mitigate the shortage of iron. Ultimately, the Norse appear to have realised that remaining in Greenland would eventually result in a shortage of iron severe enough to render their ways of life unviable and limit their ability to leave Greenland, leading to a decision to abandon their settlements and seek out more liveable locations to colonise.

This thesis tests and applies a new, physically based snow distribution and melt model at spatial scales of tens of metres and temporal scales of days across sub-arctic landscapes, in order to assess the significance of snow variability in sub-arctic human ecodynamics at resolutions relevant to human activities. A wider goal is to contribute to planning in the face of future climate change. Model tests are undertaken based on original field data collected in Sweden and Norway, and secondary data from Idaho, France and Greenland. Model applications focus on the ‘completed experiment’ of the medieval Norse in Greenland, a comparatively isolated population that relied on a combination of pastoralism and hunting for survival. A combination of local calibration based on contemporary meteorological data, customised climate reconstructions based on GCM data, new archaeological survey and new DEM are used in order to apply the model. This thesis shows, for the first time, the likely range of snow depth and duration experienced across the medieval Norse Greenland landscape as a result of climate and vegetation change. Results show that increases in snow cover could have been significant drivers of transformative change in Norse Greenland, and are therefore likely to be key in understanding the potential impact of future climate changes on similar sub-arctic and relatively marginal communities. Selected model analyses simulate the total spring (April-June) snow cover at the homefields to range from 32% cover lasting 6 days in the most favourable climate to 100% cover lasting 45 days in the most unfavourable climate at key elite inner fjord farms. At the more isolated outer fjord farms, total spring snow cover ranges from 33% cover lasting 10 days in the most favourable climate to 100% cover lasting 60 days in the most unfavourable climate. Increased climate variance and recovery times, as experienced by the Norse, are potential early warning signals of threshold-crossing change. Model results show that these signals could have been masked for the Norse decision making elite because they were located in the most favourable and least snow covered locations. Masking could have been further increased through the intensified seal hunting implemented by the Norse as an adaption strategy, and these actions could have developed into a rigidity trap. When the conjunctures of the 15th century developed in terms of increased sea ice, snow cover, storminess, culture contact, changing trade and sea level rise, it was too late to develop different responses. Whilst current populations have improved technology and knowledge relative to the Norse Greenlanders, there is a risk that adaptations will lack long-term utility, spatially restricted indications of change may be ignored, and rigidity traps develop. This thesis provides an additional tool for understanding a key element of both the past and possible futures of subarctic human ecodynamics.

This thesis examines and analyzes the extant archaeological, historical, and literary evidence for the beliefs and practices of the Greenland Norse, their influences, and their evolution over time. By critically examining previously held assumptions about the cultural, climatic, and religious conditions of Greenland during this time the available data is placed in its proper context and reveals the geoconceptual world of the Greenlanders and their place in it. This interdisciplinary approach illustrates the extent to which the physical environment and location of Greenland played a role in the transition from a collective of enterprising colonists to an established Christian community over the course of almost 500 years. Specific questions addressed within include: 1 ­ How does archaeology challenge, support, or augment the historical and literary narrative of Greenland’s transition into a Christian place?; 2 – What are the physical correlates of the Greenlanders’ beliefs and practices, and how have they been interpreted? This thesis finds that the development of Christianity was driven by the Greenlanders’ increasing perception of their place in the world as one of marginality and spiritual danger.

The aim of this thesis is to understand the role of geomorphological change in the abandonment of Norse harbours in the North Atlantic. Nodes of maritime activities that were established by Norse settlers during the Scandinavian Viking Age often developed into important towns and cities. Some of these, however, disappeared for unknown reasons. Norse harbours in the North Atlantic varied in scale. They ranged from small landing beaches used by small boats for local use through to much larger anchorages handling considerable trade and being important nodes on the transatlantic trading network. Changes in coastal geomorphology necessitated a response from seafarers. In this thesis, a conceptual framework for the formation, recovery and stability of headland-dominated sandy beaches in high-energy environments is established, based on empirical observation and on the use of the MIKE21 numerical sediment transport model. Under persistent calm climatic conditions, nearshore seabed gradient is a weak control on beach formation and persistence in embayments. However, under persistent stormy conditions, nearshore sea bed gradient becomes the prominent control. Embayments with nearshore gradients of > 0.025 m/m inhibit beach recovery on a sub-annual timescale, while gradients < 0.025 m/m promote beach recovery. These ideas are assessed in the Shetland Islands, using numerical modelling, geomorphology and OSL dating on sand blow deposits. In the late Norse era beach landing sites in Unst became prone to depletion and destruction because of increased storminess. Numerical modelling (MIKE21) supports the idea that the recovery time of different sandy beaches on Unst is dependent on average nearshore slope. The beach at Sandwick has shallow nearshore gradients and recovers quickly in the face of storminess, but beach stability at Lunda Wick is more uncertain, and thus Lunda Wick represents a more problematic landing place. The Norse harbour of The Bishop's seat at Garðar in the Eastern Settlement of Greenland is assessed to evaluate the impacts of gradual long term geomorphological change on coastlines that lack soft-sediment. A high resolution, near shore bathymetric survey shows that, due to relative sea level rise of 1 m/500 years, the landing site became more difficult to access during the later period of Norse settlement and key onshore infrastructure was disrupted. The possible role of terrestrial supplies of sediment in changing the viability of landing places is assessed through an evaluation of the Norse trading centre of Gásir in northern Iceland. Geomorphological mapping and analysis of fluvial connectivity indicate that the delta on which Gásir is located is prone to aggradation from large, irregular pulses of sediment derived from landslides in the catchment. Written sources and geomorphological mapping indicate geomorphological changes around the same time that trade was shifting to the use of boats with a deeper draft. Cultural change and environmental changes would have reinforced each other in rendering the harbour site nonviable. Geomorphological forces acting on varying spatial and temporal scales have the potential to disrupt the use of landing sites. Whether environmental changes led to the abandonment of a landing site was strongly influenced by the seafarers' competence and available technology. Higher levels of competence would enable more problematic landing sites to be used, but there are limits to this adaptation. Technological changes, such as the use of larger and deeper draft boats, would have changed the geomorphic requirements for harbour sites, and thus may have led to a passive abandonment of the site over time rather than active abandonment such as that in the face of a catastrophic change of the shoreline. Coastal geomorphology was a critical factor affecting the use of Norse harbours, as it interacted with the wider cultural and economic developments in the North Atlantic realm. This thesis demonstrates that numerical sediment transport analysis is a powerful tool in coastal archaeological research as it can illuminate processes driving observable changes in the empirical record.

By way of introduction the thesis considers Norse whaling history, in general, concepts like 'whaling tradition', 'whaling culture', and describes the approach to the divers studies of cetaceans in Norse peasant fisherman economy and culture and of Norse whaling techniques, ca 900-1900 AD. It is argued that the Icelandic littoral and inshore regime reflects the primordial Norse regime in which property zones on land are 'mirrored' in the littoral and the sea; furthermore, that the Orcadian-Shetlandic Udal ebb limit is not Norse in origin. Norse mediaeval cetology and popular views about real and fictitious whales are studied. Many whales are identified, including the now extinct North Atlantic gray whale is positively identified as previously well-known to, and hunted by, the the Icelanders. It is argued that traditional Norse whale measures in 'ells' are not exaggerated extent measures but often exact appraisement sums, using a unit called *hvalsalin ('whale ell'). Few ritual aspects are found but in West Norway peasant fisherman apparently sustained, into the 19th century, -a tradition of sacrificing whale tails to the old Norse god Njörör. Mediaeval and early modern Norwegian whale traps are discussed and land rise suggested as one reason for their disappearance. A technical and linguistic analysis demonstrates that mediaeval Norse whaling with piercing weapons, rather than being hand harpoon tow whaling, was spear whaling which continued in Norway until 1870 and in Iceland to the mid 1890s. Spear whaling explains the elaborate Icelandic system of registrating whaling shot marks and partly the wide 'driftage zone' of coastal estates there. Spearing and arrowing caused clostridium infection in the whales which usually died in a matter of days after which some were recovered. It is also argued that gaffing of larger cetaceans constitutes a separate whaling method. The Appendix contains numerous calendars and sources in the original, including transcriptions of parts of the 'Icelandic fishlore' by Jon Ölafsson frä Grunnavik, 1737, and the whole treatise by Andreas Christie, 'Account of the whaling in Sotra district', West Norway, from 1785/86, all with tentative English translations and summaries.

La colonisation médiévale scandinave au Groenland (986 – 1450 AD) et la reconquête agricole récente de la région sud-groenlandaise, favorisée par le réchauffement climatique en cours, constituent un modèle de référence particulièrement adapté à l’étude des relations entre une communauté humaine et son environnement. Dans cette perspective, une étude sédimentologique multiparamètre a été réalisée sur la séquence sédimentaire du lac d’Igaliku (N61°00’22”, W45°26’28”), situé au cœur de la principale implantation médiévale et du secteur agro-pastoral contemporain. Quatre mètres de sédiments, couvrant la totalité de l’évolution holocène du lac (~10000 ans), ont été étudiés à haute résolution temporelle. L’analyse comprend une caractérisation physico-chimique (densité, susceptibilité magnétique, diagraphie XRF, imagerie rayon-X, granulométrie laser, dosages carbone, azote et souffre, ICP-AES, isotopie δ13C et δ15N de la matière organique) et biologique (pollen, microfossiles non polliniques, diatomées) du sédiment. Vingt-huit datations radiocarbones, ainsi que la mesure l’activité du 210Pb et du 137Cs, permettent d’interpréter le signal sédimentaire dans un cadre chronologique très précis et de reconstruire l’évolution postglaciaire du lac et de son bassin versant, soumis aux contraintes glacio-isostatiques, aux forçages climatiques et aux impacts anthropiques. La première phase d’évolution du système lacustre est principalement sous contrôle isostatique avec une transition rapide d’un environnement marin pro-glaciaire vers un environnement lacustre après émersion du bassin, il y a 9500 ans. Par la suite, la séquence témoigne de l’évolution paléoclimatique de la région. Les paramètres limnologiques et terrestres suggèrent un réchauffement précoce, probablement interrompu par une période froide, sèche et venteuse entre 8600 et 8100 ans cal BP. Un second événement sec et venteux, de 5300 à 4800 ans cal BP, précède la transition néoglaciaire, qui se caractérise, à Igaliku, par une évolution vers un climat plus humide et peut-être plus froid à partir de 4800 cal BP, provoquant une mutation majeure des conditions écologiques terrestres et aquatiques. La diminution des flux de grains de pollen indique un refroidissement notable à partir de 3000 cal BP. Vers l’an 1000, suite à l’arrivée des colons scandinaves, le système lacustre passe sous un contrôle anthropique dominant. Le défrichement et l’introduction d’herbivores domestiques dans le bassin versant du lac produisent un doublement du taux d’érosion des sols (de 4 mm/siècle à 8 mm/siècle vers 1200 AD) et une modification de la qualité des influx organiques. Pour autant, les assemblages de diatomées indiquent que l’écologie du lac n’a été que faiblement affectée par l’agriculture médiévale. A partir de 1325 AD et jusqu’à la fin de la colonie scandinave, vers la moitié du XVe siècle, la végétation présente des signes de résilience et l’érosion des sols régresse. Cette déprise agro-pastorale, probablement en relation avec les prémices du Petit Âge Glaciaire, est en phase avec une importante mutation des pratiques de subsistance attestée par l’archéologie. Le retour du pastoralisme au début du XXe siècle marque une reprise des processus d’érosion, similaires, en intensité, à ceux engendrés par les colons scandinaves. En revanche, l’intensification et la modernisation des pratiques agricoles dans les années 1980 est responsable d’une érosion des sols spectaculaire (~21 mm/siècle) et d’une mutation de l’écosystème lacustre (eutrophisation) sans précédent depuis la formation du lac, il y a 9500 ans. Les effets combinés de l’agriculture et du réchauffement climatique en cours (amorcé dans les années 1920 à Igaliku) aura des conséquences environnementales difficiles à prévoir pour l’avenir de la région
The medieval Norse colonization of Greenland (986-1450 AD) and the subsequent reestablishment of agriculture in south Greenland, aided by recent climate warming, constitute a conceptual model that is particularly well adapted to understanding the relations between a community and its environment. In this perspective, a multi-parameter sedimentological study was undertaken on the sedimentary sequence of Lake Igaliku (N61°00’22”, W45°26’28”), situated in the heart of the medieval and current agricultural sector. The 4 m long sequence, covering the entire Holocene evolution of the lake (~10 000 years), was studied at high temporal resolution. The analyses included the physico-chemical characterization of the sediments (density, magnetic susceptibility, XRF, X-ray imaging, grain size, carbon, nitrogen, and sulphur content, ICP-AES, δ13C and δ15N isotopic ratios) as well as the biological components of the sediment (pollen, non-pollen palynomorphs, diatoms). 28 radiocarbon dates as well as 210Pb and 137Cs measurements created a precise temporal framework with which to reconstruct the postglacial evolution of the lake and its catchment in terms of isostatic constraints, climatic forcing and anthropogenic impacts. The first phase of basin evolution is primarily controlled by isostasy, with the rapid transition from glaciomarine conditions to a freshwater lake as the basin emerged from the fjord 9500 yr BP. Afterwards, the sedimentary sequence records the paleoclimatic evolution of the region. Paleolimnological and terrestrial proxies suggest an early warm phase likely interrupted by a cold, windy, dry period between 8600 yr BP and 8100 yr BP. A second dry, windy period between 5300 yr BP and 4800 yr BP predated the transition to neoglacial cooling, which is characterised at Igaliku by a switch to humid and perhaps cooler conditions after 4800 BP, and which caused a major shift in both aquatic and terrestrial ecology. Approximately 1000 AD, after the arrival of Norse settlers, the lacustrine system became anthropogenically dominated. Land clearing and domestic herbivores introduction in the lake catchment doubled the rate of soil erosion (from 4 mm century-1 to 8 mm century-1 by 1200 AD) and caused a major modification of the organic carbon influx. On the other hand, diatom assemblages demonstrate that the lake ecology was not strongly impacted by medieval agriculture at this site. After 1325 AD, until the end of the Norse tenure in the mid-15th century, terrestrial vegetation showed signs of rebound and soil erosion decreased. This agricultural diminishment, probably in relation to the beginning of the Little Ice Age, is consistent with an important change in subsistence patterns evidenced by archaeology in this region. The reestablishment of agriculture at the beginning of the 20th century marks the reinvigoration of erosional processes that are similar in intensity to that of the Norse settlement. On the other hand, the intensification and modernization of farming practices during the 1980s is responsible for marked soil erosion (21 mm century-1) and a shift in lake ecology (eutrophication) that is unprecedented in the 9500 yr history of the lake. The combined effects of agriculture and climate warming already underway (initiated in the 1920s at Igaliku) will have large environmental consequences for the future of this region

A large database of domestic mammal bone measurements from sites across Greenland, Iceland, the Faroe Islands, and the Northern and Western Isles of Scotland is presented. The reasons for variations in bone growth of domestic ungulates are examined in detail; nutrition is identified as a key factor in the determination of adult bone size and shape. Possible sources of variation in bone size in both time and space in the North Atlantic region are identified. Four hypotheses are proposed; firstly that bone dimensions, particularly breadth, will decrease with increasing latitude in the study region; secondly that higher status sites will raise larger livestock than lower status sites within the same time period and region; thirdly the size of domestic mammals in the Northern and Western Isles of Scotland will increase in the Later Iron Age, possibly in relation to increased fodder supply; finally at times of environmental degradation (climatic and/or landscape) domestic mammal size will decrease. The latitude hypothesis could only be partly upheld; there is no evidence for increased size with site status; a small increase in size is noted at some Scottish Iron Age sites and varying results are found for the environmental degradation hypothesis. The results are discussed with particular reference to how changes in the skeletal proportions of domestic mammals affect their human carers and beneficiaries. The potential of further expanding the dataset and integrating biometrical data with other forms of evidence to create a powerful tool for the examination of economic and environmental changes at archaeological sites is discussed.
The Division of AGES (University of Bradford), the Andy Jagger Fund (University of Bradford), the Francis Raymond Hudson Fund (University of Bradford), the Viking Society, the Prehistoric Society, SYNTHESIS and the Paddy Coker Research Fund (Biogeographical Society)

A large database of domestic mammal bone measurements from sites across Greenland, Iceland, the Faroe Islands, and the Northern and Western Isles of Scotland is presented. The reasons for variations in bone growth of domestic ungulates are examined in detail; nutrition is identified as a key factor in the determination of adult bone size and shape. Possible sources of variation in bone size in both time and space in the North Atlantic region are identified. Four hypotheses are proposed; firstly that bone dimensions, particularly breadth, will decrease with increasing latitude in the study region; secondly that higher status sites will raise larger livestock than lower status sites within the same time period and region; thirdly the size of domestic mammals in the Northern and Western Isles of Scotland will increase in the Later Iron Age, possibly in relation to increased fodder supply; finally at times of environmental degradation (climatic and/or landscape) domestic mammal size will decrease. The latitude hypothesis could only be partly upheld; there is no evidence for increased size with site status; a small increase in size is noted at some Scottish Iron Age sites and varying results are found for the environmental degradation hypothesis. The results are discussed with particular reference to how changes in the skeletal proportions of domestic mammals affect their human carers and beneficiaries. The potential of further expanding the dataset and integrating biometrical data with other forms of evidence to create a powerful tool for the examination of economic and environmental changes at archaeological sites is discussed.

No
Insight into the relative importance of sheep and goat herding and of the economic significance of each species (i.e., milk vs. meat vs. wool) in Medieval Greenland is obtained through the application of Halstead et al.¿s (2002) criteria for the identification of adult ovicaprine mandibles to faunal assemblages from three Norse farmsteads: Sandnes, V52a, and Ø71S. The economic strategies identified are broadly comparable between the two species and the Eastern and Western Settlement sites examined, and are suggestive of the subsistence production of meat and milk. Comparison with farmsteads elsewhere in Greenland indicates that socio-economic status and/or farmstead size interacted with geographical location in determining the economic strategies employed by the Norse farmers. A broader use of resources and a more varied diet are evident at larger farmsteads in Greenland and this paper suggests that such sites would have been better able than their smaller counterparts to withstand environmental deterioration during the early Middle Ages. These analyses have also confirmed that goats were relatively more common in Norse sites in Greenland than in Norse sites in Iceland, Orkney, or Shetland.

碩士
國立成功大學
地球科學系
106
Greenland as the biggest island in the world, has an essential role in the global warming research. The ice covers almost 80 % of Greenland’s surface, and it is the second biggest ice on earth after Antarctica. If all the ice on Greenland melted, it will cause the rising of sea level in the world by 7 meters. We study the ambient seismic noise in Greenland and the surrounding area by using the probability density function – power spectral density (PDF-PSD) method. We have processed 34 seismic recording data during 2016 to 2017 for the Z component into PSD and spectrogram. From this PSD and spectrogram, we can divide the result into the short period band (0.1 – 1 s), secondary microseism band (3 – 10 s) and primary microseism band (10 – 20 s). The secondary microseism band shows a seasonal variation for each station, with the highest power level we can find on the winter season with a peak in February, however the lowest power we could see on summer with a peak in July or August. We classify the PSD level for each station into four clusters, one cluster for the secondary microseism band has a peak at 5 second, and the other clusters have a maximum value of 4 -5 second. The primary microseism level for all the clusters have a similar pattern with the highest value at 15 seconds. The short period band for every cluster has a different level with the period at 0.3 – 0.4 second where cluster 1 has -152 dB, cluster 2 has – 138 dB, cluster 3 has -145 dB and cluster 4 has -123 dB, respectively. As we can see the period (3 – 10 s) band is related to the climate system in Greenland, almost all the stations at cluster 1 located in arctic climate zone and the other clusters located in sub-arctic climate zone. We found that all seismic stations which are located in the central part of Greenland, it showed two peaks of secondary microseism almost the whole year. On the other hand, most seismic stations located on the east and west part showed the two peaks of secondary microseism only for two until four months. This means the stations located in central part of Greenland has a different source of secondary microseism for a whole year. Due to this problem, the investigation was conducted to study the factors which work on secondary microseism in Greenland, including the location of the source of secondary microseism band. This study will also learn the connection between microseism band and climate systems in Greenland.

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During the month of July 1987 an acoustical experiment was conducted by the United States Naval Research Laboratory (NRL) in the East Greenland Sea Marginal Ice Zone (MIZ) . Ambient noise "hot spots" or concentrated areas of relatively high noise levels were found along the ice edge using a towed array. Ambient noise levels were obtained on 27 and 28 July using AN/SSQ-57A and AN/SSQ-57XN5 calibrated sonobuoys . The temperature structure of the area was determined using XBT (ship) and AXBT (P3C aircraft) buoys placed inside and outside the ice edge. The ice edge was determined from coincident satellite photos, 90 GHz microwave imagery and P3 radar ice edge maps. Weather data (sea state and wind speed and direction) were recorded on the ship. The data seem to indicate a correlation between the high ambient noise levels of the hot spots and the presence of a large topographically controlled mesoscale eddy located at the southeastern extent of the MIZ.
http://archive.org/details/spatialvariabili00bigg
Lieutenant, United States Navy