Multidisciplinary approaches to defining historic period coastal and fluvial changes at Dunglass Burn,South East Scotland

An exceptionally thick (>2.5 m) fluvial and colluvial valley fill is described from the coastal reach of the Dunglass Burn, draining the Lammermuir Hills in south east Scotland. Buried by the valley fill is a series of charcoal accumulations interpreted as beacons to guide fishing boats, and an assemblage of large mammal bones. Radiocarbon assays on charcoal associated with these elements show them to be of early Medieval age. The onset of this extraordinary fluvial and colluvial sediment aggradation is considered to have begun at c. 1100 AD, although causation cannot be closely defined. The relations between the valley fill and securely dated built structures (buildings, bridges), an approach very infrequently explored, allow the cessation of aggradation to be dated to before the mid‐16th century AD. After c. 1600 AD incision has occurred to the present. The development of this valley fill is likely to have extensively altered the configuration of the coastline in the Medieval and early modern periods. The analyses emphasise the large magnitude of very recent landscape changes.     

They did not Live by Grass Alone: the Politics and Palaeoecology of Animal Fodder in the North Atlantic Region

Abstract

A five year research project was set up to monitor soil moisture and groundwater levels of an extensive buried, mainly alluviated landscape located at the interface between the lower Great Ouse valley and the fen-edge in western Cambridgeshire. The intention was to monitor changes in hydrology, soil structure and geochemical status before, during and after large scale gravel extraction. The results presented here concern the pre-extraction monitoring period over three years. The project has identified three major landscape zones – shallowly buried former dryland, several sets of relict palaeochannel systems which still remain waterlogged, and a marginal zone between these where the monitored parameters fluctuate on a seasonal basis. The moisture levels of the alluvial overburden, buried soils and infills of the palaeochannel systems appear to act independently of each other, controlled by a combination of rainfall, agricultural land management, height above sea level and depth of burial. It is predicted that the removal of 1–3m of overburden accompanied by water abstraction when gravel extraction commences will lead to changes in the moisture regime of the immediate area and therefore of any contained archaeological contexts and the superficial sediments in this river valley/fen-edge landscape.     

Relation between radiocarbon,archaeological dating and sediment properties on the example of colluvial deposits (NE Poland)

This study focuses on the analysis of the structural and textural features of the colluvial (deluvial) deposits in the Suwałki Lake District (NE Poland) and their absolute age. The colluvium has a thickness of up to 150 cm. The dates of the peat under colluvium or lowermost fossil humus-rich horizons point to the ages from 5405±80 BP to 480 BP. Deposition of material at the footslope is a result of a denudation triggered by human action (surface water erosion and tillage erosion) and usually corresponds with the settlement stages. The ¹⁴C dating of deposited sediment sometimes indicated to older dates of colluvium then the archaeological evidence available for examined sites. Locally, the overlying fossil humic horizon was older then the lowermost one. The textural features of the colluvial deposits such as: the content of fine fraction, weak sorting and relationship between the mean grain-size (Mz) and the sorting index (σ₁) were used to recognize sediment redeposited from the upper part of the slope. Basing on the mineral composition and electrical conductivity of fossil humus horizon it is possible to say whether the soil was degraded or aggraded. These features of the humus-rich horizons occurring between colluvial sediments can be used to explain discrepancy between the radiocarbon dating and archaeological evidence.     

Canadian Landform Examples

The flat topography of the Red River Valley reflects the morphology of underlying bedrock covered with late Quaternary glacial and glaciolacustrine sediments. The meandering Red River occupies a shallow stream‐cut valley that became incised into the Red River Valley plain following the final recession of glacial Lake Agassiz. Extreme flows carried by the river overtop the sides of the stream‐cut valley and spread laterally up to several tens of kilometres across the plain. An array of flood protection infrastructure has been constructed in the landscape to mitigate the flood hazard.     

From Pre‐Roman Bailo To Roman Baelo: Long‐Term Landscape Dynamics In The Straits Of Gibraltar

The Straits of Gibraltar have been historically an important maritime axis of connection between the Mediterranean and Atlantic areas of the Iberian Peninsula. For this reason, most of the archaeological research has focused on the coastal settlements, but its broader archaeological landscape remains mostly unknown. In this paper, we present recent intensive surveys in which a wide range of sites was detected, dating from the eighth century BC to the fourteenth AD. The ancient landscape is thus reconstructed over a long‐term perspective. Prior to the Roman expansion, the earlier Bailo‐La Silla del Papa was an urban central place that supported a dense network of subordinate settlements. Later on, the central settlement was transported from inland to the coastal town of Baelo Claudia, but the territorial structure remained based on a similar pattern.     

ANTHROPOGENIC IMPACT ON THE LANDSCAPE OF SOUTHERN BADENIA (GERMANY) DURING THE HOLOCENE—DOCUMENTED BY COLLUVIAL AND ALLUVIAL SEDIMENTS*

In the study area (the Upper Rhine Lowlands and the southern Black Forest), colluvial and alluvial sediments could be dated with the aid of ¹⁴C analysis, archaeological finds, pollen analysis and stratigraphic assessments. On the basis of these dated deposits, six different maps have been produced showing the distribution of the colluvial and alluvial sediments for the corresponding archaeological cultural periods. For each of these periods, the intensity of human impact on the environment has been estimated in relation to climatic conditions and different economic activities; for example, woodland clearance and mining activities.     

THE AMINOCHRONOLOGY OF MAN‐INDUCED SHELL MIDDENS IN CAVES IN NORTHERN SPAIN*

Here, we provide the first report on the ages of 54 archaeological levels in 38 caves in northern Spain by means of the aspartic acid d /l ratio measurements in Patella shells, with good results. For this purpose, we developed an age calculation algorithm that allows the numerical dating of deposits from other archaeological localities in the area and nearby regions. We conclude that the sample size—that is, the number of shells analysed within a single level—reinforces the importance of analysing numerous specimens per horizon and the understanding of the time‐averaging concept. The ultrastructure of different species of Patella shells was also studied, showing calcite in their apexes and aragonite at their margins.     

Assessing the later prehistoric environmental archaeology and landscape development of the Cetina Valley,Croatia

Abstract

This paper describes preliminary work on the environmental and archaeological potential of the Cetina River Valley, Croatia. Two seasons of fieldwork and assessment have suggested that the valley contains a preserved landscape, much of which is waterlogged. It is clear that there is the potential to address many local and regional questions concerning land use, subsistence and environmental change in an area where previously only limited environmental archaeology has been undertaken. One pressing issue is how to prospect for both cultural and environmental archaeological deposits within this regional landscape. This is especially true in cases where little 'base-line data' exists. This paper outlines the current practice and suggests a number of new approaches to prospecting for environmental 'hotspots'.     

ARCHAEOLOGICAL,STYLISTIC AND SCIENTIFIC RESEARCH ON 11TH–13TH CENTURY AD PAINTED FRAGMENTS FROM THE SAN GIOVANNI BATTISTA CHURCH IN CEVIO (SWITZERLAND)

The painted fragments collected during the archaeological excavation campaign in the San Giovanni Battista church in Cevio represent a unique patrimony of Romanesque wall painting in Tessin, Switzerland, having a strong stylistic linkage with the Lombardic art of the same period. The archaeological and stylistic research allowed the fragments to be dated between the 11th and 13th centuries ad and to group them in three chronological phases. The scientific research (p‐XRF, OM, SEM–EDS, FTIR and XRD) was aimed at characterizing the pigments and the pictorial techniques used. Important changes occurred in terms of some pigments used during the 11th and 12th centuries: in particular, azurite was used to decorate the earlier wall paintings while lapis lazuli was used for the 12th‐century ones. During the second period, lead‐based pigments (lead white and minium) were introduced into the palette. The use of natural yellow and red ochres and green earth was common for the three periods. The fresco technique was generally used, except for the application of azurite and lead‐based pigments, where the a secco technique was adopted. The integrated research is a contribution to the knowledge of Romanesque art in the Insubric Region.     

Paleochannel Studies in Archaeology: The Case of The Vychegda River,Northeastern European Russia

Geological and geomorphological settings are often taken into account when choosing strategy in archaeological studies. In the Vychegda River valley (Archangelsk Province, Komi Republic), at the end of the Late Pleistocene and in the Holocene, lateral channel migrations were the dominant process of riverine landscape changes and hence directly influenced human occupation of the valley. Therefore, to assess the physical settings of archaeological sites we employed paleochannel analysis, a geomorphological technique aimed at reconstructing river channel transformations in the historical and geological past. The potential application of paleochannel analysis in archaeology includes designing archaeological surveys and predicting destructive river actions at archaeological sites located in river valleys.     

Palaeolithic engravings and sedimentary environments in the Côa River Valley (Portugal): implications for the detection,interpretation and dating of open-air rock art

The pre-Magdalenian phase of the Côa River Valley open-air rock art is mostly distributed at the boundary between the rocky valley slopes and the floodplain that correspond to the most favourable geomorphological setting for the preservation of pecked and deeply superposed engravings of the most famous artistic phase of the area. The natural vertical panels of the engraved art located at this geomorphological interface have suffered weathering during two cold events of the Lateglacial. They were buried by several colluvial and alluvial deposits. The reconstruction of the sedimentary and archaeological context of the CôaRiver Valley engraving permits a better assessment of the preservation processes and interpretation of Palaeolithic open-air rock art.     

BUILDING URBANITY: SPATIAL ORGANISATION AS SOCIAL PRACTICE IN MEDIEVAL ODENSE

The article investigates the social practices of the inhabitants of the medieval town as it is expressed in the materiality of the urban landscape. It is argued that a practice‐based approach allows an understanding of how urbanity, defined as a specific set of social practices motivated by the shared space, developed in the medieval period. The town is seen as something more than a physical entity. The argument is developed through a diachronic and contextual analysis of the spatial organisation and layout of the medieval town of Odense in Denmark, as it is seen in the archaeological record of I. Vilhelm Werners Plads, representing the 9^th‐16^th centuries. The analysis demonstrates that from the mid‐12^th century, the organisation of the settlement plot and the interaction between town dwellers and townscape change. This change of practices is seen as related to a different mind‐set and perception of what it means to live in a town, that progressively has provided a sense of urbanity.     

A CASE STUDY OF ARTHROPODS PRESERVED ON ARCHAEOLOGICAL BRONZES—MICRO‐ARCHAEOLOGICAL INVESTIGATION HELPS RECONSTRUCTING PAST ENVIRONMENTS

This paper offers new perspectives for improving our knowledge of arthropods in wet and aerobic archaeological contexts. The very‐near environment of uncleaned buried bronze artefacts, two ronde‐bosse ornaments of a Celtic grave from the Iron Age (275 to 250 bc , La Fosse‐Cotheret, Roissy‐en‐France), was studied by means of optical and scanning electron microscopies. Taking into account recent knowledge on bronze corrosion (decuprification), this micro‐investigation (micro‐archaeology) allowed identification of two fossilized arthropods—Cryptophagus sp. (Insecta, Coleoptera, Cryptophagidae) and Coccotydaeolus sp. (Acari, Tydaeoidea, Iolinidae)—which sheds some light upon the complex taphonomic process that occurred after the burial of a Celtic chariot. These first results support the idea that the local corroded metal/soil system has to be investigated for a better understanding of archaeological microenvironments. Efficient minute investigation of soiled bronzes could be performed prior to systematic cleaning of artefacts.     

THE ANCIENT MINE OF SERVETTE (SAINT‐MARCEL,VAL D’AOSTA,WESTERN ITALIAN ALPS): A MINERALOGICAL,METALLURGICAL AND CHARCOAL ANALYSIS OF FURNACE SLAGS*

The Cu–Fe mining district of Servette is located in the valley of Saint‐Marcel (Val d’Aosta) at about 1800 m a.s.l. in the western Italian Alps. A large furnace slag deposit occurs near the Servette mine. Slags are mainly constituted by silicate and oxide in a glassy matrix, with disseminated sulphides and iron–copper alloys, and they record temperatures of 1380–1100°C. Radiocarbon dating of slag charcoals has shown that metallurgy in this site took place around ad 890–980. The charcoal analysis has shown that coniferous wood was mainly utilized, and intensive exploitation over the centuries led to a change in the composition of the local woods.     

Early farming in hordaland,western Norway. Problems and approaches in archaeology and pollen analysis

This article discusses the evidence of farming settlements in Neolithic times in the county of Hordaland, in western Norway, and possible ways for future research to establish the introduction of a farming economy, with its cultural and ecological implications.

Using distribution maps, Bakka demonstrates how the people of the mainly hunting and fishing sub‐Neolithic dwelling‐place culture of the Middle Neolithic period preferred a coastal area of habitation, while the find groups of Neolithic artifacts are generally to be found in those areas more suitable for farming. This change of habitat is interpreted as evidence of a general change in economic structure, with a greatly increased emphasis on agriculture.

Kaland discusses the Sub‐Boreal history of vegetation in Hordaland as revealed by pollen analysis. The earliest phase of agriculture in the pollen diagrams is dated in relation to the pollenanalytical leading horizons, the shore‐line displacement, radiocarbon measurements and the archaeological chronology. He puts forward the working hypothesis that in the sub‐Neolithic culture of the Middle Neolithic period some animal husbandry may have been practised in zone VIII b as a supplementary means of livelihood, and that this was followed by a phase of cereal growing in zone VIII c. The Late Neolithic culture appears to be responsible for this more intensive mixed farming, and this corresponds to the archaeological evidence of the introduction of cereal cultivation, which demands the better‐soils of the later farming land.     

Bridging theoretical gaps in geoarchaeology: archaeology,geoarchaeology, and history in the Yellow River valley,China

While geoarchaeology as a practice within archaeology grew out of many historical roots, a major role has been the explication of site formation processes and site-level contextual analysis. In recent years, geoarchaeological research has branched out to encompass larger geographic scales, and to play a greater role in environmental archaeological investigations. This paper argues that geoarchaeology has a great deal to contribute to the understanding of human history and to archaeological theory through the application of multiscalar approaches that place human behavior in a physical, environmental and ecological context and by creating linkages between physical processes and human responses. We use geoarchaeological data from the Yellow River valley to show that drainage/irrigation canal and bank/levee building had commenced in the lower reaches by ca. 2900–2700 cal B.P. The emphasis on flood plain flood control infrastructure was a result of long-term increases in sedimentation caused by large populations farming with increasingly efficient technologies in the fragile environments of the Loess Plateau. Ever increasing sedimentation set in motion a cycle of further investment in flood control works eventually leading to a massive flood catastrophe in the first 20 years of the first millennium A.D. as the Yellow River exceeded natural and human geomorphic thresholds that constrained it in its previous course. These floods arguably triggered the social and political events that brought down the Western Han Dynasty but the root causes are clearly more complex. Geoarchaeology thus contributes to an understanding of the multiple causes and consequences of large-scale social and political collapse.     

The Historic Landscape of the Saga of the People of Vatnsdalur: Exploring the Saga Writer's Use of the Landscape and Archaeological Remains to Serve Political Interests

Abstract

The saga of the People of Vatnsdalur (Vatnsdaelasaga) provides a case study for a new approach to the Sagas of Icelanders (Íslendingasögur). This treats the saga as a cultural product of the 13th century that can give insights into its creator's ideas and worldviews. Fieldwork at five sites in the Vatnsdalur valley in NW Iceland seeks to establish what these places were like in the 13th century. This knowledge, alongside the saga and place-name evidence, illustrates how the saga writer, presumed to come from a powerful 13th-century family, systematically used the landscape and archaeological remains in the valley to serve his political interests when describing 10th-century events.     

Dating problems in Icelandic archaeology

For many decades tephrochronology has been used as a scientific method for dating archaeological as well as geological remains in Iceland. Recently, parts of the tephrochronology for the eruptions of the famous volcano Hekla have been questioned by the author. This is due to obvious differences in dating results of archaeological artefacts from the valley of Thjórsárdalur in southern Iceland and the current tephrochronological dating of its devastation. While the devastation of the valley has been dated to AD 1104 and is thought to have been caused by a huge eruption of mount Hekla in that year, the artefacts from excavations and stray finds, as well as new ¹⁴C results, show somewhat later 12th‐13th century dates. The paper deals with this obvious discrepancy, which has hitherto been ignored, together with the results of archaeological excavations in 1983–86 at Stóng in Thjórsárdalur; it also gives a critical analysis of the historical methodology of the tephrochronologists.     

NEOLITHIC SOILS, MIDDENS AND ALLUVIUM IN THE LOWER WELLAND VALLEY

Summary. The soil micromorphological analysis of buried soils and probable 'midden' deposits buried beneath alluvium from six sites in the lower Welland valley between Maxey and Etton (Cambridgeshire) has revealed a deforested early Neolithic landscape which quickly became subject to seasonal alluviation. This paper suggests that the Neolithic/Bronze Age use of this landscape is directly related to its interpretation as an alluviated floodplain rather than an alluviated, former dry-land landscape.