scholarly journals Bronze Age “pristinity”, Iron Age anthropization and Medieval intensification of human impact around Lake Montcortès (southern-central Pyrenees): a possible mid-elevation pattern and its significance for the definition of the Anthropocene

2021 ◽  
Author(s):  
Valentí Rull ◽  
Teresa Vegas-Vilarrúbia ◽  
Juan Pablo Corella ◽  
Blas Valero-Garcé
Keyword(s):  
Bronze Age ◽  
Human Impact ◽  
Iron Age ◽  
Late Bronze Age ◽  
Medieval Period ◽  
Human Pressure ◽  
Early Medieval ◽  
Early Medieval Period ◽  
Definition Of ◽  
Central Pyrenees

Abstract The varved sediments of Lake Montcortès (central Pyrenees) have provided a continuous and well-dated high-resolution record of the last ca. 3000 years. Previous chronological and sedimentological studies of this record have furnished detailed paleoenvironmental reconstructions. However, palynological studies are only available for the last millennium, and the vegetation and the landscape around the lake had already been transformed by humans by this time. Therefore, the primeval vegetation of Montcortès and the history of its anthropogenic transformations remains unknown. This paper presents a palynological analysis of the interval between the Late Bronze Age (ca. 1100 BCE) and the Early Medieval period (820 CE), aimed at recording the preanthropic conditions, the anthropization onset and the further landscape transformations. During the Late Bronze Age (ca. 1100 BCE to 770 BCE), the vegetation did not show any evidence of human impact. The decisive anthropogenic transformation of the Montcortès catchment vegetation and landscape started at the beginning of the Iron Age (770 BCE) and continued during Roman and Medieval times in the form of recurrent burning, grazing, cultivation, silviculture, hemp retting and other human activities. Some intervals of lower human pressure were recorded, but the original vegetation never returned. The anthropization that took place during the Iron Age did not cause relevant changes in the sediment yield to the lake, but a significant limnological shift occurred, as manifested in the initiation of varve formation, a process that has been continuous until today. Climatic shifts seem to have played a secondary role in influencing catchment vegetation and landscape changes from the Iron Age onwards. These results contrast with previous inferences of low anthropogenic impact until the Medieval Period, at a regional level (central Pyrenees). The intensification of human pressure in Early Medieval times (580 CE onwards) has also been observed in Lake Montcortès, but the overall anthropization of its watershed had already commenced a couple of millennia before, at the beginning of the Iron Age. It could be interesting to verify whether the same pattern – i.e., Late Bronze “pristinity”, Iron Age anthropization and Early Medieval intensification of human pressure – may be a recurrent pattern for mid-elevation Pyrenean landscapes below the tree line. This pattern complicates the definition of the “Anthropocene”, as it adds a new dimension, i.e., elevational diachronism, to the anthropization of mountain ranges, in general.

scholarly journals Bronze Age to Medieval vegetation dynamics and landscape anthropization in the central pre-Pyrenees

2021 ◽  
Author(s):  
Valentí Rull ◽  
Teresa Vegas-Vilarrúbia ◽  
Juan Pablo Corella ◽  
Blas Lorenzo Valero-Garcés
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Late Bronze Age ◽  
Medieval Period ◽  
Human Pressure ◽  
Early Medieval ◽  
Early Medieval Period ◽  
History Of ◽  
Original Vegetation ◽  
Landscape Transformations

The varved sediments of Lake Montcortès (central Pre-Pyrenees) have provided a continuous high-resolution record of the last ca. 3000 years. Previous chronological and sedimentological studies of this record have furnished detailed paleoenvironmental reconstructions. However, palynological studies are only available for the last millennium, when the landscape around the lake had already been transformed by humans. Therefore, the primeval vegetation of Montcortès and the history of its anthropogenic transformations remains unknown. This paper presents a palynological analysis of the interval between the Late Bronze Age and the Early Medieval period, aimed at recording the preanthropic conditions, the anthropization onset and the further landscape transformations. During the Late Bronze Age (ca. 1100 BCE to 770 BCE), the vegetation did not show any evidence of human impact. The decisive anthropogenic transformation of the Montcortès catchment vegetation and landscape started at the beginning of the Iron Age (770 BCE) and continued during Roman and Medieval times in the form of recurrent burning, grazing, cultivation, silviculture and hemp retting. Some intervals of lower human pressure were recorded, but the original vegetation never returned. The anthropization that took place during the Iron Age did not cause relevant changes in the sediment yield to the lake, but a significant limnological shift occurred, as manifested in the initiation of varve formation, a process that has been continuous until today. Climatic shifts seem to have played a secondary role in influencing vegetation and landscape changes. These results contrast with previous inferences of low anthropogenic impact until the Medieval Period, at a regional level. It could be interesting to verify whether the same pattern – i.e., Iron Age anthropization and Early Medieval intensification of human pressure – may be a recurrent pattern for mid-elevation Pyrenean landscapes below the tree line.

scholarly journals Bronze Age to Medieval vegetation dynamics and landscape anthropization in the central pre-Pyrenees 

2021 ◽  
Author(s):  
Valentí Rull ◽  
Teresa Vegas-Vilarrúbia ◽  
Juan Pablo Corella ◽  
Blas Valero-Garcé
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Late Bronze Age ◽  
Medieval Period ◽  
Human Pressure ◽  
Early Medieval ◽  
Early Medieval Period ◽  
History Of ◽  
Original Vegetation ◽  
Landscape Transformations

Abstract The varved sediments of Lake Montcortès (central Pre-Pyrenees) have provided a continuous high-resolution record of the last ca. 3000 years. Previous chronological and sedimentological studies of this record have furnished detailed paleoenvironmental reconstructions. However, palynological studies are only available for the last millennium, when the landscape around the lake had already been transformed by humans. Therefore, the primeval vegetation of Montcortès and the history of its anthropogenic transformations remains unknown. This paper presents a palynological analysis of the interval between the Late Bronze Age and the Early Medieval period, aimed at recording the preanthropic conditions, the anthropization onset and the further landscape transformations. During the Late Bronze Age (ca. 1100 BCE to 770 BCE), the vegetation did not show any evidence of human impact. The decisive anthropogenic transformation of the Montcortès catchment vegetation and landscape started at the beginning of the Iron Age (770 BCE) and continued during Roman and Medieval times in the form of recurrent burning, grazing, cultivation, silviculture and hemp retting. Some intervals of lower human pressure were recorded, but the original vegetation never returned. The anthropization that took place during the Iron Age did not cause relevant changes in the sediment yield to the lake, but a significant limnological shift occurred, as manifested in the initiation of varve formation, a process that has been continuous until today. Climatic shifts seem to have played a secondary role in influencing vegetation and landscape changes. These results contrast with previous inferences of low anthropogenic impact until the Medieval Period, at a regional level. It could be interesting to verify whether the same pattern – i.e., Iron Age anthropization and Early Medieval intensification of human pressure – may be a recurrent pattern for mid-elevation Pyrenean landscapes below the tree line.

Bogs, Bodies and Burnt Mounds: Visits to the Soar Wetlands in the Neolithic and Bronze Age

2012 ◽  
Vol 78 ◽  
pp. 173-206 ◽  
Author(s):  
Susan Ripper ◽  
Matthew Beamish ◽  
A. Bayliss ◽  
C. Bronk Ramsey ◽  
A. Brown ◽  
...  
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Radiocarbon Dating ◽  
Violent Death ◽  
Late Bronze Age ◽  
Medieval Period ◽  
Early Medieval Period ◽  
Long Period ◽  
Animal Bones ◽  
The Bronze Age

The recording and analysis of a burnt mound and adjacent palaeochannel deposits on the floodplain of the River Soar in Leicestershire revealed that the burnt mound was in use, possibly for a number of different purposes, at the transition from the Neolithic to the Bronze Age. An extensive radiocarbon dating programme indicated that the site was revisited. Human remains from the palaeochannel comprised the remains of three individuals, two of whom pre-dated the burnt mound by several centuries while the partial remains of a third, dating from the Late Bronze Age, provided evidence that this individual had met a violent death. These finds, along with animal bones dating to the Iron Age, and the remains of a bridge from the early medieval period, suggest that people were drawn to this location over a long period of time.

scholarly journals Etnesjøen – en førromersk landsby på Vestlandet

Viking ◽  
2021 ◽  
Vol 85 (1) ◽  
Author(s):  
Søren Diinhoff
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Late Bronze Age ◽  
Medieval Period ◽  
Settlement Area ◽  
Early Medieval Period ◽  
Western Norway ◽  
Top Soil ◽  
University Museum ◽  
The University

In the summer months of 2013, the University Museum of Bergen conducted an archeological excavation of a large prehistoric settlement area at Etnesjøen in Etne parish, Western Norway. By use of mechanized top soil stripping numerous buildings, inhumation burials, cooking pits and kilns were uncovered. The site dates from the Late Bronze Age to Early Medieval Period. The focus of the article is the discovery of a Pre-Roman Iron Age village, formed of up to six farms chronologically spanning up to five generations of continuous occupation. At the time of the excavation, this was only the second pre-historic village of its kind found in Norway, indicating a significant and important discovery. 

Feeding Infants from the Iron Age to the Early Medieval Period in Britain

2018 ◽  
Author(s):  
Rebecca C. Redfern
Keyword(s):  
Social Identity ◽  
Iron Age ◽  
Medieval Period ◽  
Early Medieval ◽  
Developmental Processes ◽  
Human Relationships ◽  
Early Medieval Period

The feeding and rearing of infants are sociocultural and developmental processes, each with their own timetables that can either unite or diverge, depending on the wellbeing and physiological growth of the infant, and the needs of the mother or carer and the society in which they live. They are highly emotive and complex topics, which go to the heart of human relationships and behaviours, because they are regarded as important steps to achieving personhood and a social identity. Furthermore, because these processes begin during pregnancy, they rely on the intimate connections between a mother and foetus, and carer and baby. This chapter will examine these processes from pregnancy through to childhood, providing a framework to understand the practices and choices made by the Iron Age, Roman and Saxon communities in Britain and Europe.

scholarly journals A Later prehistoric house and Early Medieval buildings in Northern Scotland: excavations at Loch Shurrery and Lambsdale Leans, Caithness, 1955, with a note on Lower Dounreay

2003 ◽  
Vol 5 ◽  
Author(s):  
Alastair MacLaren ◽  
Ewan Campbell ◽  
Gordon Cook ◽  
Janet Hooper ◽  
L Wells ◽  
...  
Keyword(s):  
Iron Age ◽  
The Other ◽  
Medieval Period ◽  
The South ◽  
Early Medieval ◽  
Early Medieval Period ◽  
The North ◽  
Two Samples ◽  
First Millennium ◽  
Northern Edge

Two rescue excavations at the northern edge of a rather sparsely occupied part of the interior of Caithness are reported here, lying near to one of the largest clusters of archaeological sites in the modern county. In the event, the monuments were not threatened, and survive.Because of the limited nature of the excavation at Loch Shurrery (NGR ND 043568),the main value of the evidence about the hut circle relates to its structure and dating. The excavated remains represented a medium-sized oval house with a west-facing entrance. It had an off-centre hearth of rectangular construction. It was rather different in structure to the majority of the small group of such sites which have been excavated in the northern part of the Scottish mainland, as it did not appear to have an internal ring of post holes. In addition, its western entrance is not matched at the other sites, where entrance orientations are to the south, east or south-east. The wall of the Loch Shurrery house was fairly thick and the excavation suggested that it was complex, while the entrance passageway was quite long. The existence of door checks is also an unusual feature and may relate to the entrance structures of brochs and other substantial roundhouses. Two samples of charcoal from the hearth inside the hut circle were submitted for radiocarbon dating: the determinations produce calibrated ranges (at 2-sigma) of 346-4 cal BC and 341 cal BC-1 cal AD. It is likely that most of the excavated, undecorated pottery is also Iron Age, part of a broad tradition of very coarsely tempered pottery. Not-withstanding evidence of extended occupation, the whole period of construction and occupation may have occurred within the Iron Age.The mound of Lambsdale Leans (NGR ND 051548)lies in Reay parish, situated on low-lying ground at the head of Loch Shurrery and close to where its main tributary (the Torran Water) enters the loch from the south. The main characteristics of the this partially-excavated site are the presence of what appeared to be two extended inhumations and the remnants of possible structures associated with several layers of burnt material. Lambsdale Leans itself was a natural mound, of elongated shape and composed largely of sand, into which were set the burials and structural remains. The burials (one certainly female, the other probably so) were not in cists. The structural remains, while not fully excavated, accord well with the general tenor of the available evidence of later first millennium AD buildings in the north of Scotland. Both structures at Lambsdale Leans had floors comprising roughly laid paving, edged with upright slabs, and with an outer kerb of stones. The earliest-dated pottery sherds, unstratified, are from a single grass- tempered handmade vessel whose form cannot be determined. Overall,on one interpretation the Lambsdale Leans evidence favours a context within the Early Medieval period in Caithness. The pottery however, being mostly C12-C13 oxidised wheel-thrown vessels, can be seen to support the suggestion that occupation on the site may have begun in the Medieval period.

scholarly journals Exploring Linear Earthworks across Time and Space – Introducing the ‘Monumentality and Landscape: Linear Earthworks in Britain’ Project

2021 ◽  
Vol 3 ◽  
pp. 129
Author(s):  
Nicky Garland ◽  
Barney Harris ◽  
Tom Moore ◽  
Andrew Reynolds
Keyword(s):  
Comparative Study ◽  
Middle Ages ◽  
Iron Age ◽  
First Year ◽  
Medieval Period ◽  
Early Medieval ◽  
Early Middle Ages ◽  
Preliminary Results ◽  
Early Medieval Period ◽  
Landscape Research

Linear earthworks of a monumental character are an enigmatic part of the British landscape. Research in Britain suggests that such features range in date from the early 1st millennium BC to the Early Middle Ages. While the  roles of these monuments in past societies cannot be understated, they remain a relatively under-researched phenomenon. This article introduces the Leverhulme Trust-funded ‘Monumentality and Landscape: Linear Earthworks in Britain’ project, which aims to provide a comparative study of linear earthworks focusing on those dating to the Iron Age and early medieval period. This contribution reviews our approach and shares preliminary results from the project’s first year, identifying wider implications for the study of linear earthworks.

Shifting perspectives on 1st-millennia Scotland

2021 ◽  
Vol 150 ◽  
pp. 247-278
Author(s):  
Ronan Toolis
Keyword(s):  
Iron Age ◽  
Medieval Period ◽  
The South ◽  
Early Medieval ◽  
Early Medieval Period ◽  
South West ◽  
Cultural Traits

Underlying much research on Iron Age Scotland is a pervasive regionalism. This has led to the underplaying of cultural traits that are evident across the country. The examination of south-west Scotland, a region that does not have a distinctive later prehistoric character and which is often viewed as somewhat peripheral to understanding Iron Age Scotland, however, reveals underlying patterns of settlement and culture that are embedded across Scotland but markedly different to Iron Age societies to the south. Moreover, cultural traits apparent across Scotland but absent south of the border continued into the early medieval period, suggesting significant cultural divergences between 400 BC and AD 650.

An archaeological theory of the sea

2011 ◽  
Author(s):  
Robert Van de Noort
Keyword(s):  
Bronze Age ◽  
North Sea ◽  
Archaeological Theory ◽  
Medieval Period ◽  
Early Medieval ◽  
Long Distance ◽  
Early Medieval Period ◽  
The North ◽  
The Social ◽  
The North Sea

Despite the wealth of information available on the North Sea, surprisingly few archaeologists have set out to study how people related to and connected to this sea, and other seas, in the past. In fact, we can distinguish four established traditions in archaeological research of the sea, all of which originated in the 20th century. First, many (or most) land-locked archaeologists working on any side of the North Sea have simply disregarded the sea itself, seeing it merely as the natural boundary of their study areas rather than considering its role in any significant way. At best, they are seeing the sea from the land, without genuinely engaging with it (cf. Cooney 2003: 323), although the panorama is slowly changing (e.g. cf. Bradley 1984 with Bradley 2007). Second, there are those archaeologists with an interest in long-distance exchange and exotic objects, who focused initially on the Neolithic and Bronze Age periods but have also been concerned, in more recent decades, with the early medieval period. Although these archaeologists have recognized the seas as conduits of long-distance exchange, they have rarely questioned how the practice of travel across the sea impacted on the social products of such exchange (e.g. Butler 1963, O’Connor 1980, Bradley 1984, Clarke, Cowie, and Foxon 1985, for the Neolithic and early Bronze Age; Hodges 1982, Loveluck and Tys 2006, for the early medieval period). Third, a group of archaeologists have studied the exploitation of the sea, especially for fish and salt, and the occupation and the reclamation of the edges of the sea in the Roman period and afterwards; but these studies have generally not strayed beyond the functional utilization of the sea and coast both for food and for land for food production (e.g. Clark 1961; Van den Broeke 1985; Andersen 1995, 2007; Rippon 2000; Smart 2003; Milner et al. 2004; De Kraker and Borger 2007). And fourth, maritime archaeologists’ focus has been on ships and waterside structures directly relating to shipping activities, but the development of a fuller appreciation of the significance of the sea and seafaring to past societies remains something of a distant aspiration (e.g. Ellmers 1972; McGrail 2003: 1).

Is There Anybody Out There? A Reconsideration of the Environmental Evidence from the Breiddin Hillfort, Powys, Wales

2001 ◽  
Vol 81 ◽  
pp. 51-76 ◽  
Author(s):  
Paul C Buckland ◽  
Mike Parker Pearson ◽  
Andy Wigley ◽  
Maureen A Girling
Keyword(s):  
Bronze Age ◽  
Human Impact ◽  
Human Activity ◽  
Iron Age ◽  
Natural Water ◽  
Water Reservoir ◽  
Late Bronze Age ◽  
Archaeological Evidence ◽  
Natural Pond ◽  
Evidence Of Absence

Researchers have often assumed that the Iron Age hillforts of the Welsh borders were densely occupied centres of population. One of these is the Breiddin, occupied in the Late Bronze Age and Iron Age, which was excavated in 1969–76. At its centre was a natural water reservoir, Buckbean Pond, which provided a radiocarbon dated sequence of deposition contemporary with the later prehistoric occupation of the hillfort. The beetle assemblage from these deposits was never properly studied or published due to Maureen Girling's death and, as a result, its implications for understanding the human impact on the pond's immediate environment were not fully appreciated. Despite the remains of four-post structures close to the pond and of roundhouses and associated deposits in the vicinity, both flora and insect faunas indicate a quiet natural pond with little disturbance other than casual grazing by animals. This ‘evidence of absence’ does not square with the archaeological evidence which is here interpreted as deriving from human activity which was neither permanent nor intensive.

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