scholarly journals Mountains, Herds and Crops: Notes on New Evidence from the Early Neolithic in the Southern Central Pyrenees

2021 ◽  
Vol 7 (1) ◽  
pp. 1015-1034
Author(s):  
Ermengol Gassiot-Ballbè ◽  
Niccolò Mazzucco ◽  
Sara Díaz-Bonilla ◽  
Laura Obea-Gómez ◽  
Javier Rey-Lanaspa ◽  
...  

Abstract After years of intense fieldwork, our knowledge about the Neolithisation of the Pyrenees has considerably increased. In the southern central Pyrenees, some previously unknown Neolithic sites have been discovered at subalpine and alpine altitudes (1,000–1,500 m a.s.l.). One of them is Cueva Lóbrica, 1,170 m a.s.l., which has an occupation phase with impressed pottery dated ca. 5400 cal BCE. Another is Coro Trasito, 1,558 m a.s.l., a large rock shelter that preserves evidence of continuous occupations in the Early Neolithic, 5300–4600 cal BCE. Evidence of human occupation at higher altitudes has also been documented. In the Axial Pyrenees, at the Obagues de Ratera rock shelter, 2,345 m a.s.l., an occupation has been dated to around 5730–5600 cal BCE. At Cova del Sardo, in the Sant Nicolau Valley, at 1,780 m a.s.l., a series of occupations have been excavated, dated to ca. 5600–4500 cal BCE. These sites allow us to discuss patterns of occupation of the mountainous areas between the Late Mesolithic and Early Neolithic. Recent data suggest that the last hunter–gatherer occupied all altitudinal stages of the Pyrenees, both in the outer and inner ranges. A change in the settlement pattern seems to have occurred in the Early Neolithic, which consisted of a concentration of occupations in the valley bottom and mid-slopes, in biotopes favourable to both herding and agriculture.

Author(s):  
Sérgio Monteiro-Rodrigues

Recentemente obtiveram-se cinco novas datações pelo radiocarbono para as ocupações holocénicas do sítio pré-histórico do Prazo. Quatro delas apresentam resultados compatíveis com os já divulgados em publicações anteriores. No conjunto, dispõe-se agora de uma série de vinte e seis datações 14C que seconsideram válidas. Estas datações permitem remeter a fase que se atribuiu ao Epipaleolítico para os finais do X/ meados do IX milénio cal BC; o Mesolítico mais antigo para o terceiro quartel do VIII milénio cal BC; o Mesolítico final para o período compreendido entre o segundo quartel do VII milénio cal BCe os meados do VI milénio cal BC; e o Neolítico Antigo para o intervalo balizado entre os finais do VI milénio cal BC e um momento indeterminado posterior ao terceiro quartel do V milénio cal BC. Entre estes períodos com ocupações humanas observam-se intervalos temporais para os quais não existem datações absolutas. Sugere-se que este facto possa estar relacionado com as dinâmicas sedimentares do local no decurso do Holocénico e não necessariamente com um padrão de povoamento caracterizado pela descontinuidade. New radiocarbon dating for the Holocene occupations of the prehistoric site of Prazo (Freixo de Numão, Vila Nova de Foz Côa, Northern Portugal) - Recently, five new radiocarbon dates for the Holocene occupations of the prehistoric site of Prazo were obtained. Four of them show results that are consistent with those previously published. At the moment, there are twenty-six 14C dates that are considered to be valid. These dates assign the supposed Epipalaeolithic to the end of the 10th/ middle of the 9th millennium cal BC; the earliest Mesolithic to the third quarter of the 8th millennium cal BC; the late Mesolithic to the interval between the second quarter of the 7th millennium cal BC and the middle of the 6th millennium cal BC; and the early Neolithic to the interval between the end of the 6th millennium cal BC and an undetermined moment after the third quarter of the 5th millennium cal BC. Among these periods with human occupation there are intervals for which there is no absolute dating. It is suggested that this may be related to the sedimentary dynamics of the site during the Holocene and not necessarily to a settlement pattern characterized by discontinuity.


1994 ◽  
Vol 21 (3) ◽  
pp. 73-76 ◽  
Author(s):  
E. Gili ◽  
Enric Vicens ◽  
A. Obrador ◽  
Peter William Skelton ◽  
Gregorio López

Author(s):  
Richard Bradley ◽  
Colin Haselgrove ◽  
Marc Vander Linden ◽  
Leo Webley

The Later Prehistory of North-West Europe provides a unique, up-to-date, and easily accessible synthesis of the later prehistoric archaeology of north-west Europe, transcending political and language barriers that can hinder understanding. By surveying changes in social forms, landscape organization, monument types, and ritual practices over six millennia, the volume reassesses the prehistory of north-west Europe from the late Mesolithic to the end of the pre-Roman Iron Age. It explores how far common patterns of social development are apparent across north-west Europe, and whether there were periods when local differences were emphasized instead. In relation to this, it also examines changes through time in the main axes of contact between the various regions of continental Europe, Britain, and Ireland. Key to the volume's broad scope is its focus on the vast mass of new evidence provided by recent development-led excavations. The authors collate data that has been gathered on thousands of sites across Britain, Ireland, northern France, the Low Countries, western Germany, and Denmark, using sources including unpublished 'grey literature' reports. The results challenge many aspects of previous narratives of later prehistory, allowing the volume to present a distinctively fresh perspective.


The Holocene ◽  
2021 ◽  
pp. 095968362110332
Author(s):  
Valentí Rull ◽  
Núria Cañellas-Boltà ◽  
Teresa Vegas-Vilarrúbia

Palynological analysis of the last ca. 4300 cal year BP using a sediment core taken from high mountain (ca. 1900 m elevation) Lake Sant Maurici sediments (southern-central Pyrenees) showed remarkable vegetation constancy during the Bronze Age and the Middle Ages. Records of the Iron Age and the Roman period were missing due to a major sedimentary gap. During the studied periods, the vegetation around the lake was largely dominated by pine ( Pinus) forests with birch ( Betula), oak ( Quercus) and hazel ( Corylus) trees, as is the case today. The composition of these forests and the abundance of their components remained quite stable, despite the occurrence of temperature and moisture shifts. The degree of human disturbance, notably that of pastoralism and cereal cultivation by scattered and temporary settlements, was very low and had little or no effect on the dominant forests. This situation contrasts with most high-elevation (subalpine and alpine) environments of the central Pyrenees that were massively anthropized during the Middle Ages. Further research should be aimed at finding sediments corresponding to the Iron Age and the Roman period to verify whether the vegetation constancy can be extended throughout the Late-Holocene. Past records of this type may allow the estimation of natural and anthropogenic thresholds for irreversible forest changes, which would be useful for conservation purposes.


Radiocarbon ◽  
2012 ◽  
Vol 54 (3-4) ◽  
pp. 783-794 ◽  
Author(s):  
Natalia E Zaretskaya ◽  
Sönke Hartz ◽  
Thomas Terberger ◽  
Svetlana N Savchenko ◽  
Mikhail G Zhilin

Two well-known archaeological sites, the peat bogs of Shigir and Gorbunovo (Middle Urals, Russia), have been radiocarbon dated (61 conventional and accelerator mass spectrometry [AMS] dates from various natural and artifact samples). For the first time, a detailed chronology of Early to Late Mesolithic and Early Neolithic occupation for this region has been obtained, and a paleoenvironmental history reconstructed. Based on these results, we propose that the Mesolithic settlement of the Middle Urals region started in the early Holocene, at the same time as in central and eastern Europe.


2019 ◽  
Vol 9 (1) ◽  
Author(s):  
Pierre Antoine ◽  
Marie-Hélène Moncel ◽  
Pierre Voinchet ◽  
Jean-Luc Locht ◽  
Daniel Amselem ◽  
...  

Abstract The dispersal of hominin groups with an Acheulian technology and associated bifacial tools into northern latitudes is central to the debate over the timing of the oldest human occupation of Europe. New evidence resulting from the rediscovery and the dating of the historic site of Moulin Quignon demonstrates that the first Acheulian occupation north of 50°N occurred around 670–650 ka ago. The new archaeological assemblage was discovered in a sequence of fluvial sands and gravels overlying the chalk bedrock at a relative height of 40 m above the present-day maximal incision of the Somme River and dated by ESR on quartz to early MIS 16. More than 260 flint artefacts were recovered, including large flakes, cores and five bifaces. This discovery pushes back the age of the oldest Acheulian occupation of north-western Europe by more than 100 ka and bridges the gap between the archaeological records of northern France and England. It also challenges hominin dispersal models in Europe showing that hominins using bifacial technology, such as Homo heidelbergensis, were probably able to overcome cold climate conditions as early as 670–650 ka ago and reasserts the importance of the Somme valley, where Prehistory was born at the end of the 19th century.


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