Charcoal and pollen analyses and vegetation reconstruction of the Alpine foreland in West Hungary

2012 ◽  
Vol 4 (4) ◽  
Author(s):  
Katalin Náfrádi ◽  
Pál Sümegi ◽  
Tünde Törőcsik
Keyword(s):  
Bronze Age ◽  
Middle Ages ◽  
Iron Age ◽  
The Holocene ◽  
Related Information ◽  
Late Iron Age ◽  
Imperial Period ◽  
Alpine Foreland ◽  
And Migration ◽  
Pollen Analyses

AbstractIn the area of archaeological excavations that were performed prior to the construction of Main Road No. 86 in Vas County (West Hungary) in the Alpine foreland new geoarchaeological analyses have been conducted. We used anthracology and pollen analyses to reconstruct the former vegetation cover at the study site. Charcoal data provide site-related information about the local woodland composition, management and human impact, while pollen data provide information on the arboreal and non-arboreal vegetation on a regional or local scale. Adequate samples for anthracological analyses derive from the Bronze Age, Iron Age, Imperial and Migration Periods and Middle-Ages archaeological objects. The core for pollen analyses originates from alluvial sediments of the Borzó Creek and covers the late Pleistocene and the Holocene until the Medieval Period. Charcoal analyses show the dominance of Quercus trees in the vicinity of the human settlements that might indicate a strong human selection, or the fragmentation of samples. Pollen analyses indicate thermophilous vegetation from the beginning of the Holocene, with increasing values of Fagus and Carpinus. Pollens of cereals indicate human activity, which is also demonstrated by the presence of pollen from Juglans and Vitis in the Iron Age sequence. Extensive forest clearance occurred in the Late Iron Age and the Imperial Period.

scholarly journals Archaeology and Zooarchaeology of the Late Iron Age-Roman Transition in the Province of Raetia (100 bc–100 ad)

2017 ◽  
Vol 20 (3) ◽  
pp. 431-450 ◽  
Author(s):  
Simon Trixl ◽  
Bernd Steidl ◽  
Joris Peters
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Temporal Analysis ◽  
Faunal Remains ◽  
Late Iron Age ◽  
Burial Customs ◽  
La Tène ◽  
Alpine Foreland ◽  
La Tene ◽  
Transitional Phase

The incorporation of the region north of the Alpine divide and its foreland into the Imperium Romanum initiated major changes in economic and social structure and in everyday life in the newly-founded province of Raetia. Controversy exists, however, about the continuity of local La Tène traditions into early Roman times, since the archaeological evidence recorded to date tends to give the impression that the northern Alpine foreland was largely unpopulated at the time of the Roman conquest in 15 bc. However, ongoing excavations in this region are gradually enhancing the archaeological visibility of this transitional phase. Compared to early Roman provincial populations settled along the Via Claudia Augusta and its hinterland, a culturally unique community stands out: the Heimstetten group. This group is located in the eastern Raetian hinterlands and dates to around 30–60 ad. Its building tradition, settlement structure, and burial customs show close affinities with the La Tène culture, thus suggesting continuity in autochthonous culture at the time of the early Roman occupation. Since faunal remains can potentially act as cultural markers, additional insights can be gained from a spatial-temporal analysis of livestock composition and breeding practices. The results presented here clearly show that, during the Iron Age, marked regional differences in species composition are visible, implying the possibility of distinct developments during early Romanization. In addition to evaluating faunal developments in the study area between c. 100 bc–100 ad, the issue of cattle breeding—traditionally the mainstay of livestock economies in many regions and especially in the Munich Gravel Plain at least since the Bronze Age—is addressed in greater detail.

Anarchistic action. Social organization and dynamics in southern Scandinavia from the Iron Age to the Middle Ages

2019 ◽  
Vol 26 (2) ◽  
pp. 61-73
Author(s):  
Trine Louise Borake
Keyword(s):  
Social Organization ◽  
Middle Ages ◽  
Iron Age ◽  
Social Engagement ◽  
General Interest ◽  
Network Organization ◽  
Late Iron Age ◽  
Human Intentionality ◽  
And Migration ◽  
The Middle Ages

AbstractA general interest in centralized institutions, state formation and prestige objects has dominated research on social organization and dynamics in Scandinavia from the Late Iron Age to the Middle Ages. Accordingly, a focus on kingly power, aristocratic influence, hierarchies and warrior might has dominated archaeological research designs for the last forty years. Subsequently, other perspectives have been evaded and their significance has been diminished. In this article, I use anarchistic principles as an analytic perspective and present examples of anarchistic actions – network organization, justified leaders and decentralization – drawing on well-known but ambiguous phenomena such as thing sites, the southern Danish defence system Danevirke, and migration and mobility. I suggest a perspective that recognizes resistance, authority and decentralization as well as centralization and institutionalization, allowing a broad spectrum of social engagement and interrelations to influence social organization. I will argue that human intentionality has been overlooked in favour of structures and institutions, and that the power of network organization and decentralization is influential in shaping social organization and dynamics.

scholarly journals Early human impact on soils and hydro-sedimentary systems: Multi-proxy geoarchaeological analyses from La Narse de la Sauvetat (France)

The Holocene ◽  
2020 ◽  
Vol 30 (12) ◽  
pp. 1780-1800
Author(s):  
Alfredo Mayoral ◽  
Salomé Granai ◽  
Anne-Lise Develle ◽  
Jean-Luc Peiry ◽  
Yannick Miras ◽  
...  
Keyword(s):  
Bronze Age ◽  
Middle Ages ◽  
Iron Age ◽  
Late Antiquity ◽  
Environmental Changes ◽  
Anthropogenic Impacts ◽  
Late Neolithic ◽  
Societal Factors ◽  
Late Iron Age ◽  
Middle Bronze Age

We analysed the late-Holocene pedo-sedimentary archives of La Narse de la Sauvetat, a hydromorphic depression in the southern Limagne plain (central France), where chronologically accurate studies are scarce. The multi-proxy geoarchaeological and palaeoenvironmental analysis of two cores from different areas of the basin was carried out through sedimentological, geochemical, micromorphological and malacological investigations. Integration of these datasets supported by a robust radiocarbon-based chronology allowed discussion of socio-environmental interactions and anthropogenic impacts from Late Neolithic to Early Middle Ages. Until the Middle Bronze Age, there was no clear evidence of anthropogenic impact on soils and hydro-sedimentary dynamics of the catchment, but two peaks of high alluvial activity probably related to the 4.2 and 3.5 kyr. BP climate events were first recorded in Limagne. Significant anthropogenic impacts started in the Late Bronze Age with increased erosion of the surrounding volcanic slopes. However, a major threshold was reached c. 2600 cal BP with a sharp increase in the catchment erosion interpreted as resulting from strong anthropogenic environmental changes related to agricultural activities and drainage. This implies an anthropogenic forcing on soils and hydro-sedimentary systems much earlier than was usually considered in Limagne. These impacts then gradually increased during Late Iron Age and Roman periods, but environmental effects were certainly contained by progress in agricultural management. Late Antiquity environmental changes are consistent with regional trend to drainage deterioration in lowlands, but marked asynchrony in this landscape change suggests that societal factors implying differential land management were certainly predominant here.

Vegetation history reconstructed from anthracology and pollen analysis at the rescue excavation of the MO Motorway, Hungary

2011 ◽  
Vol 3 (4) ◽  
Author(s):  
Katalin Náfrádi ◽  
Elvira Bodor ◽  
Tünde Törőcsik ◽  
Pál Sümegi
Keyword(s):  
Bronze Age ◽  
Middle Ages ◽  
Iron Age ◽  
Vegetation History ◽  
Analytical Data ◽  
Fruit Trees ◽  
Climatic Conditions ◽  
Copper Age ◽  
Migration Period ◽  
Late Iron Age

AbstractThe significance of geoarchaeological investigations is indisputable in reconstructing the former environment and in studying the relationship between humans and their surroundings. Several disciplines have developed during the last few decades to give insight into earlier time periods and their climatic conditions (e.g. palynology, malacology, archaeobotany, phytology and animal osteology). Charcoal and pollen analytical studies from the rescue excavation of the MO motorway provide information about the vegetation changes of the past. These methods are used to reconstruct the environment of the former settlements and to detect the human impact and natural climatic changes. The sites examined span the periods of the Late-Copper Age, Late-Bronze Age, Middle-Iron Age, Late-Iron Age, Sarmatian period, Late Sarmatian period, Migration period, Late-Migration period and Middle Ages. The vegetation before the Copper Age is based only on pollen analytical data. Anthracological results show the overall dominance of Quercus and a great number of Ulmus, Fraxinus, Acer, Fagus, Alnus and Populus/Salix tree fossils, as well as the residues of fruit trees present in the charred wood assemblage.

scholarly journals Isolated and backward Westerwolde (Groningen, the Netherlands)? A confrontation of archaeological and historical data from the Middle Ages in a wider geographical context

2021 ◽  
pp. 273-344
Author(s):  
Henny A. Groenendijk ◽  
Remi Van Schaïk
Keyword(s):  
The Netherlands ◽  
Bronze Age ◽  
19Th Century ◽  
Middle Ages ◽  
Iron Age ◽  
Critical Study ◽  
Ecological Data ◽  
The North ◽  
Late Iron Age ◽  
The 19Th Century

The aim of this paper is to question the supposed isolated and backward position of the region of Westerwolde, in the north-eastern part of the Netherlands. Westerwolde’s geographically rather isolated position has traditionally been brought forward to explain its backward image. Progressive peat growth ever since the Bronze Age occupation had transformed Westerwolde into an island. It was abandoned in the Late Iron Age, only to be recolonized in the early Middle Ages. During the 19th century, romantics were still admiring Westerwolde’s arcadian scenery and cultural traditions. In contrast, from the mid-19th century until well into the 20th century, protagonists of modern agriculture criticized its backward farming methods and standard of living, as well as its poor infrastructure. The central issues we address here is whether critics were justified in describing it as backward in the 19th century and whether concrete indications for this assumed backwardness are to be found in previous centuries. To jump from early medieval times to the 19th century is too big a leap, but combining archaeological and ecological data with a renewed and more critical study of written sources against the background of huge landscape transformations has brought a nuanced understanding of how Westerwolde evolved. We present new insights for the period starting with the conquest of Frisia and Saxony by the Carolingians and the introduction of Christianity, when missionaries and newly founded monasteries acquired agricultural assets and rights in the conquered region, up to the late Middle Ages. We therefore analyze church foundations, livelihoods or economic conditions of existence in connection with occupation structures, infrastructure and exchange of consumer goods interdisciplinarily. Conservatism appears easily confused with backwardness, and an aversion to innovation, with indifference, as underlying external factors often forced the inhabitants to adopt a wait-and-see attitude. Westerwolde is viewed continuously in connection with the adjacent regions of Drenthe and Lower Saxon Emsland.

scholarly journals Late-Holocene forest resilience in the central Pyrenean highlands as deduced from pollen analysis of Lake Sant Maurici sediments

The Holocene ◽  
2021 ◽  
pp. 095968362110332
Author(s):  
Valentí Rull ◽  
Núria Cañellas-Boltà ◽  
Teresa Vegas-Vilarrúbia
Keyword(s):  
Bronze Age ◽  
Middle Ages ◽  
Iron Age ◽  
Late Holocene ◽  
High Elevation ◽  
Roman Period ◽  
High Mountain ◽  
Southern Central ◽  
Central Pyrenees ◽  
The Middle Ages

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.

scholarly journals medieval fisheries of Galicia (Northwestern Iberia): A preliminary archaeozoological overview

Archaeofauna ◽  
2021 ◽  
Vol 30 ◽  
pp. 155-165
Author(s):  
EUFRASIA ROSELLÓ-IZQUIERDO ◽  
EDUARDO GONZÁLEZ-GÓMEZ DE AGÜERO ◽  
CARLOS FERNÁNDEZ-RODRÍGUEZ ◽  
LAURA LLORENTE-RODRÍGUEZ ◽  
ARTURO MORALES-MUÑIZ
Keyword(s):  
Middle Ages ◽  
Iron Age ◽  
Fish Assemblages ◽  
Late Iron Age ◽  
Late Middle Ages ◽  
Critical Issues ◽  
Fish Remains ◽  
Coastal Deposits ◽  
Fishing Fleets ◽  
Two Kingdoms

The origin and development of the Iberian Medieval fisheries is a poorly documented phenomenon both from the standpoint of historical (documentary) and material (archaeological) evidence. Such dearth of knowledge can be explained in terms of proximal (i.e., a deficient retrieval of fish remains) and ultimate causes. Among the latter, the Muslim invasion, that lasted ca. 800 years of the “medieval millennium” in the Iberian Peninsula, needs to be taken into account as it probably delayed the development of fishing fleets within the Christian kingdoms for a substantial period of time. Be it as it may, the lack of knowledge does not allow one to explore a range of critical issues of Spanish and Portuguese history, such as the role played by the ever-expanding fishing fleets of Portugal and Castilla in the process of maritime discovery and colonization that these two kingdoms fostered by the end of the Middle Ages. In this paper, the results from a comparative analysis of selected fish assemblages from primary (i.e. coastal) deposits of the northern Iberian shores are presented. The aim is to check whether changes can be documented both at the level of (1) the range of species occurring in sites from the late Iron Age (Castreña culture, IV-I BC) to the Late Middle Ages (XV AD), and (2) the skeletal spectra of certain species that could reveal a differential processing of taxa meant for local consumption and those that appear in inland sites.

North European Rock Art

2017 ◽  
Author(s):  
Joakim Goldhahn
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Rock Art ◽  
Northern Europe ◽  
Long Distance ◽  
Migration Period ◽  
Farming Communities ◽  
And Migration ◽  
The Bronze Age

This chapter offers a long-term perspective on rock art in northern Europe. It first provides an overview of research on the rock art traditions of northern Europe before discussing the societies and cultures that created such traditions. It then considers examples of rock art made by hunter-gatherer societies in northern Europe, focusing on the first rock art boom related to Neolithization. It also examines the second rock art boom, which was associated with social and religious changes within farming communities that took place around 1600–1400 bc. The chapter concludes by analysing the breakdown of long-distance networks in the transition from the Bronze Age to the Iron Age and its consequences for the making of rock art within the southern traditions, as well as the use of rock art sites during the Pre-Roman Iron Age, Roman Iron Age, and Migration Period.

CERAMICS OF THE PESTRYAKOVO LAKE SETTLEMENT (SOUTH OF WESTERN SIBERIA)

2021 ◽  
Vol 27 ◽  
pp. 205-212
Author(s):  
KIRYUSHIN K. ◽  
◽  
KIRYUSHIN Yu. ◽  
Keyword(s):  
Organic Matter ◽  
Bronze Age ◽  
Middle Ages ◽  
Iron Age ◽  
Western Siberia ◽  
Early Iron Age ◽  
Late Bronze Age ◽  
The South ◽  
Animal Hair ◽  
The Middle Ages

The article is devoted to the publication of finds of fragments of ceramic dishes discovered at the settlement of Pestryakovo Lake (Zavyalovsky district of Altai Territory). A group of ceramics which belongs to the early Iron Age and the Middle Ages, is pointed out. Single fragments find analogies in the materials of the sites of the Early and Late Bronze Age. The ceramic collection of the Pestryakovo Lake settlement includes groups of ceramics that belong to the Neolithic or Eneolithic. These are fragments of vessels ornamented with prints of a “string”, pricks, imprints of a short comb stamp, a dingle-dingle stamping. Linear-pricked and receding-pricked ceramics are quite informative. On the outer and inner surfaces, as well as in the fractures, traces of burnt-out organic matter (animal hair) are recorded. Such ceramics are widely represented in the south of Western Siberia and are associated with various settlement and burial complexes from the Ob to the Irtysh and various cultural formations of the Neolithic and Eneolithic. Keywords: settlement, ceramics, ornamentation technique, comparative typological analysis, neolithic, eneolithic

Holocene evolution of closed depressions and its relation to landscape dynamics in the loess areas of Poland

The Holocene ◽  
2019 ◽  
Vol 29 (4) ◽  
pp. 543-564 ◽  
Author(s):  
Renata Kołodyńska-Gawrysiak
Keyword(s):  
Land Use ◽  
Soil Erosion ◽  
Bronze Age ◽  
Middle Ages ◽  
Central Europe ◽  
Iron Age ◽  
Landscape Dynamics ◽  
Early Iron Age ◽  
Late Bronze Age ◽  
Atlantic Period

Past Pleistocene topography of the loess uplands is rich in local sinks (closed depressions (CDs)) influencing sediment fluxes. Soil-sediment sequences from CDs constituting geoarchives where landscape changes under natural and anthropogenic conditions have been recorded. Pedo-sedimentary archives from 10 CDs in the Polish loess belt and human settlements were analysed. Phases of the Holocene evolution of the CDs were correlated with landscape dynamics in loess areas in Poland and Central Europe. Phases of infilling of CDs occurring (2) from the late Boreal/early Atlantic Period until the (middle) late Bronze Age/early Iron Age and (4) since the early Middle Ages until today were documented. These were phases of long-term soil erosion and colluviation corresponding to the increasing agricultural land use of Polish loess uplands. Phases of soil formation related to geomorphic stabilization of CDs occurred (1) from the late Vistulian until the late Boreal/early Atlantic Period and (3) from the late Bronze Age/early Iron Age until the early/high Middle Ages. These were phases of decreased soil erosion and landform conservation in a considerable part of Poland’s loess areas. Pedo-sedimentary archives from the CDs have recorded soil erosion strongly related with human-induced land-use changes. The mean soil erosion rate in the catchment of CDs was 0.33 t·ha−1·yr−1 during prehistory and 4.0 t·ha−1·yr−1 during the last approximately 1000 years. Phases of CD evolution are representative for the main phases of sediment and landscape dynamics in Poland’s loess areas recorded in various archives, and are not synchronous with some of these phases in Central Europe.

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