scholarly journals A preliminary chronological study to understand the construction phases of a Late Copper–Early Bronze Age kurgan (kunhalom)

2019 ◽  
Vol 62 (1) ◽  
pp. 27-55
Author(s):  
Gábor Szilágyi ◽  
Katalin Náfrádi ◽  
Pál Sümegi
Keyword(s):  
Bronze Age ◽  
National Park ◽  
Late Glacial ◽  
The Body ◽  
Ice Age ◽  
Early Bronze Age ◽  
Copper Age ◽  
The Holocene ◽  
Two Phases ◽  
Undisturbed Core

The aim of this study is to identify the milestones of landscape evolution around the Ecse Mound (Karcag-Kunmadaras, Hortobágy National Park, Hungary) in the Holocene period by sedimentological and malacological analysis of strata underneath and within the body of the kurgan concerned, including that of the same characteristics of the artificially piled layers. An undisturbed core drilling was carried out and the sedimentological properties of both the mound and of the substrate baserock were revealed, analysis of which has been supported by three radiocarbon (AMS) measurements. The baserock formation during the last phase of the Ice Age, Middle and Upper Pleniglacial, and Late Glacial phases was followed by soil development in the Holocene, while the mound was constructed in two phases at the end of the Copper Age by the communities of the Pit Grave (Yamna or Ochre Grave) Culture. By publishing these preliminary data, it is also intended to draw attention to the need of focused research efforts by standardized methodology in kurgan research, in order to make the results of different studies consistent and comparable.

scholarly journals Exploring mobility in Italian Neolithic and Copper Age communities

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Flavio De Angelis ◽  
Maura Pellegrini ◽  
Cristina Martínez-Labarga ◽  
Laura Anzivino ◽  
Gabriele Scorrano ◽  
...  
Keyword(s):  
Bronze Age ◽  
Southern Italy ◽  
Sedentary Lifestyle ◽  
Human Mobility ◽  
The Body ◽  
Copper Age ◽  
Mobility Pattern ◽  
Oxygen And Carbon Isotope ◽  
Northern Areas

AbstractAs a means for investigating human mobility during late the Neolithic to the Copper Age in central and southern Italy, this study presents a novel dataset of enamel oxygen and carbon isotope values (δ18Oca and δ13Cca) from the carbonate fraction of biogenic apatite for one hundred and twenty-six individual teeth coming from two Neolithic and eight Copper Age communities. The measured δ18Oca values suggest a significant role of local sources in the water inputs to the body water, whereas δ13Cca values indicate food resources, principally based on C3 plants. Both δ13Cca and δ18Oca ranges vary substantially when samples are broken down into local populations. Statistically defined thresholds, accounting for intra-site variability, allow the identification of only a few outliers in the eight Copper Age communities, suggesting that sedentary lifestyle rather than extensive mobility characterized the investigated populations. This seems to be also typical of the two studied Neolithic communities. Overall, this research shows that the investigated periods in peninsular Italy differed in mobility pattern from the following Bronze Age communities from more northern areas.

scholarly journals Rock art and the prehistoric landscape of Galicia: the results of field survey 1992–1994

1995 ◽  
Vol 61 ◽  
pp. 347-370 ◽  
Author(s):  
Richard Bradley ◽  
Felipe Criado Boado ◽  
Ramón Fábregas Valcarce
Keyword(s):  
Bronze Age ◽  
Field Survey ◽  
Rock Art ◽  
Outer Edge ◽  
Early Bronze Age ◽  
Copper Age ◽  
North West ◽  
Abrupt Changes ◽  
Ground Conditions ◽  
The Relationship

This paper discusses the relationship between the earlier prehistoric pattern of settlement in Atlantic Europe and the creation of rock art. It investigates the organisation of the Copper Age and Early Bronze Age landscape of north-west Spain using the evidence provided by the distribution, siting, and composition of rock carvings. It presents the results of field survey in three sample areas extending from the centre to the outer edge of their distribution. Although these drawings cannot be interpreted as illustrations of daily life, they may have helped to define rights to particular resources in an area which experienced abrupt changes of ground conditions over the course of the year.

scholarly journals Emberi ábrázolás a Változások korában, 4000 és 2000 BC között

2014 ◽  
pp. 113-144
Author(s):  
Tünde Horváth
Keyword(s):  
Bronze Age ◽  
Middle Age ◽  
Late Phase ◽  
Early Bronze Age ◽  
Copper Age ◽  
Cultural Impacts ◽  
Middle Bronze Age ◽  
Archaeological Cultures ◽  
The Bronze Age

Our survey should by necessity begin earlier, from the close of the Middle Age Copper Age, and should extend to much later, at least until the onset of the Middle Bronze Age, in order to identify and analyse the appearance and spread of the cultural impacts affecting the Baden complex, their in-teraction with neighbouring cultures and, finally, their decline or transformation. Discussed here will be the archaeological cultures flourishing between 4200/4000 and 2200/2000 BC, from the late phase of the Middle Copper Age to its end (3600 BC), the Late Copper Age (ending in 2800 BC), the transi-tion between the Copper Age and the Bronze Age (ending in 2600 BC), and the Early Bronze Age 1–3 (ending in 2000 BC), which I have termed the Age of Transformation.

Holocene and latest Pleistocene fluctuations of Stutfield Glacier, Canadian Rockies

2001 ◽  
Vol 38 (8) ◽  
pp. 1141-1155 ◽  
Author(s):  
G D Osborn ◽  
B J Robinson ◽  
B H Luckman
Keyword(s):  
19Th Century ◽  
18Th Century ◽  
Late Glacial ◽  
Ice Age ◽  
Late 19Th Century ◽  
Canadian Rockies ◽  
The Holocene ◽  
The North ◽  
History Of ◽  
Glacier Advance

The Holocene and late glacial history of fluctuations of Stutfield Glacier are reconstructed using moraine stratigraphy, tephrochronology, and dendroglaciology. Stratigraphic sections in the lateral moraines contain tills from at least three glacier advances separated by volcanic tephras and paleosols. The oldest, pre-Mazama till is correlated with the Crowfoot Advance (dated elsewhere to be Younger Dryas equivalent). A Neoglacial till is found between the Mazama tephra and a paleosol developed on the Bridge River tephra. A log dating 2400 BP from the upper part of this till indicates that this glacier advance, correlated with the Peyto Advance, culminated shortly before deposition of the Bridge River tephra. Radiocarbon and tree-ring dates from overridden trees exposed in moraine sections indicate that the initial Cavell (Little Ice Age (LIA)) Advance overrode this paleosol and trees after A.D. 1271. Three subsequent phases of the Cavell Advance were dated by dendrochronology. The maximum glacier extent occurred in the mid-18th century, predating 1743 on the southern lateral, although ice still occupied and tilted a tree on the north lateral in 1758. Subsequent glacier advances occurred ca. 1800–1816 and in the late 19th century. The relative extent of the LIA advances at Stutfield differs from that of other major eastward flowing outlets of the Columbia Icefield, which have maxima in the mid–late 19th century. This is the first study from the Canadian Rockies to demonstrate that the large, morphologically simple, lateral moraines defining the LIA glacier limits are actually composite features, built up progressively (but discontinuously) over the Holocene and contain evidence of multiple Holocene- and Crowfoot-age glacier advances.

Revision of the Age of Construction Phases of a Mound Dated to the Late Copper–Early Bronze Age in Eastern Hungary Relying on14C-Based Chronologies

Radiocarbon ◽  
2018 ◽  
Vol 60 (5) ◽  
pp. 1403-1412
Author(s):  
Gábor Szilágyi ◽  
Pál Sümegi ◽  
Sándor Gulyás ◽  
Dávid Molnár
Keyword(s):  
Magnetic Susceptibility ◽  
Bronze Age ◽  
The Body ◽  
Early Bronze Age ◽  
Burial Mound ◽  
The Absolute ◽  
Geochemical Analyses

ABSTRACTEcse Mound is a burial mound in the Hortobágy region of eastern Hungary. Built by prehistoric nomadic peoples from the east, it now stands on the border between two modern settlements. The construction of the mound was assumed to be related to representatives of the Pit Grave Culture populating the area between the Late Copper and Bronze Ages. This theory considered similarities in shape, orientation, and stratigraphy of this mound with other absolute-dated ones in the Hortobágy region alone. The mound comprises two construction layers as indicated by magnetic susceptibility and on-site stratigraphic observations. According to detailed sedimentological, geochemical analyses of samples taken from the bedrock, artificial stratigraphic horizons, and the overlying topsoil, there is a marked similarity between the soil forming the body of the mound in both artificial horizons and the underlying bedrock soil. In contrast the pedological, geological character of the modern topsoil is utterly different. According to our dating results, the uppermost stratigraphic horizon is coeval with the absolute-dated mounds in the region, assigning it to the period of the Pit Grave Culture. However, the lower anthropological horizon is older and dates to between the Early and Late Copper Ages.

scholarly journals RADIOCARBON DATING THE 3RD MILLENNIUM BC IN THE CENTRAL BALKANS: A RE-EXAMINATION OF THE EARLY BRONZE AGE SEQUENCE

Radiocarbon ◽  
2020 ◽  
Vol 62 (5) ◽  
pp. 1163-1191
Author(s):  
Aleksandar Bulatović ◽  
Maja Gori ◽  
Marc Vander Linden
Keyword(s):  
Material Culture ◽  
Bronze Age ◽  
Pannonian Basin ◽  
The Body ◽  
Early Bronze Age ◽  
Cultural Groups ◽  
The Balkans ◽  
Funerary Architecture ◽  
Age Sequence ◽  
Funerary Treatment

ABSTRACTLong-standing archaeological narratives suggest that the 3rd millennium cal BC is a key period in Mediterranean and European prehistory, characterized by the development of extensive interaction networks. In the Balkans for instance, the identification of such interactions relies solely upon typological arguments associated with conflicting local terminologies. Through a combination of 25 new radiocarbon (14C) dates and re-examination of the existing documentation, this paper defines the absolute chronology for groups which were previously only broadly framed into the 3rd millennium BC central Balkans (modern-day Serbia and North Macedonia). These absolute dates allow us to establish with greater clarity the chronological relations between different cultural groups that represent the main cultural units of the central Balkans sequence for the 3rd millennium cal BC: Coţofeni-Kostolac, Bubanj-Hum II, Belotić-Bela Crkva, Armenochori, and Bubanj Hum III. When comparing together the chronologies for material culture, funerary treatment of the body, and funerary architecture, there are no easily discernible patterns. We observe instead a complex mix of traits criss-crossing over a wide area encompassing the Pannonian basin, the central Balkans and the Greek peninsula.

The extent, timing and palaeoclimatic significance of Late-glacial and Holocene snowpatches and glaciers in the Marrakech High Atlas, Morocco

2021 ◽  
Author(s):  
Benjamin Bell ◽  
Philip Hughes ◽  
William Fletcher ◽  
Roger Braithwaite ◽  
Henk Cornelissen ◽  
...  
Keyword(s):  
Little Ice Age ◽  
Late Glacial ◽  
Ice Age ◽  
High Atlas ◽  
The Holocene ◽  
Exposure Dating ◽  
Ground Water Recharge ◽  
Late Glacial And Holocene ◽  
High Level ◽  
Snow And Ice

<p>Pleistocene glaciers were extensive in the Marrakech High Atlas, Morocco. Today, semi-permanent snowpatches survive in topoclimatic settings and there is evidence of niche glaciers as recently as the Little Ice Age and early 20<sup>th</sup> Century. However, little is known about the state of permanent snow and niche glaciers through the Holocene. One hypothesis is that Little Ice Age glaciers were the largest snow and ice masses since the end of the Late-glacial (Younger Dryas 12.9-11.7 ka). Another possibility is that snow and ice expanded to similar or greater extents at other points in the Holocene.</p><p>To test these hypotheses, moraine boulders have been sampled on moraine successions in the highest parts of the High Atlas, including moraine successions in front of the névé permanent below the north-facing cliffs of Tazaghart (3890 m a.s.l.), a semi-permanent snowpatch that survives many summers today. This site is bounded by prominent moraine ridges with no soil development and no lichens on surface boulders. Several other high-level sites have been targeted and over 40 samples are currently being processed for <sup>10</sup>Be and <sup>36</sup>Cl exposure dating. Establishing the relative difference in extent and altitude of Late-glacial and the most recent glaciers in the High Atlas is important for understanding landscape and climate evolution in high mountain areas in the subtropics (31ºN).</p><p>The dated geomorphological records for late-lying snow and glaciers will be compared to high-resolution <sup>14</sup>C dated continuous parasequences from sediment cores from marshes at the Yagour Plateau and Oukaïmeden, both high-level sites in the High Atlas (~2700 m a.s.l.). The proximity of these sites (5-30 km, respectively) from the snowpatch/glacier sites will provide an important independent record of environmental change, spanning the Late-glacial and Holocene. This geomorphological record of former glaciers and snowpatches (moraines and pronival ramparts) is inherently fragmentary in time and the continuous core records from these alpine marshes will provide crucial insights into changing moisture conditions over time, which at these altitudes are closely related to the extent and volume of snowpack.</p><p>The climates associated with perennial snow cover and niche glaciers, and the associated annual snowpack melt, will be quantified using degree-day modelling. This allows melt rates to be predicted and this can be compared against observed modern climate in the High Atlas region. This involves interrogation of existing meteorological datasets from across the High Atlas and the development of algorithms for interpolation and extrapolation to ungauged higher altitudes.</p><p>Changes in the nature of the cryosphere through time in the High Atlas Mountains is crucial for understanding human activity and socioeconomic development in the wider region. Today, snowmelt from the High Atlas represents the most important ground water recharge used for a wide variety of purposes. Understanding changes in snow conditions, and as a consequence the behaviour of niche glaciers, in the High Atlas through the Holocene has important implications not only for water supply for humans but also for biological refugia and the evolution of cold-adapted flora and fauna.</p>

scholarly journals On the Curious Date of the Rylstone Log-Coffin Burial

2016 ◽  
Vol 82 ◽  
pp. 383-392 ◽  
Author(s):  
Nigel D. Melton ◽  
Janet Montgomery ◽  
Benjamin W. Roberts ◽  
Gordon Cook ◽  
Susanna Harris
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Western Europe ◽  
The Body ◽  
Early Bronze Age ◽  
Early Medieval ◽  
Extended Body ◽  
Radiocarbon Dates ◽  
The Bronze Age ◽  
Grave Goods

Radiocarbon dates have been obtained from a log-coffin burial excavated in 1864 by Canon William Greenwell from a ditched round barrow at Scale House, near Rylstone, North Yorkshire. The oak tree-trunk coffin had contained an extended body wrapped in a wool textile. The body had entirely decayed and there were no other extant grave goods. In the absence of other grave goods, Greenwell attributed the burial to the Bronze Age because it lay under a ditched round barrow and had similarities with log-coffin burials from Britain and Denmark. This attribution has not been questioned since 1864 despite a number of early medieval log-coffin burials subsequently being found in northern Britain. Crucially, the example excavated near Quernmore, Lancashire in 1973, was published as Bronze Age but subsequently radiocarbon dated to ad 430–970. The Rylstone coffin and textile were radiocarbon dated to confirm that the burial was Early Bronze Age and not an early medieval coffin inserted into an earlier funerary monument. Unexpectedly, the dates were neither Early Bronze Age nor early medieval but c. 800 bc, the cusp of the Bronze Age–Iron Age transition in Britain. The burial at Rylstone is, therefore, one of only two sites in Britain, and is unparalleled elsewhere in north-western Europe at a time when disposal of the dead was primarily through dispersed cremated or unburnt disarticulated remains.

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