scholarly journals Fishery in the Tobol-Ishim interfluve in the neolithic and early metal age

2018 ◽  
Vol 7 (4) ◽  
pp. 182-192
Author(s):  
Viktor Alekseevich Zakh

Landscapes of the Tobol-Ishim interfluve were not stable in the Holocene and varied from forests and drowned floodplains at the beginning of the V and III millennia BC to steppificated territories with a lowered water level at the beginning of the Atlantic Period and in the middle of the Subboreal Period, which determined the main types of economic activities, one of them was fishing. Changes in hydrological regime of water bodies influenced the methods of fishing, including the use of different traps. Thus, in the Neolithic, when the water level decreased, the location of settlements in the system river-creek-lake (for example, Mergen 6), a large number of fish bones, bone harpoons, fishing spears, fishing tackles for catching pike and a total absence of plummets were indicative of individual fishing for large fish and, perhaps, of stop net fishery, which was facilitated by a decrease in the width of watercourses and tombolos. Stop net (stake net) fishery led to a settled lifestyle of the population, collective activities and the emergence of long-term settlements with deep foundation pits of dwellings. When the water level in rivers and lakes increased and floods became more frequent, the life support system changed, the population began to develop coasts more widely, its mobility increased, and they started to build framed above-ground dwellings. Following those changes, biconic, cigar-shaped, and corniculate plummets emerged in the Tobol River Basin and on the adjacent western and north-western territories in the III and early II millennium BC. When the water level was high, it was efficient to fish using traps, seines and, probably, nets, although the latter could also be used in drive hunting for shedding geese and ducks. Subrectangular plummets with one or two ties for fastening, and disk-shaped plummets with a tie in the center had been prevailing since the beginning of the II millennium BC; they existed until the first third of the I millennium BC. This period, the transition time from the Bronze Age to the Early Iron Age, is characterized by the absence of clay plummets, while there are large accumulations of fish scales and bones in the settlement layers. We can suppose that the population of that time (local Late Bronze Age population, mixed with northern migrants who made utensils with cross ornamentation) switched from net fishing to stop net fishing.

Author(s):  
Joakim Goldhahn

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.


2007 ◽  
Vol 2 (2) ◽  
pp. 161-175 ◽  
Author(s):  
Kristian Kristiansen

In this article I examine how long-term economic strategies in the Bronze Age of northern Europe between 2300 and 500 BCE transformed the environment and thus created and imposed new ecological constraints that finally led to a major social transformation and a "dark age" that became the start of the new long-term cycle of the Iron Age. During the last 30 years hundreds of well-excavated farmsteads and houses from south Scandinavia have made it possible to reconstruct the size and the structure of settlement and individual households through time. During the same period numerous pollen diagrams have established the history of vegetation and environmental changes. I will therefore use the size of individual households or farmsteads as a parameter of economic strength, and to this I add the role of metal as a triggering factor in the economy, especially after 1700 BCE when a full-scale bronze technology was adopted and after 500 BCE when it was replaced by iron as the dominant metal. A major theoretical concern is the relationships between micro- and macroeconomic changes and how they articulated in economic practices. Finally the nature of the "dark age" during the beginning of the Iron Age will be discussed, referring to Sing Chew's use of the concept (Chew 2006).


2017 ◽  
Vol 14 (1) ◽  
pp. 130-138
Author(s):  
Ioana-Iulia Olaru
Keyword(s):  
Iron Age ◽  

Abstract The present paper will refer to an aspect of processing metals on the territory of Romania, in Bronze Age and Iron Age (the second age habing been studied up to the moment when Prehistory ended: 1st century B.C., being continued by Antiquity). Unfortunately, few pieces were found in settlements and in necropoleis, so it is difficult to attribute the artifacts of the Metal Age to one or other of the existing cultures, though the region where they were produced can be mentioned. Consequently, their study can lead to another classification than the chronological one, and that is of the field of ornamental arts in metal. We will focus only on two types of objects that embellish the neck and the chest: necklaces and pendants, which help us create a vivid image of this important artistic field of the Iron Age on the territory of our country, these two joining the other important types of jewels: bracelets, rings, fibulae, phaleras.


AmS-Varia ◽  
2020 ◽  
pp. 77-86
Author(s):  
Marianne Lönn

This article discusses the meaning of stones and the practice of gathering stones, in graves, clearance cairns and stone-covered hillocks. The emphases are on stone-covered hillocks and their long-term usage (up to 1500 years), analyzed using the concept of longue durée. In this paper I propose that the stones in themselves have a cultic meaning as well as the actions, i.e. the remodeling of hillocks and the placing of clearance cairns among graves. In this, I see a connection between stone-covered hillocks, graves and clearance cairns. The underlying concept is a stable, but slowly changing, prehistoric religious tradition that lasted from the Bronze Age to the Migration Period and possibly also through the Late Iron Age. A basic change in this does not take place until the coming of Christianity in the Medieval Period. The reason that Medieval and later clearance cairns were placed together with graves is probably due to their similar appearance.


1987 ◽  
Vol 53 (1) ◽  
pp. 351-362 ◽  
Author(s):  
Richard Bradley

Some recent literature on the problem of hoards is reviewed, dealing particularly with the distinction between votive deposits and stores of objects. An alternative approach is developed, considering the long-term variations in the nature of intentional deposits in European prehistory. Three stages are suggested. In the initial stage, a unitary system of deposits prevailed, especially of food and selected artefacts, including metal when available. In the developed stage, characteristic of the Bronze Age, a dual system allowed both votive deposition and accumulation and recycling, especially of non-local metal. The final stage, in the later Iron Age, saw renewed emphasis on votive deposits, especially on the borders of emerging polities.


2022 ◽  
Vol 49 (4) ◽  
pp. 37-42
Author(s):  
A. P. Borodovsky

Handles of Early Iron Age bronze cauldrons from southwestern Siberia are described with reference to their ritual meaning. Typological features, such as knobs, arcuate, or square shape, are relevant for dating. Two chronological groups are established: the Tagar (second half of the 1st millennium BC) and Xiongnu-Xianbei (late 1st millennium BC to early 1st millennium AD). The interpretation of handles depends on the context. At settlements (Turunovka-4) and in certain hoards (First Dzhirim) of the Late Bronze Age, they can belong to foundry scrap. However, handles occur in long-term ritual sites such as Aidashenskaya Cave, suggesting a different interpretation. Indeed, at Eastern European forest-steppe sites of the Xiongnu era, handles of cauldrons had been intentionally buried, most often near water sources, where the summer camps of nomadic herders were situated. A similar situation is observed in southwestern Siberia, from the Baraba forest-steppe to the Middle Yenisei valley.


Author(s):  
Elga Apsīte ◽  
Mārtiņš Kriķītis ◽  
Inese Latkovska ◽  
Andrejs Zubaničs

Changes in the hydrological regime of the lakes of Latvia have been caused by several natural and human factors. This publication summarises the results of research on the long-term and seasonal changes in the water level, and thermal and ice regimes of the three biggest lakes of Latvia (Usma, Burtnieks, and Râzna) and their regional features in the period from 1926 to 2002. The levels of the lakes Usma and Râzna have been controlled, but it can be considered that changes of the water level in Lake Burtnieks have been due to the impact of natural factors during the period from 1947 to 2002. Global climate warming has caused considerable changes in the hydrological regime of the lakes during the last decades, as the water level and temperature have increased and the number of days with ice cover and the thickness of ice have decreased. A positive trend in the freezing data and statistically reliable negative trend for the ice break-up date were observed for all the lakes. Lake Usma is located in the western part of Latvia, therefore, its hydrological regime, in particular, the thermal and ice regime, differs from those of lakes Burtnieks and Râzna which are located in the northern and eastern part of Latvia, respectively.


1985 ◽  
Vol 24 (1) ◽  
pp. 87-102 ◽  
Author(s):  
Antony G. Brown ◽  
Keith E. Barber

A variety of paleoecological and sedimentary techniques were used to investigate the storage of sediment within a small lowland catchment during the Holocene. Radiocarbon dating of vertically accreted floodplain deposits allowed the calculation of inorganic accumulation rates. These rates show a dramatic increase in sediment deposition during the late Bronze Age and early Iron Age (2900-2300 yr B.P.) due to deforestation and cultivation of the catchment slopes and resultant soil erosion. The soils within the catchment were susceptible to structural damage, surface waterlogging, and slope-wash erosion. From the calculated increases in sediment storage estimates of catchment erosion were made which vary from around 20 to 140 tons km−2 yr−1. The study of alluvial chronology at this scale can provide unique information on the source areas of Holocene floodplain sediments and provide long-term erosion rates.


Radiocarbon ◽  
2017 ◽  
Vol 59 (6) ◽  
pp. 1645-1656
Author(s):  
Guy De Mulder ◽  
Mark Van Strydonck ◽  
Mathieu Boudin ◽  
Ignace Bourgeois

ABSTRACTRecently a cremation cemetery was excavated at the site of Wijnegem where 29 cremation graves and 9 funerary monuments were uncovered. Thirty radiocarbon (14C) dates were carried out, mostly on cremated bone but also 10 charcoal samples were dated. Twenty-four cremations were studied. Four ring ditches were dated by charcoal samples from the infill of the ditch. The 14C dates showed an interesting long-term occupation of the cemetery. Different phases were ascertained. The history of the cemetery starts in the northern part of the site around a circular funerary monument. Two cremations were dated at the transition of the Early to Middle Bronze Ages. Two other graves represent the transition from the Middle to the Late Bronze Ages. The main occupation period dates between the end of the Late Bronze Age and the Early Iron Age. Finally, an isolated cremation grave marks the definite abandonment of the site during the Late Iron Age.


1997 ◽  
Vol 24 (1) ◽  
pp. 3-4 ◽  
Author(s):  
FAUSTO O. SARMIENTO

In the era of space travel, ecology has continued to gain relevance as the science of the ‘spaceship Earth’. In this context, it can be said to have a mission, which is to understand the complex network of the life-support systems that keep biospheric processes operating in a way suitable to sustaining living organisms and their environment (Odum & Sarmiento 1997). With the realization that ecology, in the broad sense, provides the means to understand the mechanics of nature, scholars are using ecological understanding at the interfaces of disciplines to: (1) prevent and reverse the demise of biodiversity in marine and terrestrial ecoregions (conservation biology), (2) reduce impacts of population pressure on the resource base of people (ecological anthropology), (3) establish more parsimonious economic activities to ensure optimum yields for the long term (ecological economics), (4) plan for an appropriately-equitable and socially-integrative sustainable development (environmental design), (5) restore degraded ecosystems and landscapes (restoration ecology), and (6) model hypothetical future scenarios where predictions from ecological theory may prove valuable for the future of mankind (environmental planning).


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