Did prehistoric landscape management retard the post-glacial spread of woodland in Southwest Asia?

Antiquity ◽  
2002 ◽  
Vol 76 (294) ◽  
pp. 1002-1010 ◽  
Author(s):  
Neil Roberts

Pre-Bronze Age human impacts on the East Mediterranean environment have been hard to detect in pollen diagrams and other off-site contexts. New evidence shows that despite a relatively rapid post-glacial wetting-up of the climate, the re-advance of oak woodland across Southwest Asia was slow. Among the factors likely to have contributed to the apparent disjunction between climate and vegetation is Neolithic landscape management, particularly through regular use of late-season ground fires to encourage grasses at the expense of trees and shrubs.

The Holocene ◽  
2017 ◽  
Vol 27 (8) ◽  
pp. 1078-1091 ◽  
Author(s):  
Lorna O’Donnell

Swathes of roads and pipelines cut through the Irish landscape during the ‘Celtic Tiger’ years (approximately 1994–2008) leading to an unprecedented number of archaeological excavations and creating a unique opportunity for extensive research of past landscapes on a broad scale. The vast quantities of bulk soil samples suddenly available necessitated the development and adaptation of new methodologies. Despite the huge volumes of these samples, of which charcoal is the most ubiquitous ecofact, to date charcoal analysis has been considerably under-utilised in the study of past Irish woodlands. This research presents one of the largest Bronze Age archaeological charcoal datasets in Europe. It provides new palaeoecological evidence contributing to the understanding of woodland cover transformation on the island of Ireland during the late-Holocene period. The most common taxa identified in the charcoal assemblage compare well with regional pollen diagrams, particularly the use of Quercus and Corylus. With intensifying human activity during the middle Bronze Age, the proportion of Maloideae, a light demanding family rose. This is the first clear evidence of anthropogenic influence during the middle Bronze Age in Ireland derived from archaeological charcoal. The size of the charcoal dataset makes it possible to evaluate woodland cover and resourcing from two perspectives – both archaeological and palaeoecological.


Sixteen sites in and around a small upland bog in South Wales were investigated by means of pollen analysis and radiocarbon dating. Most of the sites have ombrogenous (blanket) peat overlying a thin basal mor with abundant charcoal. A Devensian Late-glacial basin filled with muds and reedswamp deposits is shown to underlie the blanket peat in part of the area. It is concluded that the outlet of the basin was probably blocked by the development of ombrogenous peat, perhaps around 6500 years BP (though not closely dated), which spread across the basin and later up its western shore. The pollen diagrams are divided into a series of pollen assemblage zones. The zone boundaries appear synchronous within the limits of the methods. Hazel played an important role in the woodland vegetation of the pre-peat mineral soils. This woodland had generally been replaced by heath and blanket peat by about 6000 years BP. Nevertheless, some woodland apparently persisted locally in areas where peat or mor accumulation had not yet begun. Alder appears to have been established in the basin area by ca . 7000 years BP and to have spread more widely some 500—1000 years later, possibly taking advantage of environmental damage caused by Mesolithic man, evidence of whose occupation is found in the area. It is concluded that Mesolithic man was probably responsible for making a small clearing in the woodland at ca . 8000 years BP when the first mor deposit began to accumulate. Heath vegetation first came into existence at about this time and there is circumstantial evidence of maintenance by burning. Heath conditions lasted in some areas until ca . 5500 years BP and on the more permeable soils podsolization took place. It is argued that the accumulation of relatively impermeable mor soils under heath was a major factor in the initiation of ombrogenous peat growth. This most generally began in the period ca . 5500-5800 years BP though it was both earlier ( ca . 7600 years BP) and later ( ca . 4000 years BP) in some areas. A comparison is made of the behaviour of certain pollen curves at the major sites in which it is found that sites with common features fall into spatially coherent groups. It is concluded, therefore, that the pollen diagrams often reflect vegetational changes taking place in relatively small areas. A reconstruction of the vegetational changes in the 4000 years after ca . 8000 years BP is made by means of a series of maps. The classical elm decline of the Atlantic-Sub-boreal transition ( ca . 5000-5500 years BP) is variably represented and there follows a series of three other declines or minima dated to ca . 4600 years BP, ca . 4000 years BP and ca . 2850 years BP (though again with some possible variability). The Bronze Age appears to have been a time of major human impacts on the local vegetation with some woodland regeneration taking place in the earlier Iron Age before a renewed period of clearance that persisted through Romano-British times.


2002 ◽  
Vol 97 ◽  
pp. 97-162 ◽  
Author(s):  
Sturt W. Manning ◽  
David A. Sewell ◽  
Ellen Herscher

The period from the late Middle Bronze Age to the start of the Late Bronze Age in the Levant, largely coeval with the Canaanite, ‘Hyksos“, 15th Dynasty of Egypt, is characterized by the appearance of Late Cypriot I A ceramics at a number of key sites in the east Mediterranean. The exact absolute dates to apply to this period have been the subject of controversy, in part inter-linked with debate over the date of the eruption of Thera, but scholarship recognises that this visible horizon of international trade must have been of considerable significance, especially on Cyprus itself. Here a dramatic shift in settlement to the coastal areas of the island at the beginning of the Late Cypriot period has long been recognized; this is also the time period of the formation of larger complex socio-political entities at the sites on Cyprus which go on to comprise the Late Cypriot ‘urban“ civilisation. Tombs of the relevant Middle Cypriot III–Late Cypriot I period are well known on Cyprus, but stratified settlement contexts on Cyprus, yet alone contexts directly related to such international trade, are scarce to non-existent. We report finds of just such direct relevance from a (currently) unique deposit as a result of an initial investigation of the seabed off the Late Cypriot site of MaroniTsaroukkason the south coast of Cyprus (MTSB Site 1). Consideration of these finds provides important new evidence for the Late Cypriot I A period; they also indicate routes to more sophisticated analyses of Cypriot–east Mediterranean interaction and the resolution of current problems in chronology. In particular, a review of Late Cypriot I A connections highlights the need to emphasise the central importance of the Canaanite pre-18th Dynasty (late Middle Bronze Age) world to the formative development of both Late Bronze Age Cyprus, and the Late Bronze Age Aegean.


Author(s):  
David Kaniewski ◽  
Elise Van Campo

The collapse of Bronze Age civilizations in the Aegean, southwest Asia, and the eastern Mediterranean 3200 years ago remains a persistent riddle in Eastern Mediterranean archaeology, as both archaeologists and historians believe the event was violent, sudden, and culturally disruptive. In the first phase of this period, many cities between Pylos and Gaza were destroyed violently and often left unoccupied thereafter. The palace economy of the Aegean Region and Anatolia that characterized the Late Bronze Age was replaced by the isolated village cultures of the Dark Ages. Earthquakes, attacks of the Sea Peoples, and socio-political unrest are among the most frequently suggested causes for this phenomenon. However, while climate change has long been considered a potential prime factor in this crisis, only recent studies have pinpointed the megadrought behind the collapse. An abrupt climate shift seems to have caused, or hastened, the fall of the Late Bronze Age world by sparking political and economic turmoil, migrations, and famines. The entirety of the megadrought’s effects terminated the Late Bronze Age in the eastern Mediterranean.


2020 ◽  
Vol 95 (1) ◽  
pp. 187-204
Author(s):  
Serena Sabatini

AbstractArguing for an integrated wool-textile economy in the Bronze Age, this paper assesses characteristics and scale of pastoral economy and sheepherding at the Terramare settlement of Montale (Modena province, Italy). Previous studies argued that Montale was a Bronze Age centre of wool production. The present work enhances the understanding of the local textile economy by investigating the evidence for sheepherding and landscape management at the site. It also proposes an interdisciplinary-based approach to investigate and reconstruct pastoral economy and sheepherding strategies in other prehistoric contexts as well.


The Holocene ◽  
2019 ◽  
Vol 29 (4) ◽  
pp. 633-647 ◽  
Author(s):  
Jan Sevink ◽  
Corrie C Bakels ◽  
Peter AJ Attema ◽  
Mauro A Di Vito ◽  
Ilenia Arienzo

Earlier studies on Holocene fills of upland lakes (Lago Forano and Fontana Manca) in northern Calabria, Italy, showed that these hold important palaeoecological archives, which however remained poorly dated. Their time frame is improved by new 14C dates on plant remains from new cores. Existing pollen data are reinterpreted, using this new time frame. Two early forest decline phases are distinguished. The earliest is linked to the 4.2 kyr BP climatic event, when climate became distinctly drier, other than at Lago Trifoglietti on the wetter Tyrrhenian side, where this event is less prominent. The second is attributed to human impacts and is linked to middle-Bronze Age mobile pastoralism. At Fontana Manca (c. 1000 m a.s.l.), it started around 1700 BC, in the higher uplands a few centuries later (Lago Forano, c. 1500 m a.s.l.). In the Fontana Manca fill, a thin tephra layer occurs, which appears to result from the AP2 event (Vesuvius, c. 1700 BC). A third, major degradation phase dates from the Roman period. Land use and its impacts, as inferred from the regional archaeological record for the Raganello catchment, are confronted with the impacts deduced from the palaeoarchives.


2007 ◽  
Vol 102 ◽  
pp. 219-238 ◽  
Author(s):  
Cyprian Broodbank ◽  
Thilo Rehren ◽  
Antonia-Maria Zianni

Scientific analysis of samples takes from metal objects and metallurgical products excavated during the 1960s at Kastri on Kythera provide new evidence concerning, variously, the Aegean metals trade and metallurgy on Kythera. The samples date to the Second Palace (Neopalatial), Classical and Late Roman periods. The Bronze Age material comprises fragments of copper ingots and silver cups, neither of which metal is locally available in Kythera, and the later material relates largely to local smelting and possibly smithing of iron, whose origin is uncertain. These activities are related to preliminary information concerning the distribution at each period of metallurgical activity across the island that has been generated by the intensive surface survey of the Kythera Island Project.


1972 ◽  
Vol 22 ◽  
pp. 115-128 ◽  
Author(s):  
John Evans

Following their discovery of the “Burnt Palace” at Beycesultan in the mid 1950's, Seton Lloyd and James Mellaart drew attention to a number of features of its architecture which seemed to indicate links with the palace architecture of Minoan Crete, and discussed the possible significance of these similarities (Lloyd and Mellaart, 1956 118–123, 1965 61, 62). Whatever this may be in terms of relationships between the two areas in the second millennium B.C., however, it seems clear that they cannot throw any light on the first appearance of palaces in Crete. The problems of the origin and development of the Cretan Bronze Age palaces are complex, and though they have been much discussed since the first excavations in the early years of the century, a major obstacle to progress has always been the lack of precise evidence, or even of any evidence at all, for the early stages of the process. As they stand, most of the palaces are the product of a series of rebuildings and remodellings over a long period, and it is not always clear just what they were like when first erected. Most frustrating of all, however, is the lack of evidence bearing on the question of whether they were preceded, during the Early Bronze Age, by buildings which were in any respect analogous in form and function. It has long been clear that the sites of some of the major Middle and Late Minoan palaces were occupied during the Early Minoan period, but at Phaistos and Knossos at any rate extensive clearing and levelling in preparation for the erection of the Middle Minoan palaces has obliterated practically all traces of the Early Minoan buildings. At Phaistos Branigan has hinted that the fragments of walls found by Pernier (1935, pl. VI) on the highest point of the hill might have belonged to a building of some consequence, possibly similar to the Early Minoan II mansion known as the House on the Hill at Vasiliki (Branigan 1970, p. 41). Branigan thinks that in addition to the rooms mentioned by Pernier, there may be traces of a corridor similar to that in the Vasiliki building. Only the bottom two courses of the walls survive, so that it is difficult to say much about their construction, though it seems to be poorer than that of the walls of some Early Minoan private houses later found by Levi on another part of the site.


Starinar ◽  
2016 ◽  
pp. 173-191
Author(s):  
Aleksandar Kapuran ◽  
Dragana Zivkovic ◽  
Nada Strbac

The last three years of archaeological investigations at the site Ru`ana in Banjsko Polje, in the immediate vicinity of Bor, have provided new evidence regarding the role of non-ferrous metallurgy in the economy of the prehistoric communities of north-eastern Serbia. The remains of metallurgical furnaces and a large amount of metallic slags at two neighbouring sites in the mentioned settlement reveal that locations with many installations for the thermal processing of copper ore existed in the Bronze Age. We believe, judging by the finds of material culture, that metallurgical activities in this area also continued into the Iron Age and, possibly, into the 4th century AD.


Sign in / Sign up

Export Citation Format

Share Document