Social Change and Land Use in Prehistoric Dalmatia

1993 ◽  
Vol 59 ◽  
pp. 61-104 ◽  
Author(s):  
John Chapman ◽  
Robert Shiel

The Neothermal Dalmatia Project is an Anglo-Yugoslav collaborative project whose aims are to define and explain changes in physical environment, settlement pattern and social structure in north Dalmatia over the last 12 millennia. The Project's fieldwork included archaeological field survey, analytical survey, trial excavation of Neolithic, Copper Age, Bronze Age, Iron Age and Roman sites, soil and land use mapping, ethnographic survey of modern villages and hamlets and palaeoenvironmental reconstructions (pollen, sediments, sea-level change, etc.). Within the long-term constraints of a limestone-dominated study region, the short-term events and medium-term agrarian and demographic cycles of the Dalmatian social groups have been studied in an inter-disciplinary manner. In this article, an attempt is made to examine the environmental and archaeological data within the frameworks of four explanatory models: the Land Use Capability (LUC) Model, the Cyclic Intensification–Deintensification (CID) Model, the Communal Ownership of Property (COP) Model and the Arenas of Social Power (ASP) Model. In the LUC model, reconstructions of past land use capabilities are used to derive postdictions of the most likely settlement patterns for successive periods (Neolithic–Roman); a high degree of postdictive success is met. In the CID model, Bintliff's model of cyclic variations in agricultural intensification and private land-holding is refined and tested against survey and excavation data. In the COP model, Fleming's model of communal land ownership is tested against similar data, with contrasting results. Finally, the ASP model is used to explain the expanded range of arenas of social power which develops from a place-based worldview in the early farming period. The conjoint use of these four explanatory models, which operate at different scales of duration, provides a broader basis for understanding changes in the prehistory of north Dalmatia in the Neothermal period than had previously been constructed.

2021 ◽  
Vol 6 ◽  
pp. v-v
Author(s):  
John Bintliff

Our latest volume maintains our goal to cover the broad chronological spread of Greek Archaeology, ranging from a new review of the Mesolithic occupation at Theopetra, one of the most important hunter-gatherer sites in Greece, to a detailed analysis of how the distribution of Middle Byzantine churches in the Peloponnese enlightens us into the evolution of human settlement and land use. Prehistory is richly represented in further articles, as we learn about Middle Bronze Age society on Lefkas, the dispute over exotic primates portrayed on the frescoes of Santorini, a new Minoan-style peak sanctuary on Naxos, and Post-Palatial settlement structure on Crete. Bridging prehistory to historical times, a detailed study rethinks the burial and settlement evidence for Early Iron Age Athens, then entering the Archaic period, an original article links textual analysis and material culture to investigate dedicatory behaviour in Ionian sanctuaries. As a special treat, that doyen of Greek plastic arts Andrew Stewart, asks us to look again at the evidence for the birth of the Classical Style in Greek sculpture. Greek theatres in Sicily are next contextualised into contemporary politics, while the sacred Classical landscape of the island of Salamis is explored with innovative GIS-techniques. For the seven-hundred years or so of Roman rule we are given an indepth presentation of regional economics from Central Greece, and a thorough review of harbours and maritime navigation for Late Roman Crete. Finally we must mention a methodological article, deploying the rich data from the Nemea landscape survey, to tackle issues of changing land use and the sometimes controversial topic of ancient manuring.


The Holocene ◽  
2019 ◽  
Vol 29 (4) ◽  
pp. 543-564 ◽  
Author(s):  
Renata Kołodyńska-Gawrysiak

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.


2021 ◽  
Author(s):  
Valentí Rull ◽  
Teresa Vegas-Vilarrúbia ◽  
Juan Pablo Corella ◽  
Mari C. Trapote ◽  
Encarni Montoya ◽  
...  

The Pyrenean Lake Montcortès sediments hold the longest continuous and absolutely varve-dated record of the Mediterranean region, encompassing the last three millennia, from the Late Bronze Age to the present. The reconstruction of vegetation and landscape dynamics during this time period has advanced gradually, following the progress of absolute dating by varve counting, and has been progressively published and updated in a number of papers dealing with specific time intervals at different temporal resolutions. This paper synthesizes all these studies in a single composite paleoecological sequence constrained by a single age-depth varve model. The final resolution of this reconstruction is bidecadal, on average, but some periods have been resolved at quasidecadal (Middle Ages) and subdecadal (Modern Age to present) resolutions. The study is focused on the timing of anthropization and the further development of vegetation under climatic and anthropogenic drivers until the shaping of present landscapes. An additional advantage of Montcortès is that the local history of the Pallars region, where the lake is located, is well documented and can be easily correlated with the paleoecological record. Contrary to former interpretations of general landscape anthropization of the Pyrenees during the Middle Ages, the Montcortès catchment was irreversibly transformed by anthropic activities at the beginning of the Iron Age (ca. 750-650 BCE). From this point, the catchment underwent successive transformations due to varied human uses (fire, grazing, cereal cultivation, weed/ruderal plant expansions, hemp cultivation/retting), which have been related to the different cultural phases and sociopolitical changes documented in the local historical records. The regional forests, dominated by Pinus and Quercus, experienced four main clearance events (RD) during the Iron Age (RD1; ca. 300 BCE), the Roman Period (RD2; ca. 300 CE), the Middle Ages (RD3; ca. 1000 CE) and the Modern Age (RD4; ca. 1800 CE). The detailed trends of the last two deforestation events and their causes could be studied at a decadal resolution, which significantly improved interpretation quality in ecological terms. The potential effects of climatic changes and the eventual interactions with human activities on catchment vegetation and regional forests throughout the record have also been discussed. The Montcortès record has been compared with other records at local (Pyrenees), regional (Iberian Peninsula) and biome (Mediterranean) scales. Locally and regionally, anthropization times and further ecological trends showed significant heterogeneity according to elevation, biogeographical patterns and cultural trends. The most significant coincidence is an intensification of human pressure, as noted in forest clearing and extensive land use, during several phases of the Middle Ages. At the Mediterranean level, the Montcortès record emerges as a unique sequence for the western sector of this biome that should be complemented with similar archives from the central and eastern Mediterranean. The most promising candidates for such sequences are discussed on the basis of available Mediterranean varved records.


2021 ◽  
Vol 13 (12) ◽  
Author(s):  
Knut Kaiser ◽  
Johann Friedrich Tolksdorf ◽  
Anna Maartje de Boer ◽  
Christoph Herbig ◽  
Falk Hieke ◽  
...  

AbstractColluvial sediments originating from soil erosion on slopes have proven to constitute significant evidence for tracing past human impact on mountain landscapes. In the Central European Erzgebirge (Ore) Mountains, colluvial sediments are associated with specific landforms (footslopes, slope flattenings, dells) and cover a share of 11% (11,905 ha) of the regional soil landscape. Thirteen pedosedimentary sections with colluvial layers were investigated at five forested sites (520–730 m a.s.l.) within a context of mining archaeology, integrating data from pedology, archaeology, palaeobotany, and geochronology. The thickness of the gravel-bearing loamy, silty, and sandy colluvial layers is up to 70 cm, which are mostly located on top of the sections. The geochronological ages and archaeological data reveal a high to late medieval to post-medieval age of the colluvial sediments. Pollen data show a drastic decline of the mountain forests in the late twelfth to fifteenth centuries AD accompanied by an increase of pioneer trees and spruce at the expense of fir and beech. The primary cause of soil erosion and subsequent colluvial deposition at the sites investigated is medieval to post-medieval mining and other early industrial activities. A compilation of 395 radiocarbon and OSL ages, obtained from colluvial sediments at 197 upland sites in Central Europe, shows that anthropogenically initiated colluvial dynamics go as far back as the late Bronze Age to the early Iron Age. Most ages derive from the medieval to post-medieval period, corresponding to the general intensification of settlement and land-use activities including deforestation and widespread ore mining.


1983 ◽  
Vol 10 (1) ◽  
pp. 41-71 ◽  
Author(s):  
G J Barclay

SUMMARY Myrehead has revealed the eroded remnants of activity from the Beaker period (Period A) onwards, with actual settlement evinced only from about the early first millennium be. The three houses and the cooking pits of Period B may have been constructed and used sequentially. This open settlement was probably replaced during the mid first millennium bc, possibly without a break, by a palisaded enclosure (Period C), which may have contained a ring-groove house and a four-post structure. Continued domestic activity (Period D) was suggested by a single pit outside the enclosure, dated to the late first millennium bc/early first millennium ad. The limited evidence of the economy of the settlements suggests a mixed farming system.


2015 ◽  
Author(s):  
Sheila Grecian ◽  
Safwaan Adam ◽  
Akheel Syed
Keyword(s):  
Iron Age ◽  

Author(s):  
John K. Papadopoulos

This paper begins with an overview of the bronze headbands from the prehistoric (Late Bronze to Early Iron Age) burial tumulus of Lofkënd in Albania, which were found among the richest tombs of the cemetery, all of them of young females or children. It is argued that these individuals represent a class of the special dead, those who have not attained a critical rite de passage: marriage. In their funerary attire these individuals go to the grave as brides, married to death. The significance of the Lofkënd headbands is reviewed, as is their shape and decoration, but it is their context that contributes to a better understanding of Aegean examples, including the many bronze, gold, and silver headbands found in tombs from the Early Bronze Age through the Early Iron Age, as well as those dedicated as votive offerings in sanctuaries. In addition to discussing the evidence for headbands in the Aegean and much of southeast Europe, this paper also attempts to uncover the word used in this early period in Greece for these distinctive items of personal ornament. In memory of Berit Wells.


2020 ◽  
Author(s):  
Cezary Namirski

The book is a study of the Bronze Age and Early Iron Age Nuragic settlement dynamics in two selected areas of the east coast Sardinia, placing them in a wider context of Central Mediterranean prehistory. Among the main issues addressed are the relationship between settlement and ritual sites, the use of coastline, and a chronology of settlement.


Sign in / Sign up

Export Citation Format

Share Document