Use this URL to cite or link to this record in EThOS: https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.749860
Title: Environmental change in deltaic settings and the emergence of civilsation
Author: Pennington, Benjamin Thomas
ISNI:       0000 0004 7234 3141
Awarding Body: University of Southampton
Current Institution: University of Southampton
Date of Award: 2018
Availability of Full Text:
Access from EThOS:
Full text unavailable from EThOS. Please try the link below.
Access from Institution:
Abstract:
During the mid-Holocene, some of the world's first large-scale complex societies came into being within the lower and middle reaches of a number of large river systems. Around this time, as global sea-level stabilised, the hosting fluvial environments of Lower Mesopotamia, the Nile Delta and the North China Plain were evolving from spatially varied landscapes dominated by swampy marshland, to better-drained, more uniform floodplain environments. It is necessary to consider whether such environmental changes could have guided aspects of sociocultural evolution in these settings In the Nile Delta, the setting for which most data are available, these palaeolandscape changes are comprehensively mapped through the construction of a four-dimensional aggradation model of the Holocene alluvial plain. Development of this model takes place within the context of a full reinterpretation of the Upper Quaternary stratigraphy of the Nile Delta, which is itself further informed by substantial programmes of fieldwork in the western delta. The environmental changes were forced by a decrease in the rate of relative sea-level rise within the context of decreased discharge and sediment-supply due to regional climate change. A geoarchaeological model links these changes in the landscape to sociocultural developments taking place in Egypt between 5500 and 2500 BC. Increased adoption of agricultural practices in the delta was stimulated by a decrease in the primary productivity of the landscape, which then led to population growth and shifts in settlement styles. The emergence of the first Egyptian capital of Memphis at the delta apex can also be seen as having been facilitated by changes in the palaeogeography of the fluvio-deltaic environment. Such linkages between the changing deltaic landscapes and social change are crucial in understanding the formation of the Ancient Egyptian State (c. 3100 BC), which involved increased involvement of regional elites using the delta as both an agricultural resource and trade route.
Supervisor: Sturt, Fraser Sponsor: Not available
Qualification Name: Thesis (Ph.D.) Qualification Level: Doctoral
EThOS ID: uk.bl.ethos.749860  DOI: Not available
Share: