History of the Environment and Population of the Old Town of Klaipėda, Western Lithuania

Multidisciplinary Approach to the Last Millennium

Bibliographic Data

ID9244604
AuthorsDalia Kisielienė (0000-0003-2756-444X), Ieva Masiulienė (0000-0001-7405-6646), Linas Daugnora (0000-0001-6267-9467), Miglė Stančikaitė (0000-0001-9425-5634), Jonas Mažeika (0000-0003-1168-5394), Giedrė Vaikutienė (0009-0008-5342-4700), Rimantas Petrošius
Year2012
Volume54
Issue3-4
Pages1003-1015
Publication date2012-01-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueRadiocarbon (JOURNAL)
Journal identifiersISSN: 0033-8222 • E-ISSN: 1945-5755
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s0033822200047639
OpenAlexW1863617108
LanguageEN
Citations received5
References cited8

Progressive stages in the development of the Old Town region of the city of Klaipėda (in German, Memel ) were ascertained by analyzing archaeological and historical data combined with an analysis of pollen, diatom, plant macrofossil, and osteological findings as cross-referenced with radiocarbon measurements. The port city of Klaipėda, located on the eastern part of the Baltic Sea, was an important political, economic, and religious center during the last millennium. In addition to its environmental history, the character of human activity and urbanization of the area during the 16th–17th centuries AD were examined. The chronology of these records is based on archaeological, historical, and 14 C data. The results obtained indicate the predominance of a wet boggy environment and the presence of a pond in the investigated territory of Klaipėda during the late 15th and early 16th centuries AD. The formation of a new Danė River channel created an island town, resulting in a defensible residual area for the town inhabitants. An ongoing deposition of a cultural layer began in the mid-16th century AD. Rich zooarchaeological data found in this layer provided new details on human diet and exposed a predominance of domestic animals, especially cattle. Due to intensive amelioration of this area, layers of sandy and clayey deposits were formed during the second half of the 16th century AD. A significant presence of cultivars, ruderals, and weeds were recorded, indicating substantial human activity and increasing urbanization of the landscape. According to the paleobotanical, archaeological, and historical data, the culmination of this process took place at the end of the 16th and beginning of the 17th centuries AD, when residential areas were established

Archaeology · Geography · Holocene · Human settlement · Macrofossil · Population · Radiocarbon dating · Urbanization · Ancient Mediterranean Archaeology and History · Archaeology and ancient environmental studies · Demography · Historical and Archaeological Studies · Ecology