We describe a combination of methods applied to obtain reliable estimations of population density using archaeological data. The combination is based on a hierarchical model of scale levels. The necessary data and methods used to obtain the results are chosen so as to define transfer functions from one scale level to another. We apply our method to data sets from western Germany that cover early Neolithic, Iron Age, Roman, and Merovingian times as well as historical data from AD 1800. Error margins and natural and historical variability are discussed. Our results for nonstate societies are always lower than conventional estimations compiled from the literature, and we discuss the reasons for this finding. At the end, we compare the calculated local and global population densities with other estimations from different parts of the world.
Keywordssettlement archaeology, population density, site density, Bandkeramik settlements, LBK culture, Aldenhovener Platte, Rhineland, Germany, Neolithic.
Cover Page FootnoteWe thank Irmela Herzog (LVR-Bodendenkmalpfl ege Rheinland, Bonn) for her kernel density estimation computer program; Irmela Herzog and Thomas Frank (Universität zu Köln) for the preparation of the actual Bandkeramik data set from the lower Rhine basin; and Niels Müller-Scheessel (Römisch-GermanischeKommission, Frankfurt am Main) for the isoline circumscribing the Hallstatt necropolises of southern Germany. The remarks of the referees were very useful for improving the text. And last but not least, we are grateful to the German Research Foundation (DFG) for funding the archaeological project of the Rhine-LUCIFS framework.This open access article is available in Human Biology: http://digitalcommons.wayne.edu/humbiol/vol81/iss2/13
Estimations of Population Density for Selected Periods Between the Neolithic and AD 1800Andreas Zimmermann, 1 Johanna Hilpert, 1 and Karl Peter Wendt 1 Abstract We describe a combination of methods applied to obtain reliable estimations of population density using archaeological data. The combination is based on a hierarchical model of scale levels. The necessary data and methods used to obtain the results are chosen so as to defi ne transfer functions from one scale level to another. We apply our method to data sets from western Germany that cover early Neolithic, Iron Age, Roman, and Merovingian times as well as historical data from AD 1800. Error margins and natural and historical variability are discussed. Our results for nonstate societies are always lower than conventional estimations compiled from the literature, and we discuss the reasons for this fi nding. At the end, we compare the calculated local and global population densities with other estimations from different parts of the world.