Fig 1.
Diachronic studies with a focus on statistical analyses of long-term human-environment interactions between the Neolithic and the middle ages in Germany.
(1) Region between Lake Schwerin and Stepenitz [58], (2) north-west Saxony [57], (3) former district of Riesa-Großenhain [56], (4) Gotha landscape [33], (5) Weiße Elster river catchment (present project), (6) widening of the Elbe valley at Dresden [41], (7) northern Wetterau [59], (8) district of Groß-Gerau [29], (9) north-western Main triangle [55], (10) eastern landscape of Lower Franconia [54], (11) southern Main triangle [9], (12) Brenz-Kocher valley in the eastern Swabian Jura [10], (13) lower valley of the Altmühl river [53], (14) Danube valley near Regensburg [52], (15) southern Upper Rhine valley [32] and (16) the Baar and adjacent landscapes [12]. Furthermore, the three main landscape units of Germany are shown. Rivers are derived from the European Catchments and Rivers network system [60]. The topography is based on the SRTM 90 m Digital Elevation Database version 4.1 [61–63].
Fig 2.
Study area with respect to borders of federal states, international (intl.) borders, local topography and large urban areas mentioned in the text.
The outlines of the study area were extracted from the Catchment Characterisation Model database [82]. The political borders are drawn according to the Saxon State Office for Environment, Agriculture and Geology, the Saxony-Anhalt State Office for Surveying and Geoinformation and the Thuringian State Office for Land Management and Geoinformation. Rivers and urban areas are derived from the urban morphological zones dataset and the European Catchments and Rivers network system [83]. The topography is based on the SRTM 90 m Digital Elevation Database version 4.1 [61–63]. Topography and rivers have been modified according to older topographic maps (S2 Fig).
Fig 3.
Terminology and chronology of Neolithic periods in Germany.
For the Neolithic in Central Germany a selection of characteristic pottery and stone tools is added, drawings by Jan Miera.
Fig 4.
Random forests confusion matrix according to van Rijsbergen [120].
Fig 5.
Distribution of Neolithic sites with respect to their modes of discovery against the background of areas investigated by field surveys and aerial photography.
Rivers were plotted according to the European Catchments and Rivers network system [60]. The topography is based on the SRTM 90 m Digital Elevation Database version 4.1 [61–63]. Topography and rivers have been modified according to older topographic maps (S2 Table). See Fig 2 for a location of the urban areas mentioned in the text.
Table 1.
Dataset used in random forests analyses.
Fig 6.
Mapping of datasets used in random forests analyses.
(a) Site depth, (b) material groups (c) depth of pottery and (d) stone tools (Table 1). Rivers are plotted according to the European Catchments and Rivers network system [60]. The topography is based on the SRTM 90 m Digital Elevation Database version 4.1 [61–63]. Topography and rivers have been modified according to older topographic maps (S2 Table). See Fig 2 for a location of the urban areas mentioned in the text.
Fig 7.
Modern land use and Neolithic site distribution in the study area.
Distribution of modern land use classes according to CORINE Land Cover data [83]. The spatial extent of the (refilled) open-cast mines has been modified according to older topographic maps (S2 Table; S2 Fig).
Table 2.
Distribution of Neolithic sites over modern land use.
Fig 8.
Neolithic site densities in the study area.
(a) Entire Neolithic, (b) Early Neolithic, (c) Middle Neolithic and (d) Late Neolithic. Rivers were plotted according to the European Catchments and Rivers network system [60]. The topography is based on the SRTM 90 m Digital Elevation Database version 4.1 [61–63]. Topography and rivers have been modified according to older topographic maps (S2 Table). See Fig 2 for a location of the urban areas mentioned in the text.
Fig 9.
Analyses of site exploitation territories.
(a) Size of modelled SET, (b) terrain elevation, (c) slope, (d) valley depth, (e) river distance and (f) soils on loess and. For more information on each terrain covariate see S1 Table.
Table 3.
Average Neolithic site frequencies per 250 km2 in the study area and adjacent landscapes.
Fig 10.
Study areas in Central Germany mentioned in the text and in Table 3.
(1) Gothaer Land [33], (2) Erfurt [200], (3) downstream section of the Bode river [201], (4) Elbe-Saale-Region [202], (5) North-West Saxony [57], (6) Lake Göttwitz [101], (7) former district of Riesa-Großenhain [56], (8) Ore Mountains [203], (9) Dresden Elbe valley [41], (10) Dresden Elbe valley and lower part of eastern Ore Mountains [204], (11) Vogtland [171], (12) catchment of the Weiße Elster river (this study).