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Research data: Continuity Amid Transformation: An Analysis of Pottery Production from the Late La Tène to Early Roman Periods in Eastern Bohemia
<p>Data used in the research presented in the article titled "Continuity Amid Transformation: An Analysis of Pottery Production from the Late La Tène to Early Roman Periods in Eastern Bohemia".</p> <p><strong>Abstract of the article:</strong></p> <p>At the end of the La Tène period and the beginning of the Roman period in the first century BC, society in Central Europe underwent a significant transformation, which included notable changes in pottery production. This transformation is often attributed to the collapse of the social structures of the La Tène period and the arrival of a new population. Pottery production, in particular, is generally considered to have undergone a complete transformation.</p> <p>However, previous studies on this transition have primarily focused on the stylistic analysis of shapes and decorations, as illustrated by the pottery assemblage from Slepotice (Eastern Bohemia). In order to obtain additional data on the transitional period, this study of pottery from Slepotice incorporates analyses of the materials used and the manufacturing process through macroscopic observation, X-ray fluorescence analysis, and thin-section analysis. These analyses provide new insights into the differences in pottery production and distribution during the first century BC.</p> <p>Our research indicates that while the transformation included the collapse of the La Tène socioeconomic network, it did not result in a complete break in the pottery production process.</p> <p>Link to the article: <a href="https://doi.org/10.1016/j.jasrep.2025.105073">https://doi.org/10.1016/j.jasrep.2025.105073</a></p> <p> </p> <p><strong>List of the files:</strong></p> <p>Supplementary Material 1<br>Settlement structure in the vicinity of Slepotice during the La Tène and Roman periods: 1 – Slepotice, 2 – České Lhotice, 3 – Brčekoly, 4 – Chrudim</p> <p>Supplementary Material 2<br>Values of pottery attributes (Mat, InMn, InVar, In, traces left from the shaping process, Po, Vy, and morphological groups) classified based on macroscopic observation</p> <p>Supplementary material 3<br>Schematic classification of rim attributes, illustrating different variants of rim direction (Op), thickening of the upper part of the rim (Oz), and trimming of the lip (Os)</p> <p>Supplementary material 4<br>Attributes of the 30 samples selected for XRF analysis based on macroscopic observation. These attributes include fabric properties, surface treatment, morphological features, and technological traces</p> <p>Supplementary material 5<br>Figures of ceramic samples (with corresponding IDs) from feature 144/1998 showing preserved rims and bases</p> <p>Supplementary material 6<br>Figures of ceramic samples (with corresponding IDs) from feature 355/2001 showing preserved rims</p> <p>Supplementary Material 7<br>Chemical composition of 30 selected samples according to XRF analysis (main oxides in wt%, and elements in ppm)</p> <p>Supplementary Material 8<br>Principal Component Analysis (PCA) results: The scree plot (top left) visualises the proportion of variance explained by each principal component. The biplots (top right and bottom right) illustrate the distribution of samples, with arrows indicating the contribution of specific elements to the observed variance. The dendrogram (bottom left) shows hierarchical clustering of the samples, aiding in the selection of representative samples for thin-section petrographic analysis</p> <p>Supplementary Material 9<br>Relationships between the dating and other attributes of pottery classified based on macroscopic observation. These attributes include fabric properties, surface treatment, morphological features, and technological traces</p> <p>Supplementary Material 10<br>Relationships between the chemical groups (determined by XRF analysis) and pottery attributes classified based on macroscopic observation. These attributes include fabric properties, surface treatment, morphological features, and technological traces</p> <p>Supplementary Material 11<br>Petrography of fabric groups and subgroups, focusing on their properties. The evaluation begins with a general assessment of each fabric group as a whole, followed by a detailed examination of its subgroups</p> <p>Supplementary Material 12<br>Petrographic characterization of ceramics using a semiquantitative scale, simplified for statistical analysis (0.1 – trace, 0.5 – rare, 1 – occasional, 2 – common, 3 – frequent, 4 – abundant, 5 – dominant)</p> <p>Supplementary Material 13<br>Thin-section samples: Description of the ceramic matrix, natural inclusions, and added tempers</p> <p>Supplementary material 14<br>Variations in chemical composition among different fabric groups</p>
Dataset for "Effects of weather and climate on fluctuations of grain prices in southwestern Bohemia, 1725–1824 CE"
<p><span>This deposit contains three .xlsx files.</span></p> <p><span>The file „01_prices_Sušice_1725-1824“ contains two sheets with mean annual prices (in Lower Austrian <em>měřice</em>) of four cereals (wheat, rye, barley and oats) in Sušice for the period 1725–1824. On the first sheet are compiled series, on the second detrended series (using high-pass filter).</span></p> <p><span>The file „02_monthly_prices_1725-1738“ contains four sheets with mean monthly prices (in Lower Austrian <em>měřice</em>) of four cereals in Sušice from July 1725 to July 1738 (July 1737 is missing). Sheets represent individual cereals – wheat, rye, barley and oats.</span></p> <p><span>The file „03_climate_char_1725-1824“ contains two sheets with mean seasonal (DJF, MAM and JJA) temperature, precipitation and scPDSI expressed in deviations relative to the 1961–1990 reference period. On the first sheet are original series, on the second detrended series (using high-pass filter). The original series are reconstructed temperatures for central Europe (Dobrovolný et al., 2010), reconstructed precipitation for the Czech Lands (Dobrovolný et al., 2015) and both of them were used for creation of scPDSI series (Brázdil et al., 2016).</span></p>
Total Viewshed of Bohemia
<p>The dataset represents a collection of <em>total viewsheds</em> (cf. Llobera et al. 2010) created for the territory of Bohemia (Czech Republic; ca. 57,000 km<sup>2</sup>). The total-viewshed calculation was based on the R2 algorithm (see Franklin and Ray 1994) and uses the viewshed function from MATLAB’s Mapping Toolbox that was significantly optimized by the authors for large-scale parallel computations. To reduce the computational time, we calculated single viewsheds using every fourth cell as the observing point (cf. Rášová 2017).</p> <p>The <em>Digital Terrain Model of the Czech Republic of the 5th Generation</em> (<a href="https://ags.cuzk.cz/arcgis2/rest/services/dmr5g/ImageServer">DMR 5G</a>) was used as input for the calculations. Prior to the calculation, the input DEM was cleared of modern landscape elements (e.g. embankments of railways and roads, quarries, etc.; for details see Novák – Pružinec 2022). Eight total visibility models of the territory of Bohemia were constructed using the IT4Innovations research infrastructure (<a href="https://www.it4i.cz/">https://www.it4i.cz/</a>). Both the observer and the target heights were set at 1.5 m. The viewsheds differ in two parameters: the visibility radius and the resolution of the input grid. As the basic radius, we have set 0.5 km and the cell size of 5 m; further layers are conceived as multiples of these parameters: 1 km/10 m, 2 km/20 m, 4 km/40 m, 8 km/80 m, 16 km/160 m and 32 km/320 m. The only exception is the model with a radius of 64 km, where we preserved the cell size of the preceding iteration (320 m). In the individual models, the visibility values are indicated in percentages corresponding to the portion of visible cells in the given radius (0–100%; rounded up to the next complete value).</p> <p>Filenames of individual rasters correspond to the parameters set above. For further details see:</p> <ul> <li>Kuna, M. – Novák, D. – Bucha Rašová, A. – Bucha, B. – Machová, B. – Havlice, J. – John, J. – Chvojka, O. 2022: Computing and testing extensive total viewsheds: a case of prehistoric burial mounds in Bohemia. Journal of Archaeological Science 142, 105596. <a href="https://doi.org/10.1016/j.jas.2022.105596">https://doi.org/10.1016/j.jas.2022.105596</a></li> <li>Novák, D. – Pružinec, F. 2022: Potential and Implications of Automated Pre-Processing of Lidar-Based Digital Elevation Models for Large-Scale Archaeological Landscape Analysis. Available at SSRN: <a href="http://dx.doi.org/10.2139/ssrn.4063514">http://dx.doi.org/10.2139/ssrn.4063514</a></li> </ul>
Fig. 8 in Early ontogenetic growth stages of Middle Ordovician orthoceratoid cephalopods from Bohemia
Fig. 8. Box-plot of diameter of initial chambers of Ordovician orthoceratoid cephalopods. Data from Ruedemann (1912), Balashov (1957), Evans (2005, 2007), Aubrechtová (2015), Kröger (2006, 2007), and Kröger et al. (2009).
Fig. 5 in Early ontogenetic growth stages of Middle Ordovician orthoceratoid cephalopods from Bohemia
Fig. 5. Drawings of known embryonic shells with initial chambers of Ordovician orthoceratoids (cf. Kröger and Mapes 2007: fig. 4 and Klug et al. 2015: fig. 1.3.). Dotted lines indicate the assumed position of the siphuncle in Arionoceras? sp. and Orthoceratida indet. sp. 2. In Orthoceratida indet. sp. 2, note a sketch of hyposeptal cameral deposits (see the text below and Fig. 7C1). The stratigraphic position of Bactroceras angustisiphonatum and Arionoceras? sp. is either uppermost Lower Ordovician, or lowermost Middle Ordovician (David Evans, personal communication 2019; see also Evans 2005 and 2007). Orthoceratidae gen. et sp. indet B (Kröger 2007) is likely to be conspecific with Transorthoceras osmundsbergense according to Kröger et al. (2011a).
Fig. 6 in Early ontogenetic growth stages of Middle Ordovician orthoceratoid cephalopods from Bohemia
Fig. 6. Apical and juvenile shell parts of orthoceratid cephalopods; Middle Ordovician, Darriwilian Stage, Šárka and Dobrotivá formations, Czech Republic. A. Bactroceras sandbergeri (Barrande, 1867), MWB S 06823, Volduchy, third phragmocone chamber (estimated based on shell diameter) and adjacent part of body chamber. B. Orthoceratida indet. sp. 4, MWB S 06827, Volduchy, counterpart of initial chamber and adjacent part of phragmocone and one corroded phragmocone septum; note longitudinal striae. C. Orthoceratida indet sp. 5, NM L 59872, Malé Přílepy, counterpart (C1), latext cast C2); note longitudinal striae.
Fig. 3 in Early ontogenetic growth stages of Middle Ordovician orthoceratoid cephalopods from Bohemia
Fig. 3. Apical shell of the orthoceratoid Bactroceras sandbergeri (Barrande, 1867); Middle Ordovician, lower Darriwilian Stage, Šárka Formation, Czech Republic. A. MWB S 06761, Mýto-Svatoštěpánský rybník, latex cast of one of counterparts in lateral view, note fine, obliquely transverse surface ornamentation. B. MWB S 06762, Mýto-Svatoštěpánský rybník, counterpart (B1) and its latex cast (B2), in lateral view (initial chamber bent towards dorsum). C. MWB S 06763, Rokycany-Díly, internal mould in lateral view, single (adoralmost) phragmocone chamber showing ventrally situated siphuncle (C1), latex cast of the second counterpart (C2).
Fig. 2 in Early ontogenetic growth stages of Middle Ordovician orthoceratoid cephalopods from Bohemia
Fig. 2. Apical shell parts of the orthoceratoid Bactroceras sandbergeri (Barrande, 1867), Middle Ordovician, lower Darriwilian Stage, Šárka Formation, Czech Republic. A. MWB S 06759, Rokycany-Díly, internal mould in ventral view (A1), with accompanying trilobite Ormatops sp., brachiopod Euorthisina sp., and indeterminate hyolith; detail (A2), note the decrease of apical angle at second phragmocone chamber; latex cast of counterpart in ventral view (A3). B. MWB S 06764, Těškov, internal mould in lateral view, venter on right hand-side (initial chamber bent towards dorsum), initial and second phragmocone chamber preserved as counterpart. C. MWB S 06760, Těškov, latex casts of both sides of counterparts (C1, C2), note suspicious surface structures. D. NM L 59577, Praha-Hanspaulka, latex cast of counterpart.
Fig. 1 in Early ontogenetic growth stages of Middle Ordovician orthoceratoid cephalopods from Bohemia
Fig. 1. Position of Ordovician rocks of the Prague Basin within the Bohemian Massif and the localities from which the herein studied specimens originate see the text below). 1, Praha-Šárka cihelna (brickyard); 2, Praha-Šárka; 3, Praha-Hanspaulka; 4, Malé Přílepy; 5, Lhotka u Berouna; 6, Těškov; 7, MýtoSvatoštěpánský rybník; 8, Rokycany-Díly; 9, Volduchy. Adapted after Manda (2008).
FIGURE 3 in A multicarpellate fruit from Late Cretaceous sediments of South Bohemia, Czech Republic
FIGURE 3. Schematic line drawings of the gynoecium of Covidifructus multicarpellatus. (A) Longitudinal median section through the gynoecium showing its complex internal morphology with a remaining floral apex and an empty space (asterisk) in the centre of the ovary; arrowheads indicate stigma positions; grey shaded areas indicate potential stigmatic secretion forming an extra-gynoecial compitum across neighbouring stigmas; pollen grains and hypothetical pathways of pollen tubes are given in orange; dashed orange line indicates hypothetical pathway of pollen tube reaching a stigma via growth through the extra-gynoecial compitum; dashed black line indicates area of postgenital carpel union in the centre of the ovary (symplicate region); arrows indicate area of irregular ovary closure shown in (B); placentation is axile with the seeds (green) attached in the distalmost part of the ovary. (B) Line drawing showing zone ovary closure (see also Figure 1C, F) as seen from above, radial lines correspond to ventral slits of individual carpels; carpel flanks meet in an irregular pattern in the centre of the gynoecium; the area of closure is flattened (compressed; indicated by dashed ellipse), and the 10 carpels are roughly arranged in a double row facing each other (dashed line in centre of figure) rather than in a smooth circle.
FIGURE 2 in A multicarpellate fruit from Late Cretaceous sediments of South Bohemia, Czech Republic
FIGURE 2. Covidifructus multicarpellatus gen. et sp. nov. specimen No. NMP F3200, scale bars equal 300 µm in all figures, series of microCT sections of premature capsular fruit. (A) Volume rendering of fruit in lateral view; lines B-F indicate approximate levels of transverse sections shown in the following images. (B) Transverse section at the level of styles and stigmas. (C) Transverse section at the level of the symplicate zone of the gynoecium where the carpels are postgenitally united in the centre of the ovary; distalmost parts of locules and seeds are visible. (D) Transverse section at the level of the empty space (asterisk) where carpels do not meet in the centre of the ovary. (E) Transverse section at the level of the synascidiate zone of the gynoecium, i.e., below the enclosed floral apex and the empty space. (F) Transverse section through the very base of the fruit showing the basal-most parts of the locules. (G) Longitudinal median section showing empty space in the centre of the ovary (asterisk) and axile ovule/seed attachment (arrow) in the distalmost part of the ovary. (H) Longitudinal tangential section with one seed rendered and coloured in green. (I) Transverse section at the level of seed attachment in the distal part of the ovary, with one seed rendered and coloured in green.
FIGURE 1 in A multicarpellate fruit from Late Cretaceous sediments of South Bohemia, Czech Republic
FIGURE 1. Covidifructus multicarpellatus gen. et sp. nov.; specimen No. NMP F3200; scale bars equal 100 µm in all figures. (A) Small premature capsular fruit in lateral view, semi-globose in overall shape; SEM. (B) Fruit seen in apical view; note preformed dorsal lines of fruit dehiscence; SEM. (C) Close-up of fruit apex showing styles and stigmatic areas (asterisks); note irregular closure of ovary in the very centre; SEM. (D) MicroCT volume rendering, lateral view, showing 10 elongate seeds (green), one seed per carpel. (E) MicroCT volume rendering, apical view, showing regular arrangement of carpels and seeds. (F) Detail of central ovary closure (dashed line); note that some of the carpel flanks (arrowheads) do not extend to the very centre of the closure zone; SEM.
Text-fig. 4. Dendrogram (Ward's method, squared Euclidean distance) showing the relationship between the studied fossil vegetation assemblages of Hrádek/N. (48), Wackersdorf (49), Berzdorf and Wiesa (50) and the Mydlovary Fm. (51) and the studied modern vegetation units from SE China and Japan (Teodoridis et al. 2011a, 2012, Appendix – this volume). in A Review Of The Early Miocene Mastixioid Flora Of The Kristina Mine At Hrádek Nad Nisou In North Bohemia (The Czech Republic)
Text-fig. 4. Dendrogram (Ward's method, squared Euclidean distance) showing the relationship between the studied fossil vegetation assemblages of Hrádek/N. (48), Wackersdorf (49), Berzdorf and Wiesa (50) and the Mydlovary Fm. (51) and the studied modern vegetation units from SE China and Japan (Teodoridis et al. 2011a, 2012, Appendix – this volume).
Text-fig. 3. Schematic geological section of the Kristina Mine near Hrádek/N. (state in 1963–1964) – height/length ratio 3:1. Explanations: vertical hatching – lignite seam, seamlet; dotted – coarse-grained sand, pea-gravel; short lines – sandy clay; white – clay; black lines – clay ironstone concretions; black dots – individual fossiliferous horizons designated as (A) plastic clay from the upper part of the main xylitic seam (about 5 m under t of the seam, (B) clay and "Blätterkohle" from the uppermost part of the first seamlet (split off the Main Coal Seam), (C) slightly sandy brown clay under the uppermost part of the Main Coal Seam, (D) base of the sandy clay with large concretions of the clay ironstone above the Main Coal Seam, (E) sandy clay (incl. clay ironstone) supplying most of leaf material with cuticles (F) 1–2 cm thin silty lenticles or thin beds of the sandy clay with xylites and Eomastixia within peagravels and coarse-grained sands, (G) coarse-grained sands with clayish silts with Fagus, Ocotea, Pterocarya, Tectocarya, (H) brown sandy clay underlying the uppermost seamlet, (I) lignite clay, base of the uppermost seamlet (J) Glyptostrobus – "Blätterkohle", base of the uppermost seamlet (according to Holý 1975, modified). in A Review Of The Early Miocene Mastixioid Flora Of The Kristina Mine At Hrádek Nad Nisou In North Bohemia (The Czech Republic)
Text-fig. 3. Schematic geological section of the Kristina Mine near Hrádek/N. (state in 1963–1964) – height/length ratio 3:1. Explanations: vertical hatching – lignite seam, seamlet; dotted – coarse-grained sand, pea-gravel; short lines – sandy clay; white – clay; black lines – clay ironstone concretions; black dots – individual fossiliferous horizons designated as (A) plastic clay from the upper part of the main xylitic seam (about 5 m under t of the seam, (B) clay and "Blätterkohle" from the uppermost part of the first seamlet (split off the Main Coal Seam), (C) slightly sandy brown clay under the uppermost part of the Main Coal Seam, (D) base of the sandy clay with large concretions of the clay ironstone above the Main Coal Seam, (E) sandy clay (incl. clay ironstone) supplying most of leaf material with cuticles (F) 1–2 cm thin silty lenticles or thin beds of the sandy clay with xylites and Eomastixia within peagravels and coarse-grained sands, (G) coarse-grained sands with clayish silts with Fagus, Ocotea, Pterocarya, Tectocarya, (H) brown sandy clay underlying the uppermost seamlet, (I) lignite clay, base of the uppermost seamlet (J) Glyptostrobus – "Blätterkohle", base of the uppermost seamlet (according to Holý 1975, modified).
Text-fig. 1. Bohemian Massif with position of the Prague Basin (in black) and distribution of Ordovician rocks in the Prague Basin, with geographic position of main localities of the siliceous nodules. in Porambonites Havliceki Sp. Nov., A New Brachiopod From The Šárka Formation (Darriwilian) From Bohemia And Its Contribution To Early History Of The Porambonitidae
Text-fig. 1. Bohemian Massif with position of the Prague Basin (in black) and distribution of Ordovician rocks in the Prague Basin, with geographic position of main localities of the siliceous nodules.
Text-fig. 2. Stratigraphic ranges of selected porambonitid taxa in West Gondwana (Iberica), Baltica, Perunica and Avalonia. Arrows indicate derivation of early Baltic porambonitids from Gondwanan Poramborthis (1), derivation of Porambonites in Perunica and Avalonia from Baltica (2), and expansion of Porambonites from Baltica and/or Avalonia to West Gondwana (3). in Porambonites Havliceki Sp. Nov., A New Brachiopod From The Šárka Formation (Darriwilian) From Bohemia And Its Contribution To Early History Of The Porambonitidae
Text-fig. 2. Stratigraphic ranges of selected porambonitid taxa in West Gondwana (Iberica), Baltica, Perunica and Avalonia. Arrows indicate derivation of early Baltic porambonitids from Gondwanan Poramborthis (1), derivation of Porambonites in Perunica and Avalonia from Baltica (2), and expansion of Porambonites from Baltica and/or Avalonia to West Gondwana (3).
Text-fig. 4. Cyclurus macrocephalus REUSS. Isolated skull bones. Specimen NMP Pc 2848. Dent: dentary; Dpal: dermopalatine; Mx: maxillary; Vo: vomer. [Photograph D. Serrette] in Complements To The Anatomical Knowledge Of Reuss (Pisces, Actinopterygii) From The Eocene Of Kučlín, Bohemia, Czech Republic
Text-fig. 4. Cyclurus macrocephalus REUSS. Isolated skull bones. Specimen NMP Pc 2848. Dent: dentary; Dpal: dermopalatine; Mx: maxillary; Vo: vomer. [Photograph D. Serrette]
Text-fig. 7. Cyclurus macrocephalus REUSS. Specimen NMP Pc 313. Right dentary. [Photograph D. Serrette] in Complements To The Anatomical Knowledge Of Reuss (Pisces, Actinopterygii) From The Eocene Of Kučlín, Bohemia, Czech Republic
Text-fig. 7. Cyclurus macrocephalus REUSS. Specimen NMP Pc 313. Right dentary. [Photograph D. Serrette]
Text-fig. 3 Pollen diagram from the locality of Bohutín. 0-0.01 m – sandy soil mixed with humus, slightly clayey, sample B11; 0.05 m – grey-blue strongly sandy clay, sample B10; 0.10-0.25 m – brown-grey sandy clay with plant remains and mixed with a small amount of peat, sample B9, sample B8 (0.15 m), sample B7 (0.20 m), sample B6 (0.25 m); 0.30-0.35 m – dark sandy clay mixed with peat and plant remains, sample B5, sample B4 (0.35 m); 0.40 m – grey strongly sandy clay mixed with peat, sample B3; 0.45-0.50 m – grey-blue strongly sandy clay, sample B2, sample B1 (0.50 m). in Reconstruction Of Vegetation Development On The Floodplain Of The Litavka River In The Holocene (Central Bohemia, Brdy Mts.)
Text-fig. 3 Pollen diagram from the locality of Bohutín. 0-0.01 m – sandy soil mixed with humus, slightly clayey, sample B11; 0.05 m – grey-blue strongly sandy clay, sample B10; 0.10-0.25 m – brown-grey sandy clay with plant remains and mixed with a small amount of peat, sample B9, sample B8 (0.15 m), sample B7 (0.20 m), sample B6 (0.25 m); 0.30-0.35 m – dark sandy clay mixed with peat and plant remains, sample B5, sample B4 (0.35 m); 0.40 m – grey strongly sandy clay mixed with peat, sample B3; 0.45-0.50 m – grey-blue strongly sandy clay, sample B2, sample B1 (0.50 m).
Text-fig. 6. Cyclurus macrocephalus REUSS. Specimen NMP Pc 2846. Right operculum. [Photograph D. Serrette] in Complements To The Anatomical Knowledge Of Reuss (Pisces, Actinopterygii) From The Eocene Of Kučlín, Bohemia, Czech Republic
Text-fig. 6. Cyclurus macrocephalus REUSS. Specimen NMP Pc 2846. Right operculum. [Photograph D. Serrette]
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