Swiss sediments according to PETERS (1969), MUMENTHALER (1979) and SCHUBERT (1987). Therefore, chlorite was used to establish firing temperatures.

<figure><img src="image_38.png" /><figcaption>**Figure 6.9:** Reconstructed special form Boleráz: samples JB013 and JB014 are respectively coming from the grey and orange parts (from LEUZINGER, 2000).</figcaption></figure>

## 6.6 CHEMICAL STUDY

### 6.6.1 Contaminated ceramics

One reconstructed special form Boleráz is composed of grey and orange sherds (Fig. 6.9; LEUZINGER, 2000, Fig. 25; DE CAPITANI, 2002, chapter 5.5). One sample of each coloured part was studied: JB013 is grey on both surfaces and black inside, and JB014 is orange and black, respectively. The orange sherds of the vessel were collected in the northern part of the excavation, whereas the grey ones came from its southern area (DE CAPITANI, 2002). The northern area was dry and the sherds deposited above the ground water level. In the opposite, the grey sherds were found in a humid environment. However, JB014 has a very high loss of ignition (14.03, Table 6.4) and contained much more water than JB013 (loss of ignition: 4.71). This fact cannot be explained, but could maybe be put in relation with a problem during its sampling in the excavations.

On table 6.4, the possibly contaminated ceramics are put into relation with the mean and the standard

<table><caption>**Table 6.4:** Chemical data of the possibly contaminated ceramics (plus JB013, non-contaminated sample) in regard to mean and standard deviation (s) of all the ceramics from Arbon Bleiche 3 except those tempered with bone (n= 158, see Appendix 9B). √, + and – respectively refer to “equal to”, “more” or “less” than the range of “mean plus or minus s” for 158 ceramics from Arbon Bleiche 3.</caption><thead><tr><th colspan="2">Oxides</th><th colspan="7">Possibly contaminated potteries from Arbon-Bleiche 3</th><th colspan="2">Other ceramics</th></tr><tr><th>Elements</th><th>Unit</th><th>JB013</th><th>JB014</th><th>JB002</th><th>JB025</th><th>JB028</th><th>JB031</th><th>JB061</th><th>mean</th><th>s</th></tr></thead><tbody><tr><td colspan="11"><strong>colour</strong></td></tr><tr><td></td><td>grey<br>borders</td><td></td><td></td><td></td><td></td><td></td><td></td><td></td><td></td><td></td></tr><tr><td>SiO2</td><td>wt.%</td><td>66.23</td><td>64.70</td><td>64.85</td><td>64.39</td><td>67.67</td><td>70.31</td><td>68.55</td><td>67.84</td><td>2.18</td></tr><tr><td>TiO2</td><td>wt.%</td><td>0.76</td><td>0.93</td><td>0.71</td><td>0.72</td><td>0.75</td><td>0.75</td><td>0.63</td><td>0.73</td><td>0.09</td></tr><tr><td>Al2O3</td><td>wt.%</td><td>18.94</td><td>23.03</td><td>17.58</td><td>17.94</td><td>17.79</td><td>17.60</td><td>17.94</td><td>17.87</td><td>1.39</td></tr><tr><td>Fe2O3</td><td>wt.%</td><td>5.38</td><td>4.47</td><td>5.72</td><td>4.59</td><td>5.35</td><td>4.24</td><td>4.46</td><td>4.61</td><td>0.70</td></tr><tr><td>MnO</td><td>wt.%</td><td>0.06</td><td>0.02</td><td>0.06</td><td>0.07</td><td>0.06</td><td>0.04</td><td>0.04</td><td>0.05</td><td>0.02</td></tr><tr><td>MgO</td><td>wt.%</td><td>1.85</td><td>1.20</td><td>1.76</td><td>1.61</td><td>1.69</td><td>1.30</td><td>1.43</td><td>1.76</td><td>0.42</td></tr><tr><td>CaO</td><td>wt.%</td><td>3.42</td><td>2.25</td><td>5.45</td><td>6.93</td><td>3.24</td><td>2.02</td><td>1.58</td><td>3.10</td><td>1.74</td></tr><tr><td>Na2O</td><td>wt.%</td><td>0.36</td><td>0.38</td><td>0.70</td><td>0.72</td><td>0.76</td><td>1.44</td><td>1.60</td><td>0.91</td><td>0.47</td></tr><tr><td>K2O</td><td>wt.%</td><td>3.02</td><td>2.59</td><td>3.27</td><td>2.72</td><td>2.66</td><td>2.33</td><td>3.47</td><td>2.88</td><td>0.42</td></tr><tr><td>P2O5</td><td>wt.%</td><td>0.19</td><td>0.42</td><td>0.21</td><td>0.29</td><td>0.22</td><td>0.21</td><td>0.23</td><td>0.23</td><td>0.09</td></tr><tr><td>Ba</td><td>ppm</td><td>676</td><td>603</td><td>392</td><td>850</td><td>623</td><td>734</td><td>838</td><td>663</td><td>133</td></tr><tr><td>Cr</td><td>ppm</td><td>128</td><td>152</td><td>112</td><td>111</td><td>116</td><td>89</td><td>98</td><td>113</td><td>18</td></tr><tr><td>Cu</td><td>ppm</td><td>40</td><td>53</td><td>33</td><td>34</td><td>38</td><td>26</td><td>31</td><td>39</td><td>8</td></tr><tr><td>Nb</td><td>ppm</td><td>17</td><td>20</td><td>17</td><td>18</td><td>14</td><td>17</td><td>16</td><td>16</td><td>3</td></tr><tr><td>Ni</td><td>ppm</td><td>65</td><td>91</td><td>56</td><td>57</td><td>63</td><td>48</td><td>48</td><td>63</td><td>13</td></tr><tr><td>Pb</td><td>ppm</td><td>30</td><td>38</td><td>28</td><td>27</td><td>29</td><td>25</td><td>30</td><td>27</td><td>5</td></tr><tr><td>Rb</td><td>ppm</td><td>169</td><td>146</td><td>183</td><td>148</td><td>155</td><td>135</td><td>182</td><td>159</td><td>23</td></tr><tr><td>Sr</td><td>ppm</td><td>218</td><td>124</td><td>214</td><td>270</td><td>202</td><td>212</td><td>279</td><td>191</td><td>55</td></tr><tr><td>V</td><td>ppm</td><td>143</td><td>160</td><td>134</td><td>132</td><td>139</td><td>109</td><td>112</td><td>122</td><td>20</td></tr><tr><td>Y</td><td>ppm</td><td>25</td><td>26</td><td>30</td><td>24</td><td>29</td><td>21</td><td>19</td><td>25</td><td>4</td></tr><tr><td>Zn</td><td>ppm</td><td>114</td><td>163</td><td>110</td><td>103</td><td>107</td><td>95</td><td>100</td><td>109</td><td>19</td></tr><tr><td>Zr</td><td>ppm</td><td>135</td><td>148</td><td>142</td><td>136</td><td>153</td><td>175</td><td>126</td><td>152</td><td>27</td></tr><tr><td>SUM</td><td>wt.%</td><td>100.39</td><td>100.16</td><td>100.46</td><td>100.17</td><td>100.36</td><td>100.41</td><td>100.12</td><td></td><td></td></tr><tr><td>FeO</td><td>wt.%</td><td>2.57</td><td>2.22</td><td>3.23</td><td>1.92</td><td>2.68</td><td>0.79</td><td>1.01</td><td></td><td></td></tr><tr><td>LiO</td><td>wt.%</td><td>4.71</td><td>14.03</td><td>3.21</td><td>9.71</td><td>3.89</td><td>4.22</td><td>2.94</td><td></td><td></td></tr></tbody></table>
deviation-for each chemical element- of every ceramic
from Arbon Bleiche 3, ceramics tempered with bone
excepted. In JB014, SiO₂, MnO, MgO, Na₂O and Sr
decreased whereas TiO₂, Al₂O₃, P₂O₅, Cr, Cu, Nb, Ni,
Pb, V and Zn increased. The other chemical elements
stayed stable. This is the opposite process of the well
described leaching, which decreases chemical ele-
ments such as P and Na. The orange sherd (JB014)
chemically differs from almost all the other analysed
ceramics: on Fig. 6.14 it is represented in the excep-
tions (Fig. 6.14E) whereas the grey one not (JB013,
Fig. 6.14A). Hence, these chemical changes due to the
deposition of the sherd in the sediment are high enough
to be perceived by the analyses.

Other partially orange samples were analysed, but
often, the colouration was only visible on one surface,
in opposition with JB014. It can be observed that
JB013 (grey borders) and JB028 (one orange surface)
are in the range of the mean, except for three and one
elements respectively (Fe₂O₃tot, Na₂O, V). JB025,
JB002, JB061, JB031 and JB014 have respectively 5,
6, 6, 8 and 15 elements out of the range of the mean.
JB025 is depleted in SiO₂ and enriched in MnO, CaO,
Ba and Sr. JB002 has too high SiO₂ and Ba whereas
Fe₂O₃tot, CaO, Rb and Y are too high compared to the
mean. JB061 is depleted in Ni, Y whereas Na₂O, K₂O,
Ba and Sr are too high. JB031 has too low MgO, K₂O,
Cr, Cu, Ni, Rb, and too high SiO₂ and Na₂O. Apart
from Na₂O, the contamination is different for these
two letter samples, because the elements do not follow
the same trend. The way all these samples (JB002,
JB014, JB025, JB028, JB031, JB061) were contami-
nated cannot be understood in detail.

However (except for JB014), these samples were
not contaminated enough to be chemically separated
from the other samples, but their results shall be used
with precautions.

The little standard deviation and variation coeffi-
cient for Na₂O and the very low concentration of P₂O₅
(max. for 158 ceramics equal 0.7 wt.%) imply an
absence of contamination during the deposition of the
other sherds in the ground (WEDEPOHL, 1969-1978).
All the samples contain between 12 ppm and 66 ppm
Pb, except one, JB030, which contains 1863 ppm Pb.
This latter value is correlated with an analytical prob-
lem and is therefore not included in the statistical anal-
yses.

Even if some exceptions were evidenced at the
time, all the samples will be used further on for statis-
tical analyses. If these exceptions can be evidenced

according to various statistical methods, they will be
finally defined as real outliers.

6.6.2 Statistical treatment of the data

6.6.2.1 Introduction

The raw chemical data can be found in Appendix 8.

The statistical methods used are as follows:

1. The high number of data were first simplified and reduced to several numbers (mean, standard deviation...) that describe them. These latter summarise the different aspects contained in the data (Descriptive Statistics).

2. Classify the samples by their resemblances (Cluster Analysis)

3. Identify the characteristic elements of each chemical group by reducing the number of variables (Principal Component Analysis, PCA)

4. Assign samples of indeterminate origin to the chemical groups resulting from PCA (Discriminant Analysis and Mahalanobis Distance)

As explained in RAPP AND HILL (1988), “cluster
analysis is useful for identifying completely separate
groups but less helpful for identifying groups that
overlap, whereas discriminant analysis seeks to dis-
cover and use those attributes which discriminate
between known groups in order to assign unknowns to
one of the groups.”

6.6.2.2 Descriptive statistics

The chemical characteristics of the ceramics of
every group are printed on Appendix 9. For each
chemical element the minimum and maximum values,
the range containing the values and their means and
standard deviations are given. The standard deviation
(σ, s) is a measurement of the dispersion of the data in
one group (for one chemical element), which has the
same unit as the data (weight percent for the major
elements and parts per million for the traces). Inversely,
the variation coefficient, equal to the standard devia-
tion divided by the mean, has no unit and permits to
compare the dispersion of data measured in different
units.

The examination of the dispersion of one chemical
element is important: Picon (1984) proposed to neglect
the elements with a high standard deviation and a high
variation coefficient for the statistical analyses. As it
can be observed on Appendix 9B, no chemical element presents a high standard deviation and a high variation coefficient. Hence, all the measured elements are considered for the statistical analyses. In Appendix 9C, JB012 contains 444 ppm Y whereas all the other samples contain between 16 ppm and 52 ppm Y. This sample is a particular one, containing bone temper. Hence, this particularity is not assigned to an analytical error and will be taken into account.

PICON (1991) showed that the chemical components measured by XRF have a variable aptitude to separate the samples into different groups. Ca is the best, followed by K, Mg, Al, Ti, Mn, Si and Fe. Normally, $Al_2O_3$, $TiO_2$, MgO, $Fe_2O_3$, $K_2O$, Cr, Ni, Rb, V and Zn are positively correlated with the clay content (SIGG ET AL., 1986; BÉARAT AND BAUER, 1994; WOLF, 1999). Using several correlation diagrams ($SiO_2/Al_2O_3$, MgO/CaO, $TiO_2/Fe_2O_3$, $Na_2O/K_2O$, Ba/Zr, Cu/Zn, Ni/Cr and Rb/Sr), distinct groups resulting from different chemistry of clays and of tempering were searched; abnormal samples are evidenced that way (MAGGETTI AND GALETTI, 1993). All these correlations were studied, and some are presented in Fig. 6.10.

The petrographical group AIV is tempered with gabbro. This kind of rock normally contains a high proportion of MgO, $Fe_2O_3$, Cr, Ni and V (KILKA AND GALETTI, 1994, 1108; MAGGETTI ET AL., 1998, 26; NUNGÄSSER ET AL., 1992; DURUZ AND MAGGETTI, 1997; HERTLI ET AL., 1999; GIACOMINI, 2001). Unfortunately, AIV does not show a good chemical separation from the other petrographical groups for those elements. This fact shall be put into relation with the small amount of gabbro tempering the clay. On figure 6.10: A and B, the samples tempered exclusively with granite (AI*), mostly with gabbro (AIV) and exclusively with grog (AV*) are plotted together. These three groups are the most different of Arbon Bleiche 3, petrographically speaking. In the graphs showing the major elements (Fig. 6.10A), only $Na_2O$ permits to separate AV* from the other groups. AIV and AV* overlap the higher range of values of AI* for $TiO_2$, MgO and its lower values for $K_2O$. AV* overlaps the higher values of AI* and AIV for Cr, Cu, Ni and Zn. Hence, for these chemical elements and for the other element not illustrated, AIV cannot be separated from AI*. Moreover, there is no way to chemically split AIV from AI*. Hence, all the ceramics from Arbon Bleiche 3 are chemically very similar; even the most different petrographical groups (AI* vs. AIV vs. AV*) cannot be separated chemically. The outliers visible on these figures will be discussed further.

As said before, one could have thought that so many different petrographical groups would also divide into several chemical groups. Unfortunately, this is not the case. All the samples form, indeed, a single large homogeneous chemical group. Fig. 6.11 shows that there is, however, a tendency for the ceramics from Arbon Bleiche 3 (ceramics tempered with bone excepted) to chemically differ: on the left hand, the petrographical group AI (mainly tempered with granite) tends to split up from the petrographical group AV (mainly tempered with grog) visible on the right-hand side of the graph. These two petrographical groups were the most dissimilar of this study (except AVI, petrographical group with bone temper), and tend to split up only for $Na_2O$ and Ni.

Hence, because such a partition is very difficult to evidence, we propose that a single type of clay was used to produce almost all the ceramics from Arbon Bleiche 3. Accordingly, only small chemical differences due to the main temper present in the samples can be put into light, such as in Fig. 6.11.

### 6.6.2.3 Cluster analysis

The multivariate statistics permit us to study the correlation between the chemical variables. The cluster analysis groups the samples of similar chemical compositions (Fig. 6.12). Fig. 6.13: A-E illustrates the dendrogram with each sketch of the ceramics and the petrographical group they belong to. On Fig. 6.12, the separation between the pages of Fig. 6.13 is represented by a horizontal line. These separations do not imply any chemical grouping or any separation.

In a dendrogram, "each ceramic is represented by a vertical line at the basis of the diagram. The similarities that exist between two or more ceramics are more and more important as the horizontal line that unites them together is next to the basis of the diagram." (PICON, 1992, 6).

No clear grouping either of typological or petrographical groups was evidenced by such a dendrogram (Fig. 6.12). Only some typologically and petrographically similar ceramics can be put into evidence as very close chemically. The first group is indicated on Fig. 6.12 and 6.13: B, C by one asterisk; these are six Pfyn / Horgen pots (JB023, JB032, JB054, JB093, JB100, JB104) and one spindle whorl (JB114), mostly tempered with granite (petrographical group AI). The second group is indicated on Fig. 6.12 and 6.13D with two asterisks. These are six Pfyn / Horgen pots (JB038, JB044, JB056, JB061, JB062, JB135) and one special form
Bayern (JB153); all seven samples belong to group AI.
However, when discussing these chemical and petro-
graphical resemblances with A. de Capitani, she
explained that, from the archaeological point of view,
the vessels of these two groups do not have any similar
details (form, decoration...) and would not be consid-
ered as made by the same potter by an archaeologist.

The opposite has to be considered too: DE CAPITANI
(2002, 177) noticed that the spatial repartition of some
ceramics in the excavation showed several concentra-

tions of vessels with similar details. If these groups
could have been defined also archaeometrically, one
could have imagined a single potter, using one single
clay and one kind of temper for manufacturing vessels
in his own personal style. This is obviously not the
case: the groups with similar details as presented in DE
CAPITANI (2002) are shown with small letters (a to j)
on Fig. 6.13. There is no chemical proximity between
the samples of these groups. Hence, it is not possible
to describe groups of ceramics from Arbon Bleiche 3
surely made by one single potter.

<figure><img src="image_39.png" /><figcaption>Figure 6.10A: Petrographical groups AIV in relation with AI* and AV*; major elements (Fe₂O₃* as Fe₂O₃tot; numbers = sample numbers: JB...).</figcaption></figure>
<figure><img src="image_40.png" /></figure>

B

<figure><img src="image_41.png" /></figure>

<figure><img src="image_42.png" /></figure>

<figure><img src="image_43.png" /></figure>

<figure><img src="image_44.png" /></figure>

<figure><img src="image_45.png" /></figure>

**Figure 6.10B:** Petrographical groups AIV in relation with Al* and AV*; minor elements (numbers = sample numbers: JB...)

**Figure 6.11:** Na₂O versus Ni: petrographical groups Al and AV tend to split. For petrographical groups definitions see Table 5.1 and text (number = sample number: JB006)..
HIERARCHICAL CLUSTER ANALYSIS
Dendrogram using Average Linkage (Between Groups)

<figure><img src="image_46.png" /></figure>

<figure><img src="image_47.png" /></figure>

**Figure 6.12:** Dendrogram showing the results of the cluster analysis. * shows seven ceramics of the petrographical group AI chemically alike, six Pfyn/Horgen pots and one spindle whorl. ** show seven ceramics of the petrographical group AI chemically alike, six Pfyn/Horgen pots and one special form Bayern. Fig. 6.13A-E will show this dendrogram with the ceramics grouped as proposed here. Horizontal lines show the splitting of this dendrogram into several pages in Fig. 6.13 A-E.
<figure><img src="image_48.png" /><figcaption>**Figure 6.13A:** Illustration of the dendrogram (Fig. 6.12): each ceramic is presented (drawing de Capitani, AATG, M. Lier and E. Schön) and the typological and petrographical group (see Table 5.1) it belongs to is mentioned. Small letters (a, b, c, etc.) represent the ceramics with similar details (after DE CAPITANI 2002).</figcaption></figure>
<figure><img src="image_49.png" /><figcaption>**Figure 6.13B:** Illustration of the dendrogram (Fig. 6.12): each ceramic is presented (drawing AATG, M. Lier and E. Schön) and the typological and petrographical group (see Table 5.1) it belongs to is mentioned. Small letters (a, b, c, etc.) represent the ceramics with similar details (after DE CAPITANI 2002). * shows seven ceramics of the petrographical group AI chemically alike, six Pfyn/Horgen pots and one spindle whorl.</figcaption></figure>
<figure><img src="image_50.png" /><figcaption>**Figure 6.13C:** Illustration of the dendrogram (Fig. 6.12): each ceramic is presented (drawing AATG, M. Lier and E. Schön) and the typological and petrographical group (see Table 5.1) it belongs to is mentioned. Small letters (a, b, c, etc.) represent the ceramics with similar details (after DE CAPITANI 2002). * shows seven ceramics of the petrographical group AI chemically alike, six Pfyn/Horgen pots and one spindle whorl.</figcaption></figure>
<figure><img src="image_51.png" /><figcaption>**Figure 6.13D:** Illustration of the dendrogram (Fig. 6.12): each ceramic is presented (drawing AATG, M. Lier and E. Schön) and the typological and petrographical group (see Table 5.1) it belongs to is mentioned. Small letters (a, b, c, etc.) represent the ceramics with similar details (after DE CAPITANI 2002). ** show seven ceramics of the petrographical group AI chemically alike, six Pfyn/Horgen pots and one special form Bayern.</figcaption></figure>
As previously shown with the bivariate plots, all the ceramic samples presented here do not chemically match the typological or petrographical groups, being chemically similar (except some rare outliers discussed after). Therefore different provenance of the samples seems not plausible. Only small chemical differences (same clay, but several beds for example, or same clay, but various temper types or amounts) can lead to such a dendrogram. The exceptions presented at the end of Fig. 6.13E are put as outliers because of their position, separated from the other groups, in the dendrogram; they will be discussed below.

### 6.6.2.4 Principal component analysis (PCA)

As shown on Fig. 6.14A, no petrographical group can be separated in the ceramic from Arbon Bleiche 3 (except those tempered with bone that are not repre-

sented). Only some samples can be considered as exceptions, such as JB012 and JB070. Hence, we took the three major petrographical groups of Arbon Bleiche 3 (AI, 83 samples; AIV, 11 samples and AV, 49 samples, see Table 5.1) and repeated the PCA only with these samples (Fig. 6.14B). The result is somewhat better, but the groups are still not well separated. If we only include the groups AI and AV (Fig. 6.14C), and finally only the Pfyn / Horgen pots belonging to the group AI and the special form Boleráz belonging to group AV (Fig. 6.14D), the results become clearer, but even these latter two groups are not easy to differentiate. As mentioned in the last subsection, only small chemical differences can induce such a difficulty in separating the samples into groups.

PCA using the recalculated compositions of the samples containing bone as temper (see subsection 4.2.1.6.) shows that three potteries now figure in the

<figure><img src="image_52.png" /><figcaption>**Figure 6.13E:** Illustration of the dendrogram (Fig. 6.12): each ceramic is presented (drawing AATG, M. Lier and E. Schön) and the typological and petrographical group (see Table 5.1) it belongs to is mentioned. Small letters (a, b, c, etc.) represent the ceramics with similar details (after DE CAPITANI 2002). The drawings of the four ceramics containing bone temper are added, even if they are chemically very different from all the ceramics of Arbon Bleiche 3.</figcaption></figure>
<figure><img src="image_53.png" /></figure>

**Figure 6.14:** PCA results for: A: all the petrographical groups (see Table 6.3), B: the petrographical groups AI, AIV, AV; C: the petrographical groups AI and AV, D: Pfyn / Horgen pots AI and SF Boleráz AV. Note that the groups gradually separate better, but there is no way to split them totally (numbers = sample numbers: JB...).

<figure><img src="image_54.png" /></figure>

**Figure 6.15:** PCA of recalculated ceramics tempered with bone versus the main petrographical groups from Arbon Bleiche 3 (* for recalculated composition, numbers = sample numbers: JB...).

**Figure 6.16:** DA on the petrographical groups AI, AIV and AV (see Table 5.1). A fairly good separation between groups is almost achieved.
<figure><img src="image_55.png" /><figcaption>**Figure 6.17:** Histogram of the Mahalanobis distance (MD) for the special forms Boleráz (petrographical group AV) calculated in relation to the petrographical group Pfyn / Horgen pots (petrographical group AI). Both histograms overlap (one square = one sample; number in squares: sample number).</figcaption></figure>

<table><caption>**Fig. 6.18:** Possible exceptions in the samples from Arbon Bleiche 3 as a function of different chemical methods (descr. stat.: descriptive statistics; cluster: cluster analysis; PCA: principal component analysis; DA: discriminant analysis; JB....: sample numbers). On the right-hand side, drawing of the ceramics present two or more times in the table (drawings AATG, M. Lier and E. Schön), the typological and petrographical groups it belongs to (see Table 5.1).</caption><thead><tr><th colspan="6">Possible exceptions</th></tr><tr><th>Contamination</th><th>Descr. stat.</th><th>Cluster</th><th>PCA</th><th>DA</th><th>Mahalanobis</th></tr></thead><tbody><tr><td>JB002 ?</td><td></td><td>JB003</td><td></td><td></td><td></td></tr><tr><td></td><td>JB005</td><td>JB003</td><td></td><td>JB005</td><td></td></tr><tr><td></td><td>JB006</td><td>JB006</td><td>JB006</td><td></td><td></td></tr><tr><td></td><td>JB007</td><td>JB007</td><td></td><td></td><td></td></tr><tr><td>JB014</td><td></td><td>JB014</td><td>JB014</td><td></td><td>JB014</td></tr><tr><td></td><td>JB019</td><td>JB019</td><td>JB019</td><td></td><td></td></tr><tr><td>JB025 ?<br>JB028 ?<br>JB031 ?</td><td></td><td>JB047</td><td>JB047</td><td>JB047</td><td>JB047</td></tr><tr><td></td><td>JB034</td><td>JB047</td><td>JB047</td><td>JB052</td><td>JB052</td></tr><tr><td></td><td>JB047</td><td>JB047</td><td>JB047</td><td></td><td></td></tr><tr><td>JB056</td><td></td><td>JB059</td><td></td><td></td><td>JB059</td></tr><tr><td></td><td>JB070</td><td>JB070</td><td>JB070</td><td>JB070</td><td>JB070</td></tr><tr><td></td><td>JB073</td><td>JB073</td><td>JB073</td><td>JB092</td><td>JB092</td></tr><tr><td>JB061 ?</td><td></td><td>JB101</td><td>JB102</td><td></td><td>JB101</td></tr><tr><td></td><td>JB113</td><td>JB101</td><td>JB102</td><td></td><td></td></tr><tr><td></td><td>JB118</td><td>JB102</td><td>JB102</td><td></td><td></td></tr><tr><td></td><td>JB136</td><td>JB136</td><td>JB136</td><td></td><td></td></tr><tr><td></td><td>JB136</td><td>JB136</td><td>JB151</td><td>JB146</td><td>JB146</td></tr><tr><td></td><td>JB163</td><td>JB158</td><td></td><td></td><td></td></tr><tr><td></td><td>JB173</td><td>JB158</td><td></td><td></td><td></td></tr><tr><td></td><td>JB183</td><td>JB175</td><td>JB175</td><td></td><td>JB175</td></tr><tr><td></td><td>JB186</td><td>JB186</td><td>JB186</td><td></td><td></td></tr><tr><td></td><td>JB188</td><td>JB188</td><td>JB188</td><td></td><td></td></tr></tbody></table>

<figure><img src="image_56.png" /></figure>
range of the ceramic samples that do not contain bone (Fig. 6.15). This means that the clay used for these bone tempered samples is probably similar to the clays used for the other potteries. Only JB012, which also contains high proportions of TiO₂, Al₂O₃, Fe₂O₃, Ba, Cr, Nb, Ni, Pb, Sr, V, Y, Zn and Zr, whereas MgO, CaO, Na₂O and K₂O are lower, still stays apart from the other ceramics. A different clay must have been used to make this ceramic.

### 6.6.2.5 Discriminant analysis (DA)

DA calculates factors that maximise the differences between the pre-established groups (in this case, the petrographical groups). That statistical method did not permit to separate the ceramics into several well-distinguishe groups (Fig. 6.16); only the distinction due to the kind of temper used is perceptible and leads to this partial grouping of the samples.

### 6.6.2.6 Mahalanobis distance (MD)

The comparison between the two most different typological and petrographical groups of Arbon Bleiche 3, Pfyn / Horgen pots AI vs. the special form Boleráz AV is shown on Fig. 6.17. We can only observe a small difference between the two histograms of the MD. The histogram of the Pfyn / Horgen pots AI has the majority of its samples between 15 and 25, whereas those of the special form Boleráz AV are mainly between 20 and 35.

The grouping of the samples is very good: each histogram on Fig. 6.17 can be represented by a Gaussian curve. Moreover, even if one single histogram is made by the grouping of the two presented, a single Gaussian curve still includes all the samples.

The matching of both histograms is clear evidence that both groups are chemically similar and therefore of a same origin, i.e. there is no way to detect two different origins of the samples.

### 6.6.2.7 Exceptions

Fig. 6.18 shows the outliers put into light by the diverse methods presented higher. It was said before that one sample was surely contaminated, JB014. This one was an exception in three different methods, i.e.

cluster, PCA and DA. Other samples were possibly contaminated (2, 25, 28, 31, 61); they were never present in the outliers, whatever was the method used. These five samples were not contaminated enough to be considered as chemical exceptions.

Other ceramics, present as exceptions in only one method, were not chemically different enough form the other samples to be considered as outliers. It is the case for JB003, JB007, JB052, JB056, JB065, JB092, JB113, JB118, JB146, JB151, JB158, JB163, JB173 and JB183. Some samples are exceptions in two different methods (JB005, JB019, JB034, JB059, JB101, JB102, JB136 and JB188) or in three (JB006, JB014, JB047, JB070, JB073, JB175 and JB186). Note that in these latter samples, JB014 is contaminated and JB047 (petrographical group CI) is a sherd of a ceramic made of a carbonate-rich clay (CaO = 12.84 wt.%), which could be made with a similar clay than the one used to manufacture the non-ceramic material (mean CaO: 14.92 wt.%).

Hence, on 159 ceramics from Arbon Bleiche 3 (bone tempered ones excepted), only five (JB006, JB070, JB073, JB175 and JB186) are chemically quite different. These are surely made of a different clay. The other eight outliers present twice in Fig. 6.18 are also probably made of a dissimilar clay, but this affirmation shall be taken with care.

The 15 ceramics drawn on Fig. 6.18 are now considered as outliers and will not be part of the reference group of Arbon Bleiche 3.

## 6.7 REFERENCE GROUPS

### 6.7.1 Arbon Bleiche 3 – a new reference group

The potteries from Arbon Bleiche 3 are chemically similar and form one single group (in this case, the 13 outliers, plus JB014 – contaminated – and JB047 – made of a CaO-rich clay – are not part of this group). It is not possible to distinguish chemically the different petrographical groups. The question whereas the ceramics are local or imported can be answered with comparing this group to others reference groups.
## 6.7.2 Swiss Neolithic chemical reference groups versus Arbon Bleiche 3 ceramics

In this study, 163 pottery samples have been analysed, a number that is sufficient to delimit different chemical reference groups, if they are present, and to evaluate their homogeneity. Eight Neolithic reference groups of different Swiss sites (Appendix 10) were used for comparison.

First, the samples studied in Zürich (Kleiner Hafner) by SCHUBERT (1987). Second, the two reference groups defined in BENGHEZAL (1994A) as Vinelz-Sutz-Auvernier-Portalban-St. Blaise. Those groups, separated one from the other by their content in CaO, were not considered as homogeneous; as DI PIERRO (2002) discussed, both groups contain potteries, cob fragments, and loom weights together. We only used the raw chemical analyses of potteries of all these sites, as if they were five separated reference groups (Vinelz, Sutz, Auvernier, Portalban and St. Blaise). Third, the ceramics studied by DI PIERRO (2002): he defined two reference groups, Portalban and St. Blaise.

The Mahalanobis distances were calculated for all these samples in relation with those of Arbon Bleiche 3. The calculation was done with 18 available elements for Zürich (SiO₂, TiO₂, Al₂O₃, Fe₂O₃, MnO, MgO, CaO, Na₂O, K₂O, P₂O₅, Ba, Cr, Cu, Ni, Rb, Sr, Zn and Zr) and 22 elements for the other reference groups (the same ones plus Nb, Pb, V and Y). Figure 6.19 shows the Mahalanobis distances of the ceramics from Zürich versus those of Arbon Bleiche 3. Figure 6.20 shows the distances measured for all the other reference groups versus Arbon Bleiche 3. In both figures, the possible belonging of each ceramic to one or another reference group can be observed. Higher is the distance, lower is the probability for the sample to belong to the reference group.

The majority of the ceramics from Arbon Bleiche 3 (D2 < 25) can be distinguished from those of Zürich (D2 > 25, Fig. 6.19). However, the samples from Arbon Bleiche 3 with a Mahalanobis distance higher than 25 (23 samples) cannot be chemically distinguished. This overlap is attributed to the geographical proximity of these two sites and moreover, their similar geology (mollasic beds of the eastern Swiss).

All the samples from Arbon Bleiche 3 (D2 < 60, Fig. 6.20) are easily separated from those of Auvernier and St. Blaise. Only one sample (D2 < 55) from Portalban (BENGHEZAL, 1994A), Sutz and respectively

Vinelz superposes the higher distances of Arbon Bleiche 3 ceramics. However, the samples of DI PIERRO (2002) from Portalban do not separated well. This fact is difficult to explain, because those of BENGHEZAL (1994A) from Portalban separate much better.

All the mentioned reference sites lie in the Molasse basin (Fig. 6.21). Arbon Bleiche 3 and Zürich are between the Alps and the Jura, and were covered by the Rhine glacier, which carried moraine deposits from the Eastern Alps to the Constance Lake. Below the glacial deposits Upper Marine Molasse beds are present in Arbon Bleiche 3 and Zürich. In Zürich Upper Freshwater Molasse outcrops can also be found. These geological similarities explain the superposition of the samples observed on Fig. 6.19.

Vinelz, Sutz and Portalban are closer to the Jura Mountains, from which they are separated by the lakes of Biel and Neuchâtel. St. Blaise and Auvernier are lying on the Western side of the lake Neuchâtel, directly on the foot of the Jura chain. These last five sites were covered by the Rhône and partially the Aar glaciers during the glaciations, which carried material from the Western Alps. In Vinelz, Sutz and Portalban, the moraine deposits are underlain by Upper Marine Molasse and of Lower Freshwater Molasse beds. In St. Blaise and Auvernier, Mesozoic rocks related to the Jura Mountains are also close to the surface. These geological differences can explain the separations between the samples of the sites presented on Fig. 6.20, except for Portalban (DI PIERRO, 2002).

As a conclusion, the samples of Arbon Bleiche 3 cannot be attributed to an existing reference group, and, hence, are defined as a new Swiss Neolithic reference group. The chemical differences within the Pfyn / Horgen pots, the special forms and the spindle whorls are small enough to form one single reference group, despite the petrographical differences described in the samples.

As specified in MAGGETTI (1995A, 236), "the results concerning the reference groups should be taken with care, because a sample today resembling a reference group can be tomorrow better correlated with a new defined reference group. A reference group is established with only a few samples (n= 30-100), which is not a guaranty of the representativeness of all the production site."
<figure><img src="image_57.png" /><figcaption>**Figure 6.19:** Histogram of the Mahalanobis distance (MD) for the reference group Zürich Kleiner Hafner calculated in relation to the ceramics from Arbon Bleiche 3. The histograms are separated (one square = one sample; number in white squares: sample number).</figcaption></figure>
<figure><img src="image_58.png" /><figcaption>**Figure 6.20:** Histogram of the Mahalanobis distance (MD) for seven Swiss Neolithic reference groups calculated in relation to the ceramics from Arbon Bleiche 3. Each histogram is separated from that of Arbon Bleiche 3 (one square = one sample; number in white squares: sample number).</figcaption></figure>
## 6.8 SPATIAL REPARTITION

PÉTREQUIN ET AL. (1994, 1996) describe the domestic production of pottery in Chalain during final Neolithic as follows: each household exploits its own raw material to manufacture the ceramics it needs. In this case, temper and matrix used in one house should be differentiable from those used in other houses if the potters used different clays and/or tempers.

DE CAPITANI (2002) observed no correlation between the archaeological typology and no spatial distribution in the houses.

The petrographical and chemical groups defined in this work did neither show any particular relation with houses. Even the smallest groups of ceramics (AII: n=4; AVI: n=4; BI: n=2; B2: n=3 and CI: n=5) were not found in a single house (Fig. 6.22).

<figure><img src="image_59.png" /><figcaption>**Figure 6.21:** Map of Switzerland with the emplacement of the Swiss Neolithic reference groups; AB: Arbon Bleiche 3, AU: Auvernier La Saunerie, PO: Portalban, SB: St. Blaise, SU: Sutz, ZU: Zürich Kleiner Hafner.</figcaption></figure>

As defined in the beginning, the Pfyn / Horgen pots are though by the archaeologists to be local ceramics, due to their typology, number abundance and manufacturing process. As shown by the chemistry, the local clays could correspond with the clays used to manufacture these Pfyn / Horgen pots. Moreover, all the ceramics from Arbon Bleiche 3 (except 15 outliers, plus JB012, tempered with bone) show only small chemical variations, but cannot be split into several groups. Hence, we propose that all the ceramics from Arbon Bleiche 3 (except these 16 outliers) were made of local clays.

The presence of one kind of clay used to manufacture ~90% of the studied ceramics induces the idea of one or several potter(s) producing ceramics for the whole village. The source of clay was certainly a precise pit, local, and bound to a single geological bed. In such a case, it is no surprise that so many ceramics show so few chemical variations (see chapter 8).

<figure><img src="image_60.png" /><figcaption>**Figure 6.22:** Map of the excavations of Arbon Bleiche 3 with the precise location of the studied sherds for several small petrographical groups (AII, AIII, AIV, AVI, BI, BII, CI, CII, CIII).</figcaption></figure>
# 7 - ARCHAOMETRICAL RESULTS CONCERNING THE CERAMIC MATERIAL: THE 14 SAMPLES OF POTTERIES FROM THE WESTERN CARPATHIAN BASIN

## 7.1 INTRODUCTION

The archaeological typology and the presence of bone temper in four ceramic pieces from Arbon Bleiche 3 have induced a necessary comparison with 14 sherds coming from the western Carpathian Basin (Baden culture). The 14 samples studied come from three different regions: five ceramics from Mödling “Jennyberg” (A), five from Žlkovce (SK) and four from Náměšť na Hané (CZ) (DE CAPITANI, 2002, 214).

## 7.2 MACROSCOPIC DESCRIPTION

All the sherds resemble strongly to those of the special form Boleráz from Arbon Bleiche 3: the sherds are thin (< 8 mm), black or grey with a black core and tempered with small beige to brown grains (grog). One sample also contains white grains or fragments (rock) as temper.

## 7.3 PETROGRAPHICAL STUDY

The petrographical study showed that all the samples from the western Carpathian Basin have an inclusion-poor and silicate-rich matrix. 93% of the ceramics were mostly tempered with grog (13 samples have a similar aspect to those of petrographical group AV of Arbon Bleiche 3). Granite mostly tempered only one sample (this sample from Mödling, JB201, is alike petrographical group AI of Arbon Bleiche 3).

None of these fourteen samples was tempered with bone, but six thin sections contained a few small fragments of bone (JB202, JB203, JB208, JB212: one fragment; JB200: two fragments; JB213: three). A

direct correlation between these ceramics and the petrographical group AVI of Arbon Bleiche 3 (ceramics tempered with bone) is not possible, but this can go back to the insufficient number of samples studied.

## 7.4 CHEMICAL DESCRIPTION

First goal of the chemical investigation of the 14 samples from the western Carpathian Basin was to detect chemical differences to those from Arbon Bleiche 3. We also wanted to know if some potteries from Arbon Bleiche 3 could be chemically alike these samples and therefore show a far provenance.

A comparison between the ceramics from the three sites of the western Carpathian Basin (Mödling, Appendix 9D; Žlkovce, Appendix 9E and Náměšť na Hané, Appendix 9F) and those from Arbon Bleiche 3 mainly tempered with grog and with less or no granite (petrographical group AV, Appendix 9G) was done with descriptive statistics. The ceramics made in Mödling contained less SiO₂, Cu and Zn, and more TiO₂, Al₂O₃, Fe₂O₃, MnO, Cr, Pb, V, Y and Zr than those from Arbon Bleiche 3. Those from Žlkovce contained less Cu and more Fe₂O₃, MnO, Na₂O, K₂O, Sr, Y and Zr whereas those of Náměšť na Hané were poorer in CaO, Ba, Cu, Ni, Sr and Zn and richer in TiO₂, Fe₂O₃, P₂O₅, Y and Zr. As shown on Fig. 7.1, PCA permit to distinguish the petrographical group AV from Arbon Bleiche 3 from the ceramics from the three western Carpathian Basin sites, respectively Mödling (Fig. 7.1A), Žlkovce (Fig. 7.1B) and Náměšť na Hané (Fig. 7.1C). Only one sample, JB175, a chemical outlier in the ceramics from Arbon Bleiche 3 can maybe be put into relation with the ceramics from Žlkovce, due to their proximity on Fig. 7.1B.
All three western Carpathian Basin groups are too different from the ceramics of the petrographical group AV of Arbon Bleiche 3 to think of an importation of ceramics from the western Carpathian Basin to Arbon.

All the ceramics from the western Carpathian Basin have a higher content of Y (up to 51 ppm) than the potteries from Arbon Bleiche 3. We mentioned before, that sample JB012 from Arbon Bleiche 3, the possible exogenous ceramic, has a high proportion of Y (444 ppm). Hence, the content of Y in the samples from the western Carpathian Basin is too low to show a relation with JB012. The value of 444 ppm Y is very uncommon, and it will be a challenge for the future to find the provenance of this clay.

Fig. 7.2 presents the Mahalanobis distances (MD) of the Pfyn / Horgen pots of the petrographical group AI and the special form Boleráz of the petrographical group AV from Arbon Bleiche 3 versus the ceramics from the western Carpathian Basin. The relation between these histograms is very different from that of Fig. 6.17. The MD of the majority of the samples from the western Carpathian Basin is high, between 45 and 55, whereas the one of the ceramics from Arbon Bleiche 3 (Pfyn / Horgen pots AI and special form Boleráz AV) is between 10 and 35. Hence, we can deduce by the chemistry that the samples from Arbon Bleiche 3 have a different provenance than those of the western Carpathian Basin.

<figure><img src="image_61.png" /><figcaption>**Figure 7.1:** PCA for the petrographical group AV from Arbon Bleiche 3 (mainly tempered with grog) versus the ceramics from the western Carpathian Basin; A: Mödling, B: Žlkovce, C: Náměšt na Haně</figcaption></figure>
<figure><img src="image_62.png" /><figcaption>**Figure 7.2:** Histogram of the Mahalanobis distance for the ceramics from the Western Carpathian Basin calculated in relation to the reference groups Pfyn / Horgen pots (petrographical group AI) and SF Boleráz (petrographical group AV). The histograms are quite dissimilar (one square = one sample; number in squares: sample number).</figcaption></figure>
The samples circled on Fig. 7.2 are considered as exceptions and were previously discussed (subsection 6.6.2.7). Even if these potteries show a Mahalanobis distance just below or in the range of that of the ceramics

from the western Carpathian Basin, a relationship cannot be deduced. Indeed, the PCA presented before have shown a clear division between these exceptions and the samples from the western Carpathian Basin (Fig. 7.1).
# 8 - ARCHAOMETRICAL RESULTS CONCERNING THE POTENTIAL TEMPER AND CLAY RESSOURCES OF THE NEOLITHIC VILLAGE

## 8.1 THE ROCKS

On the lake shore near Arbon, a "museum of erratic blocks" was created in the 1930s. These rocks were all discovered in-situ and were brought there by the Rhine glacier. According to WEGELIN (1936), they are composed of (Fig. 8.1): (1). Suretta-Rofna-Porphyroid. (Quartz-porphyroid, rich in orthoclase, provenience: Via Mala, travel distance: 135 km along the Rhine valley); (2). Syenite (Taspin Alps, coarse-grained,

crystalline rock with big, white feldspars, small grey quartz and pale green to grey micas; (3). Epidote-Chlorite-Hornblende Schist (from the Valsertal region); (4). Granite from the Julier region; (5). Light coloured granites (uncertain provenance); (6) Banded gneiss (from Val Somvix, Greina or Val Gonda or Gotthardmassiv, West Val Medels); (7). Paragneiss (from Silvretta or Adula or Gotthardmassiv); (8). Granite (from Julier or Albula, Amphibole-biotite granite with apple-green plagioclases); (9). Pegmatite (from Tavetsch and Somvitg); (10). Red Verrucano (from the region of Davos, conglomerate with pebbles of quartzite, rhyolite and ophiolite); (11). Amphibolite (maybe from Val Puntaiglas or Medelser Gipfeln or Piz Valdrans); (12). Granite (from Val Puntaiglas, with big orthoclase twinning and titanite); (13) Many kinds of limestones, including one shelly sandstone.

<figure><img src="image_63.png" /><figcaption>**Figure 8.1:** The Rhine River Basin and the provenance of the rocks described in the "museum of erratic blocks"; the number refer to text.</figcaption></figure>

<table><caption>**Table 8.1:** Relation between the nomenclature used for the names of rocks in this work and in WEGELIN (1936); the numbers refer to text and to figure 8.1.</caption><thead><tr><th colspan="4">Bonzon</th></tr></thead><tbody><tr><th colspan="2">Granite</th><th>Rhyolite</th><th>Chert</th><th>Gabbro</th></tr><tr><td colspan="2">large grains of:<br>quartz<br>alcaline feldspars<br>plagioclases<br>micas</td><td>large grains of:<br>quartz<br>alcaline feldspars<br>plagioclases<br>micas</td><td>very small<br>grains of:<br>quartz</td><td>large grains of:<br>plagioclases<br>pyroxenes<br>sometimes with<br>hornblende,<br>olivines, micas</td></tr><tr><td colspan="2">no matrix</td><td>glassy matrix</td><td>no matrix</td><td>no matrix</td></tr><tr><th colspan="4">Wegelin (1936)</th></tr><tr><th colspan="2">Granite<br>Pegmatite</th><th colspan="2">Porphyroïde</th></tr><tr><td colspan="2">numbers:<br>4, 5, 8 & 12<br>9</td><td colspan="2">number:<br>1</td></tr><tr><td colspan="2">Present as<br>pebbles in<br>Verrucano<br>number 10</td><td colspan="2">Present as<br>pebbles in<br>Verrucano<br>number 10</td></tr><tr><td colspan="2">Present as<br>pebbles in<br>Verrucano<br>number 10</td><td colspan="2">Present as<br>pebbles in<br>Verrucano<br>number 10</td></tr></tbody></table>
The relation between the rocks described as temper in this thesis and those used by WEGELIN (1936) are shown on Table 8.1.

The Neolithic people used mainly granites and smaller amounts of gabbros, rhyolites and cherts to temper their potteries. All those rocks are still present on the shore of Lake Constance, near Arbon. Various kinds of coarse granitic rocks are available in the morainic deposits (numbers 4, 5, 8, 9 and 12 in the above description). Gabbros, rhyolites and cherts are also present: the gabbros could have been carried from the ophiolite zones described near Arosa and Platta sheet or from calc-schists in the southern part of the Rhine River, between Chur and the Splügen pass. The rhyolites can come from the upper part of the Rhine River basin, in the dykes and effusive rocks of the Permian, in the south-west region of Davos. The cherts are frequent as nodules in the limestones of the Cretaceous Period, between Buchs and the Lake of Walenstadt area or in the neighbourhood of Landquart (SPICHER, 1980). It is also possible to find those kinds of rocks as pebbles in the Verrucano conglomerate (number 10).

Our microscopic observations, made on small fragments of rock in ceramic sherds, do not allow a more precise identification of a rock from a specific region of the Alps.

## 8.2 THE LOCAL CLAYS

### 8.2.1 Description of the CaO-rich clays

The eight CaO-rich samples were collected in the surroundings of Arbon, three in the moraines, JB300, JB302, JB303 and five in the Molasse, JB306–JB310 (precise provenance see Fig. 2.11). These yellow to beige samples have an inclusion-rich matrix and are petrographically very similar. Their matrix is homogeneous, containing 10 to 30 vol.% quartz grains (<0.01–0.5 mm) as natural inclusions. The smaller inclusions are rounded to sub-rounded; larger grains are sub-angular to angular.

As special features, JB308 contains one sub-angular grain of sandstone (10 mm Ø), and JB310 one grain of rounded amphibolite (0.5 mm Ø).

<table><caption>**Table 8.2:** Chemical data of the local clays collected in the surroundings of Arbon.</caption><thead><tr><th rowspan="2">Oxide, Element</th><th colspan="10">Carbonate-rich clays</th><th colspan="5">Silicate-rich clays</th></tr><tr><th>JB300</th><th>JB302</th><th>JB303</th><th>JB306</th><th>JB307</th><th>JB308</th><th>JB309</th><th>JB310</th><th>Std. Deviation</th><th>Variation Coefficient</th><th>JB301</th><th>JB304</th><th>JB305</th><th>Std. Deviation</th><th>Variation Coefficient</th></tr></thead><tbody><tr><td>SiO2 (wt.%)</td><td>70.64</td><td>74.07</td><td>64.91</td><td>59.94</td><td>56.56</td><td>56.97</td><td>56.22</td><td>53.51</td><td>7.48</td><td>0.140</td><td>73.71</td><td>70.22</td><td>77.70</td><td>3.74</td><td>0.048</td></tr><tr><td>TiO2 (wt.%)</td><td>0.39</td><td>0.49</td><td>0.40</td><td>0.57</td><td>0.62</td><td>0.46</td><td>0.46</td><td>0.47</td><td>0.08</td><td>0.167</td><td>0.78</td><td>0.78</td><td>0.74</td><td>0.03</td><td>0.036</td></tr><tr><td>Al2O3 (wt.%)</td><td>6.81</td><td>9.28</td><td>7.23</td><td>11.41</td><td>12.84</td><td>10.26</td><td>10.23</td><td>10.61</td><td>2.02</td><td>0.191</td><td>13.94</td><td>14.49</td><td>11.93</td><td>1.35</td><td>0.113</td></tr><tr><td>Fe2O3 (wt.%)</td><td>2.38</td><td>3.52</td><td>2.66</td><td>4.37</td><td>4.76</td><td>3.66</td><td>3.73</td><td>3.88</td><td>0.79</td><td>0.205</td><td>5.51</td><td>5.70</td><td>4.48</td><td>0.66</td><td>0.147</td></tr><tr><td>FeO (wt.%)</td><td>1.50</td><td>0.94</td><td>1.57</td><td>0.57</td><td>0.66</td><td>1.33</td><td>1.28</td><td>1.54</td><td>0.40</td><td>0.259</td><td>1.23</td><td>0.58</td><td>0.54</td><td>0.39</td><td>0.717</td></tr><tr><td>MnO (wt.%)</td><td>0.09</td><td>0.06</td><td>0.09</td><td>0.07</td><td>0.09</td><td>0.08</td><td>0.08</td><td>0.08</td><td>0.01</td><td>0.134</td><td>0.13</td><td>0.09</td><td>0.08</td><td>0.03</td><td>0.331</td></tr><tr><td>MgO (wt.%)</td><td>2.04</td><td>1.68</td><td>1.74</td><td>2.65</td><td>2.59</td><td>3.63</td><td>3.83</td><td>5.14</td><td>1.20</td><td>0.234</td><td>1.95</td><td>1.61</td><td>1.28</td><td>0.34</td><td>0.262</td></tr><tr><td>CaO (wt.%)</td><td>15.09</td><td>8.34</td><td>20.35</td><td>18.51</td><td>19.90</td><td>21.74</td><td>22.43</td><td>23.59</td><td>4.95</td><td>0.210</td><td>3.74</td><td>0.99</td><td>1.57</td><td>1.45</td><td>0.923</td></tr><tr><td>Na2O (wt.%)</td><td>0.97</td><td>0.86</td><td>0.78</td><td>0.22</td><td>0.20</td><td>0.97</td><td>0.98</td><td>0.73</td><td>0.32</td><td>0.444</td><td>0.83</td><td>0.29</td><td>0.38</td><td>0.29</td><td>0.761</td></tr><tr><td>K2O (wt.%)</td><td>1.43</td><td>1.67</td><td>1.42</td><td>2.17</td><td>2.34</td><td>2.04</td><td>1.97</td><td>2.05</td><td>0.34</td><td>0.167</td><td>2.38</td><td>2.44</td><td>2.06</td><td>0.20</td><td>0.099</td></tr><tr><td>P2O5 (wt.%)</td><td>0.18</td><td>0.11</td><td>0.27</td><td>0.12</td><td>0.09</td><td>0.12</td><td>0.13</td><td>0.12</td><td>0.06</td><td>0.479</td><td>0.13</td><td>0.07</td><td>0.06</td><td>0.04</td><td>0.631</td></tr><tr><td>Ba (ppm)</td><td>240</td><td>273</td><td>291</td><td>249</td><td>278</td><td>258</td><td>261</td><td>270</td><td>16.4</td><td>0.061</td><td>382</td><td>325</td><td>294</td><td>44.6</td><td>0.152</td></tr><tr><td>Cr (ppm)</td><td>61</td><td>71</td><td>60</td><td>87</td><td>90</td><td>78</td><td>70</td><td>73</td><td>10.9</td><td>0.149</td><td>106</td><td>109</td><td>98</td><td>5.7</td><td>0.058</td></tr><tr><td>Cu (ppm)</td><td>32</td><td>62</td><td>37</td><td>39</td><td>32</td><td>26</td><td>28</td><td>25</td><td>11.9</td><td>0.477</td><td>29</td><td>32</td><td>30</td><td>1.5</td><td>0.051</td></tr><tr><td>Nb (ppm)</td><td>8</td><td>10</td><td>8</td><td>14</td><td>14</td><td>10</td><td>10</td><td>11</td><td>2.3</td><td>0.211</td><td>16</td><td>16</td><td>14</td><td>1.2</td><td>0.083</td></tr><tr><td>Ni (ppm)</td><td>24</td><td>32</td><td>28</td><td>43</td><td>47</td><td>39</td><td>40</td><td>40</td><td>7.9</td><td>0.196</td><td>57</td><td>54</td><td>43</td><td>7.4</td><td>0.171</td></tr><tr><td>Pb (ppm)</td><td>46</td><td>17</td><td>40</td><td>15</td><td>16</td><td>18</td><td>15</td><td>13</td><td>12.8</td><td>0.986</td><td>32</td><td>24</td><td>21</td><td>5.7</td><td>0.271</td></tr><tr><td>Rb (ppm)</td><td>65</td><td>86</td><td>73</td><td>120</td><td>132</td><td>98</td><td>98</td><td>100</td><td>22.3</td><td>0.223</td><td>145</td><td>145</td><td>124</td><td>12.1</td><td>0.098</td></tr><tr><td>Cr (ppm)</td><td>332</td><td>201</td><td>335</td><td>492</td><td>596</td><td>574</td><td>580</td><td>531</td><td>146.8</td><td>0.276</td><td>145</td><td>83</td><td>90</td><td>34.0</td><td>0.377</td></tr><tr><td>Sr (ppm)</td><td>41</td><td>71</td><td>52</td><td>105</td><td>109</td><td>82</td><td>78</td><td>82</td><td>23.3</td><td>0.285</td><td>109</td><td>122</td><td>94</td><td>14.0</td><td>0.149</td></tr><tr><td>V (ppm)</td><td>25</td><td>28</td><td>25</td><td>28</td><td>25</td><td>25</td><td>26</td><td>24</td><td>1.5</td><td>0.062</td><td>34</td><td>40</td><td>33</td><td>3.8</td><td>0.115</td></tr><tr><td>Y (ppm)</td><td>151</td><td>56</td><td>78</td><td>121</td><td>62</td><td>64</td><td>69</td><td>64</td><td>33.3</td><td>0.483</td><td>92</td><td>97</td><td>75</td><td>11.5</td><td>0.154</td></tr><tr><td>Zr (ppm)</td><td>258</td><td>201</td><td>257</td><td>227</td><td>149</td><td>174</td><td>172</td><td>154</td><td>43.9</td><td>0.285</td><td>223</td><td>264</td><td>303</td><td>40.0</td><td>0.132</td></tr></tbody></table>

+, √, -: value respectively under, in, and over the range shown in appendix 9A (see text)
All these clays are composed of illite, quartz, K-feldspars, plagioclases, calcite and dolomite (Fig. 8.2). Chlorite is present in JB302, JB308, JB309 and JB310 and hematite in JB300, JB308, JB309 and JB310. Note that the presence of dolomite is typical in clays from the North-East Switzerland, as shown in MUMENTHALER (1979).

The CaO-rich local clays (Table 8.2) were chemically compared to the samples of the loom weight and the cobs (Fig. 5.1; Appendix 9A), in order to demonstrate if some clay could correspond to those used to manufacture this kind of material. JB302 (see Table 8.2) is the one that fits best: 18 elements are in the same ranges as those on Appendix 9A. SiO₂ is a little bit low, but it can vary a lot from one bed to another and also in the same geological bed (SIGG ET AL. 1986). This value is near enough to the range to be acceptable.

## 8.2.2 Description of the CaO-poor clays

Three clays with a silicate-rich matrix (JB301, JB304, JB305) were collected. They are grey, greyish-white or bluish-grey.

JB301 (Fig. 5.1L) contains natural, non-plastic inclusions similar to those described in the thin sections of the ceramics from Arbon Bleiche 3, such as granite and chert, quartz, amphiboles and rare calcite grains, ARF and little iron oxide nodules.

JB304 matrix can be divided into different zones, each containing more or less important percentage of

natural inclusions, which was also visible in some ceramics. Only particles of granite and quartz are visible as natural inclusions.

JB305 contains a very high percentage of natural inclusions, and could only be used to manufacture the ceramics with an inclusion-rich and silicate-rich matrix (petrographical groups B, hence 5 on 163 samples, see Table 5.1).

The granulometric study of these three clays shows that JB301 has a unimodal grain size distribution in contrast to JB304 and JB305, which have respectively a bi- and tri-modal grain size distribution (Fig. 8.3). These two last clays contain one class of bigger particles (15-50 µm), which is not present in JB301. This method, however, did not permit to define a proper signature for each clay that could have assured their distinction.

JB301, JB304 and JB305 contain similar clay minerals: a mixed layer illite / smectite, chlorite and illite in both argillaceous fractions ($<2 \mu m$, 2-16 µm; Table 8.3), plus quartz, K-feldspar and plagioclase. The three silicate-rich matrix clays are very similar; only the quantity of natural inclusions varies.

A chemical comparison was made between the CaO-poor clays (Table 8.2) and the ceramics from Arbon Bleiche 3 of Appendix 9B. JB301 fits the best with all the 23 chemical elements of the ceramics from Arbon Bleiche 3 (even if MnO = 0.13 wt.% and the minimum value of the range is 0.14 wt.% MnO).

As demonstrated by DI PIERRO (2002), a calculated ideal solution (Fig. 8.4A) shows that the mixing of a

<figure><img src="image_64.png" /><figcaption>**Figure 8.2:** X-ray diffractograms of eleven local clays permitting to separate carbonate-rich and silicate-rich matrixes (cc: calcite, ch: chlorite, dol: dolomite, hm: hematite, il: illite, Kf: K-feldspars, pl: plagioclase, qz: quartz).</figcaption></figure>
<figure><img src="image_65.png" /><figcaption>**Figure 8.3:** Granulometric study of the matrix of the three silicate-rich local clays; horizontal axis: grain size diameter, vertical axis: volume percent of the grains (histogram and cumulative curve).</figcaption></figure>
<table><caption>**Table 8.3:** The mineral present in two fractions (2-16 µm, < 2 µm) of the three silicate-rich local clays.</caption><thead><tr><th rowspan="2">Local clays</th><th colspan="3">2-16 µm</th><th colspan="3">&lt; 2 µm</th></tr><tr><th>Mix. I/S</th><th>Chlorite</th><th>Illite</th><th>Mix. I/S</th><th>Chlorite</th><th>Illite</th></tr></thead><tbody><tr><td>JB301</td><td>2</td><td>3</td><td>3</td><td>2</td><td>3</td><td>3</td></tr><tr><td>JB304</td><td>2</td><td>2</td><td>2</td><td>3</td><td>3</td><td>3</td></tr><tr><td>JB305</td><td>2</td><td>2</td><td>2</td><td>3</td><td>2</td><td>2</td></tr></tbody><tfoot><tr><td colspan="7">Mix. I/S = Mixed layer Illite / Smectite<br>1: a few, 2: middle, 3: much</td></tr></tfoot></table>

clay (right hand side) and 23 vol.% of granite (temper, left hand side) giving potteries (centre) are in linear correlation. The latter are situated somewhere on the line between clay and granite as a function of their volume. The same graph is presented for the ceramics from Arbon Bleiche 3 and three silicate-rich clays (Fig. 8.4B). The silicate-rich clays sampled in the surroundings of Arbon do not correspond to the ones used to manufacture the potteries. If the clay used was represented, it would lie on the right hand side of the ceramics. The potteries being the result of the mixing of granite temper (grey area on Fig. 8.4B) and clay must lie somewhere on the correlation line between the two raw materials.

As mentioned before, the proportion of quartz in a geological bed varies a lot, linked with its depositional environment. Maybe the clay used in the Neolithic times is not far away from the JB301 clay, which was collected less than 500 m far from the village.

### 8.2.3 Interpretation

As discussed before, these observations confirm the possibility for the potters of Arbon Bleiche 3 to have found local clay in the surroundings to manufacture the ceramics. Because the local clays petrographically and mineralogically correspond to the ceramics, and as no chemical diversity was put into light within the chemical analyses, the majority of the ceramics from Arbon Bleiche 3 are surely local, as defined by archaeologists, with a well defined and proximal source.

However, as demonstrated higher, the clays sampled in the surroundings of the site do not fit perfectly well –in a chemical point of view– with the ceramics of Arbon Bleiche 3.

<figure><img src="image_66.png" /><figcaption>**Figure 8.4:** Chemical correlation for SiO₂ and Al₂O₃: A: Ideal situation: the potteries lie on the correlation line between clays and temper (Di PIERRO, 2002); B: Arbon Bleiche 3 situation: clays and tempers are both on the left hand side of the potteries.</figcaption></figure>
# 9 - FINAL CONCLUSIONS

Arbon Bleiche 3 is a typical Swiss Neolithic lacustrine village; occupied between 3384 and 3370 BC, its remains were well preserved in wet ground.

The study of the archaeological material of this site was carried over by de Capitani (2002).

In this work, 153 potteries, 10 spindle whorls, 11 cob fragments and one loom weight from Arbon Bleiche 3 were analysed petrographically, mineralogically and chemically. 12 ceramics from the western Carpathian Basin were also studied.

Several very interesting main points result from this work:

## 9.1 COMPOSITIONAL DISCREPANCY BETWEEN THE NON-CERAMIC AND THE CERAMIC MATERIAL

The non-ceramic material (cob fragments and loom weight) were made of an inclusion-rich and carbonate-rich clay, whereas 93% of the ceramics are made of an inclusion-poor and silicate-rich clay.

The cobs and loom weights are respectively non-tempered and tempered with organic material (straw, grass, hair...); on the contrary, the ceramics are tempered with rock fragments (granite, gabbro, rhyolite, chert), with grog and/or with bone.

Because the organic temper is still present in the thin section and did not disappear during a firing process, the loom weight was therefore not fired. No trace

of firing is either observed in the thin sections of the cob fragments. Only the fire that destroyed the village modified this material (black marks on external surfaces).

Only six ceramic pieces were built with that type of carbonate-rich clay (only 4% of the ceramics; Table 6.3). Even if this clay probably needed less temper to be fired – because it was containing many natural inclusions – the same proportion of rocks tempered these samples. Maybe the clay was also harder to mould. Hence, these samples must be considered as exceptions and even as manufacturing errors. The Neolithic people probably knew that this kind of clay did not suit for ceramics.

These important differences between non-ceramic and ceramic material is also constant in the western Swiss Plateau (Benghezal, 1994a; Di Pierro, 2002) and has also been observed in the French Jura (Martineau, oral communication). The Neolithic people used obviously one kind of sediment for non-fired material (cob fragments and loom weights), and a different silicate-rich clay for the fired material (potteries and spindle whorls). They knew well how to differentiate sediments and made a conscious choice to collect them.

The carbonate-rich clay used to waterproof the houses (cob) and to manufacture the loom weights is probably local (as defined in Médard, 2000) and even to be found just inside the village or at least less than 500 m from it (Leuzinger, 2000). Moreover, the high amount of clay needed to build a house is so important (Ramseyer, 1985) that a distant provenance is quite improbable.
## 9.2 CERAMICS: PETROGRAPHICAL DIVERSITY VS. CHEMICAL HOMOGENEITY

Constantin and Courtois (1985) wrote: "The sherds that have followed the same production process can be named "material group"; there is mainly a correlation between the "material groups" and the types of forms, as there is often a correlation between the types of forms and the types of adornments". Hence, it seemed reasonable to think that the typological groups defined by de Capitani (2002) would also be differentiated according to the petrographical and mineralogical observations. Nevertheless, no direct relationship between the petrographical and typological groups was noticed for the ceramics. However, this absence of relation is frequent and not linked to a preferential period or any specific area (Echallier and Courtin, 1994a, 1994b and Echallier and Thiercelin, 1991).

93% of the ceramics are made of an inclusion-poor and silicate-rich clay. These samples divide into six petrographical groups, according to their main temper (54% are mainly tempered with granite, 32% with grog, 7% with gabbro, 3% with rhyolite, 3% with bone and 1% with chert; table 5.1). This important variety of temper used is quite unusual in the Neolithic and reinforces the impression of a not well-established ceramic tradition due to the cultural mixing of the site. A conscious choice is proven, because no limestone and no dark rocks such as amphibolites are used, even if they are frequent in the surroundings of the site.

Even with such a petrographical variation and so many stylistic separations, all these ceramics form a chemically largely homogeneous group. Within it, multivariate analysis have permitted to cluster several quite identical samples (see * and ** on Fig. 6.12). Besides, 13 chemical outliers have been pointed out, together with JB014 (contaminated) and JB047 (made of a carbonate-rich clay).

Only for a few elements, like Na₂O and Ni for example, a quite good separation can be made between the two main different petrographical groups AI vs. AV, i.e. granite vs. grog temper. This is due to the differences in tempering. In this case, Na₂O is bound to the granite pieces that preferentially temper group AI, whereas Ni is typical for the clay and the grog mostly present in group AV (Fig. 6.11). Hence, the chemical variations observed in the samples are mainly linked with the kind of temper used in the ceramics.

The homogeneity of the raw chemical compositions of most pottery samples over different stylistic

categories is an interesting result. De Capitani (2002) showed typological parallelism between ceramics from Arbon Bleiche 3 and ceramics from Bavaria and the Western Carpathian Basin. The question was whether these ceramics were imported or not. Considering the chemical resemblance, a foreign origin of the pottery is quite unlikely. We propose a local provenance for almost all the potteries studied, forming one single chemical group. Only nine samples are surely chemically different, but an exact provenance cannot be suggested.

Three samples of silicate-rich clays were collected in the surroundings of Arbon. These are petrographically and mineralogically compatible with the material used to make the ceramics. JB301, collected in the near vicinity of the archaeological excavation (Fig. 2.11), fits well with the chemistry of the ceramics. Its SiO₂-content is too high, but it can be correlated with the high percentage of natural temper it contains. Moreover, SiO₂ variations in one single geological bed are typical of such sediments with a glacio-lacustrine origin (Sigg et al., 1986).

All the rocks used as temper can also be found in the surroundings of Arbon, in the Rhine moraines. These facts also incline to a local manufacturing of the ceramics.

## 9.3 OBSERVATION OF THE FIRST BONE TEMPERED SWISS NEOLITHIC CERAMICS

For the first time, bone temper was identified in Swiss Neolithic ceramics, after being described in France and Holland during Mid-Neolithic. Four samples of potteries tempered with bone were described in this work. Only 2% of the ceramics from Arbon Bleiche 3 are of this kind. The presence of bone was assured by XRD, XRF, SEM and microprobe (Bonzon, 2004b). If the assumption that bone temper was not an established temper neither in the Western Carpathian Basin nor in Switzerland is correct, the only explanation for the combination of Northern European technology with Eastern European shapes found in a Central European site, is multiple exchange of material, culture and/or technology over long distances. But a larger study in the Western Carpathian Basin should be done to prove the absence of bone temper in this region.

Based on typological analogies, De Capitani (2002) proposed a foreign origin for these peculiar ceramics: the Boleráz Stage from the Western Carpathian Basin.
Apart from one (JB012), they are chemically similar to the other potteries from Arbon Bleiche 3, which implies their local manufacturing.

Only JB012 can have been imported, since its chemistry does not correspond to any other sample (even those from the western Carpathian Basin). No geographical origin could be proposed.

Another general question that remains unanswered is the reasons behind the use of bone material as temper. As Morzadec (1993) writes “Bone has no particular technological property in the fabrication process of the ceramic”. In only one case (JB069), the bone tempering was necessary for technical reasons, i.e. because no other temper was present in this pottery. In the three other samples, the bone temper was added to a sufficient proportion of other temper, granite and/or grog. Hence, is this peculiar temper resulting of a cultural know-how? If human bone was used, would it be linked to a heritage pertaining to worship, some kind of cult of the Ancient?

## 9.4 DEFINITION OF THE TWO TRADITIONS PRESENT IN ARBON BLEICHE 3

If we follow the idea of Constantin and Courtois (1985) that a choice of material (clay, temper) corresponds to a cultural behaviour, two different cultural traditions can be put into evidence in the potteries from Arbon Bleiche 3.

The first one is bound to the AI petrographical group (ceramics mainly tempered with granite) and to the Pfyn / Horgen pots typological group. This coil-built tradition (Bonzon, 2005) is linked to Pfyn and Horgen local cultures (de Capitani 2002, 220). These forms are surely local (as defined in Arnold, 1985, 2001 and Médard, 2000), as their high percentage in the village witnesses (~70% of the ceramics studied by de Capitani 2002).

The second tradition is quite different: the potteries are thinner, darker and often polished, without coil traces (slab-building technique?). They are mainly represented in the petrographical group AV (preferentially tempered with grog) and form three on four samples of petrographical AVI (bone temper). They correspond to the Boleráz typology of the western Carpathian Basin (de Capitani 2002, 158–159). Some sherds of this region were studied. They are petro-

graphically and mineralogically close to the samples of Arbon Bleiche 3, but chemically different. Hence, no exchange of pottery was put into light between these two regions.

No noticeable chemical differences (apart from those put into relation with the kind of temper used) are evidenced in the ceramics from Arbon Bleiche 3.

We propose an interpenetration of both different traditions on the site. Some traces of this fact can be observed: 10% of Pfyn / Horgen pots are part of the petrographical groups AV, and 21% of the special forms Boleráz belong to AI and AIV groups (Table 5.1). Many samples also present both tempers mixed in various proportions, which can be considered as a mix of both traditions. In the opposite, spindle whorls are bound to one or the other tradition, without any feature of the second one. The Arbon Bleiche 3 village is changing: Pfyn culture comes to the end and Horgen culture appears. These changes are probably visible in the ceramics and may induce this mix of different technologies and typologies.

These two traditions do not chemically separate, even if they are very different from the samples of the western Carpathian Basin. Hence, the ceramics of both traditions are thought to be local. Nine samples of ceramics, plus one of bone tempered pottery are chemically different and could be imported. Unfortunately, their chemistry does not correspond with the samples from the western Carpathian Basin, and no precise provenance is proposed.

## 9.5 FIRING TECHNIQUE, ATMOSPHERE AND TEMPERATURE

All the ceramics from Arbon Bleiche 3 were certainly fired in open fire; no other technique has been described for the Neolithic, and the petrographical, mineralogical and chemical variation inside a single pot (Bonzon, 2005) let think of a fire with variable temperature.

The atmosphere of firing was mainly reducing and the temperatures reached by the potteries were less than 950°C and maybe less than 700°C.

Two samples are considered as resulting from a firing error (JB002, JB151): they are overfired (>800°C?). This high temperature can also be related to the fire that destroyed the village; there is no way to attribute this over-firing to one or to the other fact.
9.6 NO EVIDENCE
OF A DOMESTIC CERAMIC PRODUCTION
IN ARBON BLEICHE 3

The typologies of the ceramics show no evidence
of a spatial distribution in the village (de Capitani
2002, chapters 5.10.3 and 5.11.1). Moreover, the
petrography, mineralogy and chemistry of the samples
cannot have been differentiated according to the sherd
location in the settlement.

In the case of a domestic production, Pétrequin et
al. (1994) defined a relation between spatial repartition
of the ceramics and their characteristics.

Because nothing similar was observed in Arbon
Bleiche 3, a single potter or several potters are thought
to have manufactured the ceramics for the whole vil-
lage. The clay came probably from a well-defined
single pit or several pits in the same morainic deposit.
This is only in this case that we can explain so few
chemical variations in such a big village.

We have to note that in the case in which several
potters used the same pit and the same clay, no chemi-
cal differences would either be observed.
# 10 - PERSPECTIVES & ACKNOWLEDGEMENT

Coming to the end of this work, three main directions of further researches can be proposed:

## 10.1 MINERALOGICAL TRANSFORMATIONS DURING FIRING

Almost every author tests one or several clay(s) to determine the firing temperature reached by the ceramics. The results are varying much from one to another paper.

An important study on several types of clay, under oxidising, but especially under reducing atmospheres should be done to fix the subject.

## 10.2 STUDY OF THE MANUFACTURING TECHNIQUES

Martineau (2000, 2002) developed a study on the manufacturing traces observed on the surfaces of the ceramics. This study leads to very precise information concerning the potters' know-how and personal techniques, which cannot be determined in other ways. Such a study should be regularly done with prehistoric ceramics.

## 10.3 PROVENANCE OF BONE TEMPERED CERAMICS

Even if three on four ceramics tempered with bone are surely local, this technological innovation was probably imported. From where? It will be a challenge to discover the origin of this peculiar technique, because the inhabitants of Arbon Bleiche 3 were once in relation with this population.

## 10.4 ACKNOWLEDGEMENT

This work is part of a Doctoral thesis pursued at the University of Fribourg. I thank the Swiss National Foundation for financial support (Project 1253-52498.97). I am grateful to Prof. M. Maggetti and Dr. V. Serneels for their support during this PhD work and for their contribution to the improvement of the manuscript, together with Prof. B. Grobéty and Dr. S. Wolf. I also want to thank Dr. S. Di Pierro and Dr. R. Martineau for useful discussions, Dr. A. de Capitani and Dr. U. Leuzinger for their help on archaeological problems, M. J. Bürgi, Prof. S. Jacomet and Prof. J. Schibler for their support and for inviting me in the research group on Arbon Bleiche 3. A special "thank you" to Dr. P Thélin, L. Dufresne, Prof. J. Guex, Prof. P. Gex and Prof. L. Baumgartner for their constant support during these five years.
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<figure><img src="image_67.png" /></figure>
# APPENDIXES
# 1 - APPENDIX 1

List of the studied samples from Arbon Bleiche 3.

(In "Sherd Nr.": Rs: Randscherbe, sherd from the lip, Ws: Wandscherbe, sherd from the body, Bs: Bodenscherbe, sherd from the bottom. In "Bed": BRA: Brandschttschicht, bed of fired sediments, Ks: Kulturschicht, bed of cultural sediments).

The sample numbers with * were finally not analysed and with ** were only partially analysed (reasons, see text). (Modified from DE CAPITANI, 2002);

List of the studied samples from the western Carpathian Basin and list of the studied samples of local clays from the surroundings of Arbon.
## SPINDLE WHORLS AND LOOM WEIGHT

<table><thead><tr><th>Inventory Nr.</th><th>Bed</th><th>Coordinates</th><th>Type</th><th>Sample Nr.</th></tr></thead><tbody><tr><td>1994.01.4506.1</td><td>KS</td><td>75.08/217.08/394.45</td><td>flat</td><td>JB111</td></tr><tr><td>1994.01.5486.3</td><td>KS</td><td>70.00/220.00/394.62</td><td>conical</td><td>JB112</td></tr><tr><td>1995.01.7109.1</td><td>BRA</td><td>63.05/193.30/394.08</td><td>flat</td><td>JB113</td></tr><tr><td>1995.01.8756.1</td><td>BRA</td><td>65.78/217.00/394.73</td><td>bi-conical</td><td>JB114</td></tr><tr><td>1994.01.4687.1</td><td>BRA</td><td>70.00/217.00/394.63</td><td>flat</td><td>JB115</td></tr><tr><td>1994.01.5503.1</td><td>BRA</td><td>74.21/223.32/394.66</td><td>flat</td><td>JB116</td></tr><tr><td>1994.01.5220.1</td><td>KS</td><td>71.53/219.15/394.66</td><td>flat</td><td>JB117</td></tr><tr><td>1993.01.187.1</td><td>KS</td><td>65.43/238.38/395.86</td><td>flat</td><td>JB118</td></tr><tr><td>1995.01.8386.1</td><td>KS</td><td>62.14/210.68/394.65</td><td>flat</td><td>JB119</td></tr><tr><td>1993.01.2536.1</td><td>KS</td><td>73.30/229.87/394.80</td><td>flat</td><td>JB120</td></tr><tr><td>1994.01.4136.1</td><td>BRA</td><td>71.77/208.46/394.32</td><td>Loom weight</td><td>JB121</td></tr></tbody></table>

## COB FRAGMENTS

<table><thead><tr><th>Inventory Nr.</th><th>Bed</th><th>Coordinates</th><th>Type</th><th>Sample Nr.</th></tr></thead><tbody><tr><td>1994.01.5708.0</td><td>BRA</td><td>69.00/222.00/394.83</td><td>Cob</td><td>JB122</td></tr><tr><td>1995.01.9735.0</td><td>KS</td><td>66.00/221.00/394.69</td><td>Cob</td><td>JB123</td></tr><tr><td>1995.01.7032.0</td><td>KS</td><td>60.00/192.00394.18</td><td>Cob</td><td>JB124</td></tr><tr><td>1994.01.3639.0</td><td>KS</td><td>78.00/209.00/394.20</td><td>Cob</td><td>JB125</td></tr><tr><td>1994.01.5474.1</td><td>BRA</td><td>77.00/220.00/394.52</td><td>Cob</td><td>JB126</td></tr><tr><td>1994.01.3999.0</td><td>BRA</td><td>71.00/206.00/394.20</td><td>Cob</td><td>JB127</td></tr><tr><td>1994.01.4071.0</td><td>BRA</td><td>78.00/203.00/393.92</td><td>Cob</td><td>JB128</td></tr><tr><td>1995.01.8243.0</td><td>KS</td><td>61.00/209.00/?</td><td>Cob</td><td>JB129</td></tr><tr><td>1994.01.4074.0</td><td>BRA</td><td>73.00/210.00/394.33</td><td>Cob</td><td>JB130</td></tr><tr><td>1995.01.10250</td><td>KS</td><td>62.00/211.00/394.47</td><td>Cob</td><td>JB131</td></tr><tr><td>1995.01.7831.0</td><td>BRA</td><td>61.00/210.00/394.70</td><td>Cob</td><td>JB132</td></tr></tbody></table>

## POTTERIES

<table><thead><tr><th>Pottery Nr.</th><th>Sherd Nr.</th><th>Coordinates</th><th>Bed</th><th>Typological Gp.</th><th>Sample Nr.</th></tr></thead><tbody><tr><td rowspan="2">16655</td><td>Rs 93.01.1757</td><td>76/229</td><td>KS</td><td rowspan="2">Pfyn / Horgen pot</td><td rowspan="2">JB001</td></tr><tr><td>Ws 93.01.1757</td><td>76/229</td><td>KS</td></tr><tr><td rowspan="2">15463</td><td>Rs 93.01.363</td><td>63/229</td><td>BRA</td><td rowspan="2">Pfyn / Horgen pot</td><td rowspan="2">JB002</td></tr><tr><td>Ws 93.01.363</td><td>63/229</td><td>BRA</td></tr><tr><td rowspan="3">15949</td><td>Rs 93.01.1225</td><td>72/230</td><td>KS</td><td rowspan="3">Pfyn / Horgen pot</td><td rowspan="3">JB003</td></tr><tr><td>Ws 93.01.1225</td><td>72/230</td><td>KS</td></tr><tr><td>Ws 93.01.954.1</td><td>72/230</td><td>BRA</td></tr><tr><td rowspan="2">16743</td><td>Ws 94.01.5633</td><td>75/224</td><td>KS</td><td rowspan="2">USF</td><td rowspan="2">JB004</td></tr><tr><td>Ws 94.01.5368</td><td>76/224</td><td>KS</td></tr><tr><td rowspan="3">15494</td><td>Ws 94.01.1686</td><td>62/228</td><td>KS</td><td rowspan="3">USF</td><td rowspan="3">JB005</td></tr><tr><td>Ws 94.01.1686</td><td>62/228</td><td>KS</td></tr><tr><td>Ws 94.01.1686</td><td>62/228</td><td>KS</td></tr><tr><td rowspan="3">16752</td><td>Ws 93.01.98</td><td>54/227</td><td>BRA</td><td rowspan="3">SF Boleráz</td><td rowspan="3">JB006</td></tr><tr><td>Ws 93.01.98</td><td>54/227</td><td>BRA</td></tr><tr><td>Ws 93.01.98</td><td>54/227</td><td>BRA</td></tr><tr><td rowspan="2">15649</td><td>Ws 83.01.156.SII</td><td>68/229</td><td>KS</td><td rowspan="2">SF Pfyn</td><td rowspan="2">JB007</td></tr><tr><td>Ws 83.01.156.SII</td><td>68/229</td><td>KS</td></tr><tr><td rowspan="2">16741</td><td>Rs 93.01.1233</td><td>80/231</td><td>?</td><td rowspan="2">SF Bayern</td><td rowspan="2">JB008</td></tr><tr><td>Rs 93.01.1233</td><td>80/231</td><td>?</td></tr></tbody></table>
<table><thead><tr><th>Ceramic Nr.</th><th>Sherd Nr.</th><th>Coordinates</th><th>Bed</th><th>Typological Gp.</th><th>Sample Nr.</th></tr></thead><tbody><tr><td>16746</td><td>Rs 93.01.968.1</td><td>78/229</td><td>BRA</td><td>SF Pfyn</td><td>JB009</td></tr><tr><td>16745</td><td>Ws 93.01.1675</td><td>76/226</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB010</td></tr><tr><td></td><td>Ws 93.01.1767</td><td>77/227</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 93.01.1767</td><td>77/227</td><td>KS</td><td></td><td></td></tr><tr><td>15400</td><td>Rs 93.01.1571</td><td>59/225</td><td>KS</td><td>USF</td><td>JB011</td></tr><tr><td>16748</td><td>Ws 93.01.1735</td><td>77/232</td><td>KS</td><td>USF</td><td>JB012</td></tr><tr><td>16757</td><td>Ws 94.01.4152.1</td><td>73/210</td><td>KS</td><td>SF Boleráz</td><td>JB013</td></tr><tr><td>16757</td><td>Ws ?</td><td>?</td><td>?</td><td>SF Boleráz</td><td>JB014</td></tr><tr><td>17140</td><td>Ws 95.01.10356.1</td><td>60/219</td><td>KS</td><td>SF Bayern</td><td>JB015</td></tr><tr><td></td><td>Ws 95.01.10356.1</td><td>60/219</td><td>KS</td><td></td><td></td></tr><tr><td>15860</td><td>Rs 93.01.1905</td><td>71/226</td><td>BRA</td><td>USF</td><td>JB016</td></tr><tr><td></td><td>Ws 93.01.2173</td><td>71/226</td><td>BRA</td><td></td><td></td></tr><tr><td></td><td>Ws 93.01.2173</td><td>71/226</td><td>BRA</td><td></td><td></td></tr><tr><td></td><td>Ws 93.01.2173</td><td>71/226</td><td>BRA</td><td></td><td></td></tr><tr><td>15942</td><td>Ws 93.01.1261</td><td>69/231</td><td>KS</td><td>SF Boleráz</td><td>JB017</td></tr><tr><td>15943</td><td>Rs 93.01.1678</td><td>71/231</td><td>KS</td><td>USF</td><td>JB018</td></tr><tr><td></td><td>Ws 93.01.1542</td><td>70/230</td><td>KS</td><td></td><td></td></tr><tr><td>15838</td><td>Rs 93.01.2226</td><td>70/226</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB019</td></tr><tr><td>17566</td><td>Ws 95.01.5798</td><td>69/218</td><td>KS</td><td>SF Boleráz</td><td>JB020</td></tr><tr><td></td><td>Ws 95.01.10026.1</td><td>68/218</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 95.01.10026.1</td><td>68/218</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 95.01.10026.1</td><td>68/218</td><td>KS</td><td></td><td></td></tr><tr><td>17021</td><td>Rs 95.01.10674</td><td>60/219</td><td>KS</td><td>SF Bayern</td><td>JB021</td></tr><tr><td></td><td>Rs 95.01.10657</td><td>60/219</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 95.01.9239</td><td>59/219</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 95.01.9239</td><td>59/219</td><td>KS</td><td></td><td></td></tr><tr><td>17854</td><td>Rs 94.01.3158</td><td>80/221</td><td>?</td><td>Pfyn / Horgen pot</td><td>JB022</td></tr><tr><td>17557</td><td>Ws 95.01.10729</td><td>63/224</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB023</td></tr><tr><td>17568</td><td>Ws 95.01.5678</td><td>69/218</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB024</td></tr><tr><td>17000</td><td>Ws ?</td><td>?</td><td>?</td><td>Pfyn / Horgen pot</td><td>JB025</td></tr><tr><td>17106</td><td>Ws 93.01.9934.1</td><td>61/220</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB026</td></tr><tr><td>17583</td><td>Ws 94.01.5540.1</td><td>71/221</td><td>KS</td><td>USF</td><td>JB027</td></tr><tr><td>17303</td><td>Rs 93.01.1673</td><td>70/229</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB028</td></tr><tr><td></td><td>Ws 95.01.10765</td><td>63/219</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 95.01.10765</td><td>63/219</td><td>KS</td><td></td><td></td></tr><tr><td>17567</td><td>Ws 95.01.10522</td><td>68/218</td><td>KS</td><td>USF</td><td>JB029</td></tr><tr><td>17139</td><td>Ws 95.01.10515.1</td><td>61/218</td><td>KS</td><td>USF</td><td>JB030</td></tr><tr><td>17865</td><td>Ws 94.01.5574</td><td>76/218</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB031</td></tr><tr><td>17009</td><td>Rs ?</td><td>?</td><td>?</td><td>Pfyn / Horgen pot</td><td>JB032</td></tr><tr><td>18234</td><td>Rs 94.01.4865</td><td>78/215</td><td>KS</td><td>SF Boleráz</td><td>JB033</td></tr><tr><td></td><td>Ws 94.01.4865</td><td>78/215</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 94.01.4772</td><td>78/215</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 94.01.4772</td><td>78/215</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 94.01.4772</td><td>78/215</td><td>KS</td><td></td><td></td></tr><tr><td>18245</td><td>Ws 94.01.5294</td><td>70/214</td><td>KS</td><td>SF Boleráz</td><td>JB034</td></tr><tr><td></td><td>Ws 94.01.4688</td><td>74/214</td><td>KS</td><td></td><td></td></tr><tr><td>17850</td><td>Ws 94.01.5451.1</td><td>78/222</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB035</td></tr><tr><td></td><td>Ws 94.01.5451.1</td><td>78/222</td><td>BRA</td><td></td><td></td></tr><tr><td></td><td>Ws 94.01.5451.1</td><td>78/222</td><td>BRA</td><td></td><td></td></tr><tr><td>17556</td><td>Rs ?</td><td>?</td><td>?</td><td>USF</td><td>JB036</td></tr><tr><td></td><td>Ws 94.01.5649</td><td>69/220</td><td>KS</td><td></td><td></td></tr><tr><td>17573</td><td>Ws ?</td><td>?</td><td>?</td><td>SF Bayern</td><td>JB037</td></tr><tr><td></td><td>Ws 94.01.5480.1</td><td>71/218</td><td>KS</td><td></td><td></td></tr></tbody></table>
<table><thead><tr><th>Ceramic Nr.</th><th>Sherd Nr.</th><th>Coordinates</th><th>Bed</th><th>Typological Gp.</th><th>Sample Nr.</th></tr></thead><tbody><tr><td>17863</td><td>Ws ?</td><td>?</td><td>?</td><td>Pfyn / Horgen pot</td><td>JB038</td></tr><tr><td></td><td>Ws 94.01.5753</td><td>77/218</td><td>KS</td><td></td><td></td></tr><tr><td>18854</td><td>Ws 95.01.9092</td><td>66/213</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB039</td></tr><tr><td>17575</td><td>Ws 94.01.5745</td><td>74/221</td><td>BRA</td><td>USF</td><td>JB040</td></tr><tr><td></td><td>Ws 94.01.5926</td><td>73/221</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 94.01.5360</td><td>73/221</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 94.01.5360</td><td>73/221</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 94.01.5360</td><td>73/221</td><td>KS</td><td></td><td></td></tr><tr><td>18308</td><td>Rs 94.01.4946</td><td>73/215</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB041</td></tr><tr><td></td><td>Ws 94.01.4946</td><td>73/215</td><td>KS</td><td></td><td></td></tr><tr><td>18309</td><td>Rs ?</td><td>?</td><td>?</td><td>Pfyn / Horgen pot</td><td>JB042</td></tr><tr><td></td><td>Rs 94.01.5118</td><td>73/215</td><td>KS</td><td></td><td></td></tr><tr><td>18248</td><td>Ws 94.01.5084</td><td>77/211</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB043</td></tr><tr><td></td><td>Ws 94.01.5084</td><td>77/211</td><td>KS</td><td></td><td></td></tr><tr><td>18311</td><td>Ws 94.01.4969</td><td>70/213</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB044</td></tr><tr><td></td><td>Ws 94.01.5000</td><td>71/214</td><td>BRA</td><td></td><td></td></tr><tr><td>18259</td><td>Ws 94.01.4454</td><td>76/217</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB045</td></tr><tr><td>18299</td><td>Rs 94.01.4688</td><td>70/214</td><td>KS</td><td>USF</td><td>JB046</td></tr><tr><td></td><td>Rs 94.01.4688</td><td>70/214</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Rs 94.01.4755</td><td>70/214</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Rs 94.01.4630</td><td>70/214</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Rs 94.01.4455</td><td>71/206</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Rs 94.01.5104</td><td>71/215</td><td>KS</td><td></td><td></td></tr><tr><td>18251</td><td>Rs 94.01.4395</td><td>75/215</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB047</td></tr><tr><td>18303</td><td>Ws 94.01.5253</td><td>69/213</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB048</td></tr><tr><td></td><td>Ws 94.01.5080</td><td>75/217</td><td>KS</td><td></td><td></td></tr><tr><td>18846</td><td>Ws 95.01.8996.1</td><td>65/215</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB049</td></tr><tr><td></td><td>Ws 95.01.8996.1</td><td>65/215</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 95.01.8996.1</td><td>65/215</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 95.01.8996.1</td><td>65/215</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 95.01.8996.1</td><td>65/215</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 95.01.8996.1</td><td>65/215</td><td>KS</td><td></td><td></td></tr><tr><td>18842</td><td>Ws 94.01.5263</td><td>69/213</td><td>KS</td><td>SF Boleráz</td><td>JB050</td></tr><tr><td>18830</td><td>Ws 94.01.4565</td><td>70/214</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB051</td></tr><tr><td>16659</td><td>Ws 93.01.2359</td><td>77/226</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB052</td></tr><tr><td></td><td>Ws 93.01.2424</td><td>78/227</td><td>KS</td><td></td><td></td></tr><tr><td>18310</td><td>Ws ?</td><td>?</td><td>?</td><td>Pfyn / Horgen pot</td><td>JB053</td></tr><tr><td></td><td>Ws 94.01.4667</td><td>70/214</td><td>BRA</td><td></td><td></td></tr><tr><td>18865</td><td>Ws 95.01.8018</td><td>?</td><td>?</td><td>Pfyn / Horgen pot</td><td>JB054</td></tr><tr><td></td><td>Ws 95.01.8018</td><td>?</td><td>?</td><td></td><td></td></tr><tr><td>18845</td><td>Rs 94.01.3116</td><td>68/213</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB055</td></tr><tr><td></td><td>Ws 94.01.3116</td><td>68/213</td><td>KS</td><td></td><td></td></tr><tr><td>18849</td><td>Ws 95.01.9404</td><td>67/216</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB056</td></tr><tr><td>18828</td><td>Rs 94.01.4877</td><td>71/214</td><td>KS</td><td>USF</td><td>JB057</td></tr><tr><td></td><td>Ws 94.01.5331</td><td>69/212</td><td>KS</td><td></td><td></td></tr><tr><td>18831</td><td>Rs 94.01.5547</td><td>70/219</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB058</td></tr><tr><td></td><td>Ws 94.01.5896</td><td>69/220</td><td>KS</td><td></td><td></td></tr><tr><td></td><td>Ws 94.01.5896</td><td>69/220</td><td>KS</td><td></td><td></td></tr><tr><td>18847</td><td>Ws 95.01.9543</td><td>68/217</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB059</td></tr><tr><td></td><td>Ws 94.01.3150</td><td>68/217</td><td>BRA</td><td></td><td></td></tr><tr><td>18840</td><td>Rs 94.01.5710.1</td><td>78/218</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB060</td></tr><tr><td></td><td>Ws 94.01.5587</td><td>69/215</td><td>BRA</td><td></td><td></td></tr><tr><td></td><td>Ws 94.01.5350</td><td>69/215</td><td>BRA</td><td></td><td></td></tr></tbody></table>
<table><thead><tr><th>Ceramic Nr.</th><th>Sherd Nr.</th><th>Coordinates</th><th>Bed</th><th>Typological Gp.</th><th>Sample Nr.</th></tr></thead><tbody><tr><td rowspan="3">18866</td><td>Ws 94.01.3191</td><td>68/219</td><td>KS</td><td rowspan="3">Pfyn / Horgen pot</td><td rowspan="3">JB061</td></tr><tr><td>Ws ?</td><td>?</td><td>?</td></tr><tr><td>Ws 94.01.3191</td><td>68/219</td><td>KS</td></tr><tr><td rowspan="3">18867</td><td>Ws 95.01.8891</td><td>66/212</td><td>KS</td><td rowspan="3">Pfyn / Horgen pot</td><td rowspan="3">JB062</td></tr><tr><td>Ws 95.01.8891</td><td>66/212</td><td>KS</td></tr><tr><td>Ws 95.01.9096.1</td><td>66/212</td><td>KS</td></tr><tr><td rowspan="3">18930</td><td>Ws 95.01.9264</td><td>61/215</td><td>KS</td><td rowspan="3">SF Boleráz</td><td rowspan="3">JB063</td></tr><tr><td>Ws 95.01.8988</td><td>61/215</td><td>BRA</td></tr><tr><td>Ws 95.01.8988</td><td>61/215</td><td>BRA</td></tr><tr><td rowspan="2">18925</td><td>Ws 95.01.10707</td><td>64/218</td><td>KS</td><td rowspan="2">Pfyn / Horgen pot</td><td rowspan="2">JB064</td></tr><tr><td>Ws 95.01.10707</td><td>64/218</td><td>KS</td></tr><tr><td rowspan="6">19546</td><td>Rs 95.01.10028</td><td>62/211</td><td>KS</td><td rowspan="6">Pfyn / Horgen pot</td><td rowspan="6">JB065</td></tr><tr><td>Ws 95.01.10028</td><td>62/211</td><td>KS</td></tr><tr><td>Ws 95.01.10028</td><td>62/211</td><td>KS</td></tr><tr><td>Rs 95.01.10028</td><td>62/211</td><td>KS</td></tr><tr><td>Ws 95.01.10028</td><td>62/211</td><td>KS</td></tr><tr><td>Ws 95.01.8335</td><td>61/209</td><td>KS</td></tr><tr><td>19608</td><td>Ws 95.01.8917</td><td>66/216</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB066</td></tr><tr><td rowspan="2">18915</td><td>Ws 95.01.9138</td><td>61/215</td><td>BRA</td><td rowspan="2">Pfyn / Horgen pot</td><td rowspan="2">JB067</td></tr><tr><td>Ws 95.01.8970</td><td>61/215</td><td>BRA</td></tr><tr><td rowspan="4">18906</td><td>Rs 95.01.9974</td><td>63/211</td><td>KS</td><td rowspan="4">Pfyn / Horgen pot</td><td rowspan="4">JB068</td></tr><tr><td>Ws 95.01.9974</td><td>63/211</td><td>KS</td></tr><tr><td>Rs 95.01.7879</td><td>63/208</td><td>BRA</td></tr><tr><td>Ws 95.01.7879</td><td>63/208</td><td>BRA</td></tr><tr><td rowspan="5">18909</td><td>Ws 95.01.9356.1</td><td>61/215</td><td>BRA</td><td rowspan="5">SF Boleráz</td><td rowspan="5">JB069</td></tr><tr><td>Ws 95.01.8829.1</td><td>60/212</td><td>BRA</td></tr><tr><td>Ws 95.01.8959.1</td><td>61/214</td><td>BRA</td></tr><tr><td>Ws ?</td><td>?</td><td>?</td></tr><tr><td>Ws 95.01.9354.1</td><td>61/215</td><td>BRA</td></tr><tr><td rowspan="2">18973</td><td>Ws 95.01.8863.1</td><td>61/212</td><td>BRA</td><td rowspan="2">USF</td><td rowspan="2">JB070</td></tr><tr><td>Ws 95.01.9245</td><td>62/212</td><td>BRA</td></tr><tr><td rowspan="8">18917</td><td>Bs 95.01.9894.1</td><td>63/214</td><td>KS</td><td rowspan="8">USF</td><td rowspan="8">JB072</td></tr><tr><td>Bs 95.01.9894.1</td><td>63/214</td><td>KS</td></tr><tr><td>Bs 95.01.9894.1</td><td>63/214</td><td>KS</td></tr><tr><td>Bs 95.01.9894.1</td><td>63/214</td><td>KS</td></tr><tr><td>Rs 94.01.5742</td><td>78/222</td><td>KS</td></tr><tr><td>Ws 94.01.5742</td><td>78/222</td><td>KS</td></tr><tr><td>Ws 94.01.5742</td><td>78/222</td><td>KS</td></tr><tr><td>Ws 94.01.5612</td><td>78/222</td><td>BRA</td></tr><tr><td rowspan="2">18918</td><td>Ws 94.01.5612</td><td>78/222</td><td>BRA</td><td rowspan="2">SF Boleráz</td><td rowspan="2">JB073</td></tr><tr><td>Ws 94.01.5257</td><td>79/223</td><td>KS</td></tr><tr><td rowspan="6">18919</td><td>Ws 95.01.7634.1</td><td>59/213</td><td>KS</td><td rowspan="6">USF</td><td rowspan="6">JB074</td></tr><tr><td>Ws 95.01.7658.1</td><td>59/213</td><td>KS</td></tr><tr><td>Ws 95.01.7658.1</td><td>59/213</td><td>KS</td></tr><tr><td>Ws 95.01.7658.1</td><td>59/213</td><td>KS</td></tr><tr><td>Ws 95.01.7658.1</td><td>59/213</td><td>KS</td></tr><tr><td>Ws 95.01.7658.1</td><td>59/213</td><td>KS</td></tr></tbody></table>
<table><thead><tr><th>Ceramic Nr.</th><th>Sherd Nr.</th><th>Coordinates</th><th>Bed</th><th>Typological Gp.</th><th>Sample Nr.</th></tr></thead><tbody><tr><td rowspan="3">18976</td><td>Ws 94.01.5184</td><td>69/217</td><td>KS</td><td rowspan="3">USF</td><td rowspan="3">JB075</td></tr><tr><td>Ws 94.01.5804</td><td>69/220</td><td>KS</td></tr><tr><td>Ws 94.01.5804</td><td>69/220</td><td>KS</td></tr><tr><td rowspan="5">18949</td><td>Rs 95.01.7917</td><td>61/208</td><td>BRA</td><td rowspan="5">Pfyn / Horgen pot</td><td rowspan="5">JB076</td></tr><tr><td>Ws 95.01.7917</td><td>61/208</td><td>BRA</td></tr><tr><td>Ws 95.01.7917</td><td>61/208</td><td>BRA</td></tr><tr><td>Ws 95.01.7917</td><td>61/208</td><td>BRA</td></tr><tr><td>Ws unleserlich</td><td>?</td><td>?</td></tr><tr><td>18949</td><td>Ws 95.01.7917</td><td>61/208</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB077</td></tr><tr><td>18949</td><td>Ws 95.01.7917</td><td>61/208</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB078</td></tr><tr><td>18949</td><td>Ws 95.01.7917</td><td>61/208</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB079</td></tr><tr><td>18949</td><td>Ws 95.01.7917</td><td>61/208</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB080</td></tr><tr><td>18949</td><td>Ws 95.01.9113</td><td>61/212</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB081</td></tr><tr><td>18949</td><td>Ws 95.01.9113</td><td>61/212</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB082</td></tr><tr><td>18949</td><td>Ws 95.01.7657</td><td>59/212</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB083</td></tr><tr><td>18949</td><td>Ws 95.01.10725</td><td>61/211</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB084</td></tr><tr><td>18949</td><td>Bs 95.01.9245</td><td>62/212</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB085</td></tr><tr><td rowspan="7">18974</td><td>Ws 95.01.8842</td><td>63/217</td><td>BRA</td><td rowspan="7">USF</td><td rowspan="7">JB086</td></tr><tr><td>Ws 95.01.8842</td><td>63/217</td><td>BRA</td></tr><tr><td>Ws 95.01.8842</td><td>63/217</td><td>BRA</td></tr><tr><td>Ws 95.01.8842</td><td>63/217</td><td>BRA</td></tr><tr><td>Ws 95.01.8842</td><td>63/217</td><td>BRA</td></tr><tr><td>Ws 95.01.8842</td><td>63/217</td><td>BRA</td></tr><tr><td>Ws 95.01.9000.1</td><td>63/217</td><td>BRA</td></tr><tr><td rowspan="3">18977</td><td>Ws 95.01.9000.1</td><td>63/217</td><td>BRA</td><td rowspan="3">USF</td><td rowspan="3">JB087</td></tr><tr><td>Ws 95.01.9000.1</td><td>63/217</td><td>BRA</td></tr><tr><td>Ws 95.01.9000.1</td><td>63/217</td><td>BRA</td></tr><tr><td>18970</td><td>Ws 95.01.7656</td><td>59/217</td><td>KS</td><td>SF Bayern</td><td>JB088</td></tr><tr><td>19775</td><td>Ws 94.01.3852</td><td>73/205</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB089</td></tr><tr><td rowspan="4">19773</td><td>Ws 94.01.3852</td><td>73/205</td><td>BRA</td><td rowspan="4">SF Bayern</td><td rowspan="4">JB090</td></tr><tr><td>Rs 94.01.3173</td><td>79/207</td><td>?</td></tr><tr><td>Rs 94.01.3931</td><td>78/?</td><td>KS</td></tr><tr><td>Ws 94.01.4743.1</td><td>71/204</td><td>KS</td></tr><tr><td rowspan="3">19771</td><td>Ws 94.01.4743.1</td><td>71/204</td><td>KS</td><td rowspan="3">Pfyn / Horgen pot</td><td rowspan="3">JB091</td></tr><tr><td>Ws 94.01.4743.1</td><td>71/204</td><td>KS</td></tr><tr><td>Ws 94.01.4743.1</td><td>71/204</td><td>KS</td></tr><tr><td>19776</td><td>Ws 94.01.3974</td><td>71/206</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB092</td></tr><tr><td rowspan="2">19782</td><td>Ws 94.01.4300</td><td>74/204</td><td>BRA</td><td rowspan="2">Pfyn / Horgen pot</td><td rowspan="2">JB093</td></tr><tr><td>Ws 94.01.4300</td><td>74/204</td><td>BRA</td></tr><tr><td rowspan="2">19780</td><td>Ws 94.01.4300</td><td>74/204</td><td>BRA</td><td rowspan="2">Pfyn / Horgen pot</td><td rowspan="2">JB094</td></tr><tr><td>Rs 94.01.4207</td><td>71/207</td><td>KS</td></tr><tr><td rowspan="8">19777</td><td>Ws 94.01.4207</td><td>71/207</td><td>KS</td><td rowspan="8">SF Bayern</td><td rowspan="8">JB095</td></tr><tr><td>Rs 94.01.4297</td><td>70/207</td><td>KS</td></tr><tr><td>Rs 94.01.4297</td><td>70/207</td><td>KS</td></tr><tr><td>Ws 94.01.4297</td><td>70/207</td><td>KS</td></tr><tr><td>Ws 94.01.4297</td><td>70/207</td><td>KS</td></tr><tr><td>Ws 94.01.4297</td><td>70/207</td><td>KS</td></tr><tr><td>Ws 94.01.4297</td><td>70/207</td><td>KS</td></tr><tr><td>Ws 94.01.4297</td><td>70/207</td><td>KS</td></tr></tbody></table>
<table><thead><tr><th>Ceramic Nr.</th><th>Sherd Nr.</th><th>Coordinates</th><th>Bed</th><th>Typological Gp.</th><th>Sample Nr.</th></tr></thead><tbody><tr><td rowspan="3">19777 (follow)</td><td>Ws 94.01.4297</td><td>70/207</td><td>KS</td><td rowspan="3">SF Bayern</td><td rowspan="3">JB095</td></tr><tr><td>Ws 94.01.4297</td><td>70/207</td><td>KS</td></tr><tr><td>Ws 94.01.4297</td><td>70/207</td><td>KS</td></tr><tr><td>19777</td><td>Ws 94.01.4297</td><td>70/207</td><td>KS</td><td>SF Bayern</td><td>JB095</td></tr><tr><td rowspan="4">19772</td><td>Rs 94.01.4161</td><td>73/205</td><td>BRA</td><td rowspan="4">Pfyn / Horgen pot</td><td rowspan="4">JB096</td></tr><tr><td>Ws 94.01.4161</td><td>73/205</td><td>BRA</td></tr><tr><td>Ws 94.01.4161</td><td>73/205</td><td>BRA</td></tr><tr><td>Ws 94.01.3797</td><td>73/205</td><td>BRA</td></tr><tr><td rowspan="4">19629</td><td>Ws 94.01.4233</td><td>72/210</td><td>KS</td><td rowspan="4">Pfyn / Horgen pot</td><td rowspan="4">JB097</td></tr><tr><td>Ws 94.01.4202</td><td>71/209</td><td>KS</td></tr><tr><td>Ws 94.01.4329</td><td>70/209</td><td>KS</td></tr><tr><td>Ws 94.01.4410</td><td>70/208</td><td>KS</td></tr><tr><td rowspan="2">19624</td><td>Ws 94.01.3246</td><td>76/208</td><td>BRA</td><td rowspan="2">USF</td><td rowspan="2">JB098</td></tr><tr><td>Ws 94.01.3246</td><td>76/208</td><td>BRA</td></tr><tr><td rowspan="2">19623</td><td>Rs 94.01.4709.1</td><td>76/211</td><td>KS</td><td rowspan="2">SF Boleráz</td><td rowspan="2">JB099</td></tr><tr><td>Ws 94.01.4709.1</td><td>76/211</td><td>KS</td></tr><tr><td rowspan="3">19611</td><td>Rs 94.01.3656</td><td>75/205</td><td>KS</td><td rowspan="3">Pfyn / Horgen pot</td><td rowspan="3">JB100</td></tr><tr><td>Ws 94.01.3656</td><td>75/205</td><td>KS</td></tr><tr><td>Ws 94.01.3972</td><td>78/207</td><td>KS</td></tr><tr><td rowspan="5">20038</td><td>Ws 94.01.7965</td><td>66/207</td><td>BRA</td><td rowspan="5">Pfyn / Horgen pot</td><td rowspan="5">JB101</td></tr><tr><td>Ws 94.01.7965</td><td>66/207</td><td>BRA</td></tr><tr><td>Ws 94.01.7965</td><td>66/207</td><td>BRA</td></tr><tr><td>Ws 94.01.7965</td><td>66/207</td><td>BRA</td></tr><tr><td>Ws 95.01.8072</td><td>68/207</td><td>KS</td></tr><tr><td rowspan="5">20887</td><td>Ws 95.01.7647</td><td>64/200</td><td>KS</td><td rowspan="5">USF</td><td rowspan="5">JB102</td></tr><tr><td>Ws 95.01.8574.1</td><td>66/204</td><td>KS</td></tr><tr><td>Ws 95.01.7669</td><td>64/200</td><td>KS</td></tr><tr><td>Ws 95.01.7669</td><td>64/200</td><td>KS</td></tr><tr><td>Ws 95.01.7669</td><td>64/200</td><td>KS</td></tr><tr><td>20040</td><td>Ws 94.01.5580</td><td>68/211</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB103</td></tr><tr><td>18948</td><td>Ws 95.01.9410</td><td>63/212</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB104</td></tr><tr><td>Ws ?</td><td>?</td><td>?</td><td>?</td><td></td><td></td></tr><tr><td>19622</td><td>Rs 94.01.4031</td><td>74/208</td><td>BRA</td><td>USF</td><td>JB105</td></tr><tr><td rowspan="3">20204</td><td>Ws 94.01.5580</td><td>68/211</td><td>KS</td><td rowspan="3">SF Boleráz</td><td rowspan="3">JB106</td></tr><tr><td>Ws 94.01.5580</td><td>68/211</td><td>KS</td></tr><tr><td>Ws 94.01.5580</td><td>68/211</td><td>KS</td></tr><tr><td>17577</td><td>Ws 94.01.5782</td><td>73/218</td><td>BRA</td><td>USF</td><td>JB107</td></tr><tr><td rowspan="3">20212</td><td>Ws 94.01.5782</td><td>73/218</td><td>BRA</td><td></td><td></td></tr><tr><td>Ws 95.01.8603</td><td>62/208</td><td>KS</td><td rowspan="3">Pfyn / Horgen pot</td><td rowspan="3">JB108</td></tr><tr><td>Ws 95.01.8339</td><td>61/210</td><td>KS</td></tr><tr><td>Ws 95.01.8660</td><td>61/210</td><td>KS</td></tr><tr><td rowspan="5">15525</td><td>Ws 93.01.2352.1</td><td>65/229</td><td>?</td><td rowspan="5">Pfyn / Horgen pot</td><td rowspan="5">JB109</td></tr><tr><td>Ws 93.01.2352.1</td><td>65/229</td><td>?</td></tr><tr><td>Ws 93.01.2352.1</td><td>65/229</td><td>?</td></tr><tr><td>Ws 93.01.2352.1</td><td>65/229</td><td>?</td></tr><tr><td>Ws 93.01.2352.1</td><td>65/229</td><td>?</td></tr><tr><td rowspan="3">19553</td><td>Rs 95.01.10629</td><td>64/216</td><td>KS</td><td rowspan="3">SF Bayern</td><td rowspan="3">JB110</td></tr><tr><td>Rs 95.01.9964</td><td>68/220</td><td>KS</td></tr><tr><td>Rs 95.01.10099</td><td>64/216</td><td>KS</td></tr><tr><td rowspan="3">15462</td><td>Ws 93.01.569</td><td>63/231</td><td>KS</td><td rowspan="3">Pfyn / Horgen pot</td><td rowspan="3">JB133</td></tr><tr><td>Ws 93.01.385.2</td><td>62/231</td><td>KS</td></tr><tr><td>Ws 93.01.385.2</td><td>62/231</td><td>KS</td></tr></tbody></table>
<table><thead><tr><th>Ceramic Nr.</th><th>Sherd Nr.</th><th>Coordinates</th><th>Bed</th><th>Typological Gp.</th><th>Sample Nr.</th></tr></thead><tbody><tr><td rowspan="3">20028</td><td>Ws 94.01.4170.1</td><td>69/206</td><td>BRA</td><td rowspan="3">Pfyn / Horgen pot</td><td rowspan="3">JB134</td></tr><tr><td>Ws 94.01.4170.1</td><td>69/206</td><td>BRA</td></tr><tr><td>Ws 94.01.4170.1</td><td>69/206</td><td>BRA</td></tr><tr><td rowspan="3">18902</td><td>Ws 95.01.9506</td><td>60/217</td><td>BRA</td><td rowspan="3">Pfyn / Horgen pot</td><td rowspan="3">JB135</td></tr><tr><td>Ws 95.01.9506</td><td>60/217</td><td>BRA</td></tr><tr><td>Ws 95.01.9829</td><td>60/217</td><td>BRA</td></tr><tr><td rowspan="4">16725</td><td>Ws 93.01.2623</td><td>77/225</td><td>KS</td><td rowspan="4">Pfyn / Horgen pot</td><td rowspan="4">JB136</td></tr><tr><td>Ws 93.01.2265</td><td>79/226</td><td>KS</td></tr><tr><td>Ws 93.01.2432</td><td>78/226</td><td>KS</td></tr><tr><td>Ws 93.01.2232</td><td>78/226</td><td>KS</td></tr><tr><td rowspan="3">18829</td><td>Ws 95.01.9826</td><td>63/214</td><td>KS</td><td rowspan="3">Pfyn / Horgen pot</td><td rowspan="3">JB137</td></tr><tr><td>Ws 95.01.9826</td><td>63/214</td><td>KS</td></tr><tr><td>Ws 95.01.9826</td><td>63/214</td><td>KS</td></tr><tr><td>18972</td><td>Ws 95.01.9555.1</td><td>63/217</td><td>BRA</td><td>SF Boleráz</td><td>JB138</td></tr><tr><td rowspan="7">17576</td><td>Rs 94.01.5300.1</td><td>72/222</td><td>KS</td><td rowspan="7">SF Boleráz</td><td rowspan="7">JB139</td></tr><tr><td>Ws 94.01.5300.1</td><td>72/222</td><td>KS</td></tr><tr><td>Ws 94.01.5300.1</td><td>72/222</td><td>KS</td></tr><tr><td>Ws 94.01.5300.1</td><td>72/222</td><td>KS</td></tr><tr><td>Ws 94.01.5300.1</td><td>72/222</td><td>KS</td></tr><tr><td>Ws 94.01.5300.1</td><td>72/222</td><td>KS</td></tr><tr><td>Ws 94.01.5300.1</td><td>72/222</td><td>KS</td></tr><tr><td>21241</td><td>Ws 95.01.8042</td><td>59/188</td><td>KS</td><td>SF Boleráz</td><td>JB140</td></tr><tr><td rowspan="3">21240</td><td>Ws 94.01.3216</td><td>67/197</td><td>BRA</td><td rowspan="3">SF Boleráz</td><td rowspan="3">JB141</td></tr><tr><td>Ws 95.01.7652</td><td>61/202</td><td>KS</td></tr><tr><td>Ws 95.01.7123.1</td><td>62/193</td><td>BRA</td></tr><tr><td>21243</td><td>Ws 95.01.8569.1</td><td>60/189</td><td>BRA</td><td>USF</td><td>JB142</td></tr><tr><td rowspan="4">21239</td><td>Ws 95.01.7010.1</td><td>62/189</td><td>-</td><td rowspan="4">SF Bayern</td><td rowspan="4">JB143</td></tr><tr><td>Ws 95.01.7010.1</td><td>62/189</td><td>-</td></tr><tr><td>Ws 95.01.7010.1</td><td>62/189</td><td>-</td></tr><tr><td>Ws 95.01.7010.1</td><td>62/189</td><td>-</td></tr><tr><td>20627</td><td>Ws 94.01.3587</td><td>71/203</td><td>KS</td><td>SF Boleráz</td><td>JB144</td></tr><tr><td rowspan="2">20626</td><td>Ws ?</td><td>?</td><td>?</td><td>SF Boleráz</td><td>JB145</td></tr><tr><td>Ws 94.01.3402</td><td>72/199</td><td>KS</td><td>SF Boleráz</td><td>JB145</td></tr><tr><td>21034</td><td>Ws 95.01.7022</td><td>60/195</td><td>BRA</td><td>SF Boleráz</td><td>JB146</td></tr><tr><td rowspan="3">18833</td><td>Ws 95.01.7022</td><td>60/195</td><td>BRA</td><td>SF Boleráz</td><td>JB147</td></tr><tr><td>Ws 95.01.8905.1</td><td>66/217</td><td>BRA</td><td>SF Boleráz</td><td>JB147</td></tr><tr><td>Ws 95.01.8851.1</td><td>66/217</td><td>KS</td><td>SF Boleráz</td><td>JB147</td></tr><tr><td>18927</td><td>Ws 95.01.8954.1</td><td>60/213</td><td>BRA</td><td>SF Boleráz</td><td>JB148</td></tr><tr><td rowspan="4">19787</td><td>Ws 94.01.4585</td><td>74/204</td><td>KS</td><td rowspan="4">SF Boleráz</td><td rowspan="4">JB149</td></tr><tr><td>Ws 94.01.4585</td><td>74/204</td><td>KS</td></tr><tr><td>Ws 94.01.4585</td><td>74/204</td><td>KS</td></tr><tr><td>Ws 94.01.4585</td><td>74/204</td><td>KS</td></tr><tr><td>20893</td><td>Rs 95.01.7642</td><td>63/202</td><td>KS</td><td>SF Bayern</td><td>JB150</td></tr><tr><td>20888</td><td>Ws 94.01.3725</td><td>69/202</td><td>BRA</td><td>SF Bayern</td><td>JB151</td></tr><tr><td rowspan="3">20215</td><td>Ws 95.01.8022</td><td>61/209</td><td>BRA</td><td rowspan="3">SF Boleráz</td><td rowspan="3">JB152</td></tr><tr><td>Ws 95.01.8022</td><td>61/209</td><td>BRA</td></tr><tr><td>Ws 95.01.7957</td><td>63/210</td><td>BRA</td></tr><tr><td rowspan="3">20233</td><td>Rs 95.01.10739</td><td>61/211</td><td>KS</td><td rowspan="3">SF Bayern</td><td rowspan="3">JB153</td></tr><tr><td>Rs 95.01.8236</td><td>60/207</td><td>KS</td></tr><tr><td>Rs 95.01.8209</td><td>61/207</td><td>KS</td></tr></tbody></table>
<table><thead><tr><th>Ceramic Nr.</th><th>Sherd Nr.</th><th>Coordinates</th><th>Bed</th><th>Typological Gp.</th><th>Sample Nr.</th></tr></thead><tbody><tr><td rowspan="3">18964</td><td>Ws 95.01.8967</td><td>64/214</td><td>BRA</td><td>SF Boleráz</td><td>JB154</td></tr><tr><td>Ws 95.01.7660</td><td>59/213</td><td>KS</td><td></td><td></td></tr><tr><td>Ws 95.01.7660</td><td>59/213</td><td>KS</td><td></td><td></td></tr><tr><td>20628</td><td>Bs 94.01.3473</td><td>71/202</td><td>KS</td><td>SF Boleráz</td><td>JB155</td></tr><tr><td rowspan="3">20632</td><td>Ws 94.01.3230</td><td>74/201</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB156*</td></tr><tr><td>Ws 94.01.3457</td><td>72/200</td><td>KS</td><td></td><td></td></tr><tr><td>Ws 94.01.3457</td><td>72/200</td><td>KS</td><td></td><td></td></tr><tr><td rowspan="3">20781</td><td>Ws 94.01.3759</td><td>67/199</td><td>KS</td><td>SF Bayern</td><td>JB157</td></tr><tr><td>Ws 94.01.3759</td><td>67/199</td><td>KS</td><td></td><td></td></tr><tr><td>Ws 94.01.3752</td><td>67/198</td><td>BRA</td><td></td><td></td></tr><tr><td>20782</td><td>Bs 95.01.7603</td><td>65/198</td><td>BRA</td><td>USF</td><td>JB158</td></tr><tr><td rowspan="2">20780</td><td>Ws 94.01.3384</td><td>69/200</td><td>BRA</td><td>USF</td><td>JB159</td></tr><tr><td>Ws 94.01.3717</td><td>68/199</td><td>BRA</td><td></td><td></td></tr><tr><td rowspan="3">20894</td><td>Ws 95.01.7607</td><td>61/199</td><td>KS</td><td>USF</td><td>JB160</td></tr><tr><td>Ws 95.01.7147</td><td>60/201</td><td>BRA</td><td></td><td></td></tr><tr><td>Ws 95.01.7147</td><td>60/201</td><td>BRA</td><td></td><td></td></tr><tr><td rowspan="4">20897</td><td>Ws 95.01.7386</td><td>63/199</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB161*</td></tr><tr><td>Ws 95.01.7444</td><td>62/199</td><td>BRA</td><td></td><td></td></tr><tr><td>Ws 95.01.7525</td><td>62/199</td><td>KS</td><td></td><td></td></tr><tr><td>Ws 95.01.7532</td><td>62/199</td><td>BRA</td><td></td><td></td></tr><tr><td rowspan="4">20885</td><td>Ws 95.01.7495</td><td>62/200</td><td>BRA</td><td>USF</td><td>JB162</td></tr><tr><td>Ws 95.01.7576</td><td>61/199</td><td>KS</td><td></td><td></td></tr><tr><td>Ws 95.01.7118</td><td>60/199</td><td>BRA</td><td></td><td></td></tr><tr><td>Ws 95.01.7118</td><td>60/199</td><td>BRA</td><td></td><td></td></tr><tr><td rowspan="3">20886</td><td>Ws 95.01.7495</td><td>62/200</td><td>BRA</td><td></td><td></td></tr><tr><td>Ws 95.01.7474.1</td><td>62/199</td><td>KS</td><td>USF</td><td>JB163</td></tr><tr><td>Ws 95.01.7817</td><td>69/198</td><td>KS</td><td></td><td></td></tr><tr><td rowspan="3">21032</td><td>Ws 94.01.3228</td><td>66/197</td><td>BRA</td><td></td><td></td></tr><tr><td>Ws 95.01.7198</td><td>62/194</td><td>BRA</td><td>USF</td><td>JB164</td></tr><tr><td>Ws 95.01.7198</td><td>62/194</td><td>BRA</td><td></td><td></td></tr><tr><td rowspan="2">21033</td><td>Ws 95.01.7202.1</td><td>61/195</td><td>BRA</td><td></td><td></td></tr><tr><td>Ws 95.01.7448</td><td>61/195</td><td>KS</td><td>USF</td><td>JB165</td></tr><tr><td rowspan="3">20225</td><td>Ws 95.01.7448</td><td>61/195</td><td>KS</td><td></td><td></td></tr><tr><td>Rs 95.01.8720</td><td>64/201</td><td>BRA</td><td>USF</td><td>JB166</td></tr><tr><td>Rs 95.01.7577</td><td>64/200</td><td>BRA</td><td></td><td></td></tr><tr><td rowspan="3">20221</td><td>Ws 95.01.7474</td><td>64/206</td><td>KS</td><td></td><td></td></tr><tr><td>Ws 95.01.7574</td><td>63/200</td><td>BRA</td><td></td><td></td></tr><tr><td>Ws 94.01.3440</td><td>68/201</td><td>BRA</td><td>USF</td><td>JB167</td></tr><tr><td rowspan="4">20218</td><td>Ws 94.01.3440</td><td>68/201</td><td>BRA</td><td></td><td></td></tr><tr><td>Ws 94.01.3440</td><td>68/201</td><td>BRA</td><td></td><td></td></tr><tr><td>Ws 94.01.3440</td><td>68/201</td><td>BRA</td><td></td><td></td></tr><tr><td>Ws 94.01.3440</td><td>68/201</td><td>BRA</td><td></td><td></td></tr><tr><td rowspan="2">20041</td><td>Bs 95.01.8457</td><td>62/209</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB168*</td></tr><tr><td>Bs 95.01.8036</td><td>62/209</td><td>KS</td><td></td><td></td></tr><tr><td rowspan="2">20043</td><td>Ws 95.01.8238</td><td>67/209</td><td>KS</td><td>USF</td><td>JB169</td></tr><tr><td>Ws 95.01.8080</td><td>67/206</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB170*</td></tr><tr><td rowspan="4">20044</td><td>Ws 95.01.8080</td><td>67/206</td><td>KS</td><td></td><td></td></tr><tr><td>Rs 95.01.8362</td><td>66/210</td><td>KS</td><td>SF Pfyn</td><td>JB171</td></tr><tr><td>Rs 95.01.8658</td><td>66/210</td><td>KS</td><td></td><td></td></tr><tr><td>Ws 95.01.8362</td><td>66/210</td><td>KS</td><td></td><td></td></tr><tr><td>Ws 95.01.8658</td><td>66/210</td><td>KS</td><td></td><td></td></tr><tr><td>Ws 95.01.8658</td><td>66/210</td><td>KS</td><td></td><td></td></tr></tbody></table>
<table><thead><tr><th>Ceramic Nr.</th><th>Sherd Nr.</th><th>Coordinates</th><th>Bed</th><th>Typological Gp.</th><th>Sample Nr.</th></tr></thead><tbody><tr><td rowspan="4">20045</td><td>Ws 95.01.7968</td><td>67/209</td><td>BRA</td><td rowspan="4">USF</td><td rowspan="4">JB172**</td></tr><tr><td>Ws 95.01.7915</td><td>67/209</td><td>BRA</td></tr><tr><td>Ws 95.01.7915</td><td>67/209</td><td>BRA</td></tr><tr><td>Ws 95.01.4324</td><td>69/207</td><td>KS</td></tr><tr><td>20036</td><td>Ws 94.01.4676</td><td>70/215</td><td>BRA</td><td>USF</td><td>JB173</td></tr><tr><td rowspan="3">20032</td><td>Rs 94.01.4146</td><td>74/208</td><td>KS</td><td rowspan="3">USF</td><td rowspan="3">JB174</td></tr><tr><td>Ws 94.01.3073.1</td><td>68/207</td><td>?</td></tr><tr><td>Ws 94.01.3072</td><td>68/207</td><td>?</td></tr><tr><td rowspan="2">16755</td><td>Ws 93.01.1472</td><td>59/230</td><td>BRA</td><td rowspan="2">SF Boleráz</td><td rowspan="2">JB175</td></tr><tr><td>Ws 93.01.1472</td><td>59/230</td><td>BRA</td></tr><tr><td rowspan="5">17848</td><td>Ws 95.01.8888</td><td>67/215</td><td>KS</td><td rowspan="5">Pfyn / Horgen pot</td><td rowspan="5">JB176*</td></tr><tr><td>Ws 95.01.8888</td><td>67/215</td><td>KS</td></tr><tr><td>Ws 95.01.8888</td><td>67/215</td><td>KS</td></tr><tr><td>Ws 95.01.8888</td><td>67/215</td><td>KS</td></tr><tr><td>Ws ?</td><td>?</td><td>?</td></tr><tr><td>17022</td><td>Ws 95.01.10513.1</td><td>62/219</td><td>KS</td><td>USF</td><td>JB177</td></tr><tr><td rowspan="2">17018</td><td>Ws 95.01.9944</td><td>61/219</td><td>BRA</td><td rowspan="2">USF</td><td rowspan="2">JB178</td></tr><tr><td>Ws 95.01.9944</td><td>61/219</td><td>BRA</td></tr><tr><td rowspan="3">17040</td><td>Ws 95.01.8936</td><td>59/219</td><td>KS</td><td rowspan="3">SF Boleráz</td><td rowspan="3">JB179</td></tr><tr><td>Ws 95.01.8936</td><td>59/219</td><td>KS</td></tr><tr><td>Ws 95.01.10550</td><td>62/218</td><td>KS</td></tr><tr><td rowspan="2">17041</td><td>Ws 95.01.8706</td><td>59/220</td><td>BRA</td><td rowspan="2">USF</td><td rowspan="2">JB180</td></tr><tr><td>Ws 95.01.8706</td><td>59/220</td><td>BRA</td></tr><tr><td rowspan="2">18298</td><td>Rs 94.01.5235</td><td>?</td><td>KS</td><td rowspan="2">USF</td><td rowspan="2">JB181</td></tr><tr><td>Ws 94.01.4871</td><td>70/215</td><td>KS</td></tr><tr><td rowspan="5">18838</td><td>Ws 95.01.8769</td><td>66/216</td><td>KS</td><td rowspan="5">USF</td><td rowspan="5">JB182</td></tr><tr><td>Ws 95.01.8769</td><td>66/216</td><td>KS</td></tr><tr><td>Ws 95.01.8769</td><td>66/216</td><td>KS</td></tr><tr><td>Ws 95.01.8769</td><td>66/216</td><td>KS</td></tr><tr><td>Ws 95.01.8769</td><td>66/216</td><td>KS</td></tr><tr><td rowspan="5">18832</td><td>Bs 95.01.9344</td><td>65/212</td><td>KS</td><td rowspan="5">USF</td><td rowspan="5">JB183</td></tr><tr><td>Bs 95.01.9344</td><td>65/212</td><td>KS</td></tr><tr><td>Bs 95.01.9344</td><td>65/212</td><td>KS</td></tr><tr><td>Bs 95.01.8998.1</td><td>65/213</td><td>KS</td></tr><tr><td>Bs 95.01.8998.1</td><td>65/213</td><td>KS</td></tr><tr><td>17571</td><td>Rs 94.01.3217.1</td><td>76/206</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB184*</td></tr><tr><td>17574</td><td>Ws 94.01.5346.1</td><td>72/223</td><td>BRA</td><td>SF Boleráz</td><td>JB185</td></tr><tr><td>18837</td><td>Rs 95.01.8861.1</td><td>65/215</td><td>KS</td><td>USF</td><td>JB186</td></tr><tr><td>16750</td><td>Ws 93.01.2303.1</td><td>63/233</td><td>?</td><td>USF</td><td>JB187</td></tr><tr><td>18244</td><td>Ws 94.01.4730.1</td><td>75/214</td><td>KS</td><td>USF</td><td>JB188**</td></tr><tr><td>15352</td><td>Rs 93.01.1746</td><td>62/233</td><td>KS</td><td>USF</td><td>JB189</td></tr><tr><td>16363</td><td>Ws 93.01.2454</td><td>77/226</td><td>KS</td><td>USF</td><td>JB190</td></tr><tr><td rowspan="2">17868</td><td>Rs 94.01.5255</td><td>78/223</td><td>BRA</td><td rowspan="2">Pfyn / Horgen pot</td><td rowspan="2">JB191*</td></tr><tr><td>Ws 94.01.5351</td><td>79/220</td><td>BRA</td></tr><tr><td rowspan="2">17869</td><td>Ws 94.01.3032</td><td>80/220</td><td>?</td><td rowspan="2">Pfyn / Horgen pot</td><td rowspan="2">JB192*</td></tr><tr><td>Ws 94.01.3158</td><td>80/221</td><td>?</td></tr><tr><td rowspan="2">15763</td><td>Ws 93.01.391</td><td>66/234</td><td>KS</td><td rowspan="2">Pfyn / Horgen pot</td><td rowspan="2">JB193*</td></tr><tr><td>Ws 93.01.391</td><td>66/234</td><td>KS</td></tr><tr><td rowspan="2">15524</td><td>Rs 93.01.2368</td><td>65/233</td><td>KS</td><td rowspan="2">Pfyn / Horgen pot</td><td rowspan="2">JB194*</td></tr><tr><td>Rs 93.01.2368</td><td>65/233</td><td>KS</td></tr></tbody></table>
<table><thead><tr><th>Ceramic Nr.</th><th>Sherd Nr.</th><th>Coordinates</th><th>Bed</th><th>Typological Gp.</th><th>Sample Nr.</th></tr></thead><tbody><tr><td rowspan="6">18250</td><td>Rs 94.01.4846.1</td><td>77/211</td><td>KS</td><td rowspan="6">Pfyn / Horgen pot</td><td rowspan="6">JB195*</td></tr><tr><td>Bs 94.01.4846.1</td><td>77/211</td><td>KS</td></tr><tr><td>Bs 94.01.4846.1</td><td>77/211</td><td>KS</td></tr><tr><td>Ws 94.01.4846.1</td><td>77/211</td><td>KS</td></tr><tr><td>Ws 94.01.4846.1</td><td>77/211</td><td>KS</td></tr><tr><td>Ws 94.01.4846.1</td><td>77/211</td><td>KS</td></tr><tr><td>18250 (follow)</td><td>Ws 94.01.4846.1</td><td>77/211</td><td>KS</td><td>Pfyn / Horgen pot</td><td>JB195*</td></tr><tr><td>20027</td><td>Rs 94.01.3797</td><td>73/205</td><td>BRA</td><td>Pfyn / Horgen pot</td><td>JB196*</td></tr><tr><td rowspan="3">15948</td><td>Ws 93.01.956.1</td><td>71/229</td><td>BRA</td><td rowspan="3">Pfyn / Horgen pot</td><td rowspan="3">JB197*</td></tr><tr><td>Ws 93.01.956.1</td><td>71/229</td><td>BRA</td></tr><tr><td>Ws 93.01.956.1</td><td>71/229</td><td>BRA</td></tr><tr><td rowspan="2">16543</td><td>Ws 93.01.1549</td><td>77/225</td><td>BRA</td><td rowspan="2">Pfyn / Horgen pot</td><td rowspan="2">JB198*</td></tr><tr><td>Ws 93.01.1829</td><td>78/226</td><td>KS</td></tr><tr><td rowspan="2">18306</td><td>Ws 94.01.4603</td><td>76/216</td><td>KS</td><td rowspan="2">Pfyn / Horgen pot</td><td rowspan="2">JB199*</td></tr><tr><td>Ws 94.01.4603</td><td>76/216</td><td>KS</td></tr></tbody></table>

## CERAMICS FROM THE WESTERN CARPATHIAN BASIN

<table><thead><tr><th>Exact provenance</th><th>Land</th><th>Typological Gp.</th><th>Sample Nr.</th></tr></thead><tbody><tr><td>Mödling “Jennyberg”</td><td>Austria</td><td>SF Boleráz</td><td>JB200</td></tr><tr><td>Mödling “Jennyberg”</td><td>Austria</td><td>SF Boleráz</td><td>JB201</td></tr><tr><td>Mödling “Jennyberg”</td><td>Austria</td><td>SF Boleráz</td><td>JB202</td></tr><tr><td>Mödling “Jennyberg”</td><td>Austria</td><td>SF Boleráz</td><td>JB203</td></tr><tr><td>Mödling “Jennyberg”</td><td>Austria</td><td>SF Boleráz</td><td>JB204</td></tr><tr><td>Žlkovce</td><td>Slovakia</td><td>SF Boleráz</td><td>JB205</td></tr><tr><td>Žlkovce</td><td>Slovakia</td><td>SF Boleráz</td><td>JB206</td></tr><tr><td>Žlkovce</td><td>Slovakia</td><td>SF Boleráz</td><td>JB207</td></tr><tr><td>Žlkovce</td><td>Slovakia</td><td>SF Boleráz</td><td>JB208</td></tr><tr><td>Žlkovce</td><td>Slovakia</td><td>SF Boleráz</td><td>JB209</td></tr><tr><td>Naměšť na Hané</td><td>Czech Republic</td><td>SF Boleráz</td><td>JB210</td></tr><tr><td>Naměšť na Hané</td><td>Czech Republic</td><td>SF Boleráz</td><td>JB211</td></tr><tr><td>Naměšť na Hané</td><td>Czech Republic</td><td>SF Boleráz</td><td>JB212</td></tr><tr><td>Naměšť na Hané</td><td>Czech Republic</td><td>SF Boleráz</td><td>JB213</td></tr></tbody></table>

## CLAYS

<table><thead><tr><th>Geographical Coordinates</th><th>Altitude</th><th>Geological bed</th><th>Sample Nr.</th><th>Note</th></tr></thead><tbody><tr><td>263.110 / 749.610</td><td>399</td><td>Moraines</td><td>JB300</td><td>CaO-rich</td></tr><tr><td>263.110 / 749.610</td><td>399</td><td>Moraines</td><td>JB301</td><td>CaO-poor</td></tr><tr><td>263.175 / 748.720</td><td>404</td><td>Moraines</td><td>JB302</td><td>CaO-rich</td></tr><tr><td>262.550 / 747.910</td><td>440</td><td>Moraines</td><td>JB303</td><td>CaO-rich</td></tr><tr><td>262.400 / 748.700</td><td>425</td><td>Moraines</td><td>JB304</td><td>CaO-poor</td></tr><tr><td>262.400 / 748.700</td><td>425</td><td>Moraines</td><td>JB305</td><td>CaO-poor</td></tr><tr><td>261.600 / 750.350</td><td>425</td><td>Molasse</td><td>JB306</td><td>CaO-rich</td></tr><tr><td>261.175 / 749.775</td><td>440</td><td>Molasse</td><td>JB307</td><td>CaO-rich</td></tr><tr><td>263.910 / 749.690</td><td>398</td><td>Molasse</td><td>JB308</td><td>CaO-rich</td></tr><tr><td>263.910 / 749.690</td><td>398</td><td>Molasse</td><td>JB309</td><td>CaO-rich</td></tr><tr><td>264.030 / 748.725</td><td>405</td><td>Molasse</td><td>JB310</td><td>CaO-rich</td></tr></tbody></table>
2 - APPENDIX 2

Summary table of typological and archaeometrical groups discussed in the PhD for each studied sample and estimated
ancient firing temperature.

(SF: Special form; USF: Undetermined special form; G: Grey; Y: Yellow; B: Black; O: Orange).
<table><thead><tr><th>Sample Number</th><th>Typological Group</th><th>Petrographical Group</th><th>Section Colour</th><th>Colour Group</th><th>Firing Temperature</th></tr></thead><tbody><tr><td>JB001</td><td>Pfyn / Horgen pot</td><td>AIV</td><td>G</td><td>1</td><td>600-700°C</td></tr><tr><td>JB002</td><td>Pfyn / Horgen pot</td><td>Al</td><td>G-B-O</td><td>4</td><td>&gt; 950°C</td></tr><tr><td>JB003</td><td>Pfyn / Horgen pot</td><td>Al</td><td>G</td><td>1</td><td>600-700°C</td></tr><tr><td>JB004</td><td>USF</td><td>AV</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB005</td><td>USF</td><td>Al</td><td>Y-B</td><td>5</td><td>&lt; 950°C</td></tr><tr><td>JB006</td><td>SF Boleráz</td><td>Al</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB007</td><td>SF Pfyn</td><td>AIII</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB008</td><td>SF Bayern</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB009</td><td>SF Pfyn</td><td>Al</td><td>G-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB010</td><td>Pfyn / Horgen pot</td><td>AV</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB011</td><td>USF</td><td>Al</td><td>G</td><td>1</td><td>600-700°C</td></tr><tr><td>JB012</td><td>USF</td><td>AVI</td><td>G</td><td>1</td><td>600-700°C</td></tr><tr><td>JB013</td><td>SF Boleráz</td><td>AV</td><td>G-B-G</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB014</td><td>SF Boleráz</td><td>AV</td><td>O-B-O</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB015</td><td>SF Bayern</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB016</td><td>USF</td><td>Al</td><td>Y</td><td>1</td><td>550-950°C</td></tr><tr><td>JB017</td><td>SF Boleráz</td><td>Al</td><td>B</td><td>2</td><td>&lt; 950°C</td></tr><tr><td>JB018</td><td>USF</td><td>AV</td><td>G</td><td>1</td><td>&lt; 950°C</td></tr><tr><td>JB019</td><td>Pfyn / Horgen pot</td><td>AV</td><td>Y</td><td>1</td><td>550-950°C</td></tr><tr><td>JB020</td><td>SF Boleráz</td><td>AVI</td><td>B</td><td>2</td><td>&lt; 950°C</td></tr><tr><td>JB021</td><td>SF Bayern</td><td>Al</td><td>G-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB022</td><td>Pfyn / Horgen pot</td><td>Al</td><td>Y</td><td>1</td><td>550-950°C</td></tr><tr><td>JB023</td><td>Pfyn / Horgen pot</td><td>Al</td><td>G-B-G</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB024</td><td>Pfyn / Horgen pot</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB025</td><td>Pfyn / Horgen pot</td><td>AIV</td><td>O-B-G</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB026</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB027</td><td>USF</td><td>Al</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB028</td><td>Pfyn / Horgen pot</td><td>Al</td><td>O-B-G</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB029</td><td>USF</td><td>AV</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB030</td><td>USF</td><td>Al</td><td>G-B-G</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB031</td><td>Pfyn / Horgen pot</td><td>Al</td><td>O-B-O</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB032</td><td>Pfyn / Horgen pot</td><td>Al</td><td>Y</td><td>1</td><td>550-950°C</td></tr><tr><td>JB033</td><td>SF Boleráz</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB034</td><td>SF Boleráz</td><td>AV</td><td>G-B</td><td>5</td><td>&lt; 950°C</td></tr><tr><td>JB035</td><td>Pfyn / Horgen pot</td><td>BI</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB036</td><td>USF</td><td>AIV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB037</td><td>SF Bayern</td><td>AV</td><td>Y</td><td>1</td><td>550-950°C</td></tr><tr><td>JB038</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB039</td><td>Pfyn / Horgen pot</td><td>Al</td><td>G-B</td><td>5</td><td>&lt; 950°C</td></tr><tr><td>JB040</td><td>USF</td><td>CI</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB041</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB042</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB043</td><td>Pfyn / Horgen pot</td><td>Al</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB044</td><td>Pfyn / Horgen pot</td><td>Al</td><td>G-B</td><td>5</td><td>&lt; 950°C</td></tr><tr><td>JB045</td><td>Pfyn / Horgen pot</td><td>CI</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB046</td><td>USF</td><td>Al</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB047</td><td>Pfyn / Horgen pot</td><td>CI</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB048</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB049</td><td>Pfyn / Horgen pot</td><td>CI</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB050</td><td>SF Boleráz</td><td>Al</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB051</td><td>Pfyn / Horgen pot</td><td>AV</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB052</td><td>Pfyn / Horgen pot</td><td>AIV</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB053</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB054</td><td>Pfyn / Horgen pot</td><td>Al</td><td>Y-B-G</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB055</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB056</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB057</td><td>USF</td><td>Al</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB058</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB059</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB060</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr></tbody></table>

<table><thead><tr><th>Sample Number</th><th>Typological Group</th><th>Petrographical Group</th><th>Section Colour</th><th>Colour Group</th><th>Firing Temperature</th></tr></thead><tbody><tr><td>JB061</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-O</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB062</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB063</td><td>SF Boleráz</td><td>AV</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB064</td><td>Pfyn / Horgen pot</td><td>CI</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB065</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB066</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB067</td><td>Pfyn / Horgen pot</td><td>AIV</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB068</td><td>Pfyn / Horgen pot</td><td>Al</td><td>G-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB069</td><td>SF Boleráz</td><td>AVI</td><td>G-B-G</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB070</td><td>Pfyn / Horgen pot</td><td>AIV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB071</td><td>USF</td><td>BI</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB072</td><td>USF</td><td>Al</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB073</td><td>SF Boleráz</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB074</td><td>USF</td><td>AIV</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB075</td><td>USF</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB076</td><td>Pfyn / Horgen pot</td><td>All</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB086</td><td>USF</td><td>AV</td><td>B</td><td>2</td><td>&lt; 950°C</td></tr><tr><td>JB087</td><td>USF</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB088</td><td>SF Bayern</td><td>AV</td><td>Y-B</td><td>5</td><td>&lt; 950°C</td></tr><tr><td>JB089</td><td>Pfyn / Horgen pot</td><td>All</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB090</td><td>SF Bayern</td><td>CI</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB091</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB092</td><td>Pfyn / Horgen pot</td><td>AV</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB093</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB094</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB095</td><td>SF Bayern</td><td>Al</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB096</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB097</td><td>Pfyn / Horgen pot</td><td>All</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB098</td><td>USF</td><td>Al</td><td>G-B-G</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB099</td><td>SF Boleráz</td><td>BI</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB100</td><td>Pfyn / Horgen pot</td><td>Al</td><td>G</td><td>3</td><td>600-700°C</td></tr><tr><td>JB101</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>1</td><td>&lt; 950°C</td></tr><tr><td>JB102</td><td>USF</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB103</td><td>Pfyn / Horgen pot</td><td>Al</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB104</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB105</td><td>USF</td><td>Al</td><td>B</td><td>2</td><td>&gt; 700°C</td></tr><tr><td>JB106</td><td>SF Boleráz</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB107</td><td>USF</td><td>Al</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB108</td><td>Pfyn / Horgen pot</td><td>AIV</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB109</td><td>Pfyn / Horgen pot</td><td>All</td><td>Y-B</td><td>5</td><td>&lt; 950°C</td></tr><tr><td>JB110</td><td>SF Bayern</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB111</td><td>Spindlewhorl</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB112</td><td>Spindlewhorl</td><td>AV</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB113</td><td>Spindlewhorl</td><td>Al</td><td>B</td><td>2</td><td>&lt; 950°C</td></tr><tr><td>JB114</td><td>Spindlewhorl</td><td>Al</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB115</td><td>Spindlewhorl</td><td>Al</td><td>B</td><td>2</td><td>&lt; 950°C</td></tr><tr><td>JB116</td><td>Spindlewhorl</td><td>Al</td><td>G</td><td>1</td><td>600-700°C</td></tr><tr><td>JB117</td><td>Spindlewhorl</td><td>Al</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB118</td><td>Spindlewhorl</td><td>A</td><td>G</td><td>3</td><td>600-700°C</td></tr><tr><td>JB119</td><td>Spindlewhorl</td><td>Al</td><td>Y</td><td>1</td><td>&lt; 500°C</td></tr><tr><td>JB120</td><td>Spindlewhorl</td><td>AV</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB121</td><td>Loomweight</td><td>CIII</td><td></td><td></td><td>non fired</td></tr><tr><td>JB122</td><td>Cob</td><td>CIII</td><td></td><td></td><td>non fired</td></tr><tr><td>JB123</td><td>Cob</td><td>CIII</td><td></td><td></td><td>non fired</td></tr><tr><td>JB124</td><td>Cob</td><td>CIII</td><td></td><td></td><td>non fired</td></tr><tr><td>JB125</td><td>Cob</td><td>CIII</td><td></td><td></td><td>non fired</td></tr><tr><td>JB126</td><td>Cob</td><td>CIII</td><td></td><td></td><td>non fired</td></tr><tr><td>JB127</td><td>Cob</td><td>CIII</td><td></td><td></td><td>non fired</td></tr><tr><td>JB128</td><td>Cob</td><td>CIII</td><td></td><td></td><td>non fired</td></tr><tr><td>JB129</td><td>Cob</td><td>CIII</td><td></td><td></td><td>non fired</td></tr><tr><td>JB130</td><td>Cob</td><td>CIII</td><td></td><td></td><td>non fired</td></tr><tr><td>JB131</td><td>Cob</td><td>CIII</td><td></td><td></td><td>non fired</td></tr><tr><td>JB132</td><td>Cob</td><td>CIII</td><td></td><td></td><td>non fired</td></tr></tbody></table>
<table><thead><tr><th>Sample Number</th><th>Typological Group</th><th>Petrographical Group</th><th>Section Colour</th><th>Colour Group</th><th>Firing Temperature</th></tr></thead><tbody><tr><td>JB133</td><td>Pfyn / Horgen pot</td><td>AV</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB134</td><td>Pfyn / Horgen pot</td><td>Al</td><td>Y</td><td>1</td><td>&lt; 500°C</td></tr><tr><td>JB135</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB136</td><td>Pfyn / Horgen pot</td><td>Al</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB137</td><td>Pfyn / Horgen pot</td><td>Al</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB138</td><td>SF Boleráz</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB139</td><td>SF Boleráz</td><td>AV</td><td>G-B-G</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB140</td><td>SF Boleráz</td><td>AIV</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB141</td><td>SF Boleráz</td><td>BII</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB142</td><td>USF</td><td>Al</td><td>G-B</td><td>5</td><td>&lt; 950°C</td></tr><tr><td>JB143</td><td>SF Bayern</td><td>Al</td><td>B</td><td>2</td><td>&lt; 600°C</td></tr><tr><td>JB144</td><td>SF Boleráz</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB145</td><td>SF Boleráz</td><td>AV</td><td>G</td><td>1</td><td>&lt; 600°C</td></tr><tr><td>JB146</td><td>SF Boleráz</td><td>AV</td><td>G-B-G</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB147</td><td>SF Boleráz</td><td>AVI</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB148</td><td>SF Boleráz</td><td>AV</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB149</td><td>SF Boleráz</td><td>AIV</td><td>Y</td><td>1</td><td>550-950°C</td></tr><tr><td>JB150</td><td>SF Bayern</td><td>Al</td><td>B</td><td>2</td><td>&lt; 600°C</td></tr><tr><td>JB151</td><td>SF Bayern</td><td>AV</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB152</td><td>SF Boleráz</td><td>Al</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB153</td><td>SF Bayern</td><td>Al</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB154</td><td>SF Boleráz</td><td>BII</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB155</td><td>SF Boleráz</td><td>AV</td><td>B-Y</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB157</td><td>SF Bayern</td><td>AV</td><td>G-B-G</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB158</td><td>USF</td><td>Al</td><td>B</td><td>2</td><td>&lt; 600°C</td></tr><tr><td>JB159</td><td>USF</td><td>AV</td><td>G</td><td>1</td><td>&lt; 600°C</td></tr><tr><td>JB160</td><td>USF</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB162</td><td>USF</td><td>Al</td><td>G</td><td>1</td><td>&lt; 600°C</td></tr><tr><td>JB163</td><td>USF</td><td>AIV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB164</td><td>USF</td><td>Al</td><td>G</td><td>1</td><td>&lt; 600°C</td></tr><tr><td>JB165</td><td>USF</td><td>AV</td><td>B-G</td><td>3</td><td>&lt; 950°C</td></tr><tr><td>JB166</td><td>USF</td><td>AV</td><td>B</td><td>2</td><td>&lt; 600°C</td></tr><tr><td>JB167</td><td>USF</td><td>Al</td><td>B</td><td>2</td><td>&lt; 600°C</td></tr><tr><td>JB169</td><td>USF</td><td>AV</td><td>G</td><td>1</td><td>600-700°C</td></tr><tr><td>JB171</td><td>SF Pfyn</td><td>Al</td><td>G</td><td>1</td><td>600-700°C</td></tr><tr><td>JB173</td><td>USF</td><td>Al</td><td>G</td><td>1</td><td>600-700°C</td></tr><tr><td>JB174</td><td>USF</td><td>AV</td><td>Y</td><td>1</td><td>550-950°C</td></tr><tr><td>JB175</td><td>SF Boleráz</td><td>AV</td><td>Y</td><td>1</td><td>550-950°C</td></tr><tr><td>JB177</td><td>USF</td><td>Al</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB178</td><td>USF</td><td>Al</td><td>G</td><td>1</td><td>&lt; 600°C</td></tr><tr><td>JB179</td><td>SF Boleráz</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB180</td><td>USF</td><td>AV</td><td>G</td><td>1</td><td>&lt; 600°C</td></tr><tr><td>JB181</td><td>USF</td><td>Al</td><td>G</td><td>1</td><td>600-700°C</td></tr><tr><td>JB182</td><td>USF</td><td>AV</td><td>Y-B-Y</td><td>4</td><td>&lt; 950°C</td></tr><tr><td>JB183</td><td>USF</td><td>Al</td><td>G</td><td>1</td><td>&lt; 600°C</td></tr><tr><td>JB185</td><td>SF Boleráz</td><td>AV</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB186</td><td>USF</td><td>Al</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB187</td><td>USF</td><td>Al</td><td>B</td><td>2</td><td>600-700°C</td></tr><tr><td>JB188</td><td>USF</td><td>Al</td><td>G</td><td>1</td><td>600-700°C</td></tr><tr><td>JB189</td><td>USF</td><td>AV</td><td>G</td><td>1</td><td>600-700°C</td></tr><tr><td>JB190</td><td>USF</td><td>Al</td><td>Y</td><td>1</td><td>550-950°C</td></tr></tbody></table>
3 - APPENDIX 3

Petrographical description of the thin sections.

(SF: special form, USF: undetermined special form; Si: silicate-rich matrix, Ca: carbonate-rich matrix, incl.: inclusion; in "Temper": 1: few; 2: present; 3: frequent; 4: much; GR: Granite, GA: Gabbro, GG: grog; RH: Rhyolite; CH: Chert; BO: Bone; definition of the petrographical groups, see text).
<table><thead><tr><th rowspan="2">Sample Number</th><th rowspan="2">Typological Group</th><th rowspan="2">Matrix</th><th colspan="7">Temper</th><th colspan="4">Temper Type</th><th rowspan="2">Petrographical Group</th></tr><tr><th>Rock (vol.%)</th><th>Granite</th><th>Rhyolite</th><th>Chert</th><th>Gabbro</th><th>Grog (vol.%)</th><th>Bone (vol.%)</th><th>Main</th><th>Second</th><th>Third</th><th>Fourth</th></tr></thead><tbody><tr><td>JB001</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>20</td><td>1</td><td></td><td></td><td></td><td></td><td></td><td>GA</td><td>GR</td><td>GG</td><td></td><td>AIV</td></tr><tr><td>JB002</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>10</td><td>2</td><td>1</td><td></td><td></td><td></td><td></td><td>GR</td><td>RH</td><td>GG</td><td></td><td>AI</td></tr><tr><td>JB003</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>20</td><td>3</td><td></td><td></td><td></td><td></td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB004</td><td>USF</td><td>Si, incl. poor</td><td>10</td><td></td><td></td><td></td><td></td><td></td><td></td><td>GG</td><td></td><td></td><td></td><td>AV</td></tr><tr><td>JB005</td><td>USF</td><td>Si, incl. poor</td><td>5</td><td>2</td><td></td><td></td><td></td><td></td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB006</td><td>SF Boleráz</td><td>Si, incl. poor</td><td>10</td><td>2</td><td></td><td></td><td></td><td></td><td></td><td>GR</td><td>GG</td><td></td><td></td><td>AI</td></tr><tr><td>JB007</td><td>SF Pfyn</td><td>Si, incl. poor</td><td>15</td><td>1</td><td></td><td>3</td><td>1</td><td>3</td><td></td><td>CH</td><td>GR</td><td>GA</td><td>GG</td><td>AIII</td></tr><tr><td>JB008</td><td>SF Bayern</td><td>Si, incl. poor</td><td>5</td><td>2</td><td>1</td><td></td><td>1</td><td>10</td><td></td><td>GG</td><td>GR</td><td>RH</td><td>GA</td><td>AV</td></tr><tr><td>JB009</td><td>SF Pfyn</td><td>Si, incl. poor</td><td>25</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td>CH</td><td></td><td></td><td>AI</td></tr><tr><td>JB010</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>0</td><td></td><td></td><td></td><td></td><td>7</td><td></td><td>GG</td><td></td><td></td><td></td><td>AV</td></tr><tr><td>JB011</td><td>USF</td><td>Si, incl. poor</td><td>20</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB012</td><td>USF</td><td>Si, incl. poor</td><td>0</td><td></td><td></td><td></td><td></td><td>10</td><td>10, black</td><td>BO</td><td>GG</td><td></td><td></td><td>AVI</td></tr><tr><td>JB013</td><td>USF</td><td>Si, incl. poor</td><td>20</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>SG</td><td>GG</td><td>CH</td><td></td><td>AIV</td></tr><tr><td>JB014</td><td>SF Boleráz</td><td>Si, incl. poor</td><td>3</td><td>2</td><td></td><td></td><td></td><td>7</td><td></td><td>GG</td><td>GR</td><td></td><td></td><td>AV</td></tr><tr><td>JB015</td><td>SF Bayern</td><td>Si, incl. poor</td><td>5</td><td>2</td><td></td><td></td><td></td><td>10</td><td></td><td>GG</td><td>GR</td><td></td><td></td><td>AV</td></tr><tr><td>JB016</td><td>USF</td><td>Si, incl. poor</td><td>5</td><td>2</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB017</td><td>SF Boleráz</td><td>Si, incl. poor</td><td>5</td><td>2</td><td>2</td><td></td><td></td><td>2</td><td></td><td>GR</td><td>RH</td><td>GG</td><td></td><td>AI</td></tr><tr><td>JB018</td><td>USF</td><td>Si, incl. poor</td><td>2</td><td>2</td><td></td><td></td><td></td><td>5</td><td></td><td>GG</td><td>GR</td><td></td><td></td><td>AV</td></tr><tr><td>JB019</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>2</td><td>2</td><td></td><td></td><td></td><td>5</td><td></td><td>GG</td><td>GR</td><td></td><td></td><td>AV</td></tr><tr><td>JB020</td><td>SF Boleráz</td><td>Si, incl. poor</td><td>5</td><td>2</td><td></td><td></td><td></td><td>10</td><td>20</td><td>BO</td><td>GG</td><td>GR</td><td></td><td>AVI</td></tr><tr><td>JB021</td><td>SF Bayern</td><td>Si, incl. poor</td><td>10</td><td>2</td><td></td><td></td><td></td><td>5</td><td></td><td>GR</td><td>GG</td><td></td><td></td><td>AI</td></tr><tr><td>JB022</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>25</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB023</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>25</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td>CH</td><td></td><td></td><td>AI</td></tr><tr><td>JB024</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>5</td><td>2</td><td></td><td></td><td></td><td>10</td><td></td><td>GG</td><td>GR</td><td></td><td></td><td>AV</td></tr><tr><td>JB025</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>10</td><td>1</td><td></td><td></td><td>2</td><td>0</td><td></td><td>GA</td><td>GR</td><td></td><td></td><td>AIV</td></tr><tr><td>JB026</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>20</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB027</td><td>USF</td><td>Si, incl. poor</td><td>10</td><td>2</td><td>1</td><td></td><td></td><td>2</td><td></td><td>GR</td><td>RH</td><td>GG</td><td></td><td>AI</td></tr><tr><td>JB028</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>5</td><td>2</td><td></td><td></td><td></td><td>2</td><td></td><td>GR</td><td>CH</td><td>GG</td><td></td><td>AI</td></tr><tr><td>JB029</td><td>USF</td><td>Si, incl. poor</td><td>2</td><td>2</td><td></td><td></td><td></td><td>5</td><td></td><td>GG</td><td>GR</td><td></td><td></td><td>AV</td></tr><tr><td>JB030</td><td>USF</td><td>Si, incl. poor</td><td>15</td><td>3</td><td></td><td></td><td></td><td>2</td><td></td><td>GR</td><td>GG</td><td></td><td></td><td>AI</td></tr><tr><td>JB031</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>25</td><td>3</td><td>1</td><td></td><td></td><td>0</td><td></td><td>GR</td><td>RH</td><td></td><td></td><td>AI</td></tr><tr><td>JB032</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>10</td><td>2</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td>CH</td><td></td><td></td><td>AI</td></tr><tr><td>JB033</td><td>SF Boleráz</td><td>Si, incl. poor</td><td>0</td><td></td><td></td><td></td><td></td><td>2</td><td></td><td>GG</td><td></td><td></td><td></td><td>AV</td></tr><tr><td>JB034</td><td>SF Boleráz</td><td>Si, incl. poor</td><td>0</td><td></td><td></td><td></td><td></td><td>2</td><td></td><td>GG</td><td></td><td></td><td></td><td>AV</td></tr><tr><td>JB035</td><td>USF</td><td>Si, incl. rich</td><td>15</td><td>2</td><td></td><td></td><td></td><td>2</td><td></td><td>GR</td><td>CH</td><td>GG</td><td></td><td>AIV</td></tr><tr><td>JB036</td><td>USF</td><td>Si, incl. poor</td><td>15</td><td>2</td><td></td><td></td><td>2</td><td>0</td><td></td><td>GA</td><td>GR</td><td></td><td></td><td>AIV</td></tr><tr><td>JB037</td><td>SF Bayern</td><td>Si, incl. poor</td><td>3</td><td>2</td><td></td><td></td><td></td><td>10</td><td></td><td>GG</td><td>GR</td><td></td><td></td><td>AV</td></tr><tr><td>JB038</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>20</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB039</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>20</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB040</td><td>USF</td><td>Ca, incl. rich</td><td>10</td><td>2</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>CI</td></tr><tr><td>JB041</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>20</td><td>3</td><td>1</td><td></td><td></td><td>0</td><td></td><td>GR</td><td>RH</td><td></td><td></td><td>AI</td></tr><tr><td>JB042</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>25</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB043</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>7</td><td>2</td><td></td><td></td><td></td><td>2</td><td></td><td>GR</td><td>GG</td><td></td><td></td><td>AI</td></tr><tr><td>JB044</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>25</td><td>3</td><td></td><td></td><td></td><td>2</td><td></td><td>GR</td><td>GA</td><td>GG</td><td></td><td>AI</td></tr><tr><td>JB045</td><td>Pfyn / Horgen pot</td><td>Ca, incl. rich</td><td>25</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>CI</td></tr><tr><td>JB046</td><td>USF</td><td>Si, incl. poor</td><td>10</td><td>2</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB047</td><td>Pfyn / Horgen pot</td><td>Ca, incl. rich</td><td>10</td><td>2</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>CI</td></tr><tr><td>JB048</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>2</td><td>2</td><td></td><td></td><td></td><td>2</td><td></td><td>GR</td><td>GG</td><td></td><td></td><td>AI</td></tr><tr><td>JB049</td><td>Pfyn / Horgen pot</td><td>Ca, incl. rich</td><td>10</td><td>2</td><td></td><td></td><td></td><td>2</td><td></td><td>GR</td><td>GA</td><td>GG</td><td></td><td>CI</td></tr><tr><td>JB050</td><td>SF Boleráz</td><td>Si, incl. poor</td><td>5</td><td>2</td><td></td><td></td><td></td><td>2</td><td></td><td>GR</td><td>GG</td><td></td><td></td><td>AI</td></tr><tr><td>JB051</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>3</td><td>2</td><td></td><td></td><td></td><td>15</td><td></td><td>GG</td><td>GR</td><td></td><td></td><td>AV</td></tr><tr><td>JB052</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>25</td><td></td><td></td><td>1</td><td>3</td><td>0</td><td></td><td>GA</td><td>CH</td><td></td><td></td><td>AIV</td></tr><tr><td>JB053</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>7</td><td>2</td><td></td><td></td><td></td><td>3</td><td></td><td>GR</td><td>GG</td><td></td><td></td><td>AI</td></tr><tr><td>JB054</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>15</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB055</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>15</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB056</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>15</td><td>3</td><td></td><td></td><td></td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB057</td><td>USF</td><td>Si, incl. poor</td><td>15</td><td>3</td><td></td><td></td><td></td><td>3</td><td></td><td>GR</td><td>GG</td><td></td><td></td><td>AI</td></tr><tr><td>JB058</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>20</td><td>3</td><td></td><td></td><td></td><td>2</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr><tr><td>JB059</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>10</td><td>2</td><td>1</td><td></td><td>2</td><td>0</td><td></td><td>GR</td><td>GA</td><td>RH</td><td></td><td>AI</td></tr><tr><td>JB060</td><td>Pfyn / Horgen pot</td><td>Si, incl. poor</td><td>10</td><td>2</td><td></td><td></td><td>0</td><td>0</td><td></td><td>GR</td><td></td><td></td><td></td><td>AI</td></tr></tbody></table>