| Among the Gaulish workshops, La Graufesenque
(Aveyron, France) was a very important Terra Sigillata
ceramics centre. After copying Italian sigillata between
10BC and 20AC, this workshop started a large-scale production of
high quality sigillata (20AC, 120AC), which was sold in
most of the Roman world (Fig. 1). This workshop had an industrial
organisation, with collective firing in very big kilns (capacity:
10000 to 40000 vessels).
Fig.1 Distribution map of the Terra sigillata
from La Graufesenque workshop.
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The excavations of the Montans
workshop (Tarn, France) suggest a smaller scale production. The
production of sigillata also started during the Tiberian
period (15 AC, 38 AC), following a test period when (where) Italian
models were copied. The main diffusion was along the Atlantic coasts.
With the archaeologists of the Unité Toulousaine d’Archéologie
et d’Histoire (UTAH) of the university Toulouse-Le
Mirail, we have decided to study together these two workshops
with two aims:
• compare their productions:
o Did the Gaulish potters use the same technical solutions as the
Italian potters?
o Did the workshop organisation have an influence on the quality
of the sigillata ware?
• study the transition period (proto-sigillata (or
imitation) —> sigillata), to understand how the
production of high quality sigillata started .
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| The investigations are carried out by SEM (Scanning
Electron Microscopy), X-ray diffraction and TEM (Transmission
Electron Microscopy) with EELS analysis (Fig. 2).
In both cases, different clays were used for preparing the body
and the slip respectively. The ceramic body was prepared from the
calcareous local clay close to the workshops. |
On the other hand, the slip was obtained from a
non-calcareous clay of illitic type. Chemical and mineral compositions
are much more homogeneous at La Graufesenque, likely because of
the more industrial organisation with collective clay preparations
and collective firings. These small variations of the mineral composition
confirm the great mastery of the firing under oxidising atmosphere.
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