Raw material sources for the Roman Bracarense ceramics (NW Iberian Peninsula)

The Bracarense ceramics are characterized by a fine, pale yellow paste covered with a brownish yellow slip. The name is derived from Bracara Augusta, the Roman town located in the north of Portugal, where this type of ceramic paste was first found and identified. Various forms with the same type of paste occur, such as imitations of sigillata, terra sigillata and thin walls from the Augustus-Tiberius period, and common ware. Later, similar ceramics were also found in other archeological sites, e.g. Aquis Querquennis (Galiza, Spain), which question the location of the production center of this type of ceramic paste.Mineralogical and chemical analyses showed that the majority of the Bracarense shards studied differ from the common ware of the Braga region. Despite minor differences, the Bracarense shards collected in Aquis Querquennis have the same geochemical pattern as those found in Bracara Augusta, i.e. they appear to have been manufactured with the same clay type. The firing products found indicate a kaolin character of the source clay, and point to firing temperatures near 900°C. The Aquis Querquennis shards have greater Br contents, which can be explained by use-wear and/or post-depositional processes, as this site is located in a thermal-water region.

[1]  M. S. Braga,et al.  Weathering of granites in a temperate climate (NW Portugal): granitic saprolites and arenization , 2002 .

[2]  Isabelle C. Druc,et al.  Archaeological ceramic materials : origin and utilization , 1999 .

[3]  Udayan Senapati,et al.  Porcelain—Raw Materials, Processing, Phase Evolution, and Mechanical Behavior , 1998 .

[4]  K. Govindaraju,et al.  1994 REPORT ON ZINNWALDITE ZW‐C ANALYSED BY NINETY‐TWO GIT‐IWG MEMBER‐LABORATORIES , 1994 .

[5]  K. Govindaraju,et al.  1994 compilation of working values and sample description for 383 geostandards , 1994 .

[6]  S. K. Guha,et al.  Minerological studies on five plastic fire clays , 1992 .

[7]  M. F. Reis,et al.  Factor for correcting the ruthenium interference in instrumental neutron activation analysis of barium in uraniferous samples. , 1991, International Journal of Radiation Applications and Instrumentation. Part A: Applied Radiation and Isotopes.

[8]  Manuela Martins,et al.  História e arqueologia de uma cidade em devir: Bracara Augusta , 1989 .

[9]  J. Cabral,et al.  Identification of clay sources used for Conimbriga and Santa Olaia pottery making , 1989 .

[10]  C. Gomes,et al.  Argilas: O Que São e Para Que Servem , 1988 .

[11]  M. Gouveia,et al.  Instrumental neutron activation analysis of NBS-97A flint clay and NBS-98A plastic clay reference samples with a view to their use as standards for archaeological pottery studies and clay studies , 1988 .

[12]  M. Freitas,et al.  Interference from uranium fission products in the determination of rare earths, zirconium and ruthenium by instrumental neutron activation analysis in rocks and minerals , 1987 .

[13]  M. Gouveia,et al.  Instrumental Neutron Activation Analysis of Two French Geochemical Reference Samples - Basalt BR and Biotite Mica-Fe , 1986 .

[14]  G. C. Amstutz,et al.  Process mineralogy of ceramic materials , 1984 .

[15]  G. W. Brindley,et al.  X-Ray diffraction procedures for clay mineral identification , 1980 .

[16]  A. Alarcão,et al.  Uma cerâmica aparentada com as «paredes finas» de Mérida , 1976 .

[17]  T. F. Bates The kaolin minerals , 1971 .