Geochemical Study of Bitumen Residues on Potsherds from the al-Qusur Monastery (7th-9th c. CE): Composition and Origin

  • 1Université de Strasbourg, 23 rue Antoine de Saint-Exupéry, 64000 Pau, France.
  • 2French Research Centre in the Arabian Peninsula, USR3141, Kuwait City 92438, Kuwait.
  • 3LA3M-UMR 7298, Aix-Marseille University, 13100 Aix-en-Provence, France.
  • 4School of Geosciences, The University of Oklahoma, 100 East Boyd Street, Norman, OK 73019-1009, USA.
  • 5Laboratoire Interdisciplinaire des Environnements Continentaux, UMR7360, Site Chamois, 15 Avenue de Chamois, 54500 Vandeouvre-les-Nancy, France.
  • 6GeoMark Research Inc., 9748 Whithorn Drive, Houston, TX 77095, USA.
  • 7Institut Le Bel, UMR 7177, Université de Strasbourg, 4 rue Blaise Pascal, 67000 Strasbourg, France.

Abstract

Geochemical and isotopic analysis of bitumen lining potsherds from the al-Qusur monastery (second half of the 7th c. CE and the middle of the 9th c. CE), at the central part of Failaka Island (Kuwait Bay), confirms the presence of two distinct compositional categories that can be matched to contemporary sources from two different areas of Iran: the Kermanshah province on one side, and the Khuzestan-Fars-Busher provinces on the other side. Potsherds comprise different types: TORP-S amphorae, TORP-C amphorae, SPORC storage jar, turquoise alkaline-glazed jar (TURQ.T), and CREAC jar. There is no relationship between the type of potsherd and the origin of bitumen. The bitumen coating SPORC jar, first identified as a kind of juice strainer to filter the «garum-like juice», was examined in greater details to try to identify traces of fish sauce mentioned in the Arabic kitchen books as 'murri', and quite similar to the Roman garum. The mineralogical analysis exhibits the classical minerals of archaeological mixtures (quartz, calcite, dolomite) and no halite. Hydrocarbons, alcohols, and methyl esters show a typical biodegraded bitumen signature but no fatty acids and terpenoids. It seems that the bitumen matrix has not adsorbed any molecules from the presumed «garum» filtered in the basin.

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