• Digital Humanities and Cultural Heritage
• Research data close
• Research software close
• Other research products close
• Refubium - Repositorium der Freien ... close

The organic residue analyses were carried out at the core facillity BioSupraMol of the departement of Biology, Chemistry, and Pharmacy (Freie Univ. Berlin). Two extractions protocols have been applied in order to extract lipids (Pecci et al. 2013 [A]), and other small organic acids (Pecci et al. 2013a [B]) from the powdered ceramic samples. A. 2 g samples are extracted in 50 ml chloroform/methanol (2:1 v/v) for 2×15 min in an ultrasonic bath. The samples are then centrifuged for 10 min and the supernatant is evaporated to dryness under a steady stream of nitrogen. The samples are saponified with 2 ml sodium hydroxide solution (2M in MeOH) for 1 h at 70° C. After cooling, it is acidified with 15 drops of concentrated hydrochloric acid, the pH value is checked (pH 1). It is then extracted twice with 3 ml of chloroform. Then the solvent of the organic phase is removed under a constant stream of nitrogen and the sample is transferred to a sample vial with two times 50 μl of chloroform. The sample is then evaporated off and the sample is derivatized with 25 μl of BSTFA at 70° C for 1 hour. After the addition of 75 µl n-hexane and 5 µl internal standard (dotriacontane in hexane, see respective table of results for concentration), the samples are analysed by GC-MS. B. 500 mg sample is extracted in 3 ml potassium hydroxide solution (1M in H2O) for 90 min at 70°C. The samples are then centrifuged for 10 min and the supernatant is acidified with 15 drops of concentrated hydrochloric acid, and the pH value (pH 1) is checked. Then the samples are shaken intensively with 3 ml ethyl acetate for 2 min and centrifuged for 10 min. This step is repeated 3 times in total. The supernatant (organic phase) is concentrated under a constant stream of nitrogen and transferred to a sample vial with two 50 μl portions of ethyl acetate. The solvent is then evaporated off and the sample is derivatized with 25 μl of BSTFA at 70° C. for 1 hour. After the addition of 75 µl n-hexane and 5 µl internal standard (dotriacontane in hexane, see respective table of results for concentration), the samples are analysed by GC-MS. All samples were analysed using Agilent 7820A GC system and Agilent 5977 MSD, equipped with HP5-MS capillary column and EI as ion source. Initial oven temperature 50°C with a temperature ramp of 5 °C/min to 320 °C and hold time of 10 min. For this method a split ratio of 1:10 has been used. Pecci, A., Cau, M.A., Garnier N., Identifying wine and oil pro- duction: analysis of residues from Roman and Late Antique plastered vats. Journal of Archaeological Science, 40, 2013, 4491–4498 Pecci, A., G. Giorgi, L. Salvini, Cau Ontiveros M.A., Identifying Wine Markers in Ceramics and Plasters with Gas Chromatography — Mass Spectrometry. Experimental and Archaeological Materials. Journal of Archaeological Science 40, 2013a, 109–115 Twenty-four (24) samples of cooking wares (olle) from the excavation of the high-mountain hut and enclosures at Busa delle Vette (1858 m asl; Parco delle Dolomiti Bellunesi, Belluno Province, Veneto, Northern Italy) have been considered for GC-MS analysis of the amorphous organic residue absorbed and kept in the ceramic pores. The in 2018 unearthed samples come from the excavation area B (US 303, 304, 315 and 322) at Busa delle Vette conducted within the framework of the UPLanD project directed by F. Cavulli and F. Carrer. The results of GC-MS analysis of the samples are listed in the table. Trace compounds are also listed and marked as (traces). All compounds listed fulfil at least the following criteria: automated detection of the structure-specific signals. For all compounds, three m/z and their respective ratios expected from comparison to pure standards analysed on the same instrument were used, and only if the peak was higher than 7 times S/N at the respective m/z.

Radiocarbon dating of two bone samples from the archaeological excavation of the farm at Ain Wassel (High Tunisian Tell). The analysed material comes from the archaeological excavation at Ain Wassel carried out by the University of Trento (Italy) and the Institut National du Patrimoine of Tunisia, under the joint direction of Mustapha Khanoussi and Mariette de Vos Raaijmakers (1994- 1996). See: http://rusafricum.org/en/thuggasurvey/home/ The samples, a pork (KIA-55574) and a chicken (KIA-55575) bone, come from a fill layer including very mixed heretogeneous material dating to the Byzantine period and adhered to the wall of a ceramic vessel (closed form in common ware). The analysis have been carried out by the The Leibniz Laboratory for Radiometric Dating and Stable Isotope Research (AMS 14C Lab). For methodology and references, see: Reimer, P., Austin, W., Bard, E., Bayliss, A., Blackwell, P., Bronk Ramsey, C., . . . Talamo, S. (2020). The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP). Radiocarbon, 62(4), 725-757. doi:10.1017/RDC.2020.41 Ramsey, C., & Lee, S. (2013). Recent and Planned Developments of the Program OxCal. Radiocarbon, 55(2), 720-730. doi:10.1017/S0033822200057878 Longin R. New method of collagen extraction for radiocarbon dating. Nature. 1971 Mar 26;230(5291):241-2. doi: 10.1038/230241a0 Stuiver, M., & Polach, H. (1977). Discussion Reporting of 14C Data. Radiocarbon, 19(3), 355-363. doi:10.1017/S0033822200003672