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Attia EA, Belal DM, El Samahy MH, El Hamamsy MH

Thus, incremental 34 S analysis of hypsodont tooth dentine collagen, as has been conducted for 13 C and 15 N (Dez-Canseco and Tornero, Figures 4AC), perhaps with seasonal climate signals constrained by incremental analysis of 18 O in enamel bioapatite adjusted for differences in timing and mineralization processes between dentine and enamel (Balasse, 6 Conclusions This work highlights the dynamic nature of sulfur isotope baselines affected by sulfur cycling in wet and waterlogged environments, while acknowledging the complexity of establishing local dryland 34 S baselines derived from geological and marine sulfur against which to assess potential wetland signals for archaeological applications

Adjusting Dosage: Based on response and under medical supervision

Psychiatry 65, 489494