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Both oven-dried and pre-fired specimens wrapped in Ni-Fe foil within the ( poorly) vented assembly were recovered essentially dry after 50-100 h of annealing at 1300 degrees C followed by slow staged cooling. The results for those specimens indicate broadly similar absorption-band viscoelastic behaviour, but with systematic differences in the frequency dependence of strain-energy dissipation Q(-1), attributed to differences in the small volume fraction of silicate melt and its spatial distribution. In contrast, it has been demonstrated that a new assembly involving a welded Pt capsule retains aqueous fluid during prolonged exposure to high temperatures allowing the first high-temperature torsional forced-oscillation measurements under high aqueous fluid pore pressure P-f. At temperatures>1000 degrees C, a marked reduction in shear modulus, without concomitant increase in Q(-1), is attributed to the widespread wetting of grain boundaries resulting from grain-scale hydrofracturing and the maintenance of conditions of low differential pressure P-d=P-c-P-f. Staged cooling from 1000 degrees C is accompanied by decreasing Pf and progressive restoration of significantly positive differential pressure resulting in a microstructural regime in which the fluid on grain boundaries is increasingly restricted to arrays of pores. The more pronounced viscoelastic behaviour observed within this regime for the Pt-encapsulated specimen compared with the essentially dry specimens may reflect both water-enhanced solid-state relaxation and the direct influence of the fluid phase. The scenario of overpressurized fluids and hydrofracturing in the Pt-encapsulated dunite specimen may have some relevance to the high Q(-1) and low-velocity zones observed in subduction-zone environments. 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