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overlying Orea Shales of glaciogenic origin, interpreted as dispersed by drifting icebergs. Daroca, our destination for the second night of the excursion, was another walled town of considerable antiquity and distinctive architecture. The third and final day of the excursion visited outcrops of Lower Ordovician strata in the western Iberian Chain, where the stratotype section of the Valconchan, Dere and Santed Formations was examined. This was a very instructive sedimentological sequence comprised of stacked shallowing-upwards parasequence sets, largely devoid of fossils except for rare horizons characterised by lingulide brachiopods. The well-exposed road section up to Santed Summit again proved the serendipitous nature of conference excursions, as Nicolay Sennikov (Novosibirsk) discovered graptoloids that provided the first-ever confirmation of the Early Ordovician (Tremadocian) age of these rocks. A traditional Spanish banquet concluded the post-symposium excursion, which was notable for its excellent organisation, accommodation, food, and of course superb outcrops.

episodes

International Conference on Neoproterozoic Sedimentary Basins, Neoproterozoic Subcommission Workshop on Ediacaran Paleobiology, and IGCP Field Excursion to the East Sayan Mountain Range