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There are two main themes that run through most of the papers in this volume. (1) Biostratigraphical control is commonly so good in much of Britain that precise correlations are possible within and between basins. For this reasons, many of the British outcrop sections serve as standards that can be compared to the other areas around the world. (2) Many geologists have to work with the rocks they are given, rather than the rocks they would interpret by choice. Many, perhaps all, of the successions described in this volume may rightly be considered as difficult to interpret. However, as is demonstrated, sequence stratigraphical ideas can cast new light on problematic facies, and in return problematic facies can offer critical insights into the sequence stratigraphical model.