Based on recent vegetation distribution and an integration of macropalaeobotanical and palynological information, a palaeocommunity model is explored that may permit detailed interpretations of quantitative sporomorph distribution patterns in the Jurassic and Early Cretaceous of NW-Europe in terms of changes in palaeoenvironment (sea-level, climate). The conceptual model is based on the recognition of Sporomorph Ecogroups (SEGs) that reflect broad co-existing plant communities, viz. upland, lowland, river, pioneer, coastal, and tidally-influenced SEGs. In successive palynological assemblages, shifts in the relative abundance of SEGs are thought to be indicators of sea-level changes. Climatic changes may be recognised through significant shifts within the quantitative composition of individual SEGs.

This article asks whether there is a role for weather in archaeological narratives. In archaeology, ideas of weather have been expressed almost solely through the aggregated measure of climate. A number of theoretical and practical problems arise from this, specifically in questioning how climatic change can be related to social change. The article reviews how other disciplines have developed a sense of climate that is more embedded in the human experience of landscape. A case study of a township in Cumbria uses the inhabited perspectives of two 18th-century diarists to explore how we might develop and apply these ideas in an archaeological context. The conclusion outlines some of the challenges for future research, arguing that we should consider weather as a material condition of the landscape – something as much open to archaeological investigation as any other aspect of the past.