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Holocene sea-level change in the Severn Estuary, southwest England: A diatom-based sea-level transfer function for macrotidal settings (2007)
Journal Article

The recent growth in the use of microfossil-based transfer functions in late-Quaternary sea-level reconstructions reflects their potential to accurately quantify palaeo sea-level changes. This study details the development of a diatom-based sea-level... Read More about Holocene sea-level change in the Severn Estuary, southwest England: A diatom-based sea-level transfer function for macrotidal settings.