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Coastal resilience and late Holocene tidal inlet history: The evolution of Dungeness Foreland and the Romney Marsh depositional complex (U.K.) (2006)
Journal Article
Long, A., Waller, M., & Plater, A. (2006). Coastal resilience and late Holocene tidal inlet history: The evolution of Dungeness Foreland and the Romney Marsh depositional complex (U.K.). Geomorphology, 82(3-4), 309-330. https://doi.org/10.1016/j.geomorph.2006.05.010

Dungeness Foreland is a large sand and gravel barrier located in the eastern English Channel that during the last 5000 years has demonstrated remarkable geomorphological resilience in accommodating changes in relative sea-level, storm magnitude and f... Read More about Coastal resilience and late Holocene tidal inlet history: The evolution of Dungeness Foreland and the Romney Marsh depositional complex (U.K.).

Early Holocene history of the west Greenland Ice Sheet and the GH-8.2 event (2006)
Journal Article
Long, A., Roberts, D., & Dawson, S. (2006). Early Holocene history of the west Greenland Ice Sheet and the GH-8.2 event. Quaternary Science Reviews, 25(9-10), 904-922. https://doi.org/10.1016/j.quascirev.2005.07.002

The margin of the Greenland Ice Sheet retreated rapidly during the first few thousand years of the Holocene. During this period of relative warmth, known as the Holocene thermal maximum, ice core records identify a significant short-lived cooling eve... Read More about Early Holocene history of the west Greenland Ice Sheet and the GH-8.2 event.

Driving mechanisms of coastal change: Peat compaction and the destruction of late Holocene coastal wetlands (2006)
Journal Article
Long, A., Waller, M., & Stupples, P. (2006). Driving mechanisms of coastal change: Peat compaction and the destruction of late Holocene coastal wetlands. Marine Geology, 225(1-4), 63-84. https://doi.org/10.1016/j.margeo.2005.09.004

This paper examines the role of peat compaction as a driving mechanism behind the widespread inundation of a late Holocene coastal wetland in southeast England, UK. Detailed stratigraphic and dating evidence (lithology, grain size, foraminifera, poll... Read More about Driving mechanisms of coastal change: Peat compaction and the destruction of late Holocene coastal wetlands.