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A 7500-year peat-based palaeoclimatic reconstruction and evidence for an 1100-year cyclicity in bog surface wetness from Temple Hill Moss, Pentland Hills, southeast Scotland

Paleoenvironmental ReconstructionPalaeo-environmental ReconstructionEngineeringPaleoenvironmental ChangeGeomorphologyGeographyTemple Hill MossBog Surface WetnessSoutheast ScotlandPaleoecologyEarth ScienceSocial Sciences