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The wonderfully named Little Piddle is a small chalk stream that flows through the central valley of Lyscombe nature reserve. After percolating through the chalk bedrock of the surrounding landscape, water emerges from the ground from several springs and seepages at the edge of a small wet woodland. From here, it flows south, overtopping a medieval fish-hatch and passing by Lyscombe Chapel, before continuing underneath an old farmyard and then along the valley through improved grassland, before being directed into a culvert pipe and underneath Drakes Lane, where it leaves the reserve. The stream joins the River Piddle just before Puddletown, with the water eventually entering Poole Harbour.
Like the overwhelming majority of watercourses in the UK, the Little Piddle has been modified to suit agriculture: straightened, culverted, and separated from its floodplain. These changes have drained the wetlands, reduced biodiversity, and allowed nutrients such as nitrogen and phosphorus to flow unchecked downstream.
Once in Poole Harbour, these pollutants feed algal blooms that choke seagrass meadows, deplete oxygen, and threaten rare species such as avocets, spoonbills, and black-tailed godwits. At Lyscombe, these changes have meant the river is no longer able to function as it used to naturally. The very name ‘Lyscombe’ is an indication of the valley’s much wetter past. It is thought that the name refers to ‘a valley (coombe) where reeds (lisc) grow’¹, which suggests the valley was once much wetter, with reeds, sedges, and other specialist wetland plants providing diverse habitats for a whole host of species. Dragonflies, amphibians, water voles, and wading birds would have thrived here. With the water now focused into a single uniform channel and disconnected from the floodplain, we have lost these precious wetland habitats.