Working with partners, Nature After Minerals is here to offer and share best-practice advice on biodiversity-led minerals restoration.
Saline lagoons are bodies of brackish to hyper-saline water that are partially connected with the sea. Some exchange of seawater occurs with the sea through over-topping an impermeable barrier, by percolation of sea water through the sediment or via man made sluices. Tidal range is greatly reduced or non-existent in the lagoon, and so there is little exposure of bed sediment. Saline lagoons occur in low-lying, often soft sediment coastlines, generally south and east England.
Opportunities to re-establish Coastal vegetated shingle are very limited. It is a rare community that is restricted to a few coastal areas where marine processes have produced stable shingle banks. These banks develop characteristic vegetation communities over a long time period.
These habitats develop on land which is periodically flooded or waterlogged by fresh or brackish water, and where agricultural management– grazing, mowing or a combination – promotes vegetation dominated by lower-growing grasses, sedges and rushes.
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