To the north, west and south-west lies the similar Celtic broadleaf forests ecoregion, which covers most of the rest of the British Isles. In addition, two further ecoregions are located in the south-western and north-western edges of Ireland, and the north-western fringes of Scotland, and beyond the Scottish Highland Boundary Fault. The whole of this Atlanticarchipelago is thus considered as originally forested, with only the far mountainous north being primarily coniferous. Across the English Channel lies the Atlantic mixed forests ecoregion in northern France and the Low Countries. The difference between the English lowlands beech forests and the Celtic broadleaf forests lies in the fact that south-eastern England is comparatively drier and warmer in climate, and lower-lying in terms of topography. Geologically, something of the distinction can be found in the dominance of the Southern England Chalk Formation in this ecoregion, and the Tees-Exe line, which divides the island of Great Britain into a sedimentary south-east, and a metamorphic and igneous north-west. However, the WWF division was preceded by that of the Hungarian biologist Miklos Udvardy, who had considered the greater part of the British Isles as just one biogeographic province in the Palearctic Realm, which he termed British Islands.
Characteristics
Historically, much of this lowland and submontane region was covered with high-canopy forests dominated by European beech, but also including other species of tree, including oak, ash, rowan and yew. In summer, the forests are generally cool and dark, because the beech produces a dense canopy, and thus restricts the growth of other species of tree and wild flowers. In the spring, however, thick carpets of bluebells can be found, flourishing before the beech leafs out and shades the forest floor. The National Vegetation Classificationplant communities associated with beech forests are:
W12 Fagus sylvatica - Mercurialis perennis woodland - c. 40%
W14 Fagus sylvatica - Rubus fruticosus woodland - c. 45%
W15 Fagus sylvatica - Deschampsia flexuosa woodland - c. 15%
River systems, the most significant of which is the Thames, were historically host to lower-canopy riverine forests dominated by black alder, and this can still be encountered occasionally today. Also included in this ecoregion are the distinctive ecosystems associated with the rivers themselves, as well as their flood-meadows and estuaries. The soils are largely based on limestone, and the climate is temperate with steady amounts of rainfall. Temperatures can fall below freezing in the winter. in the New Forest Nowadays, much of this ecoregion has been given over to agriculture - with the growing of wheat, barley and rapeseed particularly common - as well as to the raising of livestock, especially cattle and sheep. In places it is very heavily populated, with towns, suburbs and villages found nearly everywhere - although the plateau of Salisbury Plain remains largely wild. The most significant centre of population is London, at the head of the Thames estuary, one of the largest cities in the world. Due to this high population density, and to a certain amount of depredation caused by the non-native grey squirrel, edible dormice and deer, this forest ecoregion is considered at high risk, with a critical/endangered conservation status accorded it by the WWF. Air pollution may also be leading to a reduction in beech numbers, through increased susceptibility to disease. Among fauna found in this ecoregion, the West European hedgehog, red fox, Eurasian badger, European rabbit and wood mouse are relatively common, while the following are classed as near threatened on the IUCN Red List:
At the end of the last glaciation, about 10,000 years ago, the area's ecosystem was characterised by a largely treeless tundra. Pollen studies have shown that this was replaced by a taiga of birch, and then pine, before their replacement in turn by most of the species of tree encountered today - including, by 4000 BC, the beech, which seems to have been introduced from mainland Europe. This was used as a source of flour, ground from the triangular nutlets contained in the "mast", or fruit of the beech, after its tannins had been leached out by soaking. Beechmast has also traditionally been fed to pigs. However, by 4000 BC, as Oliver Rackham has indicated, the dominant tree species was not the beech, but the small-leaved lime, also known as the pry tree. The wildwood was made up of a patchwork of lime-wood areas and hazel-wood areas, interspersed with oak and elm and other species. The pry seems to have become less abundant now because the climate has turned against it, making it difficult for it to grow from seed. Nevertheless, some remnants of ancient lime-wood still remain in south Suffolk. Clearance of forests began with the introduction of farming, particularly in the higher-lying parts of the country, like the South Downs. At this time, the whole region, apart from upland areas under plough, and marshy areas, was heavily forested, with woodland stretching nearly everywhere. Notable surviving examples include:
All of these were once far more extensive than they are today. For example, according to a late 9th century writer, the Weald once stretched from Kent to Hampshire, and was long by 30 broad. The New Forest remains the largest intact forested area in this ecoregion, although the hedgerow system, which separates fields from lanes and also from other fields, is also extensive, and serves as an important habitat for otherwise displaced woodland fauna. Some species-rich hedgerows date back at least 700 years, if not 1,000. For many species of bird, significant estuarine habitats include the Thames and Severn estuaries, and the mid-Essex coast. The Mesozoic history of the area can be seen in the Jurassic CoastWorld Heritage Site, where about 180 Ma of fossil-rich sedimentary deposits have been exposed along a stretch of the Dorset and East Devon coast. The science of palaeontology can be said to have started in large measure here, with the pioneering work of Mary Anning. The Great Storm of 1987 was responsible for the uprooting of some 15 million trees in this area.
