Brandon Park Fungi 1959-2014

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Suffolk Natural History, Vol. 51

BRANDON PARK FUNGI 1959—2014 Change and Stability in Occurrence OLIVER RACKHAM This is an attempt to determine trends from the data from my 50 years of autumn visits to Brandon Park, Suffolk. The site Brandon Park is a country-house park established c. 1805. The geology is blown sand; in places there appear to be old dunes. Both in climate and soil it is one of the most arid places in Britain. On Hodskinson’s map of Suffolk (c. 1782) it is shown as open land, probably heath (rabbit warren) but could have been arable. By c.1820 (Ordnance Survey 1-inch) it was fully developed as a park around a minor country mansion; about one-fifth is shown as woodland (presumably plantation), the rest being open land with scattered small clumps of trees. Successive OS maps show not much change until the late 19th century, apart from the building of a mausoleum for the Bliss family. The present formal gardens, lawn, avenue of copper beeches, and lake date from around 1900. In the 1930s the site fell into the hands of the Forestry Commission, who infilled the grounds and remaining heath with plantations chiefly of Corsican Pine and some Scots Pine. A large area of plantation was broken or uprooted in the great storm of 1987. Much of this area was then cleared of trees and restored to heath, now grazed by sheep and cattle. The area has been a public place for many years. Around the house is a formal public Country Park. The house itself, dating from c. 1805, is a nursing home. There are probably no natural trees except birch. The plantations are mainly of beech around the house, merging into Scots Pine to the west and then into extensive Corsican Pine. Other trees include birch, oak, sycamore and larch. There are scattered ornamentals, including yew and Atlas Cedar. Not many trees date from the original park. A common pattern is for spreading, savanna-like beeches, Scots Pines, and larches, dating from the Bliss period, to be infilled with younger beech and Corsican Pine from FC times. Ground vegetation in the plantations is sparse but increasing; the pineries are conspicuously more grassy now than in the 1960s. Dead trees and rotten wood are abundant. They increased after the 1987 storm and re-creation of the heath; at one stage there was a big log-stack in the main ride. The lawn before the house is an example of Breckland-type acid grassland. Other more-or-less stable grassland follows the plantation rides. Heathland in the 1960s was reduced to remnants along rides in the plantations, but has now greatly increased. Brandon Park Heath is fully developed heathland, with dominant heather (from buried seed since before the plantations) and tracts of Cladonia lichens and Polytrichum mosses between the heather bushes. The data I was introduced to Brandon Park by Harry Hudson, who took excursions from Cambridge Botany School early in the Michaelmas Term each year. I have been nearly

Trans. Suffolk Nat. Soc. 51 (2015)


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